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Cahill" width="24" height="24" class="user-profile-pic" src="data:image/jpg;base64,iVBORw0KGgoAAAANSUhEUgAAACAAAAAgCAMAAABEpIrGAAAABGdBTUEAALGP C/xhBQAAACBjSFJNAAB6JgAAgIQAAPoAAACA6AAAdTAAAOpgAAA6mAAAF3Cc ulE8AAABmFBMVEXiX1HiXlDhXlDiYVPiYVTiY1XiYlTgVEbfUkPgVUbeSjre STnfTz/gV0jlc2fnfHDgWErdRzfka17tnZTuoprohHneTT3hX1HiYFLhWUvh W03////nfXLfUEDxt7D87+3gVkfiYFPiYlXsmpHzv7rdRTXtm5P42NXjZlnh WkzupJ342tb77Ov87+72z8vgWEnhW0zfT0D9+PfeTDzgWUrbOyr65OLlcGTg VEXkbF/vqqPmeGzqjILhWkvjaFv43NndSDjiZFbog3jdRjXxtK3lcWX539ze SjvmdWnzwbvdRjbiX1LhXE7hXU/eTj7+/v777ezaNCPYKBXzvbfjZ1rmd2vz wLvhXU7eTT777Or0xsH1yMT43drwsKrcPi3lb2P42dbiY1bjZFfmeG31y8f7 6uj++/v+/fz88/LfUUL+/f3bOinlc2b77evcPy7aNCL0x8Lne2/bOSfwrab0 xcDrlYzeSzvvqKDupp7jZVfogHX31dHfTj/++vrrkYfwraXtnpXne3Duo5vq joTfUEHeTD3iX1AAAABTrsIuAAAAAWJLR0SH+9kLywAAAAd0SU1FB+gLFRAX Ct+kawsAAAGDSURBVDgR3cEHW9NgGAXQ+96v+aCpq1pCmtdRiquKYkUxLqg4 wLZxb1x1x70V9+R3G0PLU/EfcA4WLxHB/5jAX0wJFqLJgABI4zgWxAJETy9B EDbr5pbAEN1ILF22fAVBML9yVaHPyxr2Y57QLwaqq9dYwl2riXUoDRDzhGV3 UHX9hrJ1N+qmzZUtutUdANHBfpMf2rZdh3egulOrI7t2j+qerCHahCbcq/v2 6wHv4JiO1w7ZytiEE4BoEzqHj+jRUI9NhlN6vF5mo9jbBNFBRCdOnjp95qye y53XC3WHCEoXQbQJ7aU+vXxl+qpeu35Db9ZaJrh12zRBzCFt/Y7evXd/SB+M xA/Vi6NH4/o4NMQc+sOBPnlan3z2XF+8fKWvS/EbHfUAIiUsv32n7/MzreoH /eh+mtbEZ9NjKEgJ/dKXrzNFH1Gx8K3SzH0v/PgZh4boEDZ+1SoNEpH7mzBx ruZFhujCTMsnQDiWRMZxLIhuTMwCYAJMCf4lSIkgISJYXP4AWuU2MgprCC8A AAAldEVYdGRhdGU6Y3JlYXRlADIwMjQtMTEtMjFUMTY6MjM6MDUrMDA6MDBE ZVx0AAAAJXRFWHRkYXRlOm1vZGlmeQAyMDI0LTExLTIxVDE2OjIzOjA1KzAw OjAwNTjkyAAAACB0RVh0c29mdHdhcmUAaHR0cHM6Ly9pbWFnZW1hZ2ljay5v cme8zx2dAAAAGHRFWHRUaHVtYjo6RG9jdW1lbnQ6OlBhZ2VzADGn/7svAAAA GHRFWHRUaHVtYjo6SW1hZ2U6OkhlaWdodAA2MDB63r21AAAAF3RFWHRUaHVt Yjo6SW1hZ2U6OldpZHRoADYwMOkv7egAAAAZdEVYdFRodW1iOjpNaW1ldHlw ZQBpbWFnZS9wbmc/slZOAAAAF3RFWHRUaHVtYjo6TVRpbWUAMTczMjIwNjE4 Nd22l40AAAATdEVYdFRodW1iOjpTaXplADIyNjc3QkJ+4QThAAAAO3RFWHRU aHVtYjo6VVJJAGZpbGU6Ly90bXAvbGV0dGVyX2F2YXRhcnMvMi9BQy8yMjZf OTVfODEvNjAwLnBuZ44UuXsAAAAASUVORK5CYII= " /> </div> <div class="blog-card__second-avatar"> <img alt="James McClure" width="24" height="24" class="user-profile-pic" src="data:image/jpg;base64,iVBORw0KGgoAAAANSUhEUgAAACAAAAAgCAMAAABEpIrGAAAABGdBTUEAALGP C/xhBQAAACBjSFJNAAB6JgAAgIQAAPoAAACA6AAAdTAAAOpgAAA6mAAAF3Cc ulE8AAABqlBMVEVSvIlRvIlRu4hVvYtTvIpTvIlWvYtUvIpPuodCtn5JuINL uYQ+tHs/tXxPu4c9tHtHt4FPuoZ4yqNkw5VFt4BhwpOJ0a+Ez6tQu4dOuoZ6 y6SM0rBvx5xEtn9txpz////K6tsjqWmW1reL0rA8s3pewJHF6Nc4sndWvYxR vIhUvYtpxZnB59SP07Lb8eY6snii28C95dI3sXfC59UiqWiQ1LPw+fRdwJFA tXzz+vf7/fzA5tQ3sXYjqWiO07Ke2b2t38c7s3ltxpuo3cSM0rF2yqLQ7d81 sXXJ6tpgwZK+5tNUvYpqxZnB59V0yaBsxptNuoZKuYQ5snhXvo1Gt4BpxZif 2r0vrnFvx51hwZNZv45EtoB2yqE9s3plw5Ykqmm14swep2XN69z+/v7h8+sx r3K+5dJGt4Fmw5bq9/FMuYXH6dkprG2K0q+v4Ml1yaGk28ErrW675NG14s3U 7uJFtoC3485Dtn/x+fVcwJDE6NY4sXdyyJ+a2Lqc2Lt9zaY+tHyq3sV1yaBK uIN7zKWU1bZNuoVav46n3cN7y6VAtX1XvoxXvYwAAAD4X97fAAAAAWJLR0SN Gwzi1QAAAAd0SU1FB+gLFRAXGVsaKtUAAAGeSURBVDgR3cELX0thAAbw5zzn bEczDEOl4zHG3ncrsxLFUcmIZmjKXe5yyf2S+y1y/dC2tVE/36D/H0uS46DO cfAfNqCKNViMcD1Goi4IEG7UJxYhlrXE/OXxFStBEi2rEhES/xCr/TVrk+vW b2htAxBr39gRixB/OXSDTdqc2iJtTUf9xDZpe8bQoslhNsipM9Ul7cj7JrNT KnQbWjQ5dIOcenb1arf2JLy+/r3aFxpaNJB0g5x69g9oUEMHEsM6qM7Q0GIe q7JBTj2pog4dVt/IER3VaGhoMY9wvVJwTOVUUe3HdWJEoydVCA0takiMVZKn xidUThV1+oyGzurceRVCQ4sali5c7O+tXJpU+XJRV65eu35DNyd0KzS0qKE/ dVt37sbvaWD6vh5MP5QePR7Wk25DixrSTz9V1bPn6S69qMy81Kt8h16/MbSo I1rTb9+9//CxbWzy0+fZ5JevU3Pfvv9IeEQD4c3k8z+ByGxmHF4QB+YqQYRE E+Ea44L0fvlkNkrid4lYgHXWsgGswkKOtQ6qHFQ5ABwsJX8A9m1BTHUEBgAA AAAldEVYdGRhdGU6Y3JlYXRlADIwMjQtMTEtMjFUMTY6MjM6MjUrMDA6MDAG QFsJAAAAJXRFWHRkYXRlOm1vZGlmeQAyMDI0LTExLTIxVDE2OjIzOjI1KzAw OjAwdx3jtQAAACB0RVh0c29mdHdhcmUAaHR0cHM6Ly9pbWFnZW1hZ2ljay5v cme8zx2dAAAAGHRFWHRUaHVtYjo6RG9jdW1lbnQ6OlBhZ2VzADGn/7svAAAA GHRFWHRUaHVtYjo6SW1hZ2U6OkhlaWdodAA2MDB63r21AAAAF3RFWHRUaHVt Yjo6SW1hZ2U6OldpZHRoADYwMOkv7egAAAAZdEVYdFRodW1iOjpNaW1ldHlw ZQBpbWFnZS9wbmc/slZOAAAAF3RFWHRUaHVtYjo6TVRpbWUAMTczMjIwNjIw NRcpo9wAAAATdEVYdFRodW1iOjpTaXplADE2Njk4QkI/G2xkAAAAPHRFWHRU aHVtYjo6VVJJAGZpbGU6Ly90bXAvbGV0dGVyX2F2YXRhcnMvMi9KTS84Ml8x ODhfMTM3LzYwMC5wbmdZtIhrAAAAAElFTkSuQmCC " /> </div> </div> <div> <div class="blog-card__authors-text"> <div class="blog-card-author-list" style="width: 100%;"> <a href="/users/853908"><p class="blog-card__owner">Aaron G. Cahill</p></a> <p class='blog-card__remaining-text'>and 2 more</p> </div> </div> <time datetime="2024-11-13" class="blog-card__date">November 13, 2024</time> </div> </div> </div> <div class='blog-card__preview-content-container'> <a href="/doi/full/10.22541/essoar.173152356.66772501/v1"> <div class='blog-card__preview-content'> An increasing number of legacy petroleum wells are reported to suffer integrity failure, releasing methane (CH4) into the subsurface and atmosphere. Subsurface released methane is reactively transported towards ground surface with a portion converted to carbon dioxide by soil microbes. Currently, the extent to which fugitive CH4 oxidation occurs, including microbial taxa responsible and controlling parameters are poorly understood. Here, we examined fugitive CH4 leakage at a legacy well in the Montney region of British Columbia, Canada and find up to 90% is oxidised at rates as high as 230 g of CH4 /m2 of soils/day during summer. Meanwhile, a profound difference in microbiome between soils at the wellhead and background was observed, while modelling suggests that prevailing seasonal temperature will moderate CH4 oxidation extent. Overall, we find that filtration of fugitive CH4 through natural soils can significantly reduce emissions of CH4 and mitigate climate impacts from such sources </div> </a> </div> </div> </div> <div class="blog-card"> <div class="blog-card__container"> <div class='blog-card__top-row'> </div> <div class='blog-card__heading-container '> <a href="/doi/full/10.22541/essoar.173120148.85833001/v1"> <div class="blog-card__title"> Unified Forecast System Prediction of the Madden-Julian Oscillation and East Pacific... </div> </a> </div> <div class="blog-card__author-container"> <div class="blog-card__author-information"> <div class="blog-card__images-container"> <div class="blog-card__first-avatar"> <img alt="Yu Cian Tsai" width="24" height="24" class="user-profile-pic" src="data:image/jpg;base64,iVBORw0KGgoAAAANSUhEUgAAACAAAAAgCAMAAABEpIrGAAAABGdBTUEAALGP C/xhBQAAACBjSFJNAAB6JgAAgIQAAPoAAACA6AAAdTAAAOpgAAA6mAAAF3Cc ulE8AAABBVBMVEW8qqS7qaO9q6W9q6a9rKa8q6W1oZq6qKK0oJm2o5y3o52y 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bWI6OkRvY3VtZW50OjpQYWdlcwAxp/+7LwAAABh0RVh0VGh1bWI6OkltYWdl OjpIZWlnaHQANjAwet69tQAAABd0RVh0VGh1bWI6OkltYWdlOjpXaWR0aAA2 MDDpL+3oAAAAGXRFWHRUaHVtYjo6TWltZXR5cGUAaW1hZ2UvcG5nP7JWTgAA ABd0RVh0VGh1bWI6Ok1UaW1lADE3MzIyMDYyMTEJX1aEAAAAE3RFWHRUaHVt Yjo6U2l6ZQAxMTEzOEJC/4NgqAAAAD10RVh0VGh1bWI6OlVSSQBmaWxlOi8v dG1wL2xldHRlcl9hdmF0YXJzLzIvWVQvMTg4XzE3MF8xNjQvNjAwLnBuZ169 BtwAAAAASUVORK5CYII= " /> </div> <div class="blog-card__second-avatar"> <img alt="Eric Daniel Maloney" width="24" height="24" class="user-profile-pic" src="data:image/jpg;base64,iVBORw0KGgoAAAANSUhEUgAAACAAAAAgCAMAAABEpIrGAAAABGdBTUEAALGP C/xhBQAAACBjSFJNAAB6JgAAgIQAAPoAAACA6AAAdTAAAOpgAAA6mAAAF3Cc ulE8AAABYlBMVEV4hM13g813hM13g8x6hs17h857hs55hc1reMhlc8ZmdMZm c8Z0gct1gcxpdsdsechodcdvfMlxfcqgqNywt+GpsN+psd+xuOJ8h86jq9yh qdx5hM1wfcqVntemrt6OmNVxfspndcfr7ff///+IktOFkNGttODS1u5jccXh 4/ObpNqCjdCMl9SKldORm9Zue8mKlNPq7PfL0Ovj5fRhb8Rve8lqd8iNl9WG kdJtesnx8vnw8fnQ1O1icMWCjdGLldSrs+DL0OxkcsW5v+XR1e3k5vXDyOhc asKWoNjT1+7N0ezj5vTX2/Df4vOqsd+0u+OJlNOZotlbasLT1+90gMvM0OxY Z8HKz+tYZsF8iM6FkNJzf8vP0+1OXb3i5PSIk9OBjdCMltSRmtaHktLM0exZ Z8HR1e7s7virsuCrst+qst+zueJ6hc27weaYodiuteFzgMt+ic+6wOVqeMh1 gcsAAAD1XGozAAAAAWJLR0R1qGqY+wAAAAd0SU1FB+gLFRAXDDbHzj4AAAGX SURBVDgR3cEJV1JBGAbgd/gYxjuACBWWUAKvy1XMSwEiJaFkllZmJVq2mO0L 2fr/T8wtD5x+gs+DU0U5EQxEMEyGoU8cDEhUh4BYDAIoicaM4IQIRjzbF08k R0eTECVIjaUhCiEBMmfOnstms+PncWEil4Agf/HSZCEnCAlMscTQ1DQ542lT 0OSsr0XBERg7x/nywuXFoEJeGYP2ZsirvhYFR2BsleVaPRUsNVjicjMWv3ad Ky0tCo7A2Cpv1IJUstnmKtc6+WXe5HpLi4IjMPYWnY3bDd7ZZFBbY4VbvhYF R2DsXd5bmb2/XVvggx0+fMTHu+z6WhQcgbFV6j3bygQV7j9hd5rtp+z6WhQc gbFVHnjP8pmlNp+/2OJL1g7Z9bUoOAJj5zj/6mjndf0N3+4dkRvvGtz3tSg4 AlMsMXRY5vvOyAce+JNc97UoOALkJ8a3P376/EX3vh4X6ovf0t9//DxOG8Ff Ivjl2Xg87iV+d5owQRHY7TRzonBCojoE6J5IT0Oge4IB+R+kD8NUCIjgnwhO kz/HDzgkW9/7cQAAACV0RVh0ZGF0ZTpjcmVhdGUAMjAyNC0xMS0yMVQxNjoy MzoxMiswMDowME1oYmQAAAAldEVYdGRhdGU6bW9kaWZ5ADIwMjQtMTEtMjFU MTY6MjM6MTIrMDA6MDA8NdrYAAAAIHRFWHRzb2Z0d2FyZQBodHRwczovL2lt YWdlbWFnaWNrLm9yZ7zPHZ0AAAAYdEVYdFRodW1iOjpEb2N1bWVudDo6UGFn ZXMAMaf/uy8AAAAYdEVYdFRodW1iOjpJbWFnZTo6SGVpZ2h0ADYwMHrevbUA AAAXdEVYdFRodW1iOjpJbWFnZTo6V2lkdGgANjAw6S/t6AAAABl0RVh0VGh1 bWI6Ok1pbWV0eXBlAGltYWdlL3BuZz+yVk4AAAAXdEVYdFRodW1iOjpNVGlt ZQAxNzMyMjA2MTkyWskzbwAAABN0RVh0VGh1bWI6OlNpemUAMTI5ODZCQpT4 88wAAAA9dEVYdFRodW1iOjpVUkkAZmlsZTovL3RtcC9sZXR0ZXJfYXZhdGFy cy8yL0VNLzEyMF8xMzJfMjA1LzYwMC5wbmfthtPdAAAAAElFTkSuQmCC " /> </div> </div> <div> <div class="blog-card__authors-text"> <div class="blog-card-author-list" style="width: 100%;"> <a href="/users/853890"><p class="blog-card__owner">Yu Cian Tsai</p></a> <p class='blog-card__remaining-text'>and 3 more</p> </div> </div> <time datetime="2024-11-10" class="blog-card__date">November 10, 2024</time> </div> </div> </div> <div class='blog-card__preview-content-container'> <a href="/doi/full/10.22541/essoar.173120148.85833001/v1"> <div class='blog-card__preview-content'> This study evaluates the subseasonal to seasonal (S2S) prediction skill of the Madden-Julian Oscillation (MJO) and its remote impacts on the east Pacific (EP) tropical cyclogenesis in the Unified Forecast System (UFS) during boreal summer (May–October). Utilizing four experimental versions, Prototypes 5-8, the study finds that although the UFS generally captures the MJO’s propagation characteristics near the initialization time, it encounters difficulty in accurately predicting the propagation speed and decay rate of the MJO beyond 15 days. Specifically, the phase transition rate of the MJO in the UFS is slower than observed, although this behavior is improved in Prototype 8. The UFS overestimates anomalies in the intraseasonal east Pacific genesis potential index anomalies associated with MJO phases. Analysis of the vertically integrated moist static energy (MSE) budget reveals that all four UFS prototypes underestimate the damping effect of vertical MSE advection and the amplifying effect of longwave radiative heating, indicating weaknesses in tropical convective parameterization and cloud radiative feedbacks, although these biases are somewhat improved in Prototype 8. These deficiencies result in less efficient vertical MSE export, weaker damping of MJO convection, slow MJO propagation, and delayed MJO