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Antarctic Circumpolar Current - Wikipedia

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id="vector-page-titlebar-toc" class="vector-dropdown vector-page-titlebar-toc vector-button-flush-left" > <input type="checkbox" id="vector-page-titlebar-toc-checkbox" role="button" aria-haspopup="true" data-event-name="ui.dropdown-vector-page-titlebar-toc" class="vector-dropdown-checkbox " aria-label="Toggle the table of contents" > <label id="vector-page-titlebar-toc-label" for="vector-page-titlebar-toc-checkbox" class="vector-dropdown-label cdx-button cdx-button--fake-button cdx-button--fake-button--enabled cdx-button--weight-quiet cdx-button--icon-only " aria-hidden="true" ><span class="vector-icon mw-ui-icon-listBullet mw-ui-icon-wikimedia-listBullet"></span> <span class="vector-dropdown-label-text">Toggle the table of contents</span> </label> <div class="vector-dropdown-content"> <div id="vector-page-titlebar-toc-unpinned-container" class="vector-unpinned-container"> </div> </div> </div> </nav> <h1 id="firstHeading" class="firstHeading mw-first-heading"><span class="mw-page-title-main">Antarctic Circumpolar Current</span></h1> <div id="p-lang-btn" class="vector-dropdown mw-portlet mw-portlet-lang" > <input type="checkbox" id="p-lang-btn-checkbox" role="button" aria-haspopup="true" data-event-name="ui.dropdown-p-lang-btn" class="vector-dropdown-checkbox mw-interlanguage-selector" aria-label="Go to an article in another language. Available in 45 languages" > <label id="p-lang-btn-label" for="p-lang-btn-checkbox" class="vector-dropdown-label cdx-button cdx-button--fake-button cdx-button--fake-button--enabled cdx-button--weight-quiet cdx-button--action-progressive mw-portlet-lang-heading-45" aria-hidden="true" ><span class="vector-icon mw-ui-icon-language-progressive mw-ui-icon-wikimedia-language-progressive"></span> <span class="vector-dropdown-label-text">45 languages</span> </label> <div class="vector-dropdown-content"> <div class="vector-menu-content"> <ul class="vector-menu-content-list"> <li class="interlanguage-link interwiki-ar mw-list-item"><a href="https://ar.wikipedia.org/wiki/%D8%A7%D9%84%D8%AA%D9%8A%D8%A7%D8%B1_%D8%A7%D9%84%D9%82%D8%B7%D8%A8%D9%8A_%D9%84%D9%84%D9%82%D8%B7%D8%A8_%D8%A7%D9%84%D8%AC%D9%86%D9%88%D8%A8%D9%8A" title="التيار القطبي للقطب الجنوبي – Arabic" lang="ar" hreflang="ar" data-title="التيار القطبي للقطب الجنوبي" data-language-autonym="العربية" data-language-local-name="Arabic" class="interlanguage-link-target"><span>العربية</span></a></li><li class="interlanguage-link interwiki-az mw-list-item"><a href="https://az.wikipedia.org/wiki/Q%C9%99rb_k%C3%BCl%C9%99kl%C9%99ri_c%C9%99r%C9%99yan%C4%B1" title="Qərb küləkləri cərəyanı – Azerbaijani" lang="az" hreflang="az" data-title="Qərb küləkləri cərəyanı" data-language-autonym="Azərbaycanca" data-language-local-name="Azerbaijani" class="interlanguage-link-target"><span>Azərbaycanca</span></a></li><li class="interlanguage-link interwiki-be mw-list-item"><a href="https://be.wikipedia.org/wiki/%D0%90%D0%BD%D1%82%D0%B0%D1%80%D0%BA%D1%82%D1%8B%D1%87%D0%BD%D0%B0%D0%B5_%D1%86%D1%8B%D1%80%D0%BA%D1%83%D0%BC%D0%BF%D0%B0%D0%BB%D1%8F%D1%80%D0%BD%D0%B0%D0%B5_%D1%86%D1%8F%D1%87%D1%8D%D0%BD%D0%BD%D0%B5" title="Антарктычнае цыркумпалярнае цячэнне – Belarusian" lang="be" hreflang="be" data-title="Антарктычнае цыркумпалярнае цячэнне" data-language-autonym="Беларуская" data-language-local-name="Belarusian" class="interlanguage-link-target"><span>Беларуская</span></a></li><li class="interlanguage-link interwiki-be-x-old mw-list-item"><a href="https://be-tarask.wikipedia.org/wiki/%D0%90%D0%BD%D1%82%D0%B0%D1%80%D0%BA%D1%82%D1%8B%D1%87%D0%BD%D0%B0%D1%8F_%D1%86%D1%8B%D1%80%D0%BA%D1%83%D0%BC%D0%BF%D0%B0%D0%BB%D1%8F%D1%80%D0%BD%D0%B0%D1%8F_%D0%BF%D0%BB%D1%8B%D0%BD%D1%8C" title="Антарктычная цыркумпалярная плынь – Belarusian (Taraškievica orthography)" lang="be-tarask" hreflang="be-tarask" data-title="Антарктычная цыркумпалярная плынь" data-language-autonym="Беларуская (тарашкевіца)" data-language-local-name="Belarusian (Taraškievica orthography)" class="interlanguage-link-target"><span>Беларуская (тарашкевіца)</span></a></li><li class="interlanguage-link interwiki-bg mw-list-item"><a href="https://bg.wikipedia.org/wiki/%D0%97%D0%B0%D0%BF%D0%B0%D0%B4%D0%BD%D0%BE%D0%B2%D0%B5%D1%82%D1%80%D0%BE%D0%B2%D0%BE_%D1%82%D0%B5%D1%87%D0%B5%D0%BD%D0%B8%D0%B5" title="Западноветрово течение – Bulgarian" lang="bg" hreflang="bg" data-title="Западноветрово течение" data-language-autonym="Български" data-language-local-name="Bulgarian" class="interlanguage-link-target"><span>Български</span></a></li><li class="interlanguage-link interwiki-ca mw-list-item"><a href="https://ca.wikipedia.org/wiki/Corrent_circumpolar_ant%C3%A0rtic" title="Corrent circumpolar antàrtic – Catalan" lang="ca" hreflang="ca" data-title="Corrent circumpolar antàrtic" data-language-autonym="Català" data-language-local-name="Catalan" class="interlanguage-link-target"><span>Català</span></a></li><li class="interlanguage-link interwiki-cs mw-list-item"><a href="https://cs.wikipedia.org/wiki/Z%C3%A1padn%C3%AD_p%C5%99%C3%ADhon" title="Západní příhon – Czech" lang="cs" hreflang="cs" data-title="Západní příhon" data-language-autonym="Čeština" data-language-local-name="Czech" class="interlanguage-link-target"><span>Čeština</span></a></li><li class="interlanguage-link interwiki-de mw-list-item"><a href="https://de.wikipedia.org/wiki/Antarktischer_Zirkumpolarstrom" title="Antarktischer Zirkumpolarstrom – German" lang="de" hreflang="de" data-title="Antarktischer Zirkumpolarstrom" data-language-autonym="Deutsch" data-language-local-name="German" class="interlanguage-link-target"><span>Deutsch</span></a></li><li class="interlanguage-link interwiki-et mw-list-item"><a href="https://et.wikipedia.org/wiki/L%C3%A4%C3%A4netuulte_hoovus" title="Läänetuulte hoovus – Estonian" lang="et" hreflang="et" data-title="Läänetuulte hoovus" data-language-autonym="Eesti" data-language-local-name="Estonian" class="interlanguage-link-target"><span>Eesti</span></a></li><li class="interlanguage-link interwiki-es mw-list-item"><a href="https://es.wikipedia.org/wiki/Corriente_circumpolar_ant%C3%A1rtica" title="Corriente circumpolar antártica – Spanish" lang="es" hreflang="es" data-title="Corriente circumpolar antártica" data-language-autonym="Español" data-language-local-name="Spanish" class="interlanguage-link-target"><span>Español</span></a></li><li class="interlanguage-link interwiki-eo mw-list-item"><a href="https://eo.wikipedia.org/wiki/Antarkta_%C4%88irka%C5%ADpolusa_Marfluo" title="Antarkta Ĉirkaŭpolusa Marfluo – Esperanto" lang="eo" hreflang="eo" data-title="Antarkta Ĉirkaŭpolusa Marfluo" data-language-autonym="Esperanto" data-language-local-name="Esperanto" class="interlanguage-link-target"><span>Esperanto</span></a></li><li class="interlanguage-link interwiki-eu mw-list-item"><a href="https://eu.wikipedia.org/wiki/Itsaslaster_Zirkunpolar_Antartikoa" title="Itsaslaster Zirkunpolar Antartikoa – Basque" lang="eu" hreflang="eu" data-title="Itsaslaster Zirkunpolar Antartikoa" data-language-autonym="Euskara" data-language-local-name="Basque" class="interlanguage-link-target"><span>Euskara</span></a></li><li class="interlanguage-link interwiki-fa