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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.173238571.17307721/v1"> <div class="blog-card__title"> Westward- or eastward-propagating Rossby waves: Schematic illustrations </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="Hing Ong" width="24" height="24" class="user-profile-pic" src="data:image/jpg;base64,iVBORw0KGgoAAAANSUhEUgAAACAAAAAgCAMAAABEpIrGAAAABGdBTUEAALGP C/xhBQAAACBjSFJNAAB6JgAAgIQAAPoAAACA6AAAdTAAAOpgAAA6mAAAF3Cc ulE8AAABVlBMVEVF0OJE0OJEz+FG0OJJ0eJI0OJK0eJI0eI9zuAuyt41zN8x y99Dz+E9zeAryd4xy95H0OJW1OSL4exy2+l+3upBz+Etyt6G4OyT4+513Okz y984zOAtyd6O4u3////x+/xAzuEsyd73/P03zN9E0OGI4OyI4exL0eLm+Pts 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href="/doi/full/10.22541/essoar.173238571.17307721/v1"> <div class='blog-card__preview-content'> A document by Hing Ong. Click on the document to view its contents. </div> </a> </div> </div> </div> <div class="blog-card"> <a href="/doi/full/10.22541/essoar.173238593.39547246/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.173238593.39547246/v1"> <div class="blog-card__title"> Reliable IR Line Lists for N2O and OCS Isotopologues for High Temperature Application... </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="Xinchuan Huang" width="24" height="24" class="user-profile-pic" src="data:image/jpg;base64,iVBORw0KGgoAAAANSUhEUgAAACAAAAAgCAMAAABEpIrGAAAABGdBTUEAALGP C/xhBQAAACBjSFJNAAB6JgAAgIQAAPoAAACA6AAAdTAAAOpgAAA6mAAAF3Cc ulE8AAABI1BMVEV83ut73ut73ep93ut/3ut+3ut03Olr2eh13Ol53ept2uhu 2uhs2uh33Opu2ul13OqT5O6t6vKI4exz2+ml6PGp6fGO4u2s6vKG4Ox63eqi 5/Bx2+mY5e////9m2OfC7/Xa9flb1ebN8veA3+t43epj1+e97vRc1uZk1+fF 8Pam6PH9/v7P8/ej5/HE8PZp2eh23Opq2eig5/Dm+Pto2ehk2Odv2uly2+ll 2OfY9fmB3+vH8PZn2Ofd9vmH4Oxw2+nG8Pbf9/rM8vfU9PjR8/d83eun6PHj +Prs+vyZ5e9V1OVi1+ds2ejP8veD3+y57fRe1uaE4Oz6/f7l+Puk6PG+7vWN 4u2y6/O47fSV5O6/7vWL4e2x6/No2ed/3+t73esAAADzzYgmAAAAAWJLR0Rg xbd8EAAAAAd0SU1FB+gLFRAXEVXBoucAAAFwSURBVDgR5cGJQhJRGAXgc8+9 wzjKSAWEFzqZ8mebgeSEZhZqZQvt+2L6/m8ROdDyCvV9+J84TsCx5ABO4A/0 wRNESOiDJ4gkATHj6CvpnCey+QVUqjkILi4SxBR97czZc/UkyxrNyvnWUu5j bLdjBFFi0rkgdfzFZV1aWVUr7eZRigaiRIbLy1q7siTVr17T9fmuZZIZiCnC 6jfUWdfNhWpPjb6f25DMQMwwDG5pU5tFt+ipfTsfbklmIGYck+07UtjaKe5q KjMQM45+9550f7RT7Gn/4MHDdSkzEFOPGPqHeqwng26/p6fP0vG2ZAZiij7P pecv1KxWe2oOX5KSGYgSGcZ7evX6jWTjnhrVkJtkBuKUYzJs6+3I767p3cqB WmnXohQNxClHX3n/4WMnMfv0eePL1281H+PRUYwgSo4Yfa94Ig4GrBc1T8Q0 jSB+YXLsCSKEE3/sCSIEEL9x4gRgyQGcwF8cfnIAHP5BPwAgiiixApHsJgAA ACV0RVh0ZGF0ZTpjcmVhdGUAMjAyNC0xMS0yMVQxNjoyMzoxNyswMDowMB9Q TcMAAAAldEVYdGRhdGU6bW9kaWZ5ADIwMjQtMTEtMjFUMTY6MjM6MTcrMDA6 MDBuDfV/AAAAIHRFWHRzb2Z0d2FyZQBodHRwczovL2ltYWdlbWFnaWNrLm9y Z7zPHZ0AAAAYdEVYdFRodW1iOjpEb2N1bWVudDo6UGFnZXMAMaf/uy8AAAAY dEVYdFRodW1iOjpJbWFnZTo6SGVpZ2h0ADYwMHrevbUAAAAXdEVYdFRodW1i OjpJbWFnZTo6V2lkdGgANjAw6S/t6AAAABl0RVh0VGh1bWI6Ok1pbWV0eXBl AGltYWdlL3BuZz+yVk4AAAAXdEVYdFRodW1iOjpNVGltZQAxNzMyMjA2MTk3 KqPH4AAAABN0RVh0VGh1bWI6OlNpemUAMTU4OTdCQg3j55YAAAA9dEVYdFRo dW1iOjpVUkkAZmlsZTovL3RtcC9sZXR0ZXJfYXZhdGFycy8yL1hILzEyNF8y MjJfMjM1LzYwMC5wbmcv1di6AAAAAElFTkSuQmCC " /> </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/858065"><p class="blog-card__owner">Xinchuan Huang</p></a> </div> </div> <time datetime="2024-11-23" class="blog-card__date">November 23, 2024</time> </div> </div> </div> <div class='blog-card__preview-content-container'> <a href="/doi/full/10.22541/essoar.173238593.39547246/v1"> <div class='blog-card__preview-content'> A document by Xinchuan Huang. Click on the document to view its contents. </div> </a> </div> </div> </div> <div class="blog-card"> <a href="/doi/full/10.22541/essoar.173238627.78556717/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/users/860964/articles/1243612-deriving-wmo-cloud-classes-from-ground-based-rgb-pictures-with-a-residual-neural-network-ensemble/master/file/figures/Availableobservationclasses_fullperiod_WHWonly_singleplot/Availableobservationclasses_fullperiod_WHWonly_singleplot.png?1732386278" /> </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.173238627.78556717/v1"> <div class="blog-card__title"> Deriving WMO cloud classes from ground-based RGB pictures with a residual neural netw... </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="Markus Rosenberger" width="24" height="24" class="user-profile-pic" src="data:image/jpg;base64,iVBORw0KGgoAAAANSUhEUgAAACAAAAAgCAMAAABEpIrGAAAABGdBTUEAALGP C/xhBQAAACBjSFJNAAB6JgAAgIQAAPoAAACA6AAAdTAAAOpgAAA6mAAAF3Cc ulE8AAABXFBMVEX+2hD+2g/+2Q/92Q/+2hX+2hH+2hP+2hT+2hb+2hL92Qv9 1gD91QD92Aj91wD92Q392AX92Qr+5Vf+5Vz+2xv92Ab91wL+4Dn+5mD+4kf9 2AP92Q7+6G7+52n+6Gz+4kb+3zL////+75v91AD92Qz+/vv+++f+7IX+3ir+ /vr++dr++uD+3iz+4Dv+/fL+4Dz+++r+5FT+2xr+9Lv92An++d790gD92Qn9 0QD+7pb+3Sf+7pX+/O3++NL+8KH+/PH+++j++d392Af+52T+7IT+3Sb+63/+ 6Xb90wD+6XL+3ST++uX+3B3+3i/+7pL+6nf9zwD+++n+/fP++uP+3i7+9b/+ +dz++uL+++b+2xf+4Db+/Ov+3Sj++NP90AD+6nb+9Lz+6nv+2xb+9sj+87f+ +t/92AT++Nf+87L+403+/O7+/Oz+2xj+6XT+8q7+3i3+637+5mH+6XMAAAA8 lNTOAAAAAWJLR0RzQQk9zgAAAAd0SU1FB+gLFRAXHCtw3loAAAG3SURBVDgR 3cHnVhNRGAXQ850pmTDXmQxNCIgeb0QUxRaKWBA1ECso2CtRsWHB9//hBHCx 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class="blog-card__owner">Markus Rosenberger</p></a> <p class='blog-card__remaining-text'>and 2 more</p> </div> </div> <time datetime="2024-11-23" class="blog-card__date">November 23, 2024</time> </div> </div> </div> <div class='blog-card__preview-content-container'> <a href="/doi/full/10.22541/essoar.173238627.78556717/v1"> <div class='blog-card__preview-content'> Clouds of various kinds play a substantial role in a wide variety of atmospheric processes. They are directly linked to the formation of precipitation, and significantly affect the atmospheric energy budget via radiative effects and latent heat. Moreover, knowledge of currently occurring cloud types allows the observer to draw conclusions about the short-term evolution of the state of the atmosphere and the weather. Therefore, a consistent cloud classification scheme has already been introduced almost 100 years ago. In this work, we train an ensemble of identically initialized multi-label residual neural network architectures from scratch with ground-based RGB pictures. Operational human observations, consisting of up to three out of 30 cloud classes per instance, are used as ground truth. To the best of our knowledge, we are the first to classify clouds with this methodology into 30 different classes. Class-specific resampling is used to reduce prediction biases due to a highly imbalanced ground truth class distribution. Results indicate that the ensemble mean outperforms the best single member in each cloud class. Still, each single member clearly outperforms both random and climatological predictions. Attributes diagrams indicate underconfidence in heavily augmented classes and very good calibration in all other classes. Autonomy and output consistency are the main advantages of such a trained classifier, hence we consider operational cloud monitoring as main application. Either for consistent cloud class observations or to observe the current state of the weather and its short