remote impacts on the EP. Thus, improving the UFS’ ability to simulate MJO propagation and maintenance processes is crucial for better predicting the MJO’s remote effects on EP TC genesis and enhancing S2S forecast capability for such extreme events. </div> </a> </div> </div> </div> <div class="blog-card"> <div class="blog-card__container"> <div class='blog-card__top-row'> </div> <div class='blog-card__heading-container '> <a href="/doi/full/10.22541/essoar.173152365.52571912/v1"> <div class="blog-card__title"> Predicting Methane (CH 4 ) Concentration in Transformer Oil using Linear Epsilon Supp... </div> </a> </div> <div class="blog-card__author-container"> <div class="blog-card__author-information"> <div class="blog-card__images-container"> <div class="blog-card__first-avatar"> <img alt="Angel Pinto" width="24" height="24" class="user-profile-pic" src="data:image/jpg;base64,iVBORw0KGgoAAAANSUhEUgAAACAAAAAgCAMAAABEpIrGAAAABGdBTUEAALGP C/xhBQAAACBjSFJNAAB6JgAAgIQAAPoAAACA6AAAdTAAAOpgAAA6mAAAF3Cc ulE8AAABfVBMVEXiX1HiXlDiX1DhXlDiYVPiYVTiYlTiX1LgVkffUUHhXU/g VEXfUEHfUULfU0TgV0nlcGPogHXhXE7hWUvmeGznf3PmeW7nem/lcmbeTD3g VUbhXU7fUkP+/Pz////qjoTeTDziYlXiYFLeTT388O/76+niYFPeTj7og3j3 08/dRzfeSjv76eflc2fldGflcGTwsKn65ePeTT7dRTT319T+/f30w77iZFbe SjrfTz/fUEDbPCv42tfgWUrhWkz0xL/jZFfupJzdSDjhWkvbOSj1ycXmdWni Y1XeSDjtnpbpioDcQjL9+PfeSzv76ujkbF/kbGDkal3rkoj99/bcPi3XJhPv p5/fU0PfTj/65uTmdmvldGj99vX0xsH1ycT42dbzwLrsmI/smZDtoJfohHnd RTXxta/++vn87+3gWEndRjb77Or+/v3dQzPaMyHwr6jaNiTrlIvyvLbbOin9 9PPohHrwsarkbWHgVkjgV0jsmpLrk4ruo5viY1YAAADvodF7AAAAAWJLR0R+ P7hBcwAAAAd0SU1FB+gLFRAXC6ijW50AAAFuSURBVDgR3cEJO1RhGAbg5/V8 58SZpTqV5ZheM59OaoyUJUNiEIMSrUaWSJSlTVGp/nuWGeaayy9w3zivRKqq cAYeAMAiQSUaBwRoXMdxDIgKvFBd44FEJBqricVhiHJCXLx02feBK1ev1dbV 1jcEhihDNCaua1MyZZtv6KHwZmAoKBG6LbdUb6dd25rRtjvtd/VeB0CUkG5n V/d97al2s6H29gUP+rU9YogioX04oIM5HRrOZUONxUYejepYwhBFwvz4hE4+ 1icNduqpTs88e64v4h6IIsIOZ/Tlq9faNluY0yNvog4Fx4QmMa8Li0tvdTnd m9GVd6vvI32GKBHm19Y1/ND9UXVjc0vXOqcKvkOcIPzotqY/JT9/0aavW+qx xwVxQuh2fNOdzVwqmNHw+w8dGAEpOEUb7O79/GXB3/tDwZ+/vgeinNDG0xuW BJOtLGQ9EBVo/lkCRCoFNw+iEg8IAB7DGQRHRCCC8+c/4UYxVMpi+3EAAAAl dEVYdGRhdGU6Y3JlYXRlADIwMjQtMTEtMjFUMTY6MjM6MDcrMDA6MDDT+k1d AAAAJXRFWHRkYXRlOm1vZGlmeQAyMDI0LTExLTIxVDE2OjIzOjA3KzAwOjAw oqf14QAAACB0RVh0c29mdHdhcmUAaHR0cHM6Ly9pbWFnZW1hZ2ljay5vcme8 zx2dAAAAGHRFWHRUaHVtYjo6RG9jdW1lbnQ6OlBhZ2VzADGn/7svAAAAGHRF WHRUaHVtYjo6SW1hZ2U6OkhlaWdodAA2MDB63r21AAAAF3RFWHRUaHVtYjo6 SW1hZ2U6OldpZHRoADYwMOkv7egAAAAZdEVYdFRodW1iOjpNaW1ldHlwZQBp bWFnZS9wbmc/slZOAAAAF3RFWHRUaHVtYjo6TVRpbWUAMTczMjIwNjE4NzO4 9qEAAAATdEVYdFRodW1iOjpTaXplADE3NDkxQkKBVtcuAAAAO3RFWHRUaHVt Yjo6VVJJAGZpbGU6Ly90bXAvbGV0dGVyX2F2YXRhcnMvMi9BUC8yMjZfOTVf ODEvNjAwLnBuZz4ABNgAAAAASUVORK5CYII= " /> </div> <div class="blog-card__second-avatar"> </div> </div> <div> <div class="blog-card__authors-text"> <div class="blog-card-author-list" style="width: 100%;"> <a href="/users/853711"><p class="blog-card__owner">Angel Pinto</p></a> <p class='blog-card__remaining-text'>and 1 more</p> </div> </div> <time datetime="2024-11-13" class="blog-card__date">November 13, 2024</time> </div> </div> </div> <div class='blog-card__preview-content-container'> <a href="/doi/full/10.22541/essoar.173152365.52571912/v1"> <div class='blog-card__preview-content'> The reliable operation of transformers is critical to power system stability, and early fault detection in transformers can significantly reduce the risk of catastrophic failures. Dissolved gas analysis (DGA) is a commonly used method to assess transformer health, as gas concentrations correlate with fault conditions inside the transformer. Methane (CH4), a gas indicative of thermal faults, serves as a key parameter in detecting early signs of fault. This study proposes a linear epsilon support vector regression (SVR) model fine-tuned with Grid Search for predicting methane concentration based on transformer temperature, oil temperature, winding resistance, load factor, service life, and transformer age using grey relational analysis. By predicting methane concentration in ppm, this model supports proactive fault management, optimizing maintenance schedules, and effectively reducing transformer downtime. Comparative results suggest that the proposed SVR model is an effective baseline for improving dissolved gas analysis accuracy, contributing to enhanced transformer diagnostics and preventive maintenance strategies. </div> </a> </div> </div> </div> <div class="blog-card"> <a href="/doi/full/10.22541/essoar.173120326.69513564/v1"> <div class="blog-card__image-container"> <img onerror="$(this).closest('a').remove()" height="200" class="blog-card__image-tag" loading="lazy" src="https://d197for5662m48.cloudfront.net/images/tagdashboard/banner/large-243fcdb05f224a75295a129767fd9215.jpg" /> </div> </a> <div class="blog-card__container"> <div class='blog-card__top-row'> </div> <div class='blog-card__heading-container '> <a href="/doi/full/10.22541/essoar.173120326.69513564/v1"> <div class="blog-card__title"> A European Hail and Lightning Climatology From an 11-Year Kilometer-Scale Regional Cl... </div> </a> </div> <div class="blog-card__author-container"> <div class="blog-card__author-information"> <div class="blog-card__images-container"> <div class="blog-card__first-avatar"> <img alt="Ruoyi Cui" width="24" height="24" class="user-profile-pic" src="data:image/jpg;base64,iVBORw0KGgoAAAANSUhEUgAAACAAAAAgCAMAAABEpIrGAAAABGdBTUEAALGP C/xhBQAAACBjSFJNAAB6JgAAgIQAAPoAAACA6AAAdTAAAOpgAAA6mAAAF3Cc ulE8AAABVlBMVEWPpK+OpK+Oo66QpK+SprGRprGRprCQpbCRpbCJn6p/l6OA mKSAl6SBmaWFnKiEm6d/l6SGnKifsbrBzdO4xcy6x860wsqfsbuQpa+KoKyB mKWktb6+ytC7yM+Moq29ydD////7/PybrriHnamNo67o7O7Z4OODmqa3xMvA zNKUqLKZrLb09vd+lqPf5ejEz9XW3uK/y9Gzwsl5kp+Loax2kJ3v8vOWqrR1 j5yKoKuCmaWGnai3xcyzwcmInqp4kZ7y9PZ+lqK1w8qTp7Kgsbultr/CztSh s7zU3ODj6OtzjZu5xs22xMvX3+N9laLG0da8yM+Tp7Gzwch0jpv7+/zh5ul0 jpyCmqbS2t97lKHm6+2Fm6eIn6rS2t7Fz9W7x872+Pmmt7/19/ji6OqNoq2e sLnJ09iGnamesLqouMCJn6uCmaauvcW+ytGjtL2Moax9lqIAAAA0eV+dAAAA AWJLR0Rxrwdc4gAAAAd0SU1FB+gLFRAXB6EVF7YAAAFwSURBVDgR3cHZQtNQ FAXQfXfuTQgH0oFUI5Z6NAWqWFFRsYgBwRmZnJXBEVSc+P8nqWm1vPABrIVj 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LzE0M18xNjRfMTc1LzYwMC5wbmfw+YClAAAAAElFTkSuQmCC " /> </div> <div class="blog-card__second-avatar"> </div> </div> <div> <div class="blog-card__authors-text"> <div class="blog-card-author-list" style="width: 100%;"> <a href="/users/643840"><p class="blog-card__owner">Ruoyi Cui</p></a> <p class='blog-card__remaining-text'>and 8 more</p> </div> </div> <time datetime="2024-11-10" class="blog-card__date">November 10, 2024</time> </div> </div> </div> <div class='blog-card__preview-content-container'> <a href="/doi/full/10.22541/essoar.173120326.69513564/v1"> <div class='blog-card__preview-content'> • We present a European-wide climatology of hail and lightning based on a convection-permitting climate simulation • We introduce a new radar-based European-wide observational hail dataset for the years 2013-2021 </div> </a> </div> </div> </div> <div class="blog-card"> <div class="blog-card__container"> <div class='blog-card__top-row'> </div> <div class='blog-card__heading-container '> <a href="/doi/full/10.22541/essoar.173152380.04374748/v1"> <div class="blog-card__title"> Genome-Resolved Metagenomic Insights into Aquifer Microbiome Adaptations Following Tw... </div> </a> </div> <div class="blog-card__author-container"> <div class="blog-card__author-information"> <div class="blog-card__images-container"> <div class="blog-card__first-avatar"> <img alt="Lian Guoxi" width="24" height="24" class="user-profile-pic" src="data:image/jpg;base64,iVBORw0KGgoAAAANSUhEUgAAACAAAAAgCAMAAABEpIrGAAAABGdBTUEAALGP C/xhBQAAACBjSFJNAAB6JgAAgIQAAPoAAACA6AAAdTAAAOpgAAA6mAAAF3Cc ulE8AAABJlBMVEXU40rU40nT4knU403V407T4kjP4DfQ4DrT40nU40vU40zQ 4DvO3zHP4DjT4kbh64He6XbS4ULU4krS4kXa52bl7pPm7pbd6XPP3zbR4T/S 4kT////7/fLO3zTT4kfy98z6/O3R4UDS4UP5++bO3zPN3i7q8arv9b/n7530 99DU4kn5++jO3zLQ4DnM3SjW5FTa5mPw9cDV5FHR4T7u9LjZ5mHb52jZ5mLe 6XXN3zD9/fjb6Gv5++nV5FDQ4T3a52Tw9cHN3i3c6G/2+dza52P4++XK3STQ 4DzT4kXP3zXR4T3G2hDx9sfZ5mPY5l7M3Snp8aby98vX5Vf7/O7N3i/v9Lzt 87Tl7pHk7Y7j7Y3m75ne6XTl7pTl7pXX5VjO3zDV408AAADM8yzQAAAAAWJL R0RhsrBMhgAAAAd0SU1FB+gLFRAXIXMYkksAAAFfSURBVDgR3cGJQtNAFAXQ O3cS4GVSsFKgnScRolUkARWwiAuoLG6gsghl5/+/wqY2QvEPOAd3i0HJdOA/ 7EDBsMugH2EtUSBsEFgQfYhwYBAcAiiRi+MKI+IGIhweuVcF7lNG49rY+ES9 ERHXKH5YH0wKiGTwoXZMYTqiQYniU330WMCg+USfSnVGn8XRLFGi+FSzXCA+ UY3nRuczfV4VokTxqWa50LoX+rK5MD1XX0wIokTxqWa50FYmdKnJV63lmiQg ShSfapYL7cBrXVpxb1T1rbM06KH4VN/VA/t+dU0/fMSn1rpuOEuDHopPdXNr 1bnPX1S/Vr5939YdZ2nQQ/Fes4W15daPn790N1zc29easzToofhQu3YP6r+1 cOgAokQk4dFRu318ctpgXDs7b1+sJKDBP0Q4Ged5fukEkYsv84YFcRMRFK4i DsEGQRCR6McS+BduM10oGGNwx/wB7AIjmKApYSsAAAAldEVYdGRhdGU6Y3Jl YXRlADIwMjQtMTEtMjFUMTY6MjM6MzMrMDA6MDCpOm6tAAAAJXRFWHRkYXRl Om1vZGlmeQAyMDI0LTExLTIxVDE2OjIzOjMzKzAwOjAw2GfWEQAAACB0RVh0 c29mdHdhcmUAaHR0cHM6Ly9pbWFnZW1hZ2ljay5vcme8zx2dAAAAGHRFWHRU aHVtYjo6RG9jdW1lbnQ6OlBhZ2VzADGn/7svAAAAGHRFWHRUaHVtYjo6SW1h Z2U6OkhlaWdodAA2MDB63r21AAAAF3RFWHRUaHVtYjo6SW1hZ2U6OldpZHRo ADYwMOkv7egAAAAZdEVYdFRodW1iOjpNaW1ldHlwZQBpbWFnZS9wbmc/slZO AAAAF3RFWHRUaHVtYjo6TVRpbWUAMTczMjIwNjIxM+dRN6gAAAATdEVYdFRo dW1iOjpTaXplADE0MTY3QkKTzEYUAAAAPHRFWHRUaHVtYjo6VVJJAGZpbGU6 Ly90bXAvbGV0dGVyX2F2YXRhcnMvMi9MRy8yMTJfMjI3Xzc0LzYwMC5wbmfS N6YaAAAAAElFTkSuQmCC " /> </div> <div class="blog-card__second-avatar"> <img alt="Zhang Tianjing" width="24" height="24" class="user-profile-pic" src="data:image/jpg;base64,iVBORw0KGgoAAAANSUhEUgAAACAAAAAgCAMAAABEpIrGAAAABGdBTUEAALGP C/xhBQAAACBjSFJNAAB6JgAAgIQAAPoAAACA6AAAdTAAAOpgAAA6mAAAF3Cc ulE8AAAA5FBMVEWt1n2t1nys1nys1Xyt1n6v14Cu1n+o03ah0Gui0Gyi0Guq 1Hml0nGm0nK424/Q57XK5KvL5a3L5azM5a7P57TD4aDP57PK5KzL5a7A35uo 03XR6Lf///+02Yjz+ezo89yh0Gqx2IO73ZO324663JKv14HE4aHx+Oi22oy8 3ZS83ZWq1Hin03Ok0W+ezmb3+/Op1HebzWHH46aw14Kgz2nh8M+gz2ij0W6/ 35rt9uOp1Har1Xuu1n6fz2bm8tiw14PF4qPi8NGYy1ym0nG02Ym53JDN5rDR 6LbM5a+j0W2t1X0AAAB1oD0qAAAAAWJLR0RLaQuFUAAAAAd0SU1FB+gLFRAY DcZY4mcAAAE2SURBVDgR3cGLVtNAFAXQMzlzk96WQjNBrMlFKBBeVQktgg8U lALK/38QizVAU/gD9sbb4iLARViU8DW00UuEVKKUmEvos44+6PaWOvqg0wcT PKHPllcGeSjyVbxbe58P88Hqh9ITjxxFK4vWP1q0sSlM8Ijojba2d+pd29P9 g7qyqj5cH4N4RoyXPn3+cmR1vymPJzY5LjMQLUQ6Pflqxan46dnQhmdTTyyg 6Df7fuJB0WBBhUQbffPD7Gd5TooGCyp0aGP667dN9OIcFA0WVOgwR8rppf35 W/avxhANFlToMEffTM32Z9fbW6NerQMbqNDhmaNoZVGlI72xGxU6zNFn17fF v6LIb5eztJkVs8YTLY6+7Gi329XNzBPN/wa8wwJ6iTxBL554IeGTBAnJBK+4 CG/TPZ7bG8SgcZ71AAAAJXRFWHRkYXRlOmNyZWF0ZQAyMDI0LTExLTIxVDE2 OjIzOjExKzAwOjAwfIB4+QAAACV0RVh0ZGF0ZTptb2RpZnkAMjAyNC0xMS0y MVQxNjoyMzoxMSswMDowMA3dwEUAAAAgdEVYdHNvZnR3YXJlAGh0dHBzOi8v aW1hZ2VtYWdpY2sub3JnvM8dnQAAABh0RVh0VGh1bWI6OkRvY3VtZW50OjpQ YWdlcwAxp/+7LwAAABh0RVh0VGh1bWI6OkltYWdlOjpIZWlnaHQANjAwet69 tQAAABd0RVh0VGh1bWI6OkltYWdlOjpXaWR0aAA2MDDpL+3oAAAAGXRFWHRU