mw-list-item"><a href="https://fa.wikipedia.org/wiki/%D8%AC%D8%B1%DB%8C%D8%A7%D9%86_%D9%BE%DB%8C%D8%B1%D8%A7%D9%82%D8%B7%D8%A8%DB%8C_%D8%AC%D9%86%D9%88%D8%A8%DA%AF%D8%A7%D9%86" title="جریان پیراقطبی جنوبگان – Persian" lang="fa" hreflang="fa" data-title="جریان پیراقطبی جنوبگان" data-language-autonym="فارسی" data-language-local-name="Persian" class="interlanguage-link-target"><span>فارسی</span></a></li><li class="interlanguage-link interwiki-fr mw-list-item"><a href="https://fr.wikipedia.org/wiki/Courant_circumpolaire_antarctique" title="Courant circumpolaire antarctique – French" lang="fr" hreflang="fr" data-title="Courant circumpolaire antarctique" data-language-autonym="Français" data-language-local-name="French" class="interlanguage-link-target"><span>Français</span></a></li><li class="interlanguage-link interwiki-ko mw-list-item"><a href="https://ko.wikipedia.org/wiki/%EB%82%A8%EA%B7%B9%EC%88%9C%ED%99%98%EB%A5%98" title="남극순환류 – Korean" lang="ko" hreflang="ko" data-title="남극순환류" data-language-autonym="한국어" data-language-local-name="Korean" class="interlanguage-link-target"><span>한국어</span></a></li><li class="interlanguage-link interwiki-hi mw-list-item"><a href="https://hi.wikipedia.org/wiki/%E0%A4%85%E0%A4%A3%E0%A5%8D%E0%A4%9F%E0%A4%BE%E0%A4%B0%E0%A5%8D%E0%A4%95%E0%A4%9F%E0%A4%BF%E0%A4%95%E0%A4%BE_%E0%A4%AA%E0%A5%8D%E0%A4%B0%E0%A4%B5%E0%A4%BE%E0%A4%B9" title="अण्टार्कटिका प्रवाह – Hindi" lang="hi" hreflang="hi" data-title="अण्टार्कटिका प्रवाह" data-language-autonym="हिन्दी" data-language-local-name="Hindi" class="interlanguage-link-target"><span>हिन्दी</span></a></li><li class="interlanguage-link interwiki-hr mw-list-item"><a href="https://hr.wikipedia.org/wiki/Antarkti%C4%8Dka_cirkumpolarna_struja" title="Antarktička cirkumpolarna struja – Croatian" lang="hr" hreflang="hr" data-title="Antarktička cirkumpolarna struja" data-language-autonym="Hrvatski" data-language-local-name="Croatian" class="interlanguage-link-target"><span>Hrvatski</span></a></li><li class="interlanguage-link interwiki-id mw-list-item"><a href="https://id.wikipedia.org/wiki/Arus_Lingkar_Antarktika" title="Arus Lingkar Antarktika – Indonesian" lang="id" hreflang="id" data-title="Arus Lingkar Antarktika" data-language-autonym="Bahasa Indonesia" data-language-local-name="Indonesian" class="interlanguage-link-target"><span>Bahasa Indonesia</span></a></li><li class="interlanguage-link interwiki-it mw-list-item"><a href="https://it.wikipedia.org/wiki/Corrente_circumpolare_antartica" title="Corrente circumpolare antartica – Italian" lang="it" hreflang="it" data-title="Corrente circumpolare antartica" data-language-autonym="Italiano" data-language-local-name="Italian" class="interlanguage-link-target"><span>Italiano</span></a></li><li class="interlanguage-link interwiki-kk mw-list-item"><a href="https://kk.wikipedia.org/wiki/%D0%91%D0%B0%D1%82%D1%8B%D1%81_%D0%96%D0%B5%D0%BB%D0%B4%D0%B5%D1%80_%D0%B0%D2%93%D1%8B%D1%81%D1%8B" title="Батыс Желдер ағысы – Kazakh" lang="kk" hreflang="kk" data-title="Батыс Желдер ағысы" data-language-autonym="Қазақша" data-language-local-name="Kazakh" class="interlanguage-link-target"><span>Қазақша</span></a></li><li class="interlanguage-link interwiki-ky mw-list-item"><a href="https://ky.wikipedia.org/wiki/%D0%91%D0%B0%D1%82%D1%8B%D1%88_%D1%88%D0%B0%D0%BC%D0%B0%D0%BB_%D0%B0%D0%B3%D1%8B%D0%BC%D1%8B" title="Батыш шамал агымы – Kyrgyz" lang="ky" hreflang="ky" data-title="Батыш шамал агымы" data-language-autonym="Кыргызча" data-language-local-name="Kyrgyz" class="interlanguage-link-target"><span>Кыргызча</span></a></li><li class="interlanguage-link interwiki-la mw-list-item"><a href="https://la.wikipedia.org/wiki/Flumen_Circumpolare_Antarcticum" title="Flumen Circumpolare Antarcticum – Latin" lang="la" hreflang="la" data-title="Flumen Circumpolare Antarcticum" data-language-autonym="Latina" data-language-local-name="Latin" class="interlanguage-link-target"><span>Latina</span></a></li><li class="interlanguage-link interwiki-lv mw-list-item"><a href="https://lv.wikipedia.org/wiki/Antarktikas_cirkumpol%C4%81r%C4%81_straume" title="Antarktikas cirkumpolārā straume – Latvian" lang="lv" hreflang="lv" data-title="Antarktikas cirkumpolārā straume" data-language-autonym="Latviešu" data-language-local-name="Latvian" class="interlanguage-link-target"><span>Latviešu</span></a></li><li class="interlanguage-link interwiki-lt mw-list-item"><a href="https://lt.wikipedia.org/wiki/Vakar%C5%B3_V%C4%97j%C5%B3_srov%C4%97" title="Vakarų Vėjų srovė – Lithuanian" lang="lt" hreflang="lt" data-title="Vakarų Vėjų srovė" data-language-autonym="Lietuvių" data-language-local-name="Lithuanian" class="interlanguage-link-target"><span>Lietuvių</span></a></li><li class="interlanguage-link interwiki-hu mw-list-item"><a href="https://hu.wikipedia.org/wiki/Nyugati-Sz%C3%A9l-%C3%A1raml%C3%A1s" title="Nyugati-Szél-áramlás – Hungarian" lang="hu" hreflang="hu" data-title="Nyugati-Szél-áramlás" data-language-autonym="Magyar" data-language-local-name="Hungarian" class="interlanguage-link-target"><span>Magyar</span></a></li><li class="interlanguage-link interwiki-mr mw-list-item"><a href="https://mr.wikipedia.org/wiki/%E0%A4%85%E0%A4%81%E0%A4%9F%E0%A4%BE%E0%A4%B0%E0%A5%8D%E0%A4%95%E0%A5%8D%E0%A4%9F%E0%A4%BF%E0%A4%95%E0%A4%BE_%E0%A4%A7%E0%A5%8D%E0%A4%B0%E0%A5%81%E0%A4%B5%E0%A4%AA%E0%A5%8D%E0%A4%B0%E0%A4%A6%E0%A4%95%E0%A5%8D%E0%A4%B7%E0%A4%BF%E0%A4%A3%E0%A4%BE_%E0%A4%AA%E0%A5%8D%E0%A4%B0%E0%A4%B5%E0%A4%BE%E0%A4%B9" title="अँटार्क्टिका ध्रुवप्रदक्षिणा प्रवाह – Marathi" lang="mr" hreflang="mr" data-title="अँटार्क्टिका ध्रुवप्रदक्षिणा प्रवाह" data-language-autonym="मराठी" data-language-local-name="Marathi" class="interlanguage-link-target"><span>मराठी</span></a></li><li class="interlanguage-link interwiki-ms mw-list-item"><a href="https://ms.wikipedia.org/wiki/Arus_Lilitan_Antartika" title="Arus Lilitan Antartika – Malay" lang="ms" hreflang="ms" data-title="Arus Lilitan Antartika" data-language-autonym="Bahasa Melayu" data-language-local-name="Malay" class="interlanguage-link-target"><span>Bahasa Melayu</span></a></li><li class="interlanguage-link interwiki-nl mw-list-item"><a href="https://nl.wikipedia.org/wiki/Westenwinddrift" title="Westenwinddrift – Dutch" lang="nl" hreflang="nl" data-title="Westenwinddrift" data-language-autonym="Nederlands" data-language-local-name="Dutch" class="interlanguage-link-target"><span>Nederlands</span></a></li><li class="interlanguage-link interwiki-new mw-list-item"><a href="https://new.wikipedia.org/wiki/%E0%A4%85%E0%A4%A3%E0%A5%8D%E0%A4%9F%E0%A4%BE%E0%A4%B0%E0%A5%8D%E0%A4%95%E0%A4%9F%E0%A4%BF%E0%A4%95%E0%A4%BE_%E0%A4%AA%E0%A5%8D%E0%A4%B0%E0%A4%B5%E0%A4%BE%E0%A4%B9" title="अण्टार्कटिका प्रवाह – Newari" lang="new" hreflang="new" data-title="अण्टार्कटिका प्रवाह" data-language-autonym="नेपाल भाषा" data-language-local-name="Newari" class="interlanguage-link-target"><span>नेपाल भाषा</span></a></li><li class="interlanguage-link interwiki-ja mw-list-item"><a href="https://ja.wikipedia.org/wiki/%E5%8D%97%E6%A5%B5%E7%92%B0%E6%B5%81" title="南極環流 – Japanese" lang="ja" hreflang="ja" data-title="南極環流" data-language-autonym="日本語" data-language-local-name="Japanese" class="interlanguage-link-target"><span>日本語</span></a></li><li class="interlanguage-link interwiki-no mw-list-item"><a