time evolution with high temporal resolution, e.g. in proximity of solar power plants. </div> </a> </div> </div> </div> <div class="blog-card"> <a href="/doi/full/10.22541/essoar.173238647.71952161/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/users/860919/articles/1243581-robustness-and-mechanisms-of-the-atmospheric-response-over-the-southern-ocean-to-idealized-freshwater-input-around-antarctica/master/file/figures/fig1/fig1.png?1732386471" /> </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.173238647.71952161/v1"> <div class="blog-card__title"> Robustness and mechanisms of the atmospheric response over the Southern Ocean to idea... </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="Xiaoqi Xu" width="24" height="24" class="user-profile-pic" src="data:image/jpg;base64,iVBORw0KGgoAAAANSUhEUgAAACAAAAAgCAMAAABEpIrGAAAABGdBTUEAALGP C/xhBQAAACBjSFJNAAB6JgAAgIQAAPoAAACA6AAAdTAAAOpgAAA6mAAAF3Cc ulE8AAABKVBMVEV83ut73ep+3ut/3ut93utu2uht2uh63ep03Olr2eh13Omn 6PGl6PF43ep53epy2+mL4e2u6vKQ4+6N4u2v6vKM4u133Oqk6PGo6fHW9Pj/ //++7vVn2OeS4+5z2+lo2ei57fTZ9fl23OqE4Oxc1ubB7/XA7/Vm2Oe77vTD 8PVd1uaA3+t13Opp2eii5/DS8/hw2+n7/v7L8feq6fJ/3+t83et73uvm+Pvl +Puj5/Fq2eie5vDp+fto2ed73euB3+vV9Phl2Odk2OfP8veD3+xx2+nd9vnX 9fiJ4e3r+vzj+Pqj6PHh9/rx+/xo2OfL8vfI8faw6/Ne1ubJ8fbF8Pa/7/Vv 2ung9/q37fSU5O7+/v7k+Pqy6/OO4u2a5e+Y5e+P4u6x6/MAAABIFitVAAAA AWJLR0RiK7kdPAAAAAd0SU1FB+gLFRAYJfPtSp0AAAFoSURBVDgR5cEJWtNQ GAXQe9/7aRKEBByqXmNaQQsaq0XtE6MUqsZ5REVwdv+bsHwtpW5Bz8F/hSMA 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XzIzNS82MDAucG5nZDHKVgAAAABJRU5ErkJggg== " /> </div> <div class="blog-card__second-avatar"> <img alt="Torge Martin" width="24" height="24" class="user-profile-pic" src="data:image/jpg;base64,iVBORw0KGgoAAAANSUhEUgAAACAAAAAgCAAAAABWESUoAAAABGdBTUEAALGP C/xhBQAAACBjSFJNAAB6JgAAgIQAAPoAAACA6AAAdTAAAOpgAAA6mAAAF3Cc ulE8AAAAAmJLR0QAAKqNIzIAAAAHdElNRQfoCxUQFxVSrGb+AAABd0lEQVQ4 EYXBMW/TUBiG0ef9fB07KRDRwlLRDYGEqERnJtj5lVnY+RcgVMQCRIIBBUoq QVGTWCGu74cdZykD9xxN+D8jwUgwEowEI8FICLScawROS7QCHRNbHk0eaZnc XUAAR6tGtDwvVj7IXa7Nxkq5IOCiflheCXzwa3Y/nC9y12Z8t/6GXARa9dPA 1uzzcy5eDtCfZ/tMYgYEWsWr/PL4+O10vBjC7YNluT7YB6djyD27OJ9XLOfz RcaSR2tbP2CD0zGQvBiNcvLhcBBZzB9ndfbk7CdOx+jEGB2P7qBTjn4f8l70 jJbYEq1yyvHlCdMRPeMacbP+enTn3qwK9Ix/ZMN3vOC0YMfYcXpNebY6rH6U DT1jJ5ABIgv1Rz5cZTmiE9iKwy/V9zKK1w03ptmnUXxTio4mtBzVmyK4fKWR mmqUUcU9uSDQEZ4X0eW6RfRsHJ09RRcQ2PEGkDcgb5BHEK1AT2yJlgCxYyQY CUaCkWAkGAl/AYOijygcGIgdAAAAJXRFWHRkYXRlOmNyZWF0ZQAyMDI0LTEx LTIxVDE2OjIzOjIxKzAwOjAw8g9/GgAAACV0RVh0ZGF0ZTptb2RpZnkAMjAy 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class='blog-card__preview-content'> Enhanced mass loss of the Antarctic ice sheet yields ocean surface freshening, cooling and sea ice expansion, which ought to drive change in the atmosphere. Using the Southern Ocean Freshwater Input from Antarctica (SOFIA) multi-model ensemble, we study the atmospheric response to a 100-year idealized freshwater release of 0.1 Sv. All models simulate consistently surface-intensified tropospheric cooling and lower-stratospheric warming south of 35˚S. Tropospheric cooling is attributed to sea ice expansion and hence albedo increase in winter and a colder sea surface in summer. This cooling yields a downward displacement of the tropopause, reduced stratospheric water vapor content and ultimately warming around 200 hPa. An enhanced southward eddy heat flux explains warming at 10-100 hPa during austral winter. Despite a temporally (and spatially) uniform prescribed freshwater flux, a prominent sea ice seasonal cycle and atmosphere dynamics result in a distinct seasonal pattern in the occurrence and magnitude of the responses. </div> </a> </div> </div> </div> <div class="blog-card"> <a href="/doi/full/10.22541/essoar.173238661.14573770/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/users/780327/articles/1243579-interannual-variability-of-tropical-cyclone-landfalls-in-the-eastern-north-pacific-environmental-drivers-and-implications/master/file/figures/Fig1-2_new/Fig1-2_new.png?1732386614" /> </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.173238661.14573770/v1"> <div class="blog-card__title"> Interannual Variability of Tropical Cyclone Landfalls in the Eastern North Pacific: E... </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="Jose Ocegueda Sanchez" width="24" height="24" class="user-profile-pic" src="data:image/jpg;base64,iVBORw0KGgoAAAANSUhEUgAAACAAAAAgCAMAAABEpIrGAAAABGdBTUEAALGP C/xhBQAAACBjSFJNAAB6JgAAgIQAAPoAAACA6AAAdTAAAOpgAAA6mAAAF3Cc ulE8AAABaFBMVEVSvIlRvIlRvIhRu4hVvYtTvIpUvIpWvYxPuodCtn5JuINH t4E7s3k6snhAtXxQu4dPuoZ4y6NjwpRMuYU5snhhwZOW1red2bx+zadEtn9G t4Btxpz////G6NhBtX2v4Mj6/ftRu4lUvYtpxZnA5tQmq2uEz6vd8eeK0a/q 9/HC59UgqGes38Z6y6QfqGY1sHXM69z6/fxZvo5LuYRTvInB59WFz6zq9vBg wZM8s3pCtX5Ouoa95dJAtX2y4cvx+fWg2r5UvYpqxZk3sXc6s3lrxZq85dFx yJ5BtX5KuYQ5sndFt4BXvo1pxZg2sXY/tHz1+/hQu4hEtoB2yqH0+veR1LQ4 snc9tHpmw5Yoq2za8OXz+vccp2Tc8edHuIJGt4Hw+fXE6NeX1ri4489IuIJD tn5txpv+/v5JuILY8OXL6tuDz6o9s3pvx52a2Lqb2Ls+tHxNuoVsxpqZ17mT 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This study investigates the climatological seasonal cycle and interannual variability of TC landfalls in the ENP. We find that the basin is characterized by a bimodal distribution of landfalls, with peaks in June and September–October. Using a composite analysis of high and low landfall years, we show that this distribution is primarily driven by landfall probability rather than genesis. The absence of landfalls during July is due to enhanced easterlies from the Caribbean Low-Level Jet entering the ENP through gaps in the Americas Cordillera. High landfall years feature enhanced easterly wind reversals from a northward-shifted Intertropical Convergence Zone. These additional steering winds drive hurricanes ashore in the vulnerable region of southwest Mexico. This study provides valuable insights for improving TC landfall forecasts and preparedness in the region. </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.173221975.58715449/v1"> <div class="blog-card__title"> Climate Action Maps Enable Science Centers and Museums to Make Climate Action Visible... </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="Rose Hendricks" width="24" height="24" class="user-profile-pic" src="data:image/jpg;base64,iVBORw0KGgoAAAANSUhEUgAAACAAAAAgCAMAAABEpIrGAAAABGdBTUEAALGP C/xhBQAAACBjSFJNAAB6JgAAgIQAAPoAAACA6AAAdTAAAOpgAAA6mAAAF3Cc ulE8AAABRFBMVEWPpK+OpK+Oo66RprCSprGRprGRpbCQpa+Oo6+QpbCBmaWA l6SAmKSDmqaInqqHnqmCmaWMoq2Fm6e5xs28yM+4xsy7x86ru8OWqbOKn6uh 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ZW1hZ2ljay5vcme8zx2dAAAAGHRFWHRUaHVtYjo6RG9jdW1lbnQ6OlBhZ2Vz ADGn/7svAAAAGHRFWHRUaHVtYjo6SW1hZ2U6OkhlaWdodAA2MDB63r21AAAA F3RFWHRUaHVtYjo6SW1hZ2U6OldpZHRoADYwMOkv7egAAAAZdEVYdFRodW1i OjpNaW1ldHlwZQBpbWFnZS9wbmc/slZOAAAAF3RFWHRUaHVtYjo6TVRpbWUA MTczMjIwNjE5MLTHUkMAAAATdEVYdFRodW1iOjpTaXplADE1MDE2QkL55e6P AAAAPXRFWHRUaHVtYjo6VVJJAGZpbGU6Ly90bXAvbGV0dGVyX2F2YXRhcnMv Mi9FQy8xMjBfMTMyXzIwNS82MDAucG5nPknfbQAAAABJRU5ErkJggg== " /> </div> </div> <div> <div class="blog-card__authors-text"> <div class="blog-card-author-list" style="width: 