aHVtYjo6TWltZXR5cGUAaW1hZ2UvcG5nP7JWTgAAABd0RVh0VGh1bWI6Ok1U aW1lADE3MzIyMDYxOTHDwGLVAAAAEnRFWHRUaHVtYjo6U2l6ZQA5OTEwQkKI 1U40AAAAPXRFWHRUaHVtYjo6VVJJAGZpbGU6Ly90bXAvbGV0dGVyX2F2YXRh cnMvMi9aVC8xNzNfMjE0XzEyNS82MDAucG5nE6bkjgAAAABJRU5ErkJggg== " /> </div> </div> <div> <div class="blog-card__authors-text"> <div class="blog-card-author-list" style="width: 100%;"> <a href="/users/853590"><p class="blog-card__owner">Lian Guoxi</p></a> <p class='blog-card__remaining-text'>and 10 more</p> </div> </div> <time datetime="2024-11-13" class="blog-card__date">November 13, 2024</time> </div> </div> </div> <div class='blog-card__preview-content-container'> <a href="/doi/full/10.22541/essoar.173152380.04374748/v1"> <div class='blog-card__preview-content'> Neutral in-situ leaching (ISL) is a prominent technique for extracting uranium (U) from sandstone-type U deposits. However, the intricate biogeochemical processes and associated microbial communities in environments subjected to prolonged neutral in-situ U leaching remain insufficiently understood. Here, capitalizing on groundwater samples collected from an area subjected to two decades of ISL (Undergoing-ISL) and a background aquifer (Pre-ISL) at the Qianjiadian U mining site (the first CO2+O2 ISL site located in the Songliao Basin of northern China) we investigate the responses of aquifer microbiomes to CO2+O2 ISL using genome-resolved metagenomics resulting in a total of 315 good-quality bacterial metagenome-assembled genomes (MAGs) and 5 archaeal genomes. Five putative keystone MAGs were identified based on their high connection degree and low betweenness centrality within the co-occurrence network of reconstructed MAGs, notably highlighting the prevalence of microorganisms involved in sulfur, ammonium, and Fe(Ⅱ) oxidation, which are integral to facilitating U(Ⅳ) oxidation during CO2+O2 ISL. In particular, sulfur-oxidizing bacteria and Fe(Ⅱ)-oxidizing bacteria (Rhodoferax and SHZL01) played a key role in U mobilization during long-term neutral ISL. These findings enhance our understanding of subsurface microbial ecology and hold significant implications for bioremediation strategies and groundwater management in regions affected by mining. </div> </a> </div> </div> </div> <div class="blog-card"> <div class="blog-card__container"> <div class='blog-card__top-row'> </div> <div class='blog-card__heading-container '> <a href="/doi/full/10.22541/essoar.173152395.50921473/v1"> <div class="blog-card__title"> Assessing Channel Bank-Height Adjustments and Flood Frequency Trends in a Decoupled C... </div> </a> </div> <div class="blog-card__author-container"> <div class="blog-card__author-information"> <div class="blog-card__images-container"> <div class="blog-card__first-avatar"> <img alt="JeongYeon Han" width="24" height="24" class="user-profile-pic" src="data:image/jpg;base64,iVBORw0KGgoAAAANSUhEUgAAACAAAAAgCAMAAABEpIrGAAAABGdBTUEAALGP C/xhBQAAACBjSFJNAAB6JgAAgIQAAPoAAACA6AAAdTAAAOpgAAA6mAAAF3Cc ulE8AAABVlBMVEVSvIlRvIlRu4hRvIhUvYtUvIpWvYtTvIpTvIlEtn9Gt4FO uoY+tHtDtn9KuYM9s3pKuYRQu4hyyJ9sxppIuIJVvYuL0rB6y6Rkw5WT1bVi wpRLuYRNuoX////2+/kxr3JqxZnu+PNWvYw7s3me2b2W1rfr9/EwrnLj9OxX vow8s3qY17iQ1LPr9/IwrnFlw5bk9O05snhPu4c3sXaR1LTs9/Lh8+o0sHSS 1bUvrnFnxJeU1bZMuoVMuYRmxJf3/Pm75NDE6NfG6Ni75NHa8OVAtX1MuYVl w5Xe8ukgqGcdp2WJ0a6R1LNdwJDn9e6z4cs4sndFt4Dm9e5BtX1Xvo1bv49A tXyb2Ls1sHWf2b2/5tNmw5fi8+uX1riI0a7t+PKe2byV1rdgwZKc2LuK0a+i 2r+K0q9JuINsxpur3sZpxZlJuIJUvYpHuII6s3k6sng9tHsAAAB1RjC/AAAA AWJLR0Rxrwdc4gAAAAd0SU1FB+gLFRAXDDbHzj4AAAFwSURBVDgR3cHpWtNQ FAXQnX2b5thEqZoymBwL9wrSiq2WVkURHHCeEBVlEhUVZRDf/5fFFCn9fALW wvHk4S8P/8EOgG0GvYicT+RzBBjkhehB8ERBwugkSDnVVxQS3YjT4Zmzcal/ oAgpDg6dS4ToRklDPV8e1pFIrLugo87SoAslTXTs4qCOR36lekknnKVBF0qa 6OVaXa9cbcjkqDadpcE/hpQ00Vatrteux0n5hjadpcEBQ1LSRFtTN7XjlrM0 OEDkfJm+ra3ajM7euXvv/pwOOUuDDInQPSiFD3Ws9kgfP5l0T5/pc2dpkGFQ fPHy1XzhtbbKdV148/bd4nttOkuDDBEmqjMflnR5akVXq8i7NZ2oWhpkyFLf R22blWhY1yOx7pN+dpYGHWQQfVnb+FqIG5Vv3zcRxD9+bm0HxCHu7P7a+93w Ee4tgpR4flNIHPLoW5sHCVsiwKASEEcwA7YB3Icexnho8zzs83Cs/AHwLivF /luzqwAAACV0RVh0ZGF0ZTpjcmVhdGUAMjAyNC0xMS0yMVQxNjoyMzoxMisw MDowME1oYmQAAAAldEVYdGRhdGU6bW9kaWZ5ADIwMjQtMTEtMjFUMTY6MjM6 MTIrMDA6MDA8NdrYAAAAIHRFWHRzb2Z0d2FyZQBodHRwczovL2ltYWdlbWFn aWNrLm9yZ7zPHZ0AAAAYdEVYdFRodW1iOjpEb2N1bWVudDo6UGFnZXMAMaf/ uy8AAAAYdEVYdFRodW1iOjpJbWFnZTo6SGVpZ2h0ADYwMHrevbUAAAAXdEVY dFRodW1iOjpJbWFnZTo6V2lkdGgANjAw6S/t6AAAABl0RVh0VGh1bWI6Ok1p bWV0eXBlAGltYWdlL3BuZz+yVk4AAAAXdEVYdFRodW1iOjpNVGltZQAxNzMy MjA2MTkyWskzbwAAABJ0RVh0VGh1bWI6OlNpemUAODE4NUJCCDpbMQAAADx0 RVh0VGh1bWI6OlVSSQBmaWxlOi8vdG1wL2xldHRlcl9hdmF0YXJzLzIvSkgv ODJfMTg4XzEzNy82MDAucG5ncj5YdAAAAABJRU5ErkJggg== " /> </div> <div class="blog-card__second-avatar"> <img alt="Wonsuck Kim" width="24" height="24" class="user-profile-pic" src="data:image/jpg;base64,iVBORw0KGgoAAAANSUhEUgAAACAAAAAgCAAAAABWESUoAAAABGdBTUEAALGP C/xhBQAAACBjSFJNAAB6JgAAgIQAAPoAAACA6AAAdTAAAOpgAAA6mAAAF3Cc ulE8AAAAAmJLR0QAAKqNIzIAAAAHdElNRQfoCxUQGBpFi2egAAABn0lEQVQ4 EYXBy05TARiF0W//59JSCzREipImRgeIMRIHDnwdX5WJA0dG40gSExNCpKTY Qi/ntj2FuWctnfN/QYegQ9Ah6BB0CDqktAzIgDAPZFoCUsASBslGMqIBCVuQ guWCDNVVLpoii01kVlMol0Vg2UfjRnV/IjfZi4EnB3VUMZlgmQBUvn4nFyen +1U5PhnG6WnVVB/eDEoBgaz6ir0i32VUe49pULE627n8nmMRtJIb9otBxlN0 wDoh7k6O5t+GWBCA0wWj8pCLQZ6mszJYHr8svvRkAUErNs2Iw81vnvSYSQzf 86PMLFoBOOqb2B3O5hwMuE2gn3GWVzKtAEFMec41i/GYRWr4/DPersRW0HIy 5xW3+dXw2V0RZjH7tTo6XoaBYCtZVr3Fuj9FM8vQj6+c5YUMQctJOWfq9L7k b0KQNb3bCz7KMsknEGhdXBLNavlHor5eKZttik0ZSOeAUVnliVXUvaDZJLnF 2nlikdISznJb7mETAxpZO9iClEc2ggaEDcgGASkPxJbYElviUdAh6BB0CDoE HYIO/wAMIrbhpriFWwAAACV0RVh0ZGF0ZTpjcmVhdGUAMjAyNC0xMS0yMVQx NjoyNDoyNiswMDowMNV0Wu0AAAAldEVYdGRhdGU6bW9kaWZ5ADIwMjQtMTEt MjFUMTY6MjQ6MjYrMDA6MDCkKeJRAAAAIHRFWHRzb2Z0d2FyZQBodHRwczov L2ltYWdlbWFnaWNrLm9yZ7zPHZ0AAAAYdEVYdFRodW1iOjpEb2N1bWVudDo6 UGFnZXMAMaf/uy8AAAAYdEVYdFRodW1iOjpJbWFnZTo6SGVpZ2h0ADYwMHre vbUAAAAXdEVYdFRodW1iOjpJbWFnZTo6V2lkdGgANjAw6S/t6AAAABl0RVh0 VGh1bWI6Ok1pbWV0eXBlAGltYWdlL3BuZz+yVk4AAAAXdEVYdFRodW1iOjpN VGltZQAxNzMyMjA2MjY22HpV4AAAABN0RVh0VGh1bWI6OlNpemUAMTExMzNC QvPWj0kAAAA9dEVYdFRodW1iOjpVUkkAZmlsZTovL3RtcC9sZXR0ZXJfYXZh dGFycy8yL1dLLzE5NF8xOTRfMTk0LzYwMC5wbmcSnV21AAAAAElFTkSuQmCC " /> </div> </div> <div> <div class="blog-card__authors-text"> <div class="blog-card-author-list" style="width: 100%;"> <a href="/users/853589"><p class="blog-card__owner">JeongYeon Han</p></a> <p class='blog-card__remaining-text'>and 2 more</p> </div> </div> <time datetime="2024-11-13" class="blog-card__date">November 13, 2024</time> </div> </div> </div> <div class='blog-card__preview-content-container'> <a href="/doi/full/10.22541/essoar.173152395.50921473/v1"> <div class='blog-card__preview-content'> A series of processes involving sediment delivery from channels, its dispersal onto the floodplain, and storage at their channel margins, often generates natural levees. When levees breach, they release water and sediment onto the floodplain, leading to crevasse splays or avulsions. Despite their importance in constructing floodplains and influencing channel mobility, levee growth is poorly understood. Presently, no model fully explains dynamic channel-levee evolution. A common assumption is that levee and channel bed aggradation rates are coupled. If they coevolve, levees should progressively accumulate along any aggrading channel belt, yet observations indicate otherwise. Using a one-dimensional numerical model, we investigate levee growth decoupled from channel bed aggradation across two flood scenarios wherein the flooded level: 1) exceeds the levee crest height (i.e., front loading); 2) is lower than the levee crest causing partial inundation of distal levee deposits (i.e., back loading). Initially, rapid levee aggradation confines the channel and increases bankfull depth, which mitigates flooding. As confinement slows levee growth, channel bed aggrades until bankfull depth is sufficiently reduced to trigger overflows. This releasing process increases flood likelihood and enhances overbank accumulation, promoting front loading and re-confining the channel. Our findings suggest aggradational channels may experience confined-release phases, characterized by episodic levee growth and fluctuations in bankfull depth. Rapid in-channel aggradation increases flood frequency and variability with more confined-release cycles. These results imply that river avulsions and associated floods might preferentially occur when the channel bed aggrades faster than adjacent levees, whereby the channel becomes shallower and destabilized. </div> </a> </div> </div> </div> <div class="blog-card"> <div class="blog-card__container"> <div class='blog-card__top-row'> </div> <div class='blog-card__heading-container '> <a href="/doi/full/10.22541/essoar.173160182.21037546/v1"> <div class="blog-card__title"> Solar Wind Speed Forecasting using a Hybrid CNN-LSTM Deep Learning Model </div> </a> </div> <div class="blog-card__author-container"> <div class="blog-card__author-information"> <div class="blog-card__images-container"> <div class="blog-card__first-avatar"> <img alt="A. N. Aneesh" width="24" height="24" class="user-profile-pic" src="data:image/jpg;base64,iVBORw0KGgoAAAANSUhEUgAAACAAAAAgCAMAAABEpIrGAAAABGdBTUEAALGP C/xhBQAAACBjSFJNAAB6JgAAgIQAAPoAAACA6AAAdTAAAOpgAAA6mAAAF3Cc ulE8AAABdFBMVEXiX1HhXlDiXlDiYVPgVEXfUkPfU0TgV0nmdWnnem/gV0jm eG3iYFL////ldGjlcWXiY1XeSTnuoprxs63dRTXxs6zvp6DdSDj88/H76+r4 29jfUkLhXE7hXU7fUUL43Nn76ef99/beSjrsm5LogHXognfeTT7iYlTfTj/n fnPog3nsmpHmeW3fUEHiYVTzvbfjZVj31NHdRjbdRjX2zcniY1bzwLvdRDTh W0365OHZMiDYKhj1ysbhWUrhWkzYKxjZMR/54N3gVkfhW0ziX1LiX1DiYlXe SzzqjIL0x8L1yMP54t/toJfeTT3eTj7tnJP65+XqkIbeSjvdRzf308/++/v+ /fz76+n66ObeSzv+/Pz77Ov42tfiYFP54N7bOinaNSP20c3hXU/31dHaNSTb OSj53tvgVUbxta7tnZTjZFfiZFbxtK7wrqfqj4XsmZDyubPrlYzvq6ThWkvu pp7rkYfvp5/hXE3vqqPsl47fTz8AAADzsHetAAAAAWJLR0R7T9K1/AAAAAd0 SU1FB+gLFRAXBtYSJyAAAAFxSURBVDgR5cEJQwxxHAbg9/3N1mbMW/9hGTEl g2bdV0uujWpHhygkue+jdYfw6Y3J2uQb8Dz43zCHAnP4i5nngcgRnmeG9YhS B0DAiM4SiD+RKHdtKBMk4G/s8kFiDWNQ9qTuDo/0Onsk5wc0tBlduEnaXHGk q2yRtkaOhjYiCLf1bteOGOjr186BXQlA/Gb0+ru1e4/2DqZpdZ/2H9DBQ4dp aCFd5YiOxjp2PE1PDAk1nTzlSLQQwyWdPnP2nOLz9bqGRi5c1OjYOBv4hdml CQ1MTk3r8syVq5qempzV3LWMhlVkev2GeudvLujW4uKsFm7P39HdyCOxivdG qfsPouThI2WP9eRpEj17rtoLjygYs+SlXoVLzcEJvX6jtzPNpeSd3icZDT8Z 4X/42FwOEA9/+jz3ZWUFwbL7+s0HDAUjvkd1kOgLq9UwBomxqAoaWpjWxgkQ Lk0dCBC1lGhjDjkWkGMOazQMBcuhYA38Q34ARU0uXV3st5AAAAAldEVYdGRh dGU6Y3JlYXRlADIwMjQtMTEtMjFUMTY6MjM6MDYrMDA6MDB1jUbpAAAAJXRF WHRkYXRlOm1vZGlmeQAyMDI0LTExLTIxVDE2OjIzOjA2KzAwOjAwBND+VQAA ACB0RVh0c29mdHdhcmUAaHR0cHM6Ly9pbWFnZW1hZ2ljay5vcme8zx2dAAAA GHRFWHRUaHVtYjo6RG9jdW1lbnQ6OlBhZ2VzADGn/7svAAAAGHRFWHRUaHVt Yjo6SW1hZ2U6OkhlaWdodAA2MDB63r21AAAAF3RFWHRUaHVtYjo6SW1hZ2U6 OldpZHRoADYwMOkv7egAAAAZdEVYdFRodW1iOjpNaW1ldHlwZQBpbWFnZS9w