href="https://no.wikipedia.org/wiki/S%C3%B8rishavsstr%C3%B8mmen" title="Sørishavsstrømmen – Norwegian Bokmål" lang="nb" hreflang="nb" data-title="Sørishavsstrømmen" data-language-autonym="Norsk bokmål" data-language-local-name="Norwegian Bokmål" class="interlanguage-link-target"><span>Norsk bokmål</span></a></li><li class="interlanguage-link interwiki-nn mw-list-item"><a href="https://nn.wikipedia.org/wiki/S%C3%B8rishavsstraumen" title="Sørishavsstraumen – Norwegian Nynorsk" lang="nn" hreflang="nn" data-title="Sørishavsstraumen" data-language-autonym="Norsk nynorsk" data-language-local-name="Norwegian Nynorsk" class="interlanguage-link-target"><span>Norsk nynorsk</span></a></li><li class="interlanguage-link interwiki-pl mw-list-item"><a href="https://pl.wikipedia.org/wiki/Pr%C4%85d_Wiatr%C3%B3w_Zachodnich" title="Prąd Wiatrów Zachodnich – Polish" lang="pl" hreflang="pl" data-title="Prąd Wiatrów Zachodnich" data-language-autonym="Polski" data-language-local-name="Polish" class="interlanguage-link-target"><span>Polski</span></a></li><li class="interlanguage-link interwiki-pt mw-list-item"><a href="https://pt.wikipedia.org/wiki/Corrente_Circumpolar_Ant%C3%A1rtica" title="Corrente Circumpolar Antártica – Portuguese" lang="pt" hreflang="pt" data-title="Corrente Circumpolar Antártica" data-language-autonym="Português" data-language-local-name="Portuguese" class="interlanguage-link-target"><span>Português</span></a></li><li class="interlanguage-link interwiki-ro mw-list-item"><a href="https://ro.wikipedia.org/wiki/Curentul_Antarctic_de_Vest" title="Curentul Antarctic de Vest – Romanian" lang="ro" hreflang="ro" data-title="Curentul Antarctic de Vest" data-language-autonym="Română" data-language-local-name="Romanian" class="interlanguage-link-target"><span>Română</span></a></li><li class="interlanguage-link interwiki-ru mw-list-item"><a href="https://ru.wikipedia.org/wiki/%D0%90%D0%BD%D1%82%D0%B0%D1%80%D0%BA%D1%82%D0%B8%D1%87%D0%B5%D1%81%D0%BA%D0%BE%D0%B5_%D1%86%D0%B8%D1%80%D0%BA%D1%83%D0%BC%D0%BF%D0%BE%D0%BB%D1%8F%D1%80%D0%BD%D0%BE%D0%B5_%D1%82%D0%B5%D1%87%D0%B5%D0%BD%D0%B8%D0%B5" title="Антарктическое циркумполярное течение – Russian" lang="ru" hreflang="ru" data-title="Антарктическое циркумполярное течение" data-language-autonym="Русский" data-language-local-name="Russian" class="interlanguage-link-target"><span>Русский</span></a></li><li class="interlanguage-link interwiki-sk mw-list-item"><a href="https://sk.wikipedia.org/wiki/Z%C3%A1padn%C3%BD_pr%C3%ADhon" title="Západný príhon – Slovak" lang="sk" hreflang="sk" data-title="Západný príhon" data-language-autonym="Slovenčina" data-language-local-name="Slovak" 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searchaux" style="display:none">Ocean current that flows clockwise from west to east around Antarctica</div> <p class="mw-empty-elt"> </p> <figure typeof="mw:File/Thumb"><a href="/wiki/File:Antarctic_Circumpolar_Current.png" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/7/75/Antarctic_Circumpolar_Current.png/320px-Antarctic_Circumpolar_Current.png" decoding="async" width="320" height="292" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/7/75/Antarctic_Circumpolar_Current.png 1.5x" data-file-width="429" data-file-height="391" /></a><figcaption> <div class="center" style="width:auto; margin-left:auto; margin-right:auto;">Antarctic Circumpolar Current, showing branches connecting to the larger <a href="/wiki/Thermohaline_circulation" title="Thermohaline circulation">thermohaline circulation</a></div></figcaption></figure> <figure typeof="mw:File/Thumb"><span><video id="mwe_player_0" poster="//upload.wikimedia.org/wikipedia/commons/thumb/4/4a/Thermohaline_Circulation_using_Improved_Flow_Field.ogv/320px--Thermohaline_Circulation_using_Improved_Flow_Field.ogv.jpg" controls="" preload="none" data-mw-tmh="" class="mw-file-element" width="320" height="108" data-durationhint="167" data-mwtitle="Thermohaline_Circulation_using_Improved_Flow_Field.ogv" data-mwprovider="wikimediacommons" resource="/wiki/File:Thermohaline_Circulation_using_Improved_Flow_Field.ogv"><source src="//upload.wikimedia.org/wikipedia/commons/transcoded/4/4a/Thermohaline_Circulation_using_Improved_Flow_Field.ogv/Thermohaline_Circulation_using_Improved_Flow_Field.ogv.360p.vp9.webm" type="video/webm; codecs=&quot;vp9, opus&quot;" data-transcodekey="360p.vp9.webm" data-width="640" data-height="216" /><source src="//upload.wikimedia.org/wikipedia/commons/transcoded/4/4a/Thermohaline_Circulation_using_Improved_Flow_Field.ogv/Thermohaline_Circulation_using_Improved_Flow_Field.ogv.360p.webm" type="video/webm; codecs=&quot;vp8, vorbis&quot;" data-transcodekey="360p.webm" data-width="640" data-height="216" /><source src="//upload.wikimedia.org/wikipedia/commons/4/4a/Thermohaline_Circulation_using_Improved_Flow_Field.ogv" type="video/ogg; codecs=&quot;theora&quot;" data-width="640" data-height="216" /><source src="//upload.wikimedia.org/wikipedia/commons/transcoded/4/4a/Thermohaline_Circulation_using_Improved_Flow_Field.ogv/Thermohaline_Circulation_using_Improved_Flow_Field.ogv.240p.vp9.webm" type="video/webm; codecs=&quot;vp9, opus&quot;" data-transcodekey="240p.vp9.webm" data-width="426" data-height="144" /></video></span><figcaption> Animation of the thermohaline circulation. The later part of this animation shows the Antarctic Circumpolar Current.</figcaption></figure> <p><b>Antarctic Circumpolar Current</b> (<b>ACC</b>) is an <a href="/wiki/Ocean_current" title="Ocean current">ocean current</a> that flows clockwise (as seen from the South Pole) from west to east around <a href="/wiki/Antarctica" title="Antarctica">Antarctica</a>. An alternative name for the ACC is the <b>West Wind Drift</b>. The ACC is the dominant circulation feature of the <a href="/wiki/Southern_Ocean" title="Southern Ocean">Southern Ocean</a> and has a mean transport estimated at 100–150 <a href="/wiki/Sverdrup" title="Sverdrup">Sverdrups</a> (Sv, million&#160;m<sup>3</sup>/s),<sup id="cite_ref-1" class="reference"><a href="#cite_note-1"><span class="cite-bracket">&#91;</span>1<span class="cite-bracket">&#93;</span></a></sup> or possibly even higher,<sup id="cite_ref-2" class="reference"><a href="#cite_note-2"><span class="cite-bracket">&#91;</span>2<span class="cite-bracket">&#93;</span></a></sup> making it the largest ocean current. The current is circumpolar due to the lack of any landmass connecting with Antarctica and this keeps warm ocean waters away from Antarctica, enabling that continent to maintain its huge <a href="/wiki/Ice_sheet" title="Ice sheet">ice sheet</a>. </p><p>Associated with the Circumpolar Current is the <a href="/wiki/Antarctic_Convergence" title="Antarctic Convergence">Antarctic Convergence</a>, where the cold Antarctic waters meet the warmer waters of the <a href="/wiki/Subantarctic" title="Subantarctic">subantarctic</a>, creating a zone of upwelling nutrients. These nurture high levels of <a href="/wiki/Phytoplankton" title="Phytoplankton">phytoplankton</a> with associated <a href="/wiki/Copepod" title="Copepod">copepods</a> and <a href="/wiki/Krill" title="Krill">krill</a>, and resultant <a href="/wiki/Food_chain" title="Food chain">food chains</a> supporting fish, whales, <a href="/wiki/Pinniped" title="Pinniped">seals</a>, penguins, <a href="/wiki/Albatross" title="Albatross">albatrosses</a>, and a wealth of <a href="/wiki/Wildlife_of_Antarctica" title="Wildlife of Antarctica">other species</a>. </p><p>The ACC has been known to sailors for centuries; it greatly speeds up any travel from west to east, but makes sailing extremely difficult from east to west, although this is mostly due to the prevailing <a href="/wiki/Westerlies" title="Westerlies">westerly winds</a>. <a href="/wiki/Jack_London" title="Jack London">Jack London</a>'s story "Make Westing" and the circumstances preceding the <a href="/wiki/Mutiny_on_the_Bounty" title="Mutiny on the Bounty">mutiny on the <i>Bounty</i></a> poignantly illustrate the difficulty it caused for mariners seeking to round <a href="/wiki/Cape_Horn" title="Cape Horn">Cape Horn</a> westbound on the <a href="/wiki/Clipper" title="Clipper">clipper ship</a> route from New York to California.