100%;"> <a href="/users/860162"><p class="blog-card__owner">Rose Hendricks</p></a> <p class='blog-card__remaining-text'>and 4 more</p> </div> </div> <time datetime="2024-11-21" class="blog-card__date">November 21, 2024</time> </div> </div> </div> <div class='blog-card__preview-content-container'> <a href="/doi/full/10.22541/essoar.173221975.58715449/v1"> <div class='blog-card__preview-content'> Science centers and museums are increasingly exploring a range of approaches for encouraging their visitors and communities to not only learn about climate solutions, but to discover their own pathways to sustained, meaningful participation in action. These place-based institutions have unique opportunities to cultivate a culture of hope and action thanks to their local expertise, diverse programming (e.g., field trips, special events, and community science projects), and wide reach (including both in-person and online interactions). These assets enable science centers and museums to communicate about climate solutions in ways that are visible, relatable, and accessible, all attributes that make them more likely to be taken up. One approach that several museums and other groups have piloted is the use of a GIS-based tool to invite members of their community to share the climate actions they’re undertaking and explore those of others. The tool produces open-access climate action maps that showcase real actions taking place in a particular community and provide an opportunity to leverage several evidence-based practices for communicating about climate solutions. By featuring everyday people who live in one’s community, doing actions that are broadly accessible, the maps build a sense of agency, provide inspiration, convey action-oriented norms, and build a sense of belonging in climate solutions. We will describe the ways that this flexible tool and resulting map can be embedded in a range of museum contexts and will discuss the ways that contributing to and exploring the map benefits museums, their visitors, and communities. We will also discuss opportunities for increasing impact through connections with local media, decision-makers, and K-12 school systems. This work demonstrates the role that science museums can play as hubs for collecting and coordinating climate stories and actionable resource centers for increasing community-led participation in climate action. </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.173238805.52874342/v1"> <div class="blog-card__title"> Climate Action Maps Enable Science Centers and Museums to Make Climate Action Visible... </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="Emily Coren" width="24" height="24" class="user-profile-pic" src="data:image/jpg;base64,iVBORw0KGgoAAAANSUhEUgAAACAAAAAgCAMAAABEpIrGAAAABGdBTUEAALGP C/xhBQAAACBjSFJNAAB6JgAAgIQAAPoAAACA6AAAdTAAAOpgAAA6mAAAF3Cc ulE8AAABQVBMVEV4hM13g813hM13g8x7h856hs55hc17hs54g812gsxndcdm c8ZmdMZlc8Zqd8dzf8tndcZodcd0gMt6hs2ss+Cpsd+qsd+psN+uteGiqtxx fcpndMalrd2yueJyfspreMj////4+fxsecifqNuQmdVpdsfu7/h+ic+MltSK ldONl9WLldSJk9P7+/2PmdVzgMuTndd5hM3r7fdaacJteslyf8pkcsXO0u2N l9Rca8JWZcC2veSqst/q7PdcasLw8vlwfcqXoNiAi9B1gct1gcz9/f7M0OzU 2O/T1+7e4fKDjtFueslyf8vp6/dSYr9kccXy8/qOmNV9ic90gcvs7vhfbcPV 2e+FkNFhb8RYZ8G0u+Pt7/h9iM+KlNNodsd9iM5jccWstOCVn9ittOCrsuCn r96AjNCxuOJ6hc1lcsYAAAAqBiy2AAAAAWJLR0RqJWKVDgAAAAd0SU1FB+gL FRAXCt+kawsAAAFcSURBVDgR3cGJQhJRGAXgM5zL4GUb5g4YDiW/JIqaoTUu FRqJpSnuu0mWtr7/C+SA49Yb+H14ZKwQQjErhv8wAvbgPkJ1xQnaSiVA3NVH 6GQqnU5nsmDcyWVc4xF3EFrn84X+J8UB3yvx6bOBwbJH3CIMpWuoknsuoeFq nESEMI6MjNbGxieqL2TyZX1KRNeniQhhHHn1OqiUZ2bnZP4N3r6Thqto4Rph HFlYDCqBdt9LkwmtPiwZEBHCtKSrlhXxW8ByYEDcIIyRj59WVj+vrYv4y4Bu tkDcIExbNjYzW7Ot7Lb42qO9s7sHIkIYR/YPBv1me+tQjo4TJ6eSTypauEYY R76cTXRqta87MnJe7ojYbZuIEIbS43z7LqELN04iQmh9edn40Sj+dKZLv4q/ C6j+IW71ETqXupKpkl4z9bfU9oh7CNWVAGkrpWziAUbAHjwUs0IIWVYMj8w/ UhspYbuFGIgAAAAldEVYdGRhdGU6Y3JlYXRlADIwMjQtMTEtMjFUMTY6MjM6 MTArMDA6MDDa93NNAAAAJXRFWHRkYXRlOm1vZGlmeQAyMDI0LTExLTIxVDE2 OjIzOjEwKzAwOjAwq6rL8QAAACB0RVh0c29mdHdhcmUAaHR0cHM6Ly9pbWFn ZW1hZ2ljay5vcme8zx2dAAAAGHRFWHRUaHVtYjo6RG9jdW1lbnQ6OlBhZ2Vz ADGn/7svAAAAGHRFWHRUaHVtYjo6SW1hZ2U6OkhlaWdodAA2MDB63r21AAAA F3RFWHRUaHVtYjo6SW1hZ2U6OldpZHRoADYwMOkv7egAAAAZdEVYdFRodW1i OjpNaW1ldHlwZQBpbWFnZS9wbmc/slZOAAAAF3RFWHRUaHVtYjo6TVRpbWUA MTczMjIwNjE5MLTHUkMAAAATdEVYdFRodW1iOjpTaXplADE1MDE2QkL55e6P AAAAPXRFWHRUaHVtYjo6VVJJAGZpbGU6Ly90bXAvbGV0dGVyX2F2YXRhcnMv Mi9FQy8xMjBfMTMyXzIwNS82MDAucG5nPknfbQAAAABJRU5ErkJggg== " /> </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/536851"><p class="blog-card__owner">Emily Coren</p></a> <p class='blog-card__remaining-text'>and 4 more</p> </div> </div> <time datetime="2024-11-23" class="blog-card__date">November 23, 2024</time> </div> </div> </div> <div class='blog-card__preview-content-container'> <a href="/doi/full/10.22541/essoar.173238805.52874342/v1"> <div class='blog-card__preview-content'> Science centers and museums are increasingly exploring a range of approaches for encouraging their visitors and communities to not only learn about climate solutions but also to discover their own pathways to sustained, meaningful participation in action. These institutions have unique opportunities to cultivate a culture of hope and action thanks to their local expertise, diverse programming (e.g., field trips, special events, and community science projects), and wide reach (including both in-person and online interactions). These assets enable science centers and museums to communicate about climate solutions in ways that are visible, relatable, and accessible, all attributes that make them more likely to be taken up. One approach that several museums and other groups have piloted is the use of a GIS-based tool to invite members of their community to share the climate actions they're undertaking and explore those of others. The tool produces open-access climate action maps that showcase real actions taking place in a particular community and provide an opportunity to leverage several evidence-based practices for communicating about climate solutions. By featuring everyday people who live in one's community, doing actions that are broadly accessible, the maps build a sense of agency, provide inspiration, convey action-oriented norms, and build a sense of belonging in climate solutions. We will describe (a) the ways that this flexible tool and resulting maps can be embedded in a range of museum contexts, and (b), the ways in which contributing to and exploring the map can benefit museums, their visitors, and their communities. We will also discuss opportunities for increasing impact through connections with local media, decision-makers, and K-12 school systems. This work demonstrates the role that science museums can play as hubs for collecting and coordinating climate stories and resources, and promoting community-led participation in climate action. </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.173238688.88997392/v1"> <div class="blog-card__title"> Smart Cities Configuration </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="Md