bmc/slZOAAAAF3RFWHRUaHVtYjo6TVRpbWUAMTczMjIwNjE4NkS/xjcAAAAT dEVYdFRodW1iOjpTaXplADEzODM3QkK0B+TvAAAAO3RFWHRUaHVtYjo6VVJJ AGZpbGU6Ly90bXAvbGV0dGVyX2F2YXRhcnMvMi9BQS8yMjZfOTVfODEvNjAw LnBuZ/qgv4oAAAAASUVORK5CYII= " /> </div> <div class="blog-card__second-avatar"> <img alt="Smitha V Thampi" width="24" height="24" class="user-profile-pic" src="data:image/jpg;base64,iVBORw0KGgoAAAANSUhEUgAAACAAAAAgCAMAAABEpIrGAAAABGdBTUEAALGP C/xhBQAAACBjSFJNAAB6JgAAgIQAAPoAAACA6AAAdTAAAOpgAAA6mAAAF3Cc ulE8AAABI1BMVEWiiH6ih32iiH2hh32iiH+kioGki4GiiX+jioCjiYCehHmW eW6Vd2ueg3mYfHGVd2yWeG2afnOjiX+Ye3CghXvAr6jKvLbCsaq9q6THuLLD s6zEtK7FtK7DsqzJurS4pJycgHaXem+3o5z///+/raaMa1/7+vnl3tyUd2uf hHmznpaul479/fynjoWnj4aljILLvbeqkomxm5Pc0s6BXlCRc2eSdGiObmK/ raecgXadgXefhHqdgnemjYO5pZ7Yzsqtlo2VeG3Es63Nv7n6+PjQwr2cgXeu mI/7+vqxnJSkioDIubO4pZ2TdGmFY1a/rqfFta+mjoSZfXL08fCnj4Xu6ui3 o5uVeGzaz8vGt7Gwm5Khhnyeg3iqk4rFta6hh34AAACztoomAAAAAWJLR0Rg xbd8EAAAAAd0SU1FB+gLFRAXGCwdGkMAAAFJSURBVDgR3cGNXtJQHAbg9/CO s6OTdsZECpCaf01FDbVUKqm28iPNyu+vkfd/F8UPcRBegc+DJ0fl8I/qwf84 AsPo5HXeJY3uGSOG0Ix7E17B4Jlvu/wAJDIshpOlqTK8wvMXlWqtOl1/+col +kgTzUjX7Nxr6Zlf0CTu0VmESCNYWpaVN43mqqw2G2vjIPpognV5+44bZSlt FrZa0tp6/wHEAzofKTIb+n64XWxHNalFbZfIkCb6JCKfv1hQx4kksSYxiCbE 128iO3FRx4kkVlMhQ2I3DGK7ty/fg3acSGI1FTI8iA7lx1Hz5y/5bY/jRBKr qZChOZmR07OA53Jx0rYVqVhNhQxpLsvSdXXpanst11ZTYQDpWqdaP7zxboG0 86eTOsQQ8iC1vh8UQSL1UvAOw0hXa21AgG7eJUawBwC78IicUniq/gJEPyat 1fMjEgAAACV0RVh0ZGF0ZTpjcmVhdGUAMjAyNC0xMS0yMVQxNjoyMzowOSsw MDowMIPFNgAAAAAldEVYdGRhdGU6bW9kaWZ5ADIwMjQtMTEtMjFUMTY6MjM6 MDkrMDA6MDDymI68AAAAIHRFWHRzb2Z0d2FyZQBodHRwczovL2ltYWdlbWFn aWNrLm9yZ7zPHZ0AAAAYdEVYdFRodW1iOjpEb2N1bWVudDo6UGFnZXMAMaf/ uy8AAAAYdEVYdFRodW1iOjpJbWFnZTo6SGVpZ2h0ADYwMHrevbUAAAAXdEVY dFRodW1iOjpJbWFnZTo6V2lkdGgANjAw6S/t6AAAABl0RVh0VGh1bWI6Ok1p bWV0eXBlAGltYWdlL3BuZz+yVk4AAAAXdEVYdFRodW1iOjpNVGltZQAxNzMy MjA2MTg51ADbpgAAABN0RVh0VGh1bWI6OlNpemUAMTc0NDBCQnL+ZcQAAAA9 dEVYdFRodW1iOjpVUkkAZmlsZTovL3RtcC9sZXR0ZXJfYXZhdGFycy8yL1NU LzE2Ml8xMzZfMTI2LzYwMC5wbmd8+/y2AAAAAElFTkSuQmCC " /> </div> </div> <div> <div class="blog-card__authors-text"> <div class="blog-card-author-list" style="width: 100%;"> <a href="/users/853586"><p class="blog-card__owner">A. N. Aneesh</p></a> <p class='blog-card__remaining-text'>and 3 more</p> </div> </div> <time datetime="2024-11-14" class="blog-card__date">November 14, 2024</time> </div> </div> </div> <div class='blog-card__preview-content-container'> <a href="/doi/full/10.22541/essoar.173160182.21037546/v1"> <div class='blog-card__preview-content'> Accurate prediction of the solar wind speed and arrival of solar transient events are among the most important but still open problems in space weather research. This article implements a Convolutional Neural Network (CNN) coupled Long-Short Term Memory cell (LSTM) deep-learning model for the prediction of solar wind speed at Sun-Earth L1 on a daily and 6-hourly basis. The model is trained and validated using Solar-wind speed observations at Sun-Earth L1. The proposed CNN-LSTM models are developed and trained using data for the period from 01 August 1996 to 31 December 2019 and tested with the data from 01 January 2020 to 30 June 2024. The daily prediction model can forecast solar wind speed with a RMSE of 52.12 km/s and an overall correlation coefficient of 0.79, while the 6-hourly model can forecast solar wind speed with a RMSE of 33.72 km/s and an overall correlation coefficient of 0.93. This shows that without explicitly building in physics based relationships, the Deep Learning based models are able to perform reasonably well compared to existing approaches. </div> </a> </div> </div> </div> <div class="blog-card"> <div class="blog-card__container"> <div class='blog-card__top-row'> </div> <div class='blog-card__heading-container '> <a href="/users/853579/articles/1239069-soil-physics-informed-neural-networks-to-estimate-bimodal-soil-hydraulic-properties?commit=b4c70a5aa0612e3649f66b18c194f8c78ed1e20a"> <div class="blog-card__title"> Soil Physics-Informed Neural Networks to Estimate Bimodal Soil Hydraulic Properties </div> </a> </div> <div class="blog-card__author-container"> <div class="blog-card__author-information"> <div class="blog-card__images-container"> <div class="blog-card__first-avatar"> <img alt="Jieliang Zhou" width="24" height="24" class="user-profile-pic" src="data:image/jpg;base64,iVBORw0KGgoAAAANSUhEUgAAACAAAAAgCAMAAABEpIrGAAAABGdBTUEAALGP 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</div> </div> </div> <div class='blog-card__preview-content-container'> <a href="/users/853579/articles/1239069-soil-physics-informed-neural-networks-to-estimate-bimodal-soil-hydraulic-properties?commit=b4c70a5aa0612e3649f66b18c194f8c78ed1e20a"> <div class='blog-card__preview-content'> Pedotransfer functions (PTFs) are widely used to estimate soil hydraulic properties (SHPs) from easily measurable characteristics. However, most existing PTFs rely on unimodal hydraulic models, which fail to accurately represent the bimodal SHPs caused by soil structure common in field conditions. In this study, we developed new PTFs using two bimodal soil hydraulic models and introduced soil physics-informed neural networks (SPINN) to embed the models into PTF training. The results showed that the new PTFs effectively captured bimodality in hydraulic conductivity curves, achieving an RMSE of 0.578 in the test set, compared to 0.709 for unimodal models. The PTFs also improved soil water retention curve (SWRC) predictions but struggled with bimodal SWRCs for some samples, likely due to the limited number of bimodal SWRCs in the dataset. An independent dataset evaluation revealed that the RMSE for hydraulic conductivity predicted by the new PTFs was approximately one-third of that of classic PTFs. This underscores the significant role of soil structure in SHPs, which classic PTFs fail to capture. Additionally, PTFs developed using the SPINN method outperformed those optimized fitted hydraulic parameters via machine learning, a common approach in the literature. We also found that separate versus simultaneous optimization of water retention and hydraulic conductivity greatly affects PTF performance. Finally, we provided global 1 km-resolution maps of soil hydraulic parameters for the bimodal model. </div> </a> </div> </div> </div> <div class="blog-card"> <div class="blog-card__container"> <div class='blog-card__top-row'> </div> <div class='blog-card__heading-container '> <a href="/doi/full/10.22541/essoar.173152946.64602365/v1"> <div class="blog-card__title"> Unveiling the Stochasticity of Bank Erosion: A Hybrid Deterministic and Stochastic Mo... </div> </a> </div> <div class="blog-card__author-container"> <div class="blog-card__author-information"> <div class="blog-card__images-container"> <div class="blog-card__first-avatar"> <img alt="Zhi Li" width="24" height="24" class="user-profile-pic" src="data:image/jpg;base64,iVBORw0KGgoAAAANSUhEUgAAACAAAAAgCAMAAABEpIrGAAAABGdBTUEAALGP C/xhBQAAACBjSFJNAAB6JgAAgIQAAPoAAACA6AAAdTAAAOpgAAA6mAAAF3Cc ulE8AAABBVBMVEWt1n2t1nys1Xys1nyu1n+v14Ct1n6k0W6i0Gui0Gyk0W+p 1Hej0W2t1X2q1HjI46nN5rDK5KzL5a3O5rHH46el0nG12onM5a602Ymo03X/ ///7/fiZzF6q1Hm424653JDt9uPK5Kun03Sp1HaazF/A35vl8tWgz2mj0W7L 5ayu1n6v14Gm0nOh0Grv9+a93pai0G2x2IOfz2jd7sqezmau1oCm0nKy2IX6 /Pew14LL5a6s1Xuh0Gv1+vCdzmWm0nHH46abzWGo03ar1XrV6r3g78263JK3 246424+73ZTR6Law14G63JG63JPM5a+93per1XvN5q/N5rHS6LjQ57Wx2IQA AAD+OzANAAAAAWJLR0RWCg3piQAAAAd0SU1FB+gLFRAXFsulN0QAAAElSURB VDgR3cGJOgJRGAbgb77OGecoyYTh16KyHUS2sZSt7Ev2+78VnkGaPG7A++Kf 8WL4C/ul8AuhdEzR1z4xiOCQsR/MsJ/OpMERJBDMjubGgiDIj09MhlNpn0gg OC2fZgp5yVlND/0IFkvlUpmzMl4IpWI1PSQQrE7U5uZlYXHJibOaHpJSWF6p rYisMuPEWU0PAwjU12S9sWGcOKvpYQD1Zl62ttWOdeKsJokEqmhX9iKqfevk YGlfKRB9iGbrUDaOpo9rLScnp+0o6oDoIZU5k/POxeXVdb0iN7d3pfvlDohv RJHyJdOV2EOkiG/EI3O5bhgePD1XSy9BGAavb1kQPUSzYT5YY9muW2OsKYIp /CD0F/o6BiKBv2CQFwPgxfCvvANnvhzgHMwTigAAACV0RVh0ZGF0ZTpjcmVh dGUAMjAyNC0xMS0yMVQxNjoyMzoyMiswMDowMMPnZYcAAAAldEVYdGRhdGU6 bW9kaWZ5ADIwMjQtMTEtMjFUMTY6MjM6MjIrMDA6MDCyut07AAAAIHRFWHRz b2Z0d2FyZQBodHRwczovL2ltYWdlbWFnaWNrLm9yZ7zPHZ0AAAAYdEVYdFRo dW1iOjpEb2N1bWVudDo6UGFnZXMAMaf/uy8AAAAYdEVYdFRodW1iOjpJbWFn ZTo6SGVpZ2h0ADYwMHrevbUAAAAXdEVYdFRodW1iOjpJbWFnZTo6V2lkdGgA NjAw6S/t6AAAABl0RVh0VGh1bWI6Ok1pbWV0eXBlAGltYWdlL3BuZz+yVk4A AAAXdEVYdFRodW1iOjpNVGltZQAxNzMyMjA2MjAyiU02fwAAABJ0RVh0VGh1 bWI6OlNpemUAOTkzNUJCJBdEVAAAAD10RVh0VGh1bWI6OlVSSQBmaWxlOi8v dG1wL2xldHRlcl9hdmF0YXJzLzIvWkwvMTczXzIxNF8xMjUvNjAwLnBuZ32w /xQAAAAASUVORK5CYII= " /> </div> <div class="blog-card__second-avatar"> <img alt="Eddy J. Langendoen" width="24" height="24" class="user-profile-pic" src="data:image/jpg;base64,iVBORw0KGgoAAAANSUhEUgAAACAAAAAgCAMAAABEpIrGAAAABGdBTUEAALGP C/xhBQAAACBjSFJNAAB6JgAAgIQAAPoAAACA6AAAdTAAAOpgAAA6mAAAF3Cc ulE8AAABGlBMVEV4hM13hM13g813g8x7h856hs16hs50gMtmc8ZmdMZlc8Zs ech5hc1qd8dzgMt/is+xuOKqsd+psd+osN+wt+Gcpdpqd8iZotmhqdx1gcx2 gsxtesiPmdX////p6/dWZcD3+Px1gcttesmKlNPR1e17hs6NmNWOmNWHktJi cMXt7vhzf8vHzOpXZsBwfMpxfspndMbu7/jGy+pYZ8FvfMlreMhue8mNl9R6 hc1jccXv8PmMltTu8PjM0OzU2O/W2e9kcsXu8PnEyelOXr1ndcfJzutbasJw fcpxfcppdsfQ1O2JlNPr7feLldSMl9T6+v1aacLy8/r+/v5/i8+zueKrsuCr st+krN2wt+Kqst+vtuGlrd1yfsoAAAAulkbFAAAAAWJLR0Rdnd8wAQAAAAd0 SU1FB+gLFRAXD6/On4QAAAEjSURBVDgR3cHpOgJhGAbgR0/ffFNTiETLa5kR MaRIyb6T7CTb+R+Hmh+ZmYsT6L4xZEYiffgXffAHIupRVAaIMBLajPXErYSV JIgQYnRsPDWRmkxPZaZnsjkQQVT5gnhm5+ZlQYMIorIdWSwuOcullVVxNYgg KtuRtfWyZW1UquJqEEFUtiObW7XtOmJVcTWIIKp8Qzw7zV1xNYggqvye7B8c Hh3i+ERcDZLwo7IdOT07b5qJSlWyuaJKEH5UtiMXl/qqfB2rSqtVt2qIEL+o bEduVKPdcJq3Uird3bc1QAxQ5QvieXh8kr5nGyAGCPfltfPWSaW7me57qvPx +fUNEAMktNkTiyeRjJumGW+RhB8R9Rg0on0GEcIwhEU8ACJ9GC4/Ka4gGars XrAAAAAldEVYdGRhdGU6Y3JlYXRlADIwMjQtMTEtMjFUMTY6MjM6MTUrMDA6 MDCIz1zqAAAAJXRFWHRkYXRlOm1vZGlmeQAyMDI0LTExLTIxVDE2OjIzOjE1 KzAwOjAw+ZLkVgAAACB0RVh0c29mdHdhcmUAaHR0cHM6Ly9pbWFnZW1hZ2lj ay5vcme8zx2dAAAAGHRFWHRUaHVtYjo6RG9jdW1lbnQ6OlBhZ2VzADGn/7sv AAAAGHRFWHRUaHVtYjo6SW1hZ2U6OkhlaWdodAA2MDB63r21AAAAF3RFWHRU aHVtYjo6SW1hZ2U6OldpZHRoADYwMOkv7egAAAAZdEVYdFRodW1iOjpNaW1l dHlwZQBpbWFnZS9wbmc/slZOAAAAF3RFWHRUaHVtYjo6TVRpbWUAMTczMjIw NjE5NcStpswAAAASdEVYdFRodW1iOjpTaXplADQwOThCQvL8RswAAAA9dEVY dFRodW1iOjpVUkkAZmlsZTovL3RtcC9sZXR0ZXJfYXZhdGFycy8yL0VMLzEy MF8xMzJfMjA1LzYwMC5wbmdyXFBDAAAAAElFTkSuQmCC " /> </div> </div> <div> <div class="blog-card__authors-text"> <div class="blog-card-author-list" style="width: 100%;"> <a href="/users/646317"><p class="blog-card__owner">Zhi Li</p></a> <p class='blog-card__remaining-text'>and 2 more</p> </div> </div> <time datetime="2024-11-13" class="blog-card__date">November 13, 2024</time> </div> </div> </div> <div class='blog-card__preview-content-container'> <a href="/doi/full/10.22541/essoar.173152946.64602365/v1"> <div class='blog-card__preview-content'> This paper