<sup id="cite_ref-3" class="reference"><a href="#cite_note-3"><span class="cite-bracket">&#91;</span>3<span class="cite-bracket">&#93;</span></a></sup> The eastbound <a href="/wiki/Clipper_route" title="Clipper route">clipper route</a>, which is the fastest <a href="/wiki/Sailing_Directions" title="Sailing Directions">sailing route</a> around the world, follows the ACC around three continental capes – <a href="/wiki/Cape_Agulhas" title="Cape Agulhas">Cape Agulhas</a> (Africa), <a href="/wiki/South_East_Cape" title="South East Cape">South East Cape</a> (Australia), and <a href="/wiki/Cape_Horn" title="Cape Horn">Cape Horn</a> (South America). </p><p>The current creates the <a href="/wiki/Ross_Gyre" title="Ross Gyre">Ross</a> and <a href="/wiki/Weddell_Gyre" title="Weddell Gyre">Weddell Gyres</a>. </p> <meta property="mw:PageProp/toc" /> <div class="mw-heading mw-heading2"><h2 id="Structure">Structure</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Antarctic_Circumpolar_Current&amp;action=edit&amp;section=1" title="Edit section: Structure"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <figure class="mw-default-size" typeof="mw:File/Thumb"><a href="/wiki/File:Antarctic_Circumpolar_Current.jpg" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/6/60/Antarctic_Circumpolar_Current.jpg/220px-Antarctic_Circumpolar_Current.jpg" decoding="async" width="220" height="220" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/6/60/Antarctic_Circumpolar_Current.jpg/330px-Antarctic_Circumpolar_Current.jpg 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/6/60/Antarctic_Circumpolar_Current.jpg/440px-Antarctic_Circumpolar_Current.jpg 2x" data-file-width="966" data-file-height="966" /></a><figcaption>The Antarctic Circumpolar Current is the strongest current system in the world oceans and the only ocean current linking all major oceans: the Atlantic, Indian, and Pacific Oceans. Seawater density fronts after <a href="#CITEREFOrsiWhitworthNowlin1995">Orsi, Whitworth &amp; Nowlin 1995</a>.</figcaption></figure> <p>The ACC connects the <a href="/wiki/Atlantic_Ocean" title="Atlantic Ocean">Atlantic</a>, <a href="/wiki/Pacific_Ocean" title="Pacific Ocean">Pacific</a>, and Indian Oceans, and serves as a principal pathway of exchange among them. The current is strongly constrained by <a href="/wiki/Landform" title="Landform">landform</a> and <a href="/wiki/Bathymetric" class="mw-redirect" title="Bathymetric">bathymetric</a> features. To trace it starting arbitrarily at South America, it flows through the <a href="/wiki/Drake_Passage" title="Drake Passage">Drake Passage</a> between South America and the <a href="/wiki/Antarctic_Peninsula" title="Antarctic Peninsula">Antarctic Peninsula</a> and then is split by the <a href="/wiki/Scotia_Arc" title="Scotia Arc">Scotia Arc</a> to the east, with a shallow warm branch flowing to the north in the <a href="/wiki/Falkland_Current" title="Falkland Current">Falkland Current</a> and a deeper branch passing through the Arc more to the east before also turning to the north. Passing through the Indian Ocean, the current first retroflects the <a href="/wiki/Agulhas_Current" title="Agulhas Current">Agulhas Current</a> to form the <a href="/wiki/Agulhas_Return_Current" title="Agulhas Return Current">Agulhas Return Current</a> before it is split by the <a href="/wiki/Kerguelen_Plateau" title="Kerguelen Plateau">Kerguelen Plateau</a>, and then moving northward again. Deflection is also seen as it passes over the <a href="/wiki/Mid-ocean_ridge" title="Mid-ocean ridge">mid-ocean ridge</a> in the Southeast Pacific. </p> <div class="mw-heading mw-heading3"><h3 id="Fronts">Fronts</h3><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Antarctic_Circumpolar_Current&amp;action=edit&amp;section=2" title="Edit section: Fronts"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <p>The current is accompanied by three <a href="/wiki/Front_(Oceanography)" class="mw-redirect" title="Front (Oceanography)">fronts</a>: the Subantarctic front (SAF), the <a href="/wiki/Polar_front" title="Polar front">Polar front</a> (PF), and the Southern ACC front (SACC).<sup id="cite_ref-4" class="reference"><a href="#cite_note-4"><span class="cite-bracket">&#91;</span>4<span class="cite-bracket">&#93;</span></a></sup> Furthermore, the waters of the Southern Ocean are separated from the warmer and saltier subtropical waters by the <a href="/wiki/Subtropical_front" title="Subtropical front">subtropical front</a> (STF).<sup id="cite_ref-5" class="reference"><a href="#cite_note-5"><span class="cite-bracket">&#91;</span>5<span class="cite-bracket">&#93;</span></a></sup> </p><p>The northern boundary of the ACC is defined by the northern edge of the SAF, this being the most northerly water to pass through Drake Passage and therefore be circumpolar. Much of the ACC transport is carried in this front, which is defined as the latitude at which a subsurface salinity minimum or a thick layer of unstratified Subantarctic <a href="/wiki/Mode_water" title="Mode water">mode water</a> first appears, allowed by temperature dominating density stratification. Still further south lies the PF, which is marked by a transition to very cold, relatively fresh, Antarctic Surface Water at the surface. Here a temperature minimum is allowed by salinity dominating density stratification, due to the lower temperatures. Farther south still is the SACC, which is determined as the southernmost extent of <a href="/wiki/Circumpolar_deep_water" title="Circumpolar deep water">Circumpolar deep water</a> (temperature of about 2&#160;°C at 400&#160;m). This water mass flows along the shelfbreak of the western Antarctic Peninsula and thus marks the most southerly water flowing through Drake Passage and therefore circumpolar. The bulk of the transport is carried in the middle two fronts. </p><p>The total transport of the ACC at Drake Passage is estimated to be around 135&#160;Sv, or about 135 times the transport of all the world's rivers combined. There is a relatively small addition of flow in the Indian Ocean, with the transport south of <a href="/wiki/Tasmania" title="Tasmania">Tasmania</a> reaching around 147&#160;Sv, at which point the current is probably the largest on the planet. </p> <div class="mw-heading mw-heading2"><h2 id="Dynamics">Dynamics</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Antarctic_Circumpolar_Current&amp;action=edit&amp;section=3" title="Edit