Tarif Raihan" width="24" height="24" class="user-profile-pic" src="https://d197for5662m48.cloudfront.net/images/user/667403/profile_image/thumbnail-54145989654aa11290092cdddddea678.jpeg" /> </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/667403"><p class="blog-card__owner">Md Tarif Raihan</p></a> </div> </div> <time datetime="2024-11-23" class="blog-card__date">November 23, 2024</time> </div> </div> </div> <div class='blog-card__preview-content-container'> <a href="/doi/full/10.22541/essoar.173238688.88997392/v1"> <div class='blog-card__preview-content'> This paper represents the components of the Smart Grid, issues regarding the implementation of Smart Grid concept and how battery energy storage systems can be used in the Smart Grid. The relationship between climate change and smart grid, distributed generation and microgrids have been discussed. There is an overview of smart meter, smart tariff, electricity generation, and demand. The battery's potential for Demand Side Management (DSM) has been explained. An extensive review of batteries has been given in terms of their use in the transmission, distribution, and residential sectors. In several segments, the electrical grids of New South Wales (Australia) and California has been discussed as case studies. Finally, some real-world Smart Grid examples have been included. </div> </a> </div> </div> </div> <div class="blog-card"> <a href="/doi/full/10.22541/essoar.173204262.23357804/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-e73efc713d600e97fa60b2e049b6dc4e.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.173204262.23357804/v1"> <div class="blog-card__title"> Near-Resonance between the Shelf Ocean and Semidiurnal Atmospheric Tidal Winds </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="Fucent Hsuan Wei Hsu" width="24" height="24" class="user-profile-pic" src="data:image/jpg;base64,iVBORw0KGgoAAAANSUhEUgAAACAAAAAgCAMAAABEpIrGAAAABGdBTUEAALGP C/xhBQAAACBjSFJNAAB6JgAAgIQAAPoAAACA6AAAdTAAAOpgAAA6mAAAF3Cc ulE8AAABXFBMVEVblflalflalPlalPhclvlfl/lfmPlel/ldlvlclflSj/hE hvhGh/hFh/hTj/hYk/hIiPhOjPhQjvhHiPhWkvhypPmjw/uWu/uXvPttoflX k/iVuvt/rPpUkPh2pvpimvlWkfiewPv///9hmPnp8f5ChfjH2/yArfpLi/ij xPtgmPl0pflwovl6qfrd6f1Dhfi/1vx7qvqXu/uSuPs8gfdTkPhIifhzpPne 6v1Zk/g+gve/1fx8qvqIsvordvdGiPhAg/hLivhPjfhyo/nb5/09gvc5f/e7 0/yZvfvG2vzN3/3W5P291PxBhPh1pvmavfv4+/74+v75+/7i7P11pfn0+P6+ 1fzJ3P3p8P5+q/otd/dMi/jY5v1Fhvgmcve1z/yYvPtNjPjg6/1KivhjmvnC 1/xxo/nc6P1ChPh7qfqcv/tqn/lVkfipx/uNtfqBrvqsyftmnPlUkfgAAACa lJEIAAAAAWJLR0RzQQk9zgAAAAd0SU1FB+gLFRAXGCwdGkMAAAGNSURBVDgR 3cHpWtNQFAXQfe7u7c1NE7SkkKJE8dRCRAXBGQtYcQAFnBFnUZwAx/f/oTTl q/gIrIWDRToAQYdgP8MeAxiS2Iclu6tcggsIMLAgegx9WIniOKr0HTpcBen7 kxoo2MNSODCY1uvp4NCRo8MZfN+x9PiIJ7qENj6hHfWGnky8bY7qWO4oKAht lOqp8dNnzo4M6UQSjE+e06ncUVAQ2nhaz1+ohRcvXdYrzat+5pq2ckdBQWjj VGfn5q+3byzozVthdvuOtnJHQUFo40WdWLp7b3llVbuG246CgtDG9/XBw0f6 eOaJPl0bfba8rs/bjoKC0Mapzr5IVvKXC/pqrvn6zVudyh0FBaGNp/Vd0vB2 Y0Dff2hsRh+1lTsKCkIbpZpGlkH1k36OvP2ypl9zR0FBaKMt3Yotg41VXU+8 bS7pWO4o6KLPthe3M0+/s/nte4hS/4+fv357Yo+hz5LM0xC1Shukr07ueBr0 0FtPAETZEWBQ9sS/DEmDv0gawJDEfwQFEewSHCh/ABTLLwfdO7ojAAAAJXRF WHRkYXRlOmNyZWF0ZQAyMDI0LTExLTIxVDE2OjIzOjI0KzAwOjAwoDdQvQAA ACV0RVh0ZGF0ZTptb2RpZnkAMjAyNC0xMS0yMVQxNjoyMzoyNCswMDowMNFq 6AEAAAAgdEVYdHNvZnR3YXJlAGh0dHBzOi8vaW1hZ2VtYWdpY2sub3JnvM8d nQAAABh0RVh0VGh1bWI6OkRvY3VtZW50OjpQYWdlcwAxp/+7LwAAABh0RVh0 VGh1bWI6OkltYWdlOjpIZWlnaHQANjAwet69tQAAABd0RVh0VGh1bWI6Oklt YWdlOjpXaWR0aAA2MDDpL+3oAAAAGXRFWHRUaHVtYjo6TWltZXR5cGUAaW1h Z2UvcG5nP7JWTgAAABd0RVh0VGh1bWI6Ok1UaW1lADE3MzIyMDYyMDRgLpNK AAAAEnRFWHRUaHVtYjo6U2l6ZQA0MTgwQkJ5M1mhAAAAPHRFWHRUaHVtYjo6 VVJJAGZpbGU6Ly90bXAvbGV0dGVyX2F2YXRhcnMvMi9GSC85MV8xNDlfMjQ5 LzYwMC5wbme9YlaeAAAAAElFTkSuQmCC " /> </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/859395"><p class="blog-card__owner">Fucent Hsuan Wei Hsu</p></a> <p class='blog-card__remaining-text'>and 4 more</p> </div> </div> <time datetime="2024-11-19" class="blog-card__date">November 19, 2024</time> </div> </div> </div> <div class='blog-card__preview-content-container'> <a href="/doi/full/10.22541/essoar.173204262.23357804/v1"> <div class='blog-card__preview-content'> A document by Fucent Hsuan Wei Hsu. Click on the document to view its contents. </div> </a> </div> </div> </div> <div class="blog-card"> <a href="/doi/full/10.22541/essoar.173204252.26490920/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/users/539748/articles/1242459-along-dip-variations-in-source-characteristics-of-shallow-slow-earthquakes-controlled-by-topography-of-subducted-oceanic-plate/master/file/figures/Fig01/Fig01.png?1732411843" /> </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.173204252.26490920/v1"> <div class="blog-card__title"> Along-dip variations in source characteristics of shallow slow earthquakes controlled... </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="Shunsuke Takemura" 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 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src="data:image/jpg;base64,iVBORw0KGgoAAAANSUhEUgAAACAAAAAgCAMAAABEpIrGAAAABGdBTUEAALGP C/xhBQAAACBjSFJNAAB6JgAAgIQAAPoAAACA6AAAdTAAAOpgAAA6mAAAF3Cc ulE8AAABVlBMVEWiiH6ih32iiH2hh32iiH+kioGki4GiiX+jioCkioCehHmW eW6Vd2ueg3mZfHGXe2+hhnyghnyXem+jiX+Ye3CghXvAr6jKvLbCsaqWeW29 q6S/raefhHq/rqe+q6S3o5z////ArqiKaV3i2tfHuLKUd2unjoWUdmvJurXf 1tKfhHmznpaafnOul479/fyljIKbf3T9/Pyegnidgnixm5Pc0s6BXlCRc2fD sqyJaVzSxsHGtrCHZlnJu7XLvbiTdGm/raaVd2yfhXuafnT5+PePcGT8/Pyb f3W5pZ7Yzsqtlo2WeG2UdmrKu7bh2dbNv7n6+PjQwr2VeGybgHX6+ficgXeV eG2umI/7+vqxnJSmjYSTdWnFta+TdWrIubO4pZ2FY1amjoTCsauZfXL08fCn j4Xu6ui3o5umjYPDs6zaz8vEtK7JurSwm5KdgXfSxcCeg3gAAADfq6JaAAAA AWJLR0Rxrwdc4gAAAAd0SU1FB+gLFRAXCt+kawsAAAFdSURBVDgR3cF7WwxR AAbwd/adzjnTJts2o602vSilhiIhG1l3TpEN201Xt8jy/f9iny7TPjw+QL8f Tp0gh/9gBgD/QCuGbabNki4CQUSOaEHXnu/In4nYebYAoqvYSRAZdsfJuZ4S egt9/eUESXngfEIQh0hXHFTThYuXNDR8eWRUV/KOxCGGY5DG06vXNDGp62n7 pHRjyhJH6NKbmr7F2yXdmbmryuw93Z8zJI4wLFN6EFer8dTDR3r85KmeJSCO 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Takemura</p></a> <p class='blog-card__remaining-text'>and 3 more</p> </div> </div> <time datetime="2024-11-19" class="blog-card__date">November 19, 2024</time> </div> </div> </div> <div class='blog-card__preview-content-container'> <a href="/doi/full/10.22541/essoar.173204252.26490920/v1"> <div class='blog-card__preview-content'> To discuss slip behaviors in shallow slow earthquake regions, we investigate source characteristics of shallow very low frequency earthquakes (VLFEs) southeast off the Kii Peninsula in the Nankai subduction zone. VLFEs are a kind of slow earthquakes and are clearly observed at frequencies below 0.1 Hz. A non-linear inversion technique for moment rate function estimation and the permanent ocean-bottom seismometer network provided us with precise locations and detailed kinematic source characteristics of shallow VLFEs. The high activity of shallow VLFEs around the western edge of the subducted Paleo-Zenisu ridge is similar to previous studies. A notable trend change in the along-dip dependency of shallow VLFE moment rates was found. Along