presents a novel hybrid deterministic-stochastic river morphodynamics numerical modeling approach that integrates a two-dimensional (2D) hydrodynamic model (deterministic) with a bed morphodynamic model (deterministic) and a bank erosion model (Markovian stochastic). The model solves the 2D Shallow Water Equations and the standard k-epsilon turbulence model. Bedload transport is estimated using the Meyer-Peter and Muller formula, and bed evolution is solved using the Exner Equation. The Markovian stochastic bank erosion model uses a new method to evaluate bank erosion risk. The approach was applied to a meander bend cutoff event in the Maiqu River on the Tibetan Plateau. Sixteen different bank-material critical shear stress cases were considered, representing highly erodible banks to resistant banks. Ten statistical realizations were performed for each case with different bank-material erodibility to obtain ensemble-averaged results. Flow field and bed evolution in the cutoff channel suggest that the model can successfully simulate bank erosion processes during the cutoff channel evolution, and bank topographic irregularities are reasonably captured. A newly introduced calibration parameter, the ratio of mesh size to the coupling period between the bank erosion model and the hydrodynamic & morphodynamic model, is not as intuitive as the erosion resistance calibration parameters used by the traditional bank erosion model. The proposed approach necessitates estimating the size of a typical slump failure, or 10-30% of the cutbank height, to set the size of the computational mesh. </div> </a> </div> </div> </div> <div class="blog-card"> <div class="blog-card__container"> <div class='blog-card__top-row'> </div> <div class='blog-card__heading-container '> <a href="/doi/full/10.22541/essoar.173134248.83257825/v1"> <div class="blog-card__title"> The effect of different climate sensitivity priors on projected climate: A probabilis... </div> </a> </div> <div class="blog-card__author-container"> <div class="blog-card__author-information"> <div class="blog-card__images-container"> <div class="blog-card__first-avatar"> <img alt="Joseph K Brown" width="24" height="24" class="user-profile-pic" src="data:image/jpg;base64,iVBORw0KGgoAAAANSUhEUgAAACAAAAAgCAMAAABEpIrGAAAABGdBTUEAALGP C/xhBQAAACBjSFJNAAB6JgAAgIQAAPoAAACA6AAAdTAAAOpgAAA6mAAAF3Cc ulE8AAABUFBMVEVSvIlRvIhRvIlRu4hTvIlVvYtUvIpWvYxWvYtUvYpMuYVC tX5Ft4A6sng8s3o7s3k+tHtEtn9NuoVbv496y6RcwJBCtn53yqKd2byQ1LOU 1baH0K1oxJhHt4FSu4iX1rj///+b2LsiqWjC59Xy+fZJuINTvIqR1LOV1re1 4syZ17ljwpSu38jG6dg6snmR1LS2482Czqoyr3NAtXwwrnHs+PKW1re24s19 zKYmq2uBzqm55M/4/Pr0+/je8ug0sHVNuoaS1LS448/Z8OXG6NjY8OST1bVG t4E4sndKuYNZvo49tHszsHRKuINOuoZBtX31+/hvx50jqWmFz6sqrG7j9OxM uYSM0rDH6djp9vBpxZktrW+z4ctiwpTr9/Ha8Oay4cpAtX295dJqxZmAzaib 2LpIuIKf2b2V1raP07Jux5xBtX5Dtn5Pu4dUvYsAAACcOBXZAAAAAWJLR0Rv VQhhgQAAAAd0SU1FB+gLFRAXECLGknEAAAFWSURBVDgR3cFpWxJRGAbg58wz Zw6C4xkEU9x6GczIElQU963NMpNoQcsltbTF5f9/FLzkclB/gfeNB0op5eB+ ihG4B13t0jPGxNpA3EXEE3Gv3e+wQZIecRvRmUp3PeruyfT29ScGPA6ihaKx jyUb5qRhSD8ZJlooGvtU8uEzGUk9fyGjBU0iStHYouTDMRmfKE3KVDAMIoKk sUUph9MyM1uYk5yvSdxgnbFFKYfzsrAosrS84hIRdDVidlXy4Ut59Tr3Rt4G mkQTibV379c/ZCQfTks69DcW5OMmiGsOdaX3U7U0kZHy5zH5srH59Zuw5hLX HMaCLdkOOr/Lj51dGUntZWW/AhBNBBM/pe7g0B7JlV/JNhJNim7t8Hf2uGpx 0v1n9e+//2unHhFFlyXfT3pw231rO87ONdGK0MZcEPSMMTEN4hbFK2AT7nCU QoNSynHwwFwCFvUn4E8L6UAAAAAldEVYdGRhdGU6Y3JlYXRlADIwMjQtMTEt MjFUMTY6MjM6MTYrMDA6MDC5J0Z3AAAAJXRFWHRkYXRlOm1vZGlmeQAyMDI0 LTExLTIxVDE2OjIzOjE2KzAwOjAwyHr+ywAAACB0RVh0c29mdHdhcmUAaHR0 cHM6Ly9pbWFnZW1hZ2ljay5vcme8zx2dAAAAGHRFWHRUaHVtYjo6RG9jdW1l bnQ6OlBhZ2VzADGn/7svAAAAGHRFWHRUaHVtYjo6SW1hZ2U6OkhlaWdodAA2 MDB63r21AAAAF3RFWHRUaHVtYjo6SW1hZ2U6OldpZHRoADYwMOkv7egAAAAZ dEVYdFRodW1iOjpNaW1ldHlwZQBpbWFnZS9wbmc/slZOAAAAF3RFWHRUaHVt Yjo6TVRpbWUAMTczMjIwNjE5Nl2k93YAAAATdEVYdFRodW1iOjpTaXplADE1 MjkzQkJAWlfrAAAAPHRFWHRUaHVtYjo6VVJJAGZpbGU6Ly90bXAvbGV0dGVy X2F2YXRhcnMvMi9KQi84Ml8xODhfMTM3LzYwMC5wbmclK/hKAAAAAElFTkSu QmCC " /> </div> <div class="blog-card__second-avatar"> <img alt="kalyn.dorheim" width="24" height="24" class="user-profile-pic" src="data:image/jpg;base64,iVBORw0KGgoAAAANSUhEUgAAACAAAAAgCAMAAABEpIrGAAAABGdBTUEAALGP C/xhBQAAACBjSFJNAAB6JgAAgIQAAPoAAACA6AAAdTAAAOpgAAA6mAAAF3Cc ulE8AAAA21BMVEWbzl+bzl6azV6azl6czmGdz2KbzmCUylSPyEyYzFuSyVGO x0qWy1er1nq/35iez2OYzFqPyE2v2IDC4Z6p1XaWy1idz2OMxkfd7sn///+q 1Xe+35f8/fqLxkbY7MGr1nmGwz6r1XiRyVDZ7MKh0WmTylOOyEvZ7MOez2Tr 9eC43I2KxUTa7cTn89nl8taCwji73ZLS6biXzFmj0m2AwTW/35mczmDY68CV y1Xj8dLE4qKHxD/c7si12omUylWy2YXM5q6f0GaSyVCp1HXO57G63ZGTylKM x0gAAAD+TBdCAAAAAWJLR0RI8ALU6gAAAAd0SU1FB+gLFRAYNJldam8AAADw SURBVDgR3cFZQsJAEATQ6sowEUSJih07MrigAu6iIu6K2/1vJPwmwwV4D0tI MCdYgDMAZxJE0dXAhK7miQihT1fqoGusNj0FFfTNtfVW5jY2t9rbnigTar5j RTPftY6re6JMqKFre/sHZvVDxwRlQg09Ozo2K05aRJVQQ98GQzs9GxARQg3n dmGXV0rECDX0zTp2nSsRIdTQtZuRWS11RJVQQ89u7+5tmI9BVAg1PFh7kj/a 07OSKBNq/mJFmo3MXhuOgjKO394/Pkc6/fr+mXgmKEvof/8y0KVh6pkggk5B 0LUcEcUZgHNYQDAnWDr/hfUSjyJgWYoAAAAldEVYdGRhdGU6Y3JlYXRlADIw MjQtMTEtMjFUMTY6MjQ6MDIrMDA6MDBjHnmDAAAAJXRFWHRkYXRlOm1vZGlm eQAyMDI0LTExLTIxVDE2OjI0OjAyKzAwOjAwEkPBPwAAACB0RVh0c29mdHdh cmUAaHR0cHM6Ly9pbWFnZW1hZ2ljay5vcme8zx2dAAAAGHRFWHRUaHVtYjo6 RG9jdW1lbnQ6OlBhZ2VzADGn/7svAAAAGHRFWHRUaHVtYjo6SW1hZ2U6Okhl aWdodAA2MDB63r21AAAAF3RFWHRUaHVtYjo6SW1hZ2U6OldpZHRoADYwMOkv 7egAAAAZdEVYdFRodW1iOjpNaW1ldHlwZQBpbWFnZS9wbmc/slZOAAAAF3RF WHRUaHVtYjo6TVRpbWUAMTczMjIwNjI0Mu0h83sAAAATdEVYdFRodW1iOjpT aXplADExNTQ2QkKdStPbAAAAO3RFWHRUaHVtYjo6VVJJAGZpbGU6Ly90bXAv bGV0dGVyX2F2YXRhcnMvMi9LLzE1NV8yMDZfOTUvNjAwLnBuZ/XvFmUAAAAA SUVORK5CYII= " /> </div> </div> <div> <div class="blog-card__authors-text"> <div class="blog-card-author-list" style="width: 100%;"> <a href="/users/853553"><p class="blog-card__owner">Joseph K Brown</p></a> <p class='blog-card__remaining-text'>and 5 more</p> </div> </div> <time datetime="2024-11-11" class="blog-card__date">November 11, 2024</time> </div> </div> </div> <div class='blog-card__preview-content-container'> <a href="/doi/full/10.22541/essoar.173134248.83257825/v1"> <div class='blog-card__preview-content'> Understanding equilibrium climate sensitivity (ECS, warming in response to a doubling of CO2) uncertainty is fundamental for making reliable climate projections. We leverage the Hector simple climate model in a probabilistic framework to explore how different ECS priors influence long-term (2081-2100) temperature anomalies. Specifically, we quantify how different ECS prior distributions broaden the uncertainty in temperature projections. This method demonstrates a computationally efficient probabilistic workflow that explores the effects of parameter priors on climate projections. Excluding process and paleoclimate evidence widens the resulting temperature projection uncertainty (1.12-3.03 ℃ and 1.09-3.33 ℃, respectively) while using priors that synthesize all lines of evidence leads to narrowed temperature projection uncertainty (1.24-2.89 ℃). Our study shows that excluding paleoclimate and process data in ECS priors broadens temperature projection uncertainty. In contrast, synthesized evidence provides a narrower and potentially more robust range of future temperature outcomes. </div> </a> </div> </div> </div> <div class="blog-card"> <div class="blog-card__container"> <div class='blog-card__top-row'> </div> <div class='blog-card__heading-container '> <a href="/doi/full/10.22541/essoar.173117029.91729676/v1"> <div class="blog-card__title"> Continuous Monitoring of Permafrost and Active Layer Dynamics with Automated Electric... </div> </a> </div> <div class="blog-card__author-container"> <div class="blog-card__author-information"> <div class="blog-card__images-container"> <div class="blog-card__first-avatar"> <img alt="Teddi Herring" width="24" height="24" class="user-profile-pic" src="data:image/jpg;base64,iVBORw0KGgoAAAANSUhEUgAAACAAAAAgCAAAAABWESUoAAAABGdBTUEAALGP C/xhBQAAACBjSFJNAAB6JgAAgIQAAPoAAACA6AAAdTAAAOpgAAA6mAAAF3Cc ulE8AAAAAmJLR0QAAKqNIzIAAAAHdElNRQfoCxUQFxgsHRpDAAABUElEQVQ4 EYXBPW4TURSG4fc7c2dMJjIRiAIhsgLECqBkBRQ0LC8byBLSILosIFWAIgKB EBHGY3vuOcyPLSJF4j6Pzvg/o8AoMAqMAqPAKEiMgrsEAYhRYmJiEm7yUMjC mSQgULcVg6jadT6ykK/SIsQgMdD22ZOtIFJ3dXr8ZVfl+sWvb3UISAyse/mc iV++Wp7/aLpHr2/OmwhBYuDHH9vV4zfXH076ZrN0ULALJglQVL9vO9h+3agS 7p4dMUsMFHWlBemo9Q143/fOQWIS7kG4O/COuxIjBTMBn/sq16fsJe65+N6u nr5nL3HPw9wulhwY/4QAJ3vOjjMzDowaggUJYTRiUr1lpnx7vTPU/bwJKfpP qwoEOmMS8nXdBFr3bRXKf+oHgYDETGHLcBGtPBTVSbgYJfYUmZGDUGT2Egdi JCbiwCgwCowCo8AoMAr+AmN6hahjS5oiAAAAJXRFWHRkYXRlOmNyZWF0ZQAy MDI0LTExLTIxVDE2OjIzOjI0KzAwOjAwoDdQvQAAACV0RVh0ZGF0ZTptb2Rp ZnkAMjAyNC0xMS0yMVQxNjoyMzoyNCswMDowMNFq6AEAAAAgdEVYdHNvZnR3 YXJlAGh0dHBzOi8vaW1hZ2VtYWdpY2sub3JnvM8dnQAAABh0RVh0VGh1bWI6 OkRvY3VtZW50OjpQYWdlcwAxp/+7LwAAABh0RVh0VGh1bWI6OkltYWdlOjpI ZWlnaHQANjAwet69tQAAABd0RVh0VGh1bWI6OkltYWdlOjpXaWR0aAA2MDDp L+3oAAAAGXRFWHRUaHVtYjo6TWltZXR5cGUAaW1hZ2UvcG5nP7JWTgAAABd0 RVh0VGh1bWI6Ok1UaW1lADE3MzIyMDYyMDRgLpNKAAAAEnRFWHRUaHVtYjo6 U2l6ZQAyNDQ1QkIrl0ifAAAAPXRFWHRUaHVtYjo6VVJJAGZpbGU6Ly90bXAv bGV0dGVyX2F2YXRhcnMvMi9USC8xNjNfMTYzXzE2My82MDAucG5nOJsu3wAA AABJRU5ErkJggg== " /> </div> <div class="blog-card__second-avatar"> <img alt="Mohammad Farzamian" width="24" height="24" class="user-profile-pic" src="data:image/jpg;base64,iVBORw0KGgoAAAANSUhEUgAAACAAAAAgCAMAAABEpIrGAAAABGdBTUEAALGP C/xhBQAAACBjSFJNAAB6JgAAgIQAAPoAAACA6AAAdTAAAOpgAAA6mAAAF3Cc ulE8AAABdFBMVEX+2hD+2g/+2Q/92Q/+2hP+2hX+2hT+2hH+2xb+2hb91wH9 1QD91gD92Qz92Af91wD91AD92An92AT+4Dj+5mD+4kf92Qv92Q7+5Fb+5Vz+ 3CL+4kT+6nf+52b+52j+52f+6XT+3B392Aj+8q/////+3CD+2hL+5mL+5l39 0AD+8aj+4UD+8KT+637+99D+5FT+75b+6XL+2xn+3zX+3jD+8an+/fT+/O/+ 3CH+++b+5VX+75j+5FX90wD92Qj92AP+7Yz+3zT+7ZH+6XX+5FP+4kb9zwD+ 8ab+3Sb+87P+9Ln+4UH+5FH+75v+98r+8qz+87X+98v+8aT92Qn+8qv+4Dv+ 407+75z+/fX+8J/+3i3+4Df+7Y/90gD+7Y3+8aX+3i/++NX+87D9zgD+5l/+ 2xj+8KH90QD+7IX+4Dr+8KD+5E/+5V3+8q3+3ST+++j+5Vj+4kj+7Ib+2xv+ 6G7+4kX+7If+3Sf+3SP92hD92AYAAACWRROBAAAAAWJLR0R7T9K1/AAAAAd0 SU1FB+gLFRAXGVsaKtUAAAGXSURBVDgR3cGHWhNBFAbQ/97ZZTI7CzsEwYag +Lu62JAIlhg72KJo7GJv2Hvl6U2WfBJ9BM7BWiIiKIkAsgI9tANtWjIlxSqN 4j4ooIhjq1HFtVWsokvUJj6FqqI/9QNRFnzHoFVBSW11aN1wFcDI+g0bN6Wb R7eMjY1v3TZhFR1iXNhO7kjy2O8kdxWTLO3O+lTQJsaFPeTe4HK/j9xfTPHA dO3gUNQPRYcYF2Y4eyjNk8M8wqNFnccax09kI1CUxLgww5M8lfjTPMOzRZ1z 876R5ooVYlw4x/O8EFJevMRmcZlXFq5eG037VNAhxoUWr99go8abt9gsbvPO 7Czv+lgFHWJcaHH6Hhfv88FDNos6h+d9SKGKkhgXHvFxg0/49Nkkm0Wdz/2L 3Cq6xLjwkrWlV+TrpTd8W0zxnXcGii4xLrznYvjAj2lY4KeixXHvjOIvzZPP X75OJN++Z9W5Hz/T2tivAatYJWqzMGh/+yy3WViOEr9sVdBLo4pVxJFqVLGa x1bxL22D9hD8RwSACCACQLDW/AG/qjQelpx3LQAAACV0RVh0ZGF0ZTpjcmVh dGUAMjAyNC0xMS0yMVQxNjoyMzoxMCswMDowMNr3c00AAAAldEVYdGRhdGU6 bW9kaWZ5ADIwMjQtMTEtMjFUMTY6MjM6MTArMDA6MDCrqsvxAAAAIHRFWHRz b2Z0d2FyZQBodHRwczovL2ltYWdlbWFnaWNrLm9yZ7zPHZ0AAAAYdEVYdFRo dW1iOjpEb2N1bWVudDo6UGFnZXMAMaf/uy8AAAAYdEVYdFRodW1iOjpJbWFn