section: Dynamics"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <p>The circumpolar current is driven by the strong westerly winds in the latitudes of the Southern Ocean. </p> <figure class="mw-default-size" typeof="mw:File/Thumb"><a href="//upload.wikimedia.org/wikipedia/commons/a/ab/Thermohaline_circulation.svg"><img resource="/wiki/File:Thermohaline_circulation.svg" src="//upload.wikimedia.org/wikipedia/commons/thumb/a/ab/Thermohaline_circulation.svg/220px-Thermohaline_circulation.svg.png" decoding="async" width="220" height="220" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/a/ab/Thermohaline_circulation.svg/330px-Thermohaline_circulation.svg.png 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/a/ab/Thermohaline_circulation.svg/440px-Thermohaline_circulation.svg.png 2x" data-file-width="512" data-file-height="512" /></a><figcaption>The ACC (red circle near the middle of the image) in relation to the global <a href="/wiki/Thermohaline_circulation" title="Thermohaline circulation">thermohaline circulation</a> <a class="external text" href="https://upload.wikimedia.org/wikipedia/commons/a/ab/Thermohaline_circulation.svg">(animation)</a> </figcaption></figure> <p>In latitudes where there are continents, winds blowing on light surface water can simply pile up light water against these continents. But in the Southern Ocean, the momentum imparted to the surface waters cannot be offset in this way. There are different theories on how the Circumpolar Current balances the momentum imparted by the winds. The increasing eastward momentum imparted by the winds causes water parcels to drift outward from the axis of the Earth's rotation (in other words, northward) as a result of the <a href="/wiki/Coriolis_force" title="Coriolis force">Coriolis force</a>. This northward <a href="/wiki/Ekman_transport" title="Ekman transport">Ekman transport</a> is balanced by a southward, pressure-driven flow below the depths of the major ridge systems. Some theories connect these flows directly, implying that there is significant upwelling of dense deep waters within the Southern Ocean, transformation of these waters into light surface waters, and a transformation of waters in the opposite direction to the north. Such theories link the magnitude of the Circumpolar Current with the global <a href="/wiki/Thermohaline_circulation" title="Thermohaline circulation">thermohaline circulation</a>, particularly the properties of the North Atlantic. </p><p>Alternatively, <a href="/wiki/Eddy_(fluid_dynamics)#Mesoscale_ocean_eddies" title="Eddy (fluid dynamics)">ocean eddies</a>, the oceanic equivalent of atmospheric storms, or the large-scale meanders of the Circumpolar Current may directly transport momentum downward in the water column. This is because such flows can produce a net southward flow in the troughs and a net northward flow over the ridges without requiring any transformation of density. In practice both the thermohaline and the eddy/meander mechanisms are likely to be important. </p><p>The current flows at a rate of about 4&#160;km/h (2.5&#160;mph) over the <a href="/wiki/Macquarie_Fault_Zone" title="Macquarie Fault Zone">Macquarie Ridge</a> south of New Zealand.<sup id="cite_ref-brittlestar_6-0" class="reference"><a href="#cite_note-brittlestar-6"><span class="cite-bracket">&#91;</span>6<span class="cite-bracket">&#93;</span></a></sup> The ACC varies with time. Evidence of this is the <a href="/wiki/Antarctic_Circumpolar_Wave" title="Antarctic Circumpolar Wave">Antarctic Circumpolar Wave</a>, a periodic oscillation that affects the climate of much of the southern hemisphere.<sup id="cite_ref-7" class="reference"><a href="#cite_note-7"><span class="cite-bracket">&#91;</span>7<span class="cite-bracket">&#93;</span></a></sup> There is also the <a href="/wiki/Antarctic_oscillation" title="Antarctic oscillation">Antarctic oscillation</a>, which involves changes in the location and strength of Antarctic winds. Trends in the Antarctic Oscillation have been hypothesized to account for an increase in the transport of the Circumpolar Current over the past two decades. </p> <div class="mw-heading mw-heading2"><h2 id="Formation">Formation</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Antarctic_Circumpolar_Current&amp;action=edit&amp;section=4" title="Edit section: Formation"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <p>Published estimates of the onset of the Antarctic Circumpolar Current vary, but it is commonly considered to have started at the <a href="/wiki/Eocene" title="Eocene">Eocene</a>/<a href="/wiki/Oligocene" title="Oligocene">Oligocene</a> boundary. The isolation of Antarctica and formation of the ACC occurred with the openings of the <a href="/wiki/Tasmanian_Passage" title="Tasmanian Passage">Tasmanian Passage</a> and the <a href="/wiki/Drake_Passage" title="Drake Passage">Drake Passage</a>. The Tasmanian Seaway separates East Antarctica and Australia, and is reported to have opened to water circulation 33.5&#160;million years ago (Ma).<sup id="cite_ref-8" class="reference"><a href="#cite_note-8"><span class="cite-bracket">&#91;</span>8<span class="cite-bracket">&#93;</span></a></sup> The timing of the opening of the Drake Passage, between South America and the Antarctic Peninsula, is more disputed; <a href="/wiki/Tectonic" class="mw-redirect" title="Tectonic">tectonic</a> and sediment evidence show that it could have been open as early as pre-34&#160;Ma,<sup id="cite_ref-9" class="reference"><a href="#cite_note-9"><span class="cite-bracket">&#91;</span>9<span class="cite-bracket">&#93;</span></a></sup> estimates of the opening of the Drake passage are between 20 and 40&#160;Ma.<sup id="cite_ref-Siegert-etal-2008_10-0" class="reference"><a href="#cite_note-Siegert-etal-2008-10"><span class="cite-bracket">&#91;</span>10<span class="cite-bracket">&#93;</span></a></sup> The isolation of Antarctica by the current is credited by many researchers with causing the <a href="/wiki/Glaciation" class="mw-redirect" title="Glaciation">glaciation</a> of Antarctica and global cooling in the <a href="/wiki/Eocene" title="Eocene">Eocene</a> epoch. Oceanic models have shown that the opening of these two passages limited polar heat convergence and caused a cooling of <a href="/wiki/Sea_surface_temperature" title="Sea surface temperature">sea surface temperatures</a> by several degrees; other models have shown that CO<sub>2</sub> levels also played a significant role in the glaciation of Antarctica.