the profile west side of the Paleo-Zenisu ridge, moment rates of shallow VLFEs increase with reaching the megathrust zone. Small-scale topographic fluctuations of the subducted oceanic plate exist along this profile, but large-scale seamount subduction has not been identified even from dense seismic surveys. Similar tendencies have been reported in tectonic tremors in the Nankai and Cascadia subduction zones. On the other hand, the opposite trend appeared along the profile with the Paleo-Zenisu ridge. Small shallow VLFEs were dominant near the summit of the Paleo-Zenisu ridge. Fracture networks or stress fields due to seamount subduction possibly impede large shallow VLFEs around the subducted seamount. Our results suggest that the large-scale heterogeneity of the upper surface of the subducted oceanic plate could control source characteristics of shallow slow earthquakes. </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.173204240.08166674/v1"> <div class="blog-card__title"> Extreme precipitation depiction in convection-permitting Earth System Models within t... </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="Jonathan Wille" width="24" height="24" class="user-profile-pic" src="data:image/jpg;base64,iVBORw0KGgoAAAANSUhEUgAAACAAAAAgCAMAAABEpIrGAAAABGdBTUEAALGP C/xhBQAAACBjSFJNAAB6JgAAgIQAAPoAAACA6AAAdTAAAOpgAAA6mAAAF3Cc ulE8AAABklBMVEVSvIlRvIlRu4hRvIhVvYtTvIpUvIpWvYtTvIlOuoZCtX5K uIM/tHxEtn9Ht4FAtXxKuYM9s3pLuYR5y6RgwZOM0rB4yqNJuINtxpuI0a5K uYRhwpOT1bVjwpVBtX3////C59UwrnL+/v4+tHvr9/FiwpM6sni95dJ2yqJC tn5BtX50yaDA5tQdp2XV7uJdwJBav46N0rHh8+pNuoXB59UfqGae2byAzqgs rW+CzqrL6tszsHTn9e47s3korGxxyJ6q3sUdp2TE6Nfy+vaz4csyr3NpxZms 38Y4sndWvYy+5tNQu4jU7uIgqGdnxJdGt4CG0Kx6y6R1yaG85dE5snjj9OxE toCT1bY3sXaj28BIuIJHuIJYvo1Dtn88s3qv4MlfwZIurnD6/fvS7eD2+/l8 zKWx4cqBzqn5/Prx+fa34842sXZyyJ7n9e/Z8OVMuYVbv4+/5tN3yqKP07O4 4849tHvt+PODz6pQu4doxJhFt4BUvYqb2Luc2Lt4yqJPuodGt4F+zaek3MGa 2LpDtn4AAABBfIuuAAAAAWJLR0SFFddq5wAAAAd0SU1FB+gLFRAXGVsaKtUA AAGSSURBVDgR3cGJegtRAAXgc8/cSSaVJjoVpZhThrSRWIMqYi8ZtbWIKol9 X2sNtfPgJlu/1iP0/7ESGbQYxAz+xw4wBsYcLENYF9YSTFiQbtIjliJSfauY 7gfdTJb0Vg/4Hh0sIlLJwTV+bu1QIrNuvY/hDRs3+R7RY2iDQY1s1pYswq3a 5udHNVawNOgytNuLKu3YqV3Z3dKeMNyr4bJH9BjaoKh9+w9o/OCEdOhwSkcq LogukjYoqnT0mI6fOHnqtCbP6Gw1ooMOxmxQ1LnJKZ2/oJGLunRZ02lLgw56 1rPBjK5cDa+ppuuzmr4hO+QSbSTmqjdv1YsabVRuK6c7d++V7iskiBZDW5h4 8LBSHdOjgfpjPXnaP/tMKj2PSLQY2voLvZyrvdJ48PqNNF+pvZXeNZJ00EYk Ku8Vm//gIvyoT+nmlPT5ywLRRTQbM1+/fW/8gPfz1++FspvJ/Sk3QfQQbiGf 73NBen/zKRDpRhN0sIiwUWRBgDYCQRuBWIptABgDGMNyxnEMWoxBzBisKP8A ZcQ5jXyb9esAAAAldEVYdGRhdGU6Y3JlYXRlADIwMjQtMTEtMjFUMTY6MjM6 MjQrMDA6MDCgN1C9AAAAJXRFWHRkYXRlOm1vZGlmeQAyMDI0LTExLTIxVDE2 OjIzOjI0KzAwOjAw0WroAQAAACB0RVh0c29mdHdhcmUAaHR0cHM6Ly9pbWFn ZW1hZ2ljay5vcme8zx2dAAAAGHRFWHRUaHVtYjo6RG9jdW1lbnQ6OlBhZ2Vz ADGn/7svAAAAGHRFWHRUaHVtYjo6SW1hZ2U6OkhlaWdodAA2MDB63r21AAAA F3RFWHRUaHVtYjo6SW1hZ2U6OldpZHRoADYwMOkv7egAAAAZdEVYdFRodW1i OjpNaW1ldHlwZQBpbWFnZS9wbmc/slZOAAAAF3RFWHRUaHVtYjo6TVRpbWUA MTczMjIwNjIwNGAuk0oAAAATdEVYdFRodW1iOjpTaXplADIwMzM4QkJ/9/rw AAAAPHRFWHRUaHVtYjo6VVJJAGZpbGU6Ly90bXAvbGV0dGVyX2F2YXRhcnMv Mi9KVy84Ml8xODhfMTM3LzYwMC5wbmfuZ4NwAAAAAElFTkSuQmCC " /> </div> <div class="blog-card__second-avatar"> <img alt="Rebekka Koch" width="24" height="24" class="user-profile-pic" src="data:image/jpg;base64,iVBORw0KGgoAAAANSUhEUgAAACAAAAAgCAMAAABEpIrGAAAABGdBTUEAALGP C/xhBQAAACBjSFJNAAB6JgAAgIQAAPoAAACA6AAAdTAAAOpgAAA6mAAAF3Cc ulE8AAABa1BMVEWPpK+OpK+Oo66Oo6+QpK+SprGRprGRpbCQpbCRprCJn6p/ l6OAmKSAl6SBmKWFnKiNoq2DmqaCmaafsbrBzdO4xcy6x862xMuhs7yEm6eM oq2xwMequsKKn6uLoKyJn6uywMiNoq69ydD///+ktb72+PmCmaV9laLl6uzU 3OC3xMvAzNKUqLKbrbf+/v7v8vR6k6DN19vY3+N5kp+zwsl4kp90jpvZ4OSc r7j09vduiZeMoa23xcyzwclzjZvd5OeXq7Xj6OuVqbP5+vuHnanCztShsrvK 1Nnv8vN/l6Tz9favvsZ3kZ7f5eiGnaj8/f2LoazEz9WMoazL1Nl4kZ62w8rh 5umywch2kJ19lqLs7/GCmqZ+lqPm6u25xs2Sp7Gmt8Dk6ezu8fODmqePo6+7 x86Tp7Lo7O+tvMSBmaX29/j4+vqesLnJ09iInqqarberusOGnKi1wsq0wsnI 0tiKoKt+lqKQpa8AAABCEHHmAAAAAWJLR0R41tvkRgAAAAd0SU1FB+gLFRAX DtjJrxIAAAF0SURBVDgR5cHpYgtRAAXgc4+ZO5PrSjKtSQkaHBLSVBBLSe1b bUGVKrGW2loU5fWlkon+8gB8H/4xxuAvmAF7sIk92IhBaEMbgUQUE0QuAjFE wm32W/KFYkQmBRDFkYQgMgzc6Na0NLbNbUd5x85d8Xhl91iwB0SfofV79du+ PLW/GtcO6GASg+gztL6uicZkXYcKTs3k8BEdbRHEgKH1qY4dL544qamqTp1O 1ay2AyJjaP20zrTGz57T+UQXLupS+XJEDBlan+pK4+o1zVxv68aMbt5qEH8Y Wl/SutvlDqU70t1KTAwZWp/q3mxJ9+cwK40+0MNaTCJjaP205h8tPNbkk7Ka re5TPas9JzKG1teVFjov9HKurFeLDlK4GPE1+gytf6OSX1p4q3fv9SG/1J3X x3YRxAADt7yy7HKfPq98WZ346oDVb9+n1kAMkHBdBwaVHx34BARGumsgMcQg DAj+DGPaiCByIYgNuA4cANiD/8kv8OQw4lOVTxcAAAAldEVYdGRhdGU6Y3Jl YXRlADIwMjQtMTEtMjFUMTY6MjM6MTQrMDA6MDAuuFdeAAAAJXRFWHRkYXRl Om1vZGlmeQAyMDI0LTExLTIxVDE2OjIzOjE0KzAwOjAwX+Xv4gAAACB0RVh0 c29mdHdhcmUAaHR0cHM6Ly9pbWFnZW1hZ2ljay5vcme8zx2dAAAAGHRFWHRU aHVtYjo6RG9jdW1lbnQ6OlBhZ2VzADGn/7svAAAAGHRFWHRUaHVtYjo6SW1h Z2U6OkhlaWdodAA2MDB63r21AAAAF3RFWHRUaHVtYjo6SW1hZ2U6OldpZHRo ADYwMOkv7egAAAAZdEVYdFRodW1iOjpNaW1ldHlwZQBpbWFnZS9wbmc/slZO AAAAF3RFWHRUaHVtYjo6TVRpbWUAMTczMjIwNjE5NLOqlloAAAATdEVYdFRo dW1iOjpTaXplADE4MDk5QkKLk5KDAAAAPXRFWHRUaHVtYjo6VVJJAGZpbGU6 Ly90bXAvbGV0dGVyX2F2YXRhcnMvMi9SSy8xNDNfMTY0XzE3NS82MDAucG5n 1QuJ0wAAAABJRU5ErkJggg== " /> </div> </div> <div> <div class="blog-card__authors-text"> <div class="blog-card-author-list" style="width: 100%;"> <a href="/users/602812"><p class="blog-card__owner">Jonathan D. Wille</p></a> <p class='blog-card__remaining-text'>and 3 more</p> </div> </div> <time datetime="2024-11-19" class="blog-card__date">November 19, 2024</time> </div> </div> </div> <div class='blog-card__preview-content-container'> <a href="/doi/full/10.22541/essoar.173204240.08166674/v1"> <div class='blog-card__preview-content'> As extreme precipitation events become more frequent and intense, local-scale climate services are increasingly needed to help communities adapt. We here evaluate two fully-coupled convection-permitting Earth System Models for their ability to resolve mesoscale extreme weather events. Using the Integrated Forecasting System (IFS) and Icosahedral Nonhydrostatic Weather and Climate Model (ICON) within the Next Generation Earth Modelling Systems (nextGEMS) project, we evaluate their depiction of extreme precipitation with a focus on the Mediterranean region through a comparison with high resolution reanalysis, gridded observations, a regional climate model, and a large-ensemble lower-resolution climate model. The results are then compared at a coarser resolution globally with CESM2. For dry extremes, we find that the higher resolution and hybrid/explicit representation of convection of the nextGEMS models improve the representation of dry hour frequency and alleviates the drizzle bias observed in CMIP6 models. The explicit representation of convection in ICON helps create realistic dry spell lengths over land, but also generates overly intense convective precipitation. Generally, the nextGEMS models concentrate dry spells into limited frequency yet overly long periods. For wet extremes, the nextGEMS models properly high intensities of heavy precipitation, aside from overestimation in ICON over mountainous terrain. The models appear capable of resolving extreme