ZTo6SGVpZ2h0ADYwMHrevbUAAAAXdEVYdFRodW1iOjpJbWFnZTo6V2lkdGgA NjAw6S/t6AAAABl0RVh0VGh1bWI6Ok1pbWV0eXBlAGltYWdlL3BuZz+yVk4A AAAXdEVYdFRodW1iOjpNVGltZQAxNzMyMjA2MTkwtMdSQwAAABN0RVh0VGh1 bWI6OlNpemUAMTE5NzBCQk6C7YYAAAA8dEVYdFRodW1iOjpVUkkAZmlsZTov L3RtcC9sZXR0ZXJfYXZhdGFycy8yL01GLzI1NF8yMThfMTYvNjAwLnBuZ+Sl +5cAAAAASUVORK5CYII= " /> </div> </div> <div> <div class="blog-card__authors-text"> <div class="blog-card-author-list" style="width: 100%;"> <a href="/users/853541"><p class="blog-card__owner">Teddi Herring</p></a> <p class='blog-card__remaining-text'>and 7 more</p> </div> </div> <time datetime="2024-11-09" class="blog-card__date">November 09, 2024</time> </div> </div> </div> <div class='blog-card__preview-content-container'> <a href="/doi/full/10.22541/essoar.173117029.91729676/v1"> <div class='blog-card__preview-content'> Electrical resistivity tomography (ERT) is a geophysical technique that is often used to characterize and monitor permafrost. Automated ERT (A-ERT) systems enable the collection of temporally dense datasets without the need for repeated site visits. So far, only a few A-ERT systems have been deployed in permafrost environments. We present the results of an A-ERT system installed on King George Island, Antarctica. The system withstood the harsh Antarctic environment and collected resistivity data four times a day for a full year in 2022-2023. Resistivity data captured seasonal freezing and thawing, as well as short-term meteorological events. Resistivity was used to estimate changes in unfrozen water content, and co-located temperature and soil moisture data were used to assess relationships between resistivity, soil moisture, and temperature. This work showcases the ability of A-ERT systems to monitor permafrost and soil moisture dynamics and contributes a unique dataset to global permafrost monitoring efforts. </div> </a> </div> </div> </div> <div class="blog-card"> <div class="blog-card__container"> <div class='blog-card__top-row'> </div> <div class='blog-card__heading-container '> <a href="/doi/full/10.22541/essoar.173134178.86556680/v1"> <div class="blog-card__title"> Conservative mixing of alkaline groundwater plume with saline waters at Hamelin Pool... </div> </a> </div> <div class="blog-card__author-container"> <div class="blog-card__author-information"> <div class="blog-card__images-container"> <div class="blog-card__first-avatar"> <img alt="Simon V. Hohl" width="24" height="24" class="user-profile-pic" src="data:image/jpg;base64,iVBORw0KGgoAAAANSUhEUgAAACAAAAAgCAMAAABEpIrGAAAABGdBTUEAALGP C/xhBQAAACBjSFJNAAB6JgAAgIQAAPoAAACA6AAAdTAAAOpgAAA6mAAAF3Cc ulE8AAABblBMVEWiiH6ih32hh32jioCki4GjiX+jiYCkioGYe3CVd2yVeG2c gHWafnOXem+ghXufhXubf3WbgHWZfHG5pZ7Ku7XGt7Gqkomeg3i2oprBsKmk ioCiiX+fhXrDsquznpadgnihh36cgHb6+fn////Wy8bx7uyvmJCbf3Sli4Kw m5Lm39yWeW7r5uPHt7Hp4+HGtrCLa17t6OaslYyljILg2NWUd2ufhHqMbF+Z fXKrlIvXzMiKal7u6eeqk4qtlo3h2daUdmvr5uTOwLuVeGycgXbs5uSokIef hHmrk4r6+fjk3dqhhnzs5+Xi2tfDsqzu6ujn4N6afnTc08/g2NSeg3mXem7m 393OwbuKaVzu6eighnuLa1+WeW2wmZHPwr2QcWWki4KPb2Pe1NGIZ1qul4+n j4WdgXe3o5uafXPZz8vTx8OJaFzv6+maf3SwmpLl3ty/rabJurS+rKXNv7qe hHmmjYS6p5+YfHCiiH0AAABoMPLyAAAAAWJLR0R5odzU0AAAAAd0SU1FB+gL FRAXDtjJrxIAAAGCSURBVDgR3cF7VxJBHAbgd9+ZkR3aTYSuYCH+ks3oZrSU We2WZmmS5a2yshuZWlp29eMHZ44e9I8+gM+Dw8bz8B90wDYAbMM+hNLakOzJ gCAyhuhGQ99mjyggCI+C6A1zoIc9NH35wrHjJyxPnjpd7C316zNny6AHZ4Cm ogel7Vw2HJJqdD4YlgtWkXAIU7sol3K4LFeujsi1vnpUleuxIuEQDYrcuBmO yq2x23Inb/y7kqRFEg5Rqt2T+9F4HE5kH8jk+MP4kSSpIuEM0FT0lMh0ofa4 NiNOM1UkdrGnEjyZFXn6LJ6RZG5+rinNVJFwSCz4waLlkjx/8VKWX70eM5Kk RRIOTe6NrLx9957y4eOstMqfVoclSYskHKJBkc9r0bpsfBmR0UgHLZmPFQmH VH5LOr6u2iGpbtaDLflmFYldVPno+/Z2wV8o//hZb5hfv1f+TJRI7KFaDq39 yxLyth9EI14DiS5ERmsFUmkQhFbEPuwCgG04yPPQsYOOHRwq/wCRKTQRa3L2 jQAAACV0RVh0ZGF0ZTpjcmVhdGUAMjAyNC0xMS0yMVQxNjoyMzoxNCswMDow MC64V14AAAAldEVYdGRhdGU6bW9kaWZ5ADIwMjQtMTEtMjFUMTY6MjM6MTQr MDA6MDBf5e/iAAAAIHRFWHRzb2Z0d2FyZQBodHRwczovL2ltYWdlbWFnaWNr Lm9yZ7zPHZ0AAAAYdEVYdFRodW1iOjpEb2N1bWVudDo6UGFnZXMAMaf/uy8A AAAYdEVYdFRodW1iOjpJbWFnZTo6SGVpZ2h0ADYwMHrevbUAAAAXdEVYdFRo dW1iOjpJbWFnZTo6V2lkdGgANjAw6S/t6AAAABl0RVh0VGh1bWI6Ok1pbWV0 eXBlAGltYWdlL3BuZz+yVk4AAAAXdEVYdFRodW1iOjpNVGltZQAxNzMyMjA2 MTk0s6qWWgAAABN0RVh0VGh1bWI6OlNpemUAMTc2NzhCQhSYyPIAAAA9dEVY dFRodW1iOjpVUkkAZmlsZTovL3RtcC9sZXR0ZXJfYXZhdGFycy8yL1NILzE2 Ml8xMzZfMTI2LzYwMC5wbmcAFOOXAAAAAElFTkSuQmCC " /> </div> <div class="blog-card__second-avatar"> <img alt="Yibo Lin" width="24" height="24" class="user-profile-pic" src="data:image/jpg;base64,iVBORw0KGgoAAAANSUhEUgAAACAAAAAgCAMAAABEpIrGAAAABGdBTUEAALGP C/xhBQAAACBjSFJNAAB6JgAAgIQAAPoAAACA6AAAdTAAAOpgAAA6mAAAF3Cc ulE8AAAA+VBMVEW8qqS7qaO8qaO9rKa8q6W9q6W8qaS4pZ+zn5i4pZ63pJ25 p6C5pqC4pp/Gt7LVysbEtK+3pJ7HuLPWy8fBsKu/rqjVysfCsqz///+1opu6 qKHTx8TWy8ivmpLf19TSxsK1oZrYzsvb0s6nkIjUyMT6+fiynpe2o52xnZbU ycWxnJXd1dLPwr60n5nUyMW6p6H18/L5+Pj+/v60oJqynZbZz8vQxL+znpj9 /f22opy6qKK+rKa0oJm+raf8+/u3o527qKLRxcGtl5C2o5z7+/rZz8zFtbDX zcnNv7u7qaK5p6HFtrHa0M3VycbZzsvAsKq8qqO9q6YAAABxOTBdAAAAAWJL R0RSDWAtkAAAAAd0SU1FB+gLFRAXCt+kawsAAAEUSURBVDgR5cGJVoJAGAbQ 72skRiFIzfpttTJq2mgnQYtW25f3f5nKTucw9Ajei7HCHwB/TeAfQlUI0FGA AlEySbi6ChI17XnaBwkLMRWE03Wg3mjOtGbnfBAWVmqBSJvzroi7IItaERZS LS3LSkevytp6U7paETbCp2xEmyL+lhGjFWEj1faOBLsS7nX2xWhFlBBxXQ4O j44dbcRoRZSQ6uRU5CxpJUZMokjCRvi+nPfSTBsJ+wPHAWEhYk8uLvNMG7m6 dm96KYgiIo7ltpZnuit3g+C+4aQgCog4FanmWTKUkYe2QxQQj/kwfGLFfX4x Yfj69u6DKCKo+wThRjpJksgDP2Ah1CcIQo2AKOM3gH8wVr4AcvYZ1dNOyqgA AAAldEVYdGRhdGU6Y3JlYXRlADIwMjQtMTEtMjFUMTY6MjM6MTArMDA6MDDa 93NNAAAAJXRFWHRkYXRlOm1vZGlmeQAyMDI0LTExLTIxVDE2OjIzOjEwKzAw OjAwq6rL8QAAACB0RVh0c29mdHdhcmUAaHR0cHM6Ly9pbWFnZW1hZ2ljay5v cme8zx2dAAAAGHRFWHRUaHVtYjo6RG9jdW1lbnQ6OlBhZ2VzADGn/7svAAAA GHRFWHRUaHVtYjo6SW1hZ2U6OkhlaWdodAA2MDB63r21AAAAF3RFWHRUaHVt Yjo6SW1hZ2U6OldpZHRoADYwMOkv7egAAAAZdEVYdFRodW1iOjpNaW1ldHlw ZQBpbWFnZS9wbmc/slZOAAAAF3RFWHRUaHVtYjo6TVRpbWUAMTczMjIwNjE5 MLTHUkMAAAATdEVYdFRodW1iOjpTaXplADExMTM3QkL03yeVAAAAPXRFWHRU aHVtYjo6VVJJAGZpbGU6Ly90bXAvbGV0dGVyX2F2YXRhcnMvMi9ZTC8xODhf MTcwXzE2NC82MDAucG5nMKsdRgAAAABJRU5ErkJggg== " /> </div> </div> <div> <div class="blog-card__authors-text"> <div class="blog-card-author-list" style="width: 100%;"> <a href="/users/853529"><p class="blog-card__owner">Simon V. Hohl</p></a> <p class='blog-card__remaining-text'>and 4 more</p> </div> </div> <time datetime="2024-11-11" class="blog-card__date">November 11, 2024</time> </div> </div> </div> <div class='blog-card__preview-content-container'> <a href="/doi/full/10.22541/essoar.173134178.86556680/v1"> <div class='blog-card__preview-content'> Hamelin Pool, W.-Australia, is a natural laboratory to study stromatolite formation in a hypersaline lagoon. Stromatolitic aragonites sampled at supratidal, intertidal and subtidal environments show gradual increase in Ba isotopic compositions (d138Bacarb = -0.12-0.57‰) with decreasing Ba/Ca following conservative mixing between groundwater and seawater. We observe fingerprints of the groundwater end-member in a supratidal sample showing particular light d138Bacarb corresponding with elevated Mn/Sr and low d18Ocarb as indicator for discharge from the local Tamala Limestone aquifer. In contrast, stromatolitic carbonates formed in equilibrium with a saline end-member show heavy d138Bacarb. Lagoonal d138Bafluid ranges from 0.44-0.6‰ at increasing PSU (3.6-65.6). The calculated partition coefficient for Ba into stromatolites is lowest at the subtidal (logDBa=0.45) and highest at the groundwater discharge site (logDBa=0.86). Injection of groundwaters into Hamelin Pool likely contributes to enhanced aragonite precipitation at up to 0.32mm/yr, possibly catalysed by nucleation within or onto extra-polymeric substances of microbially diverse mats. </div> </a> </div> </div> </div> <div class="blog-card"> <a href="/doi/full/10.22541/essoar.173120314.43984318/v1"> <div class="blog-card__image-container"> <img onerror="$(this).closest('a').remove()" height="200" class="blog-card__image-tag" loading="lazy" src="https://d197for5662m48.cloudfront.net/images/tagdashboard/banner/large-243fcdb05f224a75295a129767fd9215.jpg" /> </div> </a> <div class="blog-card__container"> <div class='blog-card__top-row'> </div> <div class='blog-card__heading-container '> <a href="/doi/full/10.22541/essoar.173120314.43984318/v1"> <div class="blog-card__title"> Transitions toward a Mid-heavy State of Tropical Convection </div> </a> </div> <div class="blog-card__author-container"> <div class="blog-card__author-information"> <div class="blog-card__images-container"> <div class="blog-card__first-avatar"> <img alt="Hirohiko Masunaga" width="24" height="24" class="user-profile-pic" src="data:image/jpg;base64,iVBORw0KGgoAAAANSUhEUgAAACAAAAAgCAMAAABEpIrGAAAABGdBTUEAALGP C/xhBQAAACBjSFJNAAB6JgAAgIQAAPoAAACA6AAAdTAAAOpgAAA6mAAAF3Cc ulE8AAABj1BMVEVF0OJE0OJEz+FI0OJJ0eJH0OJG0OJEz+I1zN8xy99Dz+FA zuEvyt44zN8xyt4wyt4/zuE9zeBy2+l+3upBz+FK0eKH4Oxo2ec3zN9N0uN/ 3us+zuE4zOBk1+aD3+tv2ug9zuAuyt7x+/z///82zN9i1+bQ8/ccxdtq2eex 6/IoyN07zeD+/v7r+vstyt7l+Ptf1ubG8PYbxdtl2Of3/f1Cz+F63erh9/ro +fs6zeAyy99b1eXH8fbe9vl53epM0uPM8vfn+fszy98qyd1X1ORj1+at6vL4 /f3R8/eq6fH0/P3s+vwtyd7j9/rJ8fac5e+c5u8jx9yR4+1V1OTr+fvk+Pq6 7fS97vTB7/XF8PbI8fan6PGN4u0Sw9r7/v4hxtwryd4WxNrL8vYUw9r9/v6L 4e0kx9xO0uPd9vkRw9qX5O7S8/g+zuBd1uXF8PXT9PhM0ePw+/xm2Off9/op yd1u2ugsyd6E3+uU5O6f5vB33Ok0y99P0uOe5u983eqZ5e8xy941y98ryd1I 0eIAAAD0wzfoAAAAAWJLR0SEYtBacQAAAAd0SU1FB+gLFRAXGCwdGkMAAAHB SURBVDgR3cEHW9NgFIDR97tNb7ABCUIUN/G2oFQDBqsUQSyIs46qoOBe4FYc 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LzIvSFQvNjlfMjA4XzIyNi82MDAucG5nStKkZwAAAABJRU5ErkJggg== " /> </div> </div> <div> <div class="blog-card__authors-text"> <div class="blog-card-author-list" style="width: 100%;"> <a href="/users/552254"><p class="blog-card__owner">Hirohiko Masunaga</p></a> <p class='blog-card__remaining-text'>and 1 more</p> </div> </div> <time datetime="2024-11-10" class="blog-card__date">November 10, 2024</time> </div> </div> </div> <div class='blog-card__preview-content-container'> <a href="/doi/full/10.22541/essoar.173120314.43984318/v1"> <div class='blog-card__preview-content'> A document by Hirohiko Masunaga. Click on the document to view its contents. </div> </a> </div> </div> </div> <div class="blog-card"> <div class="blog-card__container"> <div class='blog-card__top-row'> </div> <div class='blog-card__heading-container '> <a href="/doi/full/10.22541/essoar.173120498.80588022/v1"> <div class="blog-card__title"> Estimates of the Global Clear-Sky Radiative Feedback Strength from Reanalysis Data </div> </a> </div> <div class="blog-card__author-container"> <div class="blog-card__author-information"> <div class="blog-card__images-container"> <div class="blog-card__first-avatar"> <img alt="Helene Marie