<sup id="cite_ref-Siegert-etal-2008_10-1" class="reference"><a href="#cite_note-Siegert-etal-2008-10"><span class="cite-bracket">&#91;</span>10<span class="cite-bracket">&#93;</span></a></sup><sup id="cite_ref-11" class="reference"><a href="#cite_note-11"><span class="cite-bracket">&#91;</span>11<span class="cite-bracket">&#93;</span></a></sup> </p> <div class="mw-heading mw-heading2"><h2 id="Phytoplankton">Phytoplankton</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Antarctic_Circumpolar_Current&amp;action=edit&amp;section=5" title="Edit section: Phytoplankton"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <figure class="mw-default-size" typeof="mw:File/Thumb"><a href="/wiki/File:S2004341153052.L2_HCHL.MalvinasCurrent.jpg" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/7/73/S2004341153052.L2_HCHL.MalvinasCurrent.jpg/220px-S2004341153052.L2_HCHL.MalvinasCurrent.jpg" decoding="async" width="220" height="253" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/7/73/S2004341153052.L2_HCHL.MalvinasCurrent.jpg/330px-S2004341153052.L2_HCHL.MalvinasCurrent.jpg 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/7/73/S2004341153052.L2_HCHL.MalvinasCurrent.jpg/440px-S2004341153052.L2_HCHL.MalvinasCurrent.jpg 2x" data-file-width="2711" data-file-height="3117" /></a><figcaption>The <a href="/wiki/Falkland_Current" title="Falkland Current">Falkland Current</a> transports nutrient-rich cold waters from the ACC north toward the <a href="/wiki/Brazil%E2%80%93Malvinas_Confluence" class="mw-redirect" title="Brazil–Malvinas Confluence">Brazil–Malvinas Confluence</a>. Phytoplankton chlorophyll concentration are shown in blue (lower concentrations) and yellow (higher concentrations).</figcaption></figure> <p>Antarctic sea ice cycles seasonally, in February–March the amount of sea ice is lowest, and in August–September the sea ice is at its greatest extent.<sup id="cite_ref-12" class="reference"><a href="#cite_note-12"><span class="cite-bracket">&#91;</span>12<span class="cite-bracket">&#93;</span></a></sup> Ice levels have been monitored by satellite since 1973. Upwelling of deep water under the sea ice brings substantial amounts of nutrients. As the ice melts, the melt water provides stability and the critical depth is well below the mixing depth, which allows for a positive net <a href="/wiki/Primary_production" title="Primary production">primary production</a>.<sup id="cite_ref-Miller-2004_13-0" class="reference"><a href="#cite_note-Miller-2004-13"><span class="cite-bracket">&#91;</span>13<span class="cite-bracket">&#93;</span></a></sup> As the sea ice recedes epontic algae dominate the first phase of the bloom, and a strong bloom dominate by diatoms follows the ice melt south.<sup id="cite_ref-Miller-2004_13-1" class="reference"><a href="#cite_note-Miller-2004-13"><span class="cite-bracket">&#91;</span>13<span class="cite-bracket">&#93;</span></a></sup> </p><p>Another phytoplankton bloom occurs more to the north near the <a href="/wiki/Antarctic_Convergence" title="Antarctic Convergence">Antarctic Convergence</a>, here nutrients are present from <a href="/wiki/Thermohaline_circulation" title="Thermohaline circulation">thermohaline circulation</a>. Phytoplankton blooms are dominated by diatoms and grazed by copepods in the open ocean, and by krill closer to the continent. Diatom production continues through the summer, and populations of krill are sustained, bringing large numbers of <a href="/wiki/Cetacean" class="mw-redirect" title="Cetacean">cetaceans</a>, <a href="/wiki/Cephalopod" title="Cephalopod">cephalopods</a>, seals, birds, and fish to the area.<sup id="cite_ref-Miller-2004_13-2" class="reference"><a href="#cite_note-Miller-2004-13"><span class="cite-bracket">&#91;</span>13<span class="cite-bracket">&#93;</span></a></sup> </p><p>Phytoplankton blooms are believed to be limited by irradiance in the austral (southern hemisphere) spring, and by biologically available iron in the summer.<sup id="cite_ref-14" class="reference"><a href="#cite_note-14"><span class="cite-bracket">&#91;</span>14<span class="cite-bracket">&#93;</span></a></sup> Much of the biology in the area occurs along the major fronts of the current, the Subtropical, Subantarctic, and the Antarctic Polar fronts, these are areas associated with well defined temperature changes.<sup id="cite_ref-15" class="reference"><a href="#cite_note-15"><span class="cite-bracket">&#91;</span>15<span class="cite-bracket">&#93;</span></a></sup> Size and distribution of phytoplankton are also related to fronts. Microphytoplankton (&gt;20&#160;μm) are found at fronts and at sea ice boundaries, while <a href="/wiki/Nanophytoplankton" title="Nanophytoplankton">nanophytoplankton</a> (&lt;20&#160;μm) are found between fronts.<sup id="cite_ref-Knox-2007_16-0" class="reference"><a href="#cite_note-Knox-2007-16"><span class="cite-bracket">&#91;</span>16<span class="cite-bracket">&#93;</span></a></sup> </p><p>Studies of phytoplankton stocks in the southern sea have shown that the Antarctic Circumpolar Current is dominated by diatoms, while the <a href="/wiki/Weddell_Sea" title="Weddell Sea">Weddell Sea</a> has abundant <a href="/wiki/Coccolithophorid" class="mw-redirect" title="Coccolithophorid">coccolithophorids</a> and silicoflagellates. Surveys of the SW Indian Ocean have shown phytoplankton group variation based on their location relative to the Polar Front, with <a href="/wiki/Diatom" title="Diatom">diatoms</a> dominating South of the front, and dinoflagellates and <a href="/wiki/Flagellates" class="mw-redirect" title="Flagellates">flagellates</a> in higher populations North of the front.<sup id="cite_ref-Knox-2007_16-1" class="reference"><a href="#cite_note-Knox-2007-16"><span class="cite-bracket">&#91;</span>16<span class="cite-bracket">&#93;</span></a></sup> </p><p>Some research has been conducted on Antarctic phytoplankton as a <a href="/wiki/Carbon_sink" title="Carbon sink">carbon sink</a>. Areas of open water left from ice melt are good areas for phytoplankton blooms. The phytoplankton takes carbon from the atmosphere during photosynthesis. As the blooms die and sink, the carbon can be stored in sediments for thousands of years. This natural carbon sink is estimated to remove 3.5&#160;million tonnes from the ocean each year. 3.5&#160;million tonnes of carbon taken from the ocean and atmosphere is equivalent to 12.8&#160;million tonnes of carbon dioxide.<sup id="cite_ref-17" class="reference"><a href="#cite_note-17"><span class="cite-bracket">&#91;</span>17<span class="cite-bracket">&#93;</span></a></sup> </p> <div class="mw-heading mw-heading2"><h2 id="Studies">Studies</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Antarctic_Circumpolar_Current&amp;action=edit&amp;section=6" title="Edit section: Studies"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <p>An expedition in May 2008 by 19 scientists<sup id="cite_ref-18" class="reference"><a href="#cite_note-18"><span class="cite-bracket">&#91;</span>18<span class="cite-bracket">&#93;</span></a></sup> studied the geology and biology of eight <a href="/wiki/Macquarie_Fault_Zone" title="Macquarie Fault Zone">Macquarie Ridge</a> sea mounts, as well as the Antarctic Circumpolar Current to investigate the <a href="/wiki/Effects_of_climate_change" title="Effects of climate change">effects of climate change</a> of the Southern Ocean. The circumpolar current merges the waters of the Atlantic, Indian, and Pacific Oceans and carries up to 150 times the volume of water flowing in all of the world's rivers. The study found that any damage on the cold-water corals nourished by the current will have a long-lasting effect.<sup id="cite_ref-brittlestar_6-1" class="reference"><a href="#cite_note-brittlestar-6"><span class="cite-bracket">&#91;</span>6<span class="cite-bracket">&#93;</span></a></sup> After studying the circumpolar current it is clear that it strongly influences regional and global climate as well as underwater biodiversity.