weather systems like medicanes and tropical cyclones making them useful for extreme weather climatology studies. Overall, the depiction of wet and dry precipitation extremes in the Mediterranean region are representative of the nextGEMS’ models performance across the global mid-latitudes demonstrating the models’ value in simulating extreme weather systems. </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.173204229.90033008/v1"> <div class="blog-card__title"> Urbanization-Resolved Scales Amplify Torrential Rainfall in a Coastal Megacity </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="Rakesh Teja Konduru" width="24" height="24" class="user-profile-pic" src="data:image/jpg;base64,iVBORw0KGgoAAAANSUhEUgAAACAAAAAgCAMAAABEpIrGAAAABGdBTUEAALGP 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</div> <time datetime="2024-11-19" class="blog-card__date">November 19, 2024</time> </div> </div> </div> <div class='blog-card__preview-content-container'> <a href="/doi/full/10.22541/essoar.173204229.90033008/v1"> <div class='blog-card__preview-content'> This study unveils the ability of 200-m near to Large-Eddy Simulation (LES) to resolve smaller scales in urban areas of a coastal megacity Chennai in India, which are crucial for accurately modelling Urban Induced Turbulence (UIT) and Urban Heat Island (UHI) effects. Unlike physics-based ensemble (PBE) models in kilometre-scale simulations, LES captures fine-scale atmospheric dynamics, offering enhanced resolution to simulate localized turbulence and heat flux variations. With a resolution of 200 m, Weather Research Forecasting (WRF) LES simulation can convincingly resolve a higher urban heat flux, friction velocity, surface wind speeds, and moisture transport over urban areas. These factors are found to play a critical role in intensifying extreme weather events such as heavy rainfall, especially in the downwind regions of coastal megacities like Chennai. This phenomenon is driven by LES-resolved interaction between the urban heat island effect and the prevailing winds. </div> </a> </div> </div> </div> <div class="blog-card"> <a href="/doi/full/10.22541/essoar.173203125.57913538/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-0f57237e39dd0c54df15afa034038147.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.173203125.57913538/v1"> <div class="blog-card__title"> Rapid Infill of Abandoned Tidal Channels Creates Hotspots for Blue-Carbon Accumulatio... </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="Alice Puppin" 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 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class="blog-card__second-avatar"> <img alt="Davide Tognin" width="24" height="24" class="user-profile-pic" src="data:image/jpg;base64,iVBORw0KGgoAAAANSUhEUgAAACAAAAAgCAMAAABEpIrGAAAABGdBTUEAALGP C/xhBQAAACBjSFJNAAB6JgAAgIQAAPoAAACA6AAAdTAAAOpgAAA6mAAAF3Cc ulE8AAABGlBMVEWVcs+Vcc+Ucc+Ucc6Wc8+XddCXdNCVc8+PasyGXsiHYMiH X8iKY8qQa8yIYcmTcM6Ucs+khtXDsOS7peC9p+GtktqWdM+FXcijhdXDr+O7 pOC8puC8p+G8puHArOL////Ov+mJYsmGX8jEseSRbc2YdtCliNbf1fDSxOuC Wcace9Koi9eff9Omidfv6viZeNGlh9a2nt5+VMSNZ8t9U8Ts5vaKZMqOacyP a8zu6fd/VMWIYsmdfNLBreOaedGYd9Dw7PiLZcqmidbXyu2FXMfw6/idfdK9 qOHCruN+VMWNaMvh1/HSw+qFXceXdM/v6veHYMnOvumZd9H28/ukhta+qOGs kdm2n96uk9qQbMyQbM2JY8mMZsoAAAA/zPwpAAAAAWJLR0Rdnd8wAQAAAAd0 SU1FB+gLFRAXDDbHzj4AAAFZSURBVDgR3cGNQgxRGAbg98x7vs7MOabBGRuV PrVthc1WS0rYUotSK/LP/V8Ha8Yk7qDnweVijMFvpoYLElaQsIG/0YrIhCVo pQaikdClmQ9XcgHSzIexyQK8ihpteu16LG+0plx+89b0zOztWJYsQFQMJczp 2J35hbbWZNERFUPxUdudpWVduXvvfndVH/TW1gqCqBhKiLq+0X/4SLubj/2W bj/p9wmiZigharnzNCv1mX++ONDdeWmB+MNQQtQYensvdP9gsDWhQ+9INAwl 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class='blog-card__remaining-text'>and 6 more</p> </div> </div> <time datetime="2024-11-19" class="blog-card__date">November 19, 2024</time> </div> </div> </div> <div class='blog-card__preview-content-container'> <a href="/doi/full/10.22541/essoar.173203125.57913538/v1"> <div class='blog-card__preview-content'> A document by Alice Puppin. Click on the document to view its contents. </div> </a> </div> </div> </div> <div class="blog-card"> <a href="/doi/full/10.22541/essoar.173238705.53228461/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/users/859084/articles/1242446-reduced-winter-time-clear-air-turbulence-in-the-trans-atlantic-region-under-stratospheric-aerosol-injection/master/file/figures/fig1/fig1.png?1732411845" /> </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.173238705.53228461/v1"> <div class="blog-card__title"> Reduced winter-time Clear Air Turbulence in the trans-Atlantic region under Stratosph... </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="Katie Barnes" width="24" height="24" class="user-profile-pic" src="data:image/jpg;base64,iVBORw0KGgoAAAANSUhEUgAAACAAAAAgCAMAAABEpIrGAAAABGdBTUEAALGP C/xhBQAAACBjSFJNAAB6JgAAgIQAAPoAAACA6AAAdTAAAOpgAAA6mAAAF3Cc ulE8AAABblBMVEWbzl+bzl6azl6azV6bzmCdz2OczmGdz2KczmCWy1iPyEuV y1aOx0qTylOPyEyNx0mQyU6WzFik0m7A4JuWy1eez2ORyVDB4Juy2YSUylTC 4Z2/35my2YOf0GaNx0qazl/C4Z7///+QyE2z2YWQyE7S6bi/35jA4JqKxkX3 +/K43I6HxD+YzFv9/v2m03Gl03Cr1Xj2+vCv2ICSyVG/4Jl9vzDq9d7J5KmI xUKVy1V/wDO12ojB4Z2u133G46Tb7cWZzVyLxkWLxkbj8dOs1nqTylLB4Jzj 8dKXzFj9/vz5/PX7/fi+35f8/frg8M7+/v3e7srZ7MP4+/Sez2X2+/Lo89qM xkeIxEGDwjmv13/U6ruMxki83pR/wDKj0myez2SXzFmRyU+g0Gfa7MO+35jt 9uOHxED+/v6m03Dp9NvF4qKJxUPi8dHW6r2Nx0iZzV2o1HTO57LE4qHD4Z+3 24ui0WuYzFqMx0iUylUAAACsJYfJAAAAAWJLR0R5odzU0AAAAAd0SU1FB+gL FRAXC6ijW50AAAGDSURBVDgR3cEJWxJRFAbgc+a7Z2bw3qAAMyWJzyxJSSsq 201Ls4122my3fdH2fn4PMj6iP8H3le1FpUNFtEO2igBEgh6yGZw5CGKLkZhZ kgLSQ+FyfTmH2Icdki+EsNPHAtkAt6tYKpb7dxcH9gyWhioDe4erEOyTjMJC 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class="blog-card__second-avatar"> <img alt="Anthony Crawford Jones" width="24" height="24" class="user-profile-pic" src="data:image/jpg;base64,iVBORw0KGgoAAAANSUhEUgAAACAAAAAgCAMAAABEpIrGAAAABGdBTUEAALGP C/xhBQAAACBjSFJNAAB6JgAAgIQAAPoAAACA6AAAdTAAAOpgAAA6mAAAF3Cc ulE8AAABO1BMVEXiX1HhXlDiYVTiYVPfUULgVUbiX1LiXlDgVEXfUkLhXU/h Xk/hWUvnfXLlcmbgVkjmdmrhXE7iYlTfTj/ogHX////hWkvhWkziYFLeTDz8 8/LiYFPgWUrdRzf1yMTqjILeSzziYlXeSjv76ef20Mz99/b54t/dRjb76eji Y1XeSTrsmZDkbWHxsavgVkfeSjr76ujog3jvqqPkbF/xtrDYKBXaNyb99/fe SzvdRjXxs6z43Nn0xsL88O/nfHDfT0DfUEDeTD399vX77ez+/fz++/r0w77b OSf2zcn43NjgWEncPy766ObiXlHnfnPxt7DaNCLdRTXcQTH++fncQTDsmZH7 7Ov43drmd2zjZFfxs63sl47ne3DhXU7uo5vtoJfjZlnwr6jpioDdSDjsmI/t nJThX1DiY1YAAABhqqYKAAAAAWJLR0Roy2z0IgAAAAd0SU1FB+gLFRAXJu18 B+gAAAFUSURBVDgR5cEHQhNRFAXQe+cHHnwGhMQnD5gBk1AcFRP60KQqGqqA YkEEUdn/DgiQhLIEOQePDqtwg1V4iAgccYMuAHEfwUxTM1ElREurB3EX0Ra2 dzwBCQHCzvYuD+KWMJt7qvqs2wjCenq1LzLiFpmN+1UHnucphBWK6iMjGoQW Rjo4NDziSMIKL9RHRjQIk5ev9PWoZt8YCSuV1UdGNBB9cVFHxnQ8TkhYqaw+ 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class="blog-card__owner">Katie Barnes</p></a> <p class='blog-card__remaining-text'>and 3 more</p> </div> </div> <time datetime="2024-11-23" class="blog-card__date">November 23, 2024</time> </div> </div> </div> <div class='blog-card__preview-content-container'> <a href="/doi/full/10.22541/essoar.173238705.53228461/v1"> <div class='blog-card__preview-content'> Clear