Gloeckner" width="24" height="24" class="user-profile-pic" src="data:image/jpg;base64,iVBORw0KGgoAAAANSUhEUgAAACAAAAAgCAMAAABEpIrGAAAABGdBTUEAALGP C/xhBQAAACBjSFJNAAB6JgAAgIQAAPoAAACA6AAAdTAAAOpgAAA6mAAAF3Cc ulE8AAABYlBMVEVF0OJE0OJEz+FG0OJJ0eJH0OJI0OJK0eJEz+I+zuAuyt46 zeA1zN8xy95Cz+E7zeAtyt4ryd0vyt4/zuFT0+SJ4exh1+Y8zeA9zuBx2+iA 3utM0eOI4eyV5O6A3+tAzuEyy9+G4Oz///+47fQpyd3v+/wsyd6R4+1l2Od+ 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bWFnaWNrLm9yZ7zPHZ0AAAAYdEVYdFRodW1iOjpEb2N1bWVudDo6UGFnZXMA Maf/uy8AAAAYdEVYdFRodW1iOjpJbWFnZTo6SGVpZ2h0ADYwMHrevbUAAAAX dEVYdFRodW1iOjpJbWFnZTo6V2lkdGgANjAw6S/t6AAAABl0RVh0VGh1bWI6 Ok1pbWV0eXBlAGltYWdlL3BuZz+yVk4AAAAXdEVYdFRodW1iOjpNVGltZQAx NzMyMjA2MzA5H12FwAAAABN0RVh0VGh1bWI6OlNpemUAMTE0OTdCQlOCSIEA AAA8dEVYdFRodW1iOjpVUkkAZmlsZTovL3RtcC9sZXR0ZXJfYXZhdGFycy8y L0xLLzIxMl8yMjdfNzQvNjAwLnBuZwEBm/EAAAAASUVORK5CYII= " /> </div> </div> <div> <div class="blog-card__authors-text"> <div class="blog-card-author-list" style="width: 100%;"> <a href="/users/853528"><p class="blog-card__owner">Helene Marie Gloeckner</p></a> <p class='blog-card__remaining-text'>and 3 more</p> </div> </div> <time datetime="2024-11-10" class="blog-card__date">November 10, 2024</time> </div> </div> </div> <div class='blog-card__preview-content-container'> <a href="/doi/full/10.22541/essoar.173120498.80588022/v1"> <div class='blog-card__preview-content'> We use atmospheric profiles from ERA5, JRA55 and MERRA2 between 1993 and 2023 to estimate Earth’s global clear-sky longwave feedback strength on the seasonal and interannual timescale. Differences in the relationship of relative humidity with skin temperature prior to 2008 lead to interannual feedback strengths between 1.34 W m−2 K−1 (JRA55) and 1.89 W m−2 K−1 (MERRA2). Restricting the analysis to the last 16 years yields more consistent interannual estimates of 2.05 W m−2 K−1 on average, which is larger than the overall seasonal estimate of 1.91 W m−2 K−1. The mid-tropospheric drying causing this difference suggest a substantial influence of ENSO variability on the interannual timescale. This indicates a long-term feedback strength smaller than 2.0 W m−2 K−1, which is already at the lower end of previous estimates; emphasizing the importance of accurate long-term RH measurements to reliably project Earth’s clear-sky feedback strength </div> </a> </div> </div> </div> <div class="blog-card"> <div class="blog-card__container"> <div class='blog-card__top-row'> </div> <div class='blog-card__heading-container '> <a href="/doi/full/10.22541/essoar.173152967.70904987/v1"> <div class="blog-card__title"> Characteristics of Ice Nucleating Particles from the Long-Range Transport of Saharan... </div> </a> </div> <div class="blog-card__author-container"> <div class="blog-card__author-information"> <div class="blog-card__images-container"> <div class="blog-card__first-avatar"> <img alt="Ryan J. Patnaude" width="24" height="24" class="user-profile-pic" src="data:image/jpg;base64,iVBORw0KGgoAAAANSUhEUgAAACAAAAAgCAMAAABEpIrGAAAABGdBTUEAALGP C/xhBQAAACBjSFJNAAB6JgAAgIQAAPoAAACA6AAAdTAAAOpgAAA6mAAAF3Cc ulE8AAABVlBMVEWPpK+OpK+Oo66QpK+SprGRprGRpbCQpbCQpa+Jn6p/l6OA mKSAl6SBmKWFnKiNoq2GnKiIn6qfsbrBzdO4xcy6x862xMuhs7yEm6ektb6j tL2is7yWqbR+lqOMoq29ydD////W3uKFm6eNo663xMvAzNKUqLKbrbf+/v6J n6vy9PWVqbOfsbudsLni5+rH0dezwsl4kp90jpvZ4OScr7iCmaXv8vOKoKuI nqr5+vqGnai3xcyzwcl5kp+LoKxzjZvd5OeXq7WDmqbv8vR6k6CCmqbCztSh srvK1Nl/l6SLoazx9PWcrrjO19zX3uKRprDf5eju8fOKoKzEz9WMoazL1Nl4 kZ73+fmxv8e7x86gsruPpK6ywch2kJ19lqLs7/Ht8fJxjJqmt8Dk6eyDm6eS p7GTp7Lo7O+tvMSBmaX29/iesLnJ09iarberusO1wsp+lqIAAAAeMloUAAAA AWJLR0Rxrwdc4gAAAAd0SU1FB+gLFRAXD6/On4QAAAFeSURBVDgR5cFpOxtR GAbg5zwzZ5LTIzPoTItI+iKJrbSqtURFLUFr7WarrXuV4v9/QjJquy4/gPvG HaMUbsFzYAxX0XG1qz2QSHinkiQuIWEe2JqUH3hkrX+qzgNxgY6pfxhGjx6b BgSNTel0ujmTBRViito+kYrGVEIqWlrbQMQUtc1JvtCekw6/U7q6n/b0yrOM JlGlqG0oz/uCF/3y8pUM9A3aIRkuEkSVorYj8nq0NPZGxidkcqrUUJYOE4Co UtQ2lOnCzKwMvH0nc5jvXpDFzBKJKkVtIzmznC1SKt4HH0DEFLUN5eOnSD6v oCSra+vRRrkuyS+IKWo7Iptb2zvSXs7K7teU9ZEk/lPUNiehX/wm31eyMvnj p5sAcUFR23WJ7K/t3/JnT/6mQFLhEjpm/2DfLA39OziszR8ZgLiChMkY0Ok8 LsJOgMR1dFyHYNJNUHvETTwDxnD/nACJBypbsGz6rgAAACV0RVh0ZGF0ZTpj cmVhdGUAMjAyNC0xMS0yMVQxNjoyMzoxNSswMDowMIjPXOoAAAAldEVYdGRh dGU6bW9kaWZ5ADIwMjQtMTEtMjFUMTY6MjM6MTUrMDA6MDD5kuRWAAAAIHRF WHRzb2Z0d2FyZQBodHRwczovL2ltYWdlbWFnaWNrLm9yZ7zPHZ0AAAAYdEVY dFRodW1iOjpEb2N1bWVudDo6UGFnZXMAMaf/uy8AAAAYdEVYdFRodW1iOjpJ bWFnZTo6SGVpZ2h0ADYwMHrevbUAAAAXdEVYdFRodW1iOjpJbWFnZTo6V2lk dGgANjAw6S/t6AAAABl0RVh0VGh1bWI6Ok1pbWV0eXBlAGltYWdlL3BuZz+y Vk4AAAAXdEVYdFRodW1iOjpNVGltZQAxNzMyMjA2MTk1xK2mzAAAABN0RVh0 VGh1bWI6OlNpemUAMTUzNDdCQohZDloAAAA9dEVYdFRodW1iOjpVUkkAZmls ZTovL3RtcC9sZXR0ZXJfYXZhdGFycy8yL1JQLzE0M18xNjRfMTc1LzYwMC5w bmfAAxCqAAAAAElFTkSuQmCC " /> </div> <div class="blog-card__second-avatar"> <img alt="Christina S. McCluskey" width="24" height="24" class="user-profile-pic" src="data:image/jpg;base64,iVBORw0KGgoAAAANSUhEUgAAACAAAAAgCAMAAABEpIrGAAAABGdBTUEAALGP C/xhBQAAACBjSFJNAAB6JgAAgIQAAPoAAACA6AAAdTAAAOpgAAA6mAAAF3Cc ulE8AAABtlBMVEW7Zcq7ZMq6ZMm8aMu8acu7Zsq7Z8q8Z8q6Y8mzVMSxT8Ky UcO3XMa2W8azU8O1V8W6YsmzU8S4X8i7ZMm2WsbNjtjYp+DUnt2/b82xUMK3 XcfGftLRmdvKiNa5YsnPktnQltq6ZMr8+Pz////ZquG0VsToy+2/bs3SmdzP k9q0V8X79vy5YcjAcc7y4/XKh9WqPrzmx+vds+SxTsLv3PPPlNrftuapPryu SMDEetHw3fOnObrnyu369PvAcM347/mwTsLlxevHgdO1WMW9asvIgtTIg9Su ScDmyOzcseSyUMPcsOTZqeHMjdewTcHDeNC4YMjBcs7pze6vS8G0VcTr0e/J hNTMi9ewTcLDedDkwurDd9DJhtXlxuvGf9O1WcXFfNKvSsC9a8zBdM/Gf9Lf t+atRr/eteWyUsPSmtzarOKqP72oOrvmx+zDedGvScDy4fT+/v7q0e+lNLnw 3/OpPbzmxuvFfdKrQb3br+OqQL3Lite8Z8vguebnyuz69fvnyezOkNm3XMfY puDWo9/Bc8/Lida+bMy5YMi1WcbUnd3Li9fdsuTBc864Xse4X8e9acsAAAAC ipKWAAAAAWJLR0SRDw2+mgAAAAd0SU1FB+gLFRAXIAQfot0AAAG8SURBVDgR 3cGHQtNgGAXQ+90/aZpgxUKrUASBK4pacOCelIoCKg6qFVBxi3uLA/fC7SOb WhSegXOwsJgZKgxVZpiPVWAFYowZ5hDO83yCCReAAOGcT/zHRDKMahY5IrW4 FiSxJEzXgfWoYpCpzS5d1tDo55qWN+dQj5bkitaGOp+oaGMi49oVW9nRuEpa nfJdTae0JnQ0xIjk2nVqzXd1a/2GjdKmHs+PNkvZ0NEAGF16i7Zu4/Yd2rlr t9r3pP3UXu1TNnQ0AEavt6C+4n6w/8DBAQ2qPzN0SId1JHQ0AEY3XNDRYoBk 5thwQcd1YqSkk6dUDh0NgNGdLmi0GJC5luGC8mMaGteZssqhowEwer1ndW7C Q3L0/IWCLl7S5Su6ek3l0NEAGN3kdd246UbG1X3rtu7c1b37Dx4OqBw6GmJE PiU1l/BI2cdPNPX0mdT3fEwvSo6GGDndMaWKl6XolZqiLr0u9r7R29DR8BeD 0rvO9x8+Rn7q0+DnmS9fv2Vyzd9//PSJWZzOT0aNqWn6E9EMkC76mOj55bMN /xDO8xIEAw+kC8jgt0/MYRUYA2cZ5jMzVBgAQ8ywgPwBgVdDItj/QwsAAAAl dEVYdGRhdGU6Y3JlYXRlADIwMjQtMTEtMjFUMTY6MjM6MTQrMDA6MDAuuFde AAAAJXRFWHRkYXRlOm1vZGlmeQAyMDI0LTExLTIxVDE2OjIzOjE0KzAwOjAw X+Xv4gAAACB0RVh0c29mdHdhcmUAaHR0cHM6Ly9pbWFnZW1hZ2ljay5vcme8 zx2dAAAAGHRFWHRUaHVtYjo6RG9jdW1lbnQ6OlBhZ2VzADGn/7svAAAAGHRF WHRUaHVtYjo6SW1hZ2U6OkhlaWdodAA2MDB63r21AAAAF3RFWHRUaHVtYjo6 SW1hZ2U6OldpZHRoADYwMOkv7egAAAAZdEVYdFRodW1iOjpNaW1ldHlwZQBp bWFnZS9wbmc/slZOAAAAF3RFWHRUaHVtYjo6TVRpbWUAMTczMjIwNjE5NLOq lloAAAATdEVYdFRodW1iOjpTaXplADIyOTA0QkJjIBXQAAAAPXRFWHRUaHVt Yjo6VVJJAGZpbGU6Ly90bXAvbGV0dGVyX2F2YXRhcnMvMi9DTS8xODdfMTAx XzIwMi82MDAucG5nCKoURQAAAABJRU5ErkJggg== " /> </div> </div> <div> <div class="blog-card__authors-text"> <div class="blog-card-author-list" style="width: 100%;"> <a href="/users/853523"><p class="blog-card__owner">Ryan J. Patnaude</p></a> <p class='blog-card__remaining-text'>and 9 more</p> </div> </div> <time datetime="2024-11-13" class="blog-card__date">November 13, 2024</time> </div> </div> </div> <div class='blog-card__preview-content-container'> <a href="/doi/full/10.22541/essoar.173152967.70904987/v1"> <div class='blog-card__preview-content'> Transported mineral dust in a Saharan air layer (SAL) contains highly active ice-nucleating particles (INPs) that may be transported across the Atlantic Ocean and subsequently seed clouds in the Caribbean and the Americas. During an aircraft campaign around Houston and the western U.S. Gulf Coast, a widespread SAL advected into the sampling region allowing for measurement of the ice-nucleating ability of SD following long-range transport. Results showed that the mean INP concentrations were 3–4.5 times higher than non-Saharan dust (nSD), but only at temperatures < –21 ºC. Active surface site densities were also enhanced in the SD, exceeding the mean for nSD by over an order of magnitude at temperatures < –21 ºC. These INP measurements confirmed that SD remains a highly active INP even after > 8000 km westward transport across the Atlantic Ocean. </div> </a> </div> </div> </div> <div class="blog-card"> <a href="/doi/full/10.22541/essoar.173117020.08316083/v1"> <div class="blog-card__image-container"> <img onerror="$(this).closest('a').remove()" height="200" class="blog-card__image-tag" loading="lazy" src="https://d197for5662m48.cloudfront.net/images/tagdashboard/banner/large-8c382f767973d7400c0a03d93e18ff47.jpeg" /> </div> </a> <div class="blog-card__container"> <div class='blog-card__top-row'> </div> <div class='blog-card__heading-container '> <a href="/doi/full/10.22541/essoar.173117020.08316083/v1"> <div class="blog-card__title"> Supporting Information for CO2 uptake in the Pacific from 1985 to 2018: a comparative... </div> </a> </div> <div class="blog-card__author-container"> <div class="blog-card__author-information"> <div class="blog-card__images-container"> <div class="blog-card__first-avatar"> <img alt="Masao Ishii" width="24" height="24" class="user-profile-pic" src="data:image/jpg;base64,iVBORw0KGgoAAAANSUhEUgAAACAAAAAgCAMAAABEpIrGAAAABGdBTUEAALGP C/xhBQAAACBjSFJNAAB6JgAAgIQAAPoAAACA6AAAdTAAAOpgAAA6mAAAF3Cc ulE8AAABLFBMVEX+2hD+2g/+2Q/+2hP+2hX+2hT+2hL+2hb+2hH91wH91QD9 1gD92Q392AX92Ab92AT+4Dj+5mD+4kb91wL92Qz92Qr+5FP+5l7+3in91wD+ 3Sj+52r+3Sb92Q/91AD+8q/////+5mP+6nj90AD+6XP+6G7+8KT+7Y3+2xb+ 9sf+6W/+6Gr+52b+8an+/fP+/PH+3CH++t7+6XH+6Gz+52f+64D+4UP+64H+ 6nn+8ab+3Sf+87P90wD+9cD+8aT92Qn+7pb+3ir+4kn+2xr+4Dr+7In+7Yr+ 8aX+3zD90gD+/ff++d3+87T9zgD+8af+8KH+3zX90QD+7IP+4UL+8J/+52X+ 8q3+4Df+8qr+6XL+6G3+4kj+7Ib+2xv+403+3zL+7Yv92AP+2xcAAADuQXnr AAAAAWJLR0RjXL4tqgAAAAd0SU1FB+gLFRAXIXMYkksAAAFySURBVDgR3cGJ VtNQFAXQc29K7uNFqIIDUe7zaESrFVET64QURRRnccYJ6/9/hJW1wvQJ7I2j RUSwQwSA4DD9D2M6JqoqOEizzgQUUHQ6ueaWK/YTDZOxgIriWBGnsqk4HVSw R0P3+ImZWShOnjp9Zq48e25+Oih2iVs6T86XeSdeIC9Wl7gQzQUtcUuXySup l6Wr5LWqz+vRXNASt7TIG0tFmL3JW7xd1WyiuaAlbmmRdzgo413e40JVs4nm gpa4pft8wIfLBR8NWFc1m2guaIlbWuFwlfExB09YVzWbaC5oiVta4docn65z +RnrqmYTzQUtcUvPufHi5Su+fvOWdVWzieaClrild3y/+YH8uPmJ/arPz9Fc 0BK39IVf4xqXivSNW9UWv0dzwS7NJ3/8/DUsm99ld2Z9u9j+szHKFXtEQ5mG IcQihDKNslHqBhXsp1kvqHYmVLNe7vnfXHGQjkF3uKq6Cg4RASACiAAQHC3/ AIjqKjN4HK1DAAAAJXRFWHRkYXRlOmNyZWF0ZQAyMDI0LTExLTIxVDE2OjIz OjMzKzAwOjAwqTpurQAAACV0RVh0ZGF0ZTptb2RpZnkAMjAyNC0xMS0yMVQx NjoyMzozMyswMDowMNhn1hEAAAAgdEVYdHNvZnR3YXJlAGh0dHBzOi8vaW1h Z2VtYWdpY2sub3JnvM8dnQAAABh0RVh0VGh1bWI6OkRvY3VtZW50OjpQYWdl cwAxp/+7LwAAABh0RVh0VGh1bWI6OkltYWdlOjpIZWlnaHQANjAwet69tQAA ABd0RVh0VGh1bWI6OkltYWdlOjpXaWR0aAA2MDDpL+3oAAAAGXRFWHRUaHVt Yjo6TWltZXR5cGUAaW1hZ2UvcG5nP7JWTgAAABd0RVh0VGh1bWI6Ok1UaW1l