<sup id="cite_ref-19" class="reference"><a href="#cite_note-19"><span class="cite-bracket">&#91;</span>19<span class="cite-bracket">&#93;</span></a></sup> The subject has been characterized recently as "the spectral peak of the global extra-tropical circulation at ≈ 10^4 kilometers".<sup id="cite_ref-20" class="reference"><a href="#cite_note-20"><span class="cite-bracket">&#91;</span>20<span class="cite-bracket">&#93;</span></a></sup> </p><p>The current helps preserve wooden shipwrecks by preventing wood-boring "<a href="/wiki/Ship_worms" class="mw-redirect" title="Ship worms">ship worms</a>" from reaching targets such as <a href="/wiki/Ernest_Shackleton" title="Ernest Shackleton">Ernest Shackleton</a>'s ship, the <a href="/wiki/Endurance_(1912_ship)" title="Endurance (1912 ship)"><i>Endurance</i></a>.<sup id="cite_ref-21" class="reference"><a href="#cite_note-21"><span class="cite-bracket">&#91;</span>21<span class="cite-bracket">&#93;</span></a></sup> </p><p>The "State of the cryosphere" report found, that the Antarctic Circumpolar Current became weaker. By 2050 it expected to lose 20% of its strenght with "widespread impacts on ocean circulation and climate." The <a href="/wiki/Weddell_Sea_Bottom_Water" title="Weddell Sea Bottom Water">Weddell Sea Bottom Water</a> has lost 30% of its volume in the latest 32 years, and the <a href="/wiki/Antarctic_bottom_water" title="Antarctic bottom water">Antarctic Bottom Water</a> is expected to shrunk. This will impact ocean circulation, nutrients, heat content and carbon sequestration.<sup id="cite_ref-22" class="reference"><a href="#cite_note-22"><span class="cite-bracket">&#91;</span>22<span class="cite-bracket">&#93;</span></a></sup> <a href="/wiki/UNESCO" title="UNESCO">UNESCO</a> mentions that the report in the first time "notes a growing scientific consensus that melting Greenland and Antarctic ice sheets, among other factors, may be slowing important ocean currents at both poles, with potentially dire consequences for a much colder northern Europe and greater sea-level rise along the U.S. East Coast."<sup id="cite_ref-23" class="reference"><a href="#cite_note-23"><span class="cite-bracket">&#91;</span>23<span class="cite-bracket">&#93;</span></a></sup> </p> <div class="mw-heading mw-heading2"><h2 id="References">References</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Antarctic_Circumpolar_Current&amp;action=edit&amp;section=7" title="Edit section: References"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <div class="mw-heading mw-heading3"><h3 id="Notes">Notes</h3><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Antarctic_Circumpolar_Current&amp;action=edit&amp;section=8" title="Edit section: Notes"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <style data-mw-deduplicate="TemplateStyles:r1239543626">.mw-parser-output .reflist{margin-bottom:0.5em;list-style-type:decimal}@media screen{.mw-parser-output .reflist{font-size:90%}}.mw-parser-output .reflist .references{font-size:100%;margin-bottom:0;list-style-type:inherit}.mw-parser-output .reflist-columns-2{column-width:30em}.mw-parser-output .reflist-columns-3{column-width:25em}.mw-parser-output .reflist-columns{margin-top:0.3em}.mw-parser-output .reflist-columns ol{margin-top:0}.mw-parser-output .reflist-columns li{page-break-inside:avoid;break-inside:avoid-column}.mw-parser-output .reflist-upper-alpha{list-style-type:upper-alpha}.mw-parser-output .reflist-upper-roman{list-style-type:upper-roman}.mw-parser-output .reflist-lower-alpha{list-style-type:lower-alpha}.mw-parser-output .reflist-lower-greek{list-style-type:lower-greek}.mw-parser-output .reflist-lower-roman{list-style-type:lower-roman}</style><div class="reflist reflist-columns references-column-width" style="column-width: 30em;"> <ol class="references"> <li id="cite_note-1"><span class="mw-cite-backlink"><b><a href="#cite_ref-1">^</a></b></span> <span class="reference-text"><a href="#CITEREFSmithDesflotsWhiteMariano2013">Smith et al. 2013</a></span> </li> <li id="cite_note-2"><span class="mw-cite-backlink"><b><a href="#cite_ref-2">^</a></b></span> <span class="reference-text"><style data-mw-deduplicate="TemplateStyles:r1238218222">.mw-parser-output cite.citation{font-style:inherit;word-wrap:break-word}.mw-parser-output .citation q{quotes:"\"""\"""'""'"}.mw-parser-output .citation:target{background-color:rgba(0,127,255,0.133)}.mw-parser-output .id-lock-free.id-lock-free a{background:url("//upload.wikimedia.org/wikipedia/commons/6/65/Lock-green.svg")right 0.1em center/9px no-repeat}.mw-parser-output .id-lock-limited.id-lock-limited a,.mw-parser-output .id-lock-registration.id-lock-registration a{background:url("//upload.wikimedia.org/wikipedia/commons/d/d6/Lock-gray-alt-2.svg")right 0.1em center/9px no-repeat}.mw-parser-output .id-lock-subscription.id-lock-subscription a{background:url("//upload.wikimedia.org/wikipedia/commons/a/aa/Lock-red-alt-2.svg")right 0.1em center/9px no-repeat}.mw-parser-output .cs1-ws-icon a{background:url("//upload.wikimedia.org/wikipedia/commons/4/4c/Wikisource-logo.svg")right 0.1em center/12px no-repeat}body:not(.skin-timeless):not(.skin-minerva) .mw-parser-output .id-lock-free a,body:not(.skin-timeless):not(.skin-minerva) .mw-parser-output .id-lock-limited a,body:not(.skin-timeless):not(.skin-minerva) .mw-parser-output .id-lock-registration a,body:not(.skin-timeless):not(.skin-minerva) .mw-parser-output .id-lock-subscription a,body:not(.skin-timeless):not(.skin-minerva) .mw-parser-output .cs1-ws-icon a{background-size:contain;padding:0 1em 0 0}.mw-parser-output .cs1-code{color:inherit;background:inherit;border:none;padding:inherit}.mw-parser-output .cs1-hidden-error{display:none;color:var(--color-error,#d33)}.mw-parser-output .cs1-visible-error{color:var(--color-error,#d33)}.mw-parser-output .cs1-maint{display:none;color:#085;margin-left:0.3em}.mw-parser-output .cs1-kern-left{padding-left:0.2em}.mw-parser-output .cs1-kern-right{padding-right:0.2em}.mw-parser-output .citation .mw-selflink{font-weight:inherit}@media screen{.mw-parser-output .cs1-format{font-size:95%}html.skin-theme-clientpref-night .mw-parser-output .cs1-maint{color:#18911f}}@media screen and (prefers-color-scheme:dark){html.skin-theme-clientpref-os .mw-parser-output .cs1-maint{color:#18911f}}</style><cite id="CITEREFDonohue2016" class="citation journal cs1">Donohue, K.A.; et&#160;al. 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GES DISC: Goddard Earth Sciences, Data &amp; Information Services Center. May 2012. Archived from <a rel="nofollow" class="external text" href="https://disc.sci.gsfc.nasa.gov/education-and-outreach/additional/science-focus/locus/tutorials/module6.shtml">the original</a> on 18 May 2015<span class="reference-accessdate">. Retrieved <span class="nowrap">13 August</span> 2012</span>.</cite><span title="ctx_ver=Z39.88-2004&amp;rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Abook&amp;rft.genre=unknown&amp;rft.btitle=The+Southern+Ocean&amp;rft.pub=GES+DISC%3A+Goddard+Earth+Sciences%2C+Data+%26+Information+Services+Center&amp;rft.date=2012-05&amp;rft_id=http%3A%2F%2Fdisc.sci.gsfc.nasa.gov%2Feducation-and-outreach%2Fadditional%2Fscience-focus%2Flocus%2Ftutorials%2Fmodule6.shtml&amp;rfr_id=info%3Asid%2Fen.wikipedia.org%3AAntarctic+Circumpolar+Current" class="Z3988"></span></span> </li> <li id="cite_note-Knox-2007-16"><span class="mw-cite-backlink">^ <a href="#cite_ref-Knox-2007_16-0"><sup><i><b>a</b></i></sup></a> <a href="#cite_ref-Knox-2007_16-1"><sup><i><b>b</b></i></sup></a></span> <span class="reference-text"><a href="#CITEREFKnox2007">Knox 2007</a>, p.