air turbulence (CAT) is a safety threat within the aviation sector and is projected to worsen under global warming. Stratospheric aerosol injection (SAI) is a climate intervention strategy that aims to ameliorate climate change by artificially cooling Earth. Climate model simulations have found a side-effect of SAI would be a strengthening of the positive phase of the North Atlantic Oscillation (NAO). This links to a stronger North Atlantic jet stream and suggests enhanced CAT in the region. Here, we analyse simulations from the UKESM1 climate model to evaluate the impact of a realistic SAI application on winter-time trans-Atlantic CAT. We find a 23 % decrease in severe CAT frequency under SAI when compared to a baseline high-end global warming scenario. Our results indicate that the amelioration of global warming under SAI has a more dominant impact on CAT over the North Atlantic than residual impacts to the NAO. </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.173204199.97113482/v1"> <div class="blog-card__title"> Role of forest biomass change in shaping future land use and land cover 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="Meng Luo" width="24" height="24" class="user-profile-pic" src="data:image/jpg;base64,iVBORw0KGgoAAAANSUhEUgAAACAAAAAgCAMAAABEpIrGAAAABGdBTUEAALGP C/xhBQAAACBjSFJNAAB6JgAAgIQAAPoAAACA6AAAdTAAAOpgAAA6mAAAF3Cc ulE8AAABLFBMVEX+2hD+2g/+2Q/+2hL+2hX+2hT+2hb+2hH92AX91QD91gD9 2Q/92Q7+2hP92Ab+3Sf+5mD+40792Af92Q392Qn+5FD+5l/+3in91wD+3Sj+ 52r+3Sb+6XP////+3zT+4kT+6nj90AD+6G7+6Gr+8J791AD+8q7+6W/+52b+ 6G3+++X91wL92Qz92Aj+98/+6Gz+52f+5Vf+6XT+6XH+6Gv+2xv+/vr++Nf+ ++n++dr+4kn+52j+3zX+6n391wP91wH+5Vn+6G/+5Vz+52n+2xr+/O/++d7+ +dn9zwD+5Vv90gD92AL92Qv+52X+6Gn+6nr+2xj+3zD+4Dj90wD+6XL+6nf+ 4UD92AP+7Yv+5V3+5FH+3zL+6nv+6Xb+3B392AT92An+2xf+2xYAAACEUdKk AAAAAWJLR0RjXL4tqgAAAAd0SU1FB+gLFRAXDUHA/qgAAAGISURBVDgR3cGL YgtRFAXQfc7N3MmZ20RVEWSrmzEIrUkoSqJUvR8lXq1ntP//EZLRVPmEroUj RQQVEQCC/4lOYEInRFUF/1JXS6CAIqk5dd4pDhNN65YFqGIus3qjbs1UBX9p 2jw2f3xhDjixePLU6daZs+eaqeKABG9t8nzWSLIl8kJss2M+CGYkeMvJi0Ut KS6Rl2POK+aDYEaCty6v8try4gqvsx1L9swHwYwEbx122c8s5w3ejCV75oNg RoK3Vd66faewtbv3WMaSPfNBMCPB24DD+1z3nF9iGUv2zAdV7JPgrcf+Az7c oD1iGUtu2uNGAsUfErz1OIhPnq49e56zjKt88fJVK3sNRUWCtzfM4xbZj1vM Y86374aj941lKKYkeOty44MjF4oOP8ZPrHxuJSqYUrc92hnVW1++tpqjnW/Z 8Psgzzd//FxJFRXRdFyM0zTLXDouthvrhU39SlWwT92uU60lqm7XBbfnJ/ZS xQHRoKITokFVQ0VxmAAQASAApIIj5DdoayrCJRPDNwAAACV0RVh0ZGF0ZTpj cmVhdGUAMjAyNC0xMS0yMVQxNjoyMzoxMyswMDowMOsfadAAAAAldEVYdGRh dGU6bW9kaWZ5ADIwMjQtMTEtMjFUMTY6MjM6MTMrMDA6MDCaQtFsAAAAIHRF WHRzb2Z0d2FyZQBodHRwczovL2ltYWdlbWFnaWNrLm9yZ7zPHZ0AAAAYdEVY dFRodW1iOjpEb2N1bWVudDo6UGFnZXMAMaf/uy8AAAAYdEVYdFRodW1iOjpJ bWFnZTo6SGVpZ2h0ADYwMHrevbUAAAAXdEVYdFRodW1iOjpJbWFnZTo6V2lk dGgANjAw6S/t6AAAABl0RVh0VGh1bWI6Ok1pbWV0eXBlAGltYWdlL3BuZz+y Vk4AAAAXdEVYdFRodW1iOjpNVGltZQAxNzMyMjA2MTkzLc4D+QAAABN0RVh0 VGh1bWI6OlNpemUAMTE3OTlCQh68H1sAAAA8dEVYdFRodW1iOjpVUkkAZmls ZTovL3RtcC9sZXR0ZXJfYXZhdGFycy8yL01MLzI1NF8yMThfMTYvNjAwLnBu Z7OwW6kAAAAASUVORK5CYII= " /> </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/596150"><p class="blog-card__owner">Meng Luo</p></a> <p class='blog-card__remaining-text'>and 9 more</p> </div> </div> <time datetime="2024-11-19" class="blog-card__date">November 19, 2024</time> </div> </div> </div> <div class='blog-card__preview-content-container'> <a href="/doi/full/10.22541/essoar.173204199.97113482/v1"> <div class='blog-card__preview-content'> Forest biomass changes influence the forest area required to meet the demand for timber and carbon storage, and thus land use and land cover change (LULCC). The worldwide impacts of global change (e.g., climate change, CO2 fertilization, nitrogen deposition) on forest biomass have been widely recognized and examined, yet are usually ignored by existing LULCC projections. This study explores the role of forest biomass change driven by global change in future global LULCC projections and investigates the underlying drivers. We incorporated the global change impacts on forest biomass from a land surface model driven by the projections from two Earth system models (ESMs) under three Shared Socioeconomic Pathways (SSP) scenarios (SSP126, SSP370, and SSP585) into an integrated assessment model, the Global Change Analysis Model. Considering forest biomass change decreases the projected expansion of managed forests and managed pastures, reduces the loss of unmanaged pastures and unmanaged forests, and provides more areas for cropland. The relative decrease in managed forest is-4.0%,-21.7% and-31.9%, respectively under SSP126, SSP370, and SSP585 in 2100 if forest biomass change is considered. CO2 fertilization is the dominant driver of increasing forest biomass and thus LULCC, compared to the change in climate and nitrogen deposition under SSP585. Using climate forcing data from two ESMs leads to similar impacts of forest biomass change on LULCC in terms of sign and trend but different magnitudes. This study highlights the large impact of forest biomass change on shaping future LULCC dynamics and the critical role of CO2 fertilization. </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.173204180.08904483/v1"> <div class="blog-card__title"> Empirical Quantification of Topobathymetric LiDAR System Resolution using Modulation... </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="Kevin W. Sacca" width="24" height="24" class="user-profile-pic" src="https://d197for5662m48.cloudfront.net/images/user/858442/profile_image/thumbnail-519b82649341ddbeb744e387b879e155.jpeg" /> </div> <div class="blog-card__second-avatar"> <img alt="Jeffrey Thayer" width="24" height="24" class="user-profile-pic" src="data:image/jpg;base64,iVBORw0KGgoAAAANSUhEUgAAACAAAAAgCAMAAABEpIrGAAAABGdBTUEAALGP C/xhBQAAACBjSFJNAAB6JgAAgIQAAPoAAACA6AAAdTAAAOpgAAA6mAAAF3Cc ulE8AAABFFBMVEVSvIlRvIlRvIhRu4hVvYtTvIpWvYxOuoZCtX5KuYM7s3k6 snhJuIJTvIl6y6RewJGa2LqR1LSS1bWT1bWS1LSQ1LOd2bxqxZlJuINBtX15 y6T///+4485Zvo2f2r5BtX50yaC65M85snhzyZ9qxZpZvo7n9u9mxJdlw5Zx yJ5av45NuoW95dI1sHVIuIJFt4AtrXDm9e4+tHs/tHxEtn9MuYV1yaA4sndW vYvq9vBQu4c3sXfp9vBLuYRMuoV1yaFHt4FYvo1Dtn+85dFCtn6Czqr2+/l8 zKZ4yqJyyJ9AtX3O7N2G0Kw+tHw8s3rn9e9UvIo6s3m24s3K6to9s3ry+vab 2Lt8zKWH0K1AtXxQu4gAAAByjqmDAAAAAWJLR0RbdLyVNAAAAAd0SU1FB+gL FRAXGVsaKtUAAAEoSURBVDgR3cGHUsJAFAXQu7mbjQTX3uKzYC/BiooCscRe wF7//0NkhBkW9Qs4B51JeQ34D9vgD0L7ME0+8RsRdGWCsCHbbUm0IQLd0+v3 9fcPDA4Nj4yO+YRLUUfjMjEpTVOhoQeHop7Oyczs3PzCoiwtr6zGIFyKOspJ fm19Y3NLtgs7uyBcJHW0J/niwn7hQIKSsYSLdTrKSb5sbFiR5NDSg4tWWx0d Sb5sbFiRJLaEg8R68fgkzclp2diwIklsiRZFfXZ+cRnOXslp0diwIklsiRZF nV7LQXJzK3dVbWv3ksSWcJAPj09S91wF/JdXCWJLuIhS7brv7b0WgMi8fwQl EG0IP81mIx8EkX5+gfiF0MZoEAC1BvEHf6COdfiH8jyFBoVO8w2tTR9GHWtY tQAAACV0RVh0ZGF0ZTpjcmVhdGUAMjAyNC0xMS0yMVQxNjoyMzoxMiswMDow ME1oYmQAAAAldEVYdGRhdGU6bW9kaWZ5ADIwMjQtMTEtMjFUMTY6MjM6MTIr MDA6MDA8NdrYAAAAIHRFWHRzb2Z0d2FyZQBodHRwczovL2ltYWdlbWFnaWNr Lm9yZ7zPHZ0AAAAYdEVYdFRodW1iOjpEb2N1bWVudDo6UGFnZXMAMaf/uy8A AAAYdEVYdFRodW1iOjpJbWFnZTo6SGVpZ2h0ADYwMHrevbUAAAAXdEVYdFRo dW1iOjpJbWFnZTo6V2lkdGgANjAw6S/t6AAAABl0RVh0VGh1bWI6Ok1pbWV0 eXBlAGltYWdlL3BuZz+yVk4AAAAXdEVYdFRodW1iOjpNVGltZQAxNzMyMjA2 