ADE3MzIyMDYyMTPnUTeoAAAAE3RFWHRUaHVtYjo6U2l6ZQAxMTczNUJCeBsG WwAAADx0RVh0VGh1bWI6OlVSSQBmaWxlOi8vdG1wL2xldHRlcl9hdmF0YXJz LzIvTUkvMjU0XzIxOF8xNi82MDAucG5nmDqLtgAAAABJRU5ErkJggg== " /> </div> <div class="blog-card__second-avatar"> </div> </div> <div> <div class="blog-card__authors-text"> <div class="blog-card-author-list" style="width: 100%;"> <a href="/users/578667"><p class="blog-card__owner">Masao Ishii</p></a> <p class='blog-card__remaining-text'>and 12 more</p> </div> </div> <time datetime="2024-11-09" class="blog-card__date">November 09, 2024</time> </div> </div> </div> <div class='blog-card__preview-content-container'> <a href="/doi/full/10.22541/essoar.173117020.08316083/v1"> <div class='blog-card__preview-content'> A document by Masao Ishii. Click on the document to view its contents. </div> </a> </div> </div> </div> <div class="blog-card"> <div class="blog-card__container"> <div class='blog-card__top-row'> </div> <div class='blog-card__heading-container '> <a href="/doi/full/10.22541/essoar.173117017.78015455/v1"> <div class="blog-card__title"> CO 2 uptake in the Pacific from 1985 to 2018: a comparative assessment of observation... </div> </a> </div> <div class="blog-card__author-container"> <div class="blog-card__author-information"> <div class="blog-card__images-container"> <div class="blog-card__first-avatar"> <img alt="Masao Ishii" width="24" height="24" class="user-profile-pic" src="data:image/jpg;base64,iVBORw0KGgoAAAANSUhEUgAAACAAAAAgCAMAAABEpIrGAAAABGdBTUEAALGP C/xhBQAAACBjSFJNAAB6JgAAgIQAAPoAAACA6AAAdTAAAOpgAAA6mAAAF3Cc ulE8AAABLFBMVEX+2hD+2g/+2Q/+2hP+2hX+2hT+2hL+2hb+2hH91wH91QD9 1gD92Q392AX92Ab92AT+4Dj+5mD+4kb91wL92Qz92Qr+5FP+5l7+3in91wD+ 3Sj+52r+3Sb92Q/91AD+8q/////+5mP+6nj90AD+6XP+6G7+8KT+7Y3+2xb+ 9sf+6W/+6Gr+52b+8an+/fP+/PH+3CH++t7+6XH+6Gz+52f+64D+4UP+64H+ 6nn+8ab+3Sf+87P90wD+9cD+8aT92Qn+7pb+3ir+4kn+2xr+4Dr+7In+7Yr+ 8aX+3zD90gD+/ff++d3+87T9zgD+8af+8KH+3zX90QD+7IP+4UL+8J/+52X+ 8q3+4Df+8qr+6XL+6G3+4kj+7Ib+2xv+403+3zL+7Yv92AP+2xcAAADuQXnr AAAAAWJLR0RjXL4tqgAAAAd0SU1FB+gLFRAXIXMYkksAAAFySURBVDgR3cGJ VtNQFAXQc29K7uNFqIIDUe7zaESrFVET64QURRRnccYJ6/9/hJW1wvQJ7I2j RUSwQwSA4DD9D2M6JqoqOEizzgQUUHQ6ueaWK/YTDZOxgIriWBGnsqk4HVSw R0P3+ImZWShOnjp9Zq48e25+Oih2iVs6T86XeSdeIC9Wl7gQzQUtcUuXySup l6Wr5LWqz+vRXNASt7TIG0tFmL3JW7xd1WyiuaAlbmmRdzgo413e40JVs4nm gpa4pft8wIfLBR8NWFc1m2guaIlbWuFwlfExB09YVzWbaC5oiVta4docn65z +RnrqmYTzQUtcUvPufHi5Su+fvOWdVWzieaClrild3y/+YH8uPmJ/arPz9Fc 0BK39IVf4xqXivSNW9UWv0dzwS7NJ3/8/DUsm99ld2Z9u9j+szHKFXtEQ5mG IcQihDKNslHqBhXsp1kvqHYmVLNe7vnfXHGQjkF3uKq6Cg4RASACiAAQHC3/ AIjqKjN4HK1DAAAAJXRFWHRkYXRlOmNyZWF0ZQAyMDI0LTExLTIxVDE2OjIz OjMzKzAwOjAwqTpurQAAACV0RVh0ZGF0ZTptb2RpZnkAMjAyNC0xMS0yMVQx NjoyMzozMyswMDowMNhn1hEAAAAgdEVYdHNvZnR3YXJlAGh0dHBzOi8vaW1h Z2VtYWdpY2sub3JnvM8dnQAAABh0RVh0VGh1bWI6OkRvY3VtZW50OjpQYWdl cwAxp/+7LwAAABh0RVh0VGh1bWI6OkltYWdlOjpIZWlnaHQANjAwet69tQAA ABd0RVh0VGh1bWI6OkltYWdlOjpXaWR0aAA2MDDpL+3oAAAAGXRFWHRUaHVt Yjo6TWltZXR5cGUAaW1hZ2UvcG5nP7JWTgAAABd0RVh0VGh1bWI6Ok1UaW1l ADE3MzIyMDYyMTPnUTeoAAAAE3RFWHRUaHVtYjo6U2l6ZQAxMTczNUJCeBsG WwAAADx0RVh0VGh1bWI6OlVSSQBmaWxlOi8vdG1wL2xldHRlcl9hdmF0YXJz LzIvTUkvMjU0XzIxOF8xNi82MDAucG5nmDqLtgAAAABJRU5ErkJggg== " /> </div> <div class="blog-card__second-avatar"> </div> </div> <div> <div class="blog-card__authors-text"> <div class="blog-card-author-list" style="width: 100%;"> <a href="/users/578667"><p class="blog-card__owner">Masao Ishii</p></a> <p class='blog-card__remaining-text'>and 12 more</p> </div> </div> <time datetime="2024-11-09" class="blog-card__date">November 09, 2024</time> </div> </div> </div> <div class='blog-card__preview-content-container'> <a href="/doi/full/10.22541/essoar.173117017.78015455/v1"> <div class='blog-card__preview-content'> Net and anthropogenic CO 2 exchange in the Pacific represents a major contribution to the global CO 2 sink. The Pacific is thought to have turned to a net sink of CO 2 that is growing primarily due to the increasing uptake of anthropogenic CO 2. The equatorial region is key in determining net and anthropogenic CO 2 uptakes and their trends and variability in the Pacific. </div> </a> </div> </div> </div> <div class="blog-card"> <div class="blog-card__container"> <div class='blog-card__top-row'> </div> <div class='blog-card__heading-container '> <a href="/doi/full/10.22541/essoar.173134230.03179851/v1"> <div class="blog-card__title"> COMMERCIAL SYNTHETIC APERTURE RADAR DATA FOR SURFACE DEFORMATION AND CHANGE </div> </a> </div> <div class="blog-card__author-container"> <div class="blog-card__author-information"> <div class="blog-card__images-container"> <div class="blog-card__first-avatar"> <img alt="Stacey Huang" width="24" height="24" class="user-profile-pic" src="data:image/jpg;base64,iVBORw0KGgoAAAANSUhEUgAAACAAAAAgCAMAAABEpIrGAAAABGdBTUEAALGP C/xhBQAAACBjSFJNAAB6JgAAgIQAAPoAAACA6AAAdTAAAOpgAAA6mAAAF3Cc ulE8AAABblBMVEWiiH6ih32hh32jioCki4GjiX+jiYCkioGYe3CVd2yVeG2c gHWafnOXem+ghXufhXubf3WbgHWZfHG5pZ7Ku7XGt7Gqkomeg3i2oprBsKmk ioCiiX+fhXrDsquznpadgnihh36cgHb6+fn////Wy8bx7uyvmJCbf3Sli4Kw m5Lm39yWeW7r5uPHt7Hp4+HGtrCLa17t6OaslYyljILg2NWUd2ufhHqMbF+Z fXKrlIvXzMiKal7u6eeqk4qtlo3h2daUdmvr5uTOwLuVeGycgXbs5uSokIef hHmrk4r6+fjk3dqhhnzs5+Xi2tfDsqzu6ujn4N6afnTc08/g2NSeg3mXem7m 393OwbuKaVzu6eighnuLa1+WeW2wmZHPwr2QcWWki4KPb2Pe1NGIZ1qul4+n j4WdgXe3o5uafXPZz8vTx8OJaFzv6+maf3SwmpLl3ty/rabJurS+rKXNv7qe hHmmjYS6p5+YfHCiiH0AAABoMPLyAAAAAWJLR0R5odzU0AAAAAd0SU1FB+gL FRAXDtjJrxIAAAGCSURBVDgR3cF7VxJBHAbgd9+ZkR3aTYSuYCH+ks3oZrSU We2WZmmS5a2yshuZWlp29eMHZ44e9I8+gM+Dw8bz8B90wDYAbMM+hNLakOzJ gCAyhuhGQ99mjyggCI+C6A1zoIc9NH35wrHjJyxPnjpd7C316zNny6AHZ4Cm ogel7Vw2HJJqdD4YlgtWkXAIU7sol3K4LFeujsi1vnpUleuxIuEQDYrcuBmO yq2x23Inb/y7kqRFEg5Rqt2T+9F4HE5kH8jk+MP4kSSpIuEM0FT0lMh0ofa4 NiNOM1UkdrGnEjyZFXn6LJ6RZG5+rinNVJFwSCz4waLlkjx/8VKWX70eM5Kk RRIOTe6NrLx9957y4eOstMqfVoclSYskHKJBkc9r0bpsfBmR0UgHLZmPFQmH VH5LOr6u2iGpbtaDLflmFYldVPno+/Z2wV8o//hZb5hfv1f+TJRI7KFaDq39 yxLyth9EI14DiS5ERmsFUmkQhFbEPuwCgG04yPPQsYOOHRwq/wCRKTQRa3L2 jQAAACV0RVh0ZGF0ZTpjcmVhdGUAMjAyNC0xMS0yMVQxNjoyMzoxNCswMDow MC64V14AAAAldEVYdGRhdGU6bW9kaWZ5ADIwMjQtMTEtMjFUMTY6MjM6MTQr MDA6MDBf5e/iAAAAIHRFWHRzb2Z0d2FyZQBodHRwczovL2ltYWdlbWFnaWNr Lm9yZ7zPHZ0AAAAYdEVYdFRodW1iOjpEb2N1bWVudDo6UGFnZXMAMaf/uy8A AAAYdEVYdFRodW1iOjpJbWFnZTo6SGVpZ2h0ADYwMHrevbUAAAAXdEVYdFRo dW1iOjpJbWFnZTo6V2lkdGgANjAw6S/t6AAAABl0RVh0VGh1bWI6Ok1pbWV0 eXBlAGltYWdlL3BuZz+yVk4AAAAXdEVYdFRodW1iOjpNVGltZQAxNzMyMjA2 MTk0s6qWWgAAABN0RVh0VGh1bWI6OlNpemUAMTc2NzhCQhSYyPIAAAA9dEVY dFRodW1iOjpVUkkAZmlsZTovL3RtcC9sZXR0ZXJfYXZhdGFycy8yL1NILzE2 Ml8xMzZfMTI2LzYwMC5wbmcAFOOXAAAAAElFTkSuQmCC " /> </div> <div class="blog-card__second-avatar"> </div> </div> <div> <div class="blog-card__authors-text"> <div class="blog-card-author-list" style="width: 100%;"> <a href="/users/853363"><p class="blog-card__owner">Stacey Huang</p></a> <p class='blog-card__remaining-text'>and 4 more</p> </div> </div> <time datetime="2024-11-11" class="blog-card__date">November 11, 2024</time> </div> </div> </div> <div class='blog-card__preview-content-container'> <a href="/doi/full/10.22541/essoar.173134230.03179851/v1"> <div class='blog-card__preview-content'> The commercial synthetic aperture radar (SAR) market is experiencing year-over-year growth and is currently capable of imaging anywhere in the world within an hour at X-band. Surface Deformation and Change (SDC) is a mission study at NASA to investigate innovative architectures beyond the NASA-ISRO SAR (NISAR) mission in the next decade. In this article we present preliminary findings on the technical capabilities of the currently available commercial SAR data, and investigate their applicability to SDC goals, such as imaging quality and retrieval of surface motion. </div> </a> </div> </div> </div> </div> <div role="navigation" aria-label="Pagination" class="pagination"><a class="previous_page" rel="prev" href="/inst/20904?page=6">← Previous</a> <a aria-label="Page 1" href="/inst/20904?page=1">1</a> <a aria-label="Page 2" href="/inst/20904?page=2">2</a> <a aria-label="Page 3" href="/inst/20904?page=3">3</a> <a aria-label="Page 4" href="/inst/20904?page=4">4</a> <a aria-label="Page 5" href="/inst/20904?page=5">5</a> <a rel="prev" aria-label="Page 6" href="/inst/20904?page=6">6</a> <em class="current" aria-label="Page 7" aria-current="page">7</em> <a rel="next" aria-label="Page 8" href="/inst/20904?page=8">8</a> <a aria-label="Page 9" href="/inst/20904?page=9">9</a> <a aria-label="Page 10" href="/inst/20904?page=10">10</a> <a aria-label="Page 11" href="/inst/20904?page=11">11</a> <span class="gap">…</span> <a aria-label="Page 892" href="/inst/20904?page=892">892</a> <a aria-label="Page 893" href="/inst/20904?page=893">893</a> <a class="next_page" rel="next" href="/inst/20904?page=8">Next →</a></div> </div> </div> </div> </div> </div> <footer class="marketing-footer"> <div class="container"> <div class="row"> <div class="span12"> <div class="footer-logo"> <div class="paid-institution-footer"> <strong>ESS Open Archive </strong> <p>| Powered by <strong><a href="https://www.authorea.com/"> Authorea.com </a></strong></p> </div> <div class= "inst-footer"> <a target="blank" href="https://www.agu.org/"><img alt="instution-link" class="footer-image" src="https://d197for5662m48.cloudfront.net/images/footerimage/17/image/1444bc1906abd91c131276b1777bc07e.png" /></a> <a target="blank" href="https://www.agronomy.org/"><img alt="instution-link" class="footer-image" src="https://d197for5662m48.cloudfront.net/images/footerimage/18/image/cb7906734564497de0a3f31437041a3a.png" /></a> <a target="blank" href="https://www.aslo.org/"><img alt="instution-link" class="footer-image" src="https://d197for5662m48.cloudfront.net/images/footerimage/19/image/2ba7b49d4e9ebfb8d6a63594e4a197bc.png" /></a> <a target="blank" href="https://www.crops.org/"><img alt="instution-link" class="footer-image" src="https://d197for5662m48.cloudfront.net/images/footerimage/20/image/5f09f3ba01ee824640618b4fab647408.png" /></a> <a target="blank" href="https://www.esa.org/"><img alt="instution-link" class="footer-image" src="https://d197for5662m48.cloudfront.net/images/footerimage/21/image/0a84fb71c769d225d2f482e5694749f9.png" /></a> <a target="blank" href="https://www.soils.org/"><img alt="instution-link" class="footer-image" src="https://d197for5662m48.cloudfront.net/images/footerimage/24/image/07d8633dd99ed1c0623537c2f2bd3c3f.png" /></a> </div> </div> <ul class="links"> <li><a href="/"><strong>Home</strong></a></li> <li><a href="/about">About Us</a></li> <li><a href="/advisory-board">Advisory Board</a></li> <li><a href="/editorial-board">Editorial Board</a></li> <li><a href="/submission-guide">Submission Guide</a></li> <li><a href="/faqs">FAQs</a></li> </ul> </div> </div> </div> </footer> </body> </html>