MTkyWskzbwAAABJ0RVh0VGh1bWI6OlNpemUAODA4NUJCNVpygQAAADx0RVh0 VGh1bWI6OlVSSQBmaWxlOi8vdG1wL2xldHRlcl9hdmF0YXJzLzIvSlQvODJf MTg4XzEzNy82MDAucG5nQc7OugAAAABJRU5ErkJggg== " /> </div> </div> <div> <div class="blog-card__authors-text"> <div class="blog-card-author-list" style="width: 100%;"> <a href="/users/858442"><p class="blog-card__owner">Kevin W. Sacca</p></a> <p class='blog-card__remaining-text'>and 1 more</p> </div> </div> <time datetime="2024-11-19" class="blog-card__date">November 19, 2024</time> </div> </div> </div> <div class='blog-card__preview-content-container'> <a href="/doi/full/10.22541/essoar.173204180.08904483/v1"> <div class='blog-card__preview-content'> Topobathymetric scanning LiDAR deployed on unmanned aerial systems (UAS) is a powerful tool for high-resolution mapping of the dynamic interface between topography and bathymetry. However, standardized methods for empirical resolution validation have not been widely adopted across LiDAR applications. While theoretical models of idealized LiDAR sampling resolution can be used to describe topographical resolution, misrepresented or unknown behaviors in an instrument, platform, or environment can degrade expected performance or introduce georeferencing inaccuracies. Furthermore, bathymetric resolution is strongly dependent on water surface and column conditions. Thus, only empirical methods for evaluating resolution will provide reliable estimates for both topographic and bathymetric surveys. Presented is an extension of standard modulation transfer function (MTF) methods used by passive imaging systems applied to high-resolution scanning LiDAR. Compact retroreflectors characterized as point and line sources are employed to empirically assess effective LiDAR system resolution through MTF analysis in topographic and bathymetric scenes. These targets enable MTF analyses using range-height measurements without reliance on intensity data, promoting widespread applicability among LiDAR systems. Empirical MTFs calculated using these targets are compared against theory-derived counterparts as empirical measurements elucidate influences by elements that are unknown or difficult to model. Simulated point cloud data were incorporated into theoretical MTF descriptions to better represent empirically-derived topographic MTFs, revealing mirror pointing uncertainties in the across-track axis. Similarly, theoretical bathymetric MTFs augmented with simulated, subaqueous data enabled water surface slope estimation using empirical measurements of submerged retroreflector targets, where rough water surfaces strongly influenced beam steering and the corresponding point spread MTFs. </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.173238717.76577266/v1"> <div class="blog-card__title"> RAIN: Reinforcement Algorithms for Improving Numerical Weather and Climate Models </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="Pritthijit Nath" width="24" height="24" class="user-profile-pic" src="data:image/jpg;base64,iVBORw0KGgoAAAANSUhEUgAAACAAAAAgCAMAAABEpIrGAAAABGdBTUEAALGP 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class="blog-card-author-list" style="width: 100%;"> <a href="/users/858299"><p class="blog-card__owner">Pritthijit Nath</p></a> <p class='blog-card__remaining-text'>and 3 more</p> </div> </div> <time datetime="2024-11-23" class="blog-card__date">November 23, 2024</time> </div> </div> </div> <div class='blog-card__preview-content-container'> <a href="/doi/full/10.22541/essoar.173238717.76577266/v1"> <div class='blog-card__preview-content'> This study explores integrating reinforcement learning (RL) with idealised climate models to address key parameterisation challenges in climate science. Current climate models rely on complex mathematical parameterisations to represent sub-grid scale processes, which can introduce substantial uncertainties. RL offers capabilities to enhance these parameterisation schemes, including direct interaction, handling sparse or delayed feedback, continuous online learning, and long-term optimisation. We evaluate the performance of eight RL algorithms on two idealised environments: one for temperature bias correction, another for radiative-convective equilibrium (RCE) imitating real-world computational constraints. Results show different RL approaches excel in different climate scenarios with exploration algorithms performing better in bias correction, while exploitation algorithms proving more effective for RCE. These findings support the potential of RL-based parameterisation schemes to be integrated into global climate models, improving accuracy and efficiency in capturing complex climate dynamics. Overall, this work represents an important first step towards leveraging RL to enhance climate model accuracy, critical for improving climate understanding and predictions. Code accessible at https://github.com/p3jitnath/climate-rl. </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/587471/articles/1241926-detecting-millimetric-slow-slip-events-along-the-north-anatolian-fault-with-gnss?commit=e862ec6b7882367d7c1ef93656201283a8afbe92"> <div class="blog-card__title"> Detecting millimetric slow slip events along the North Anatolian Fault with GNSS </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"> </div> </div> <div> <div class="blog-card__authors-text"> <div class="blog-card-author-list" style="width: 100%;"> <span><p class="blog-card__owner">Alpay Özdemir</p></span> <p class='blog-card__remaining-text'>and 7 more</p> </div> </div> <time datetime="2024-11-17" class="blog-card__date">November 17, 2024</time> </div> </div> </div> <div class='blog-card__preview-content-container'> <a href="/users/587471/articles/1241926-detecting-millimetric-slow-slip-events-along-the-north-anatolian-fault-with-gnss?commit=e862ec6b7882367d7c1ef93656201283a8afbe92"> <div class='blog-card__preview-content'> • We propose a strategy combining geodetic reference frame definition and time series analysis to extract slow slip events from GNSS data. • We detect and characterize a shallow, 10-km-long, three-week-long SSE along the central section of the North Anatolian Fault. • We show that persistent aseismic slip and SSEs are spatially complementary and interact at shallow depth. </div> </a> </div> </div> </div> </div> <div role="navigation" aria-label="Pagination" class="pagination"><span class="previous_page disabled">← Previous</span> <em class="current" aria-label="Page 1" aria-current="page">1</em> <a rel="next" 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 aria-label="Page 6" href="/inst/20904?page=6">6</a> <a aria-label="Page 7" href="/inst/20904?page=7">7</a> <a aria-label="Page 8" href="/inst/20904?page=8">8</a> <a aria-label="Page 9" href="/inst/20904?page=9">9</a> <span class="gap">…</span> <a aria-label="Page 890" href="/inst/20904?page=890">890</a> <a aria-label="Page 891" href="/inst/20904?page=891">891</a> <a class="next_page" rel="next" href="/inst/20904?page=2">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>