&#160;23</span> </li> <li id="cite_note-17"><span class="mw-cite-backlink"><b><a href="#cite_ref-17">^</a></b></span> <span class="reference-text"><a href="#CITEREFPeckBarnesCookFleming2010">Peck et al. 2010</a></span> </li> <li id="cite_note-18"><span class="mw-cite-backlink"><b><a href="#cite_ref-18">^</a></b></span> <span class="reference-text"><a href="#CITEREFO&#39;HaraRowdenWilliams2008">O'Hara, Rowden &amp; Williams 2008</a></span> </li> <li id="cite_note-19"><span class="mw-cite-backlink"><b><a href="#cite_ref-19">^</a></b></span> <span class="reference-text"><a href="#CITEREFRintoulHughesOlbers2001">Rintoul, Hughes &amp; Olbers 2001</a>, e.g. p. 271</span> </li> <li id="cite_note-20"><span class="mw-cite-backlink"><b><a href="#cite_ref-20">^</a></b></span> <span class="reference-text">Storer, B.A., Buzzicotti, M., Khatri, H. et al. Global energy spectrum of the general oceanic circulation. <i>Nat Commun</i> 13, 5314 (2022). <a rel="nofollow" class="external free" href="https://doi.org/10.1038/s41467-022-33031-3">https://doi.org/10.1038/s41467-022-33031-3</a>. Retrieved 17 September 2022.</span> </li> <li id="cite_note-21"><span class="mw-cite-backlink"><b><a href="#cite_ref-21">^</a></b></span> <span class="reference-text"><a href="#CITEREFGloverWiklundTaboadaAvila2013">Glover et al. 2013</a></span> </li> <li id="cite_note-22"><span class="mw-cite-backlink"><b><a href="#cite_ref-22">^</a></b></span> <span class="reference-text"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1238218222"><cite class="citation book cs1"><a rel="nofollow" class="external text" href="https://articles.unesco.org/sites/default/files/medias/fichiers/2024/11/State%20of%20the%20Cryosphere%20Report%202024.pdf"><i>State of the Cryosphere 2024 Lost Ice, Global Damage</i></a> <span class="cs1-format">(PDF)</span>. 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Retrieved <span class="nowrap">20 November</span> 2024</span>.</cite><span title="ctx_ver=Z39.88-2004&amp;rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Ajournal&amp;rft.genre=unknown&amp;rft.jtitle=UNESCO&amp;rft.atitle=State+of+the+Cryosphere+Report+2024+Lost+Ice%2C+Global+Damage&amp;rft_id=https%3A%2F%2Fwww.unesco.org%2Fen%2Farticles%2Fstate-cryosphere-report-2024&amp;rfr_id=info%3Asid%2Fen.wikipedia.org%3AAntarctic+Circumpolar+Current" class="Z3988"></span></span> </li> </ol></div> <div class="mw-heading mw-heading3"><h3 id="Sources">Sources</h3><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Antarctic_Circumpolar_Current&amp;action=edit&amp;section=9" title="Edit section: Sources"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <style data-mw-deduplicate="TemplateStyles:r1239549316">.mw-parser-output .refbegin{margin-bottom:0.5em}.mw-parser-output .refbegin-hanging-indents>ul{margin-left:0}.mw-parser-output .refbegin-hanging-indents>ul>li{margin-left:0;padding-left:3.2em;text-indent:-3.2em}.mw-parser-output .refbegin-hanging-indents ul,.mw-parser-output .refbegin-hanging-indents ul li{list-style:none}@media(max-width:720px){.mw-parser-output .refbegin-hanging-indents>ul>li{padding-left:1.6em;text-indent:-1.6em}}.mw-parser-output .refbegin-columns{margin-top:0.3em}.mw-parser-output .refbegin-columns ul{margin-top:0}.mw-parser-output .refbegin-columns li{page-break-inside:avoid;break-inside:avoid-column}@media screen{.mw-parser-output .refbegin{font-size:90%}}</style><div class="refbegin refbegin-columns references-column-width" style="column-width: 30em"> <ul><li><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1238218222"><cite id="CITEREFBarkerFilippelliFlorindoMartin2007" class="citation journal cs1">Barker, P. F.; Filippelli, G. M.; Florindo, F.; Martin, E. E.; Scher, H. D. 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(2007). <a rel="nofollow" class="external text" href="https://archive.today/20120713080518/http://oceanworld.tamu.edu/resources/ocng_textbook/chapter13/chapter13_04.htm">"Deep Circulation in the Ocean: Antarctic Circumpolar Current"</a>. Department of Oceanography, Texas A&amp;M University. Archived from <a rel="nofollow" class="external text" href="http://oceanworld.tamu.edu/resources/ocng_textbook/chapter13/chapter13_04.htm">the original</a> on 13 July 2012<span class="reference-accessdate">. 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template">t</abbr></a></li><li class="nv-edit"><a href="/wiki/Special:EditPage/Template:Ocean" title="Special:EditPage/Template:Ocean"><abbr title="Edit this template">e</abbr></a></li></ul></div><div id="Ocean_currents_and_gyres" style="font-size:114%;margin:0 4em"><a href="/wiki/Ocean_current" title="Ocean current">Ocean currents</a> and <a href="/wiki/Ocean_gyre" title="Ocean gyre">gyres</a></div></th></tr><tr><th scope="row" class="navbox-group" style="width:1%"><a href="/wiki/Ocean_current" title="Ocean current">Currents</a></th><td class="navbox-list-with-group navbox-list navbox-odd hlist" style="width:100%;padding:0"><div style="padding:0 0.25em"></div><table class="nowraplinks navbox-subgroup" style="border-spacing:0"><tbody><tr><th scope="row" class="navbox-group" style="width:1%">Arctic Ocean</th><td class="navbox-list-with-group navbox-list navbox-odd" style="width:100%;padding:0"><div style="padding:0 0.25em"> <ul><li><a href="/wiki/East_Greenland_Current" title="East Greenland Current">East Greenland</a></li> <li><a href="/wiki/North_Icelandic_Jet" title="North Icelandic Jet">North Icelandic</a></li> <li><a href="/wiki/Norwegian_Current" title="Norwegian Current">Norwegian</a></li> <li><a href="/wiki/Transpolar_Drift_Stream" title="Transpolar Drift Stream">Transpolar Drift Stream</a></li></ul> </div></td></tr><tr><th scope="row" class="navbox-group" style="width:1%">Atlantic Ocean</th><td class="navbox-list-with-group navbox-list navbox-even" style="width:100%;padding:0"><div style="padding:0 0.25em"> <ul><li><a href="/wiki/Angola_Current" title="Angola Current">Angola</a></li> <li><a href="/wiki/Antilles_Current" title="Antilles Current">Antilles</a></li> <li><a href="/wiki/Azores_Current" title="Azores Current">Azores</a></li> <li><a href="/wiki/Baffin_Island_Current" title="Baffin Island Current">Baffin Island</a></li> <li><a href="/wiki/Benguela_Current" title="Benguela Current">Benguela</a></li> <li><a href="/wiki/Brazil_Current" title="Brazil Current">Brazil</a></li> <li><a href="/wiki/Canary_Current" title="Canary Current">Canary</a></li> <li><a href="/wiki/Cape_Horn_Current" title="Cape Horn Current">Cape Horn</a></li> <li><a href="/wiki/Caribbean_Current" title="Caribbean Current">Caribbean</a></li> <li><a href="/wiki/East_Greenland_Current" title="East Greenland Current">East Greenland</a></li> <li><a href="/wiki/East_Iceland_Current" title="East Iceland Current">East Iceland</a></li> <li><a href="/wiki/Falkland_Current" title="Falkland Current">Falkland</a></li> <li><a href="/wiki/Florida_Current" title="Florida Current">Florida</a></li> <li><a href="/wiki/Guinea_Current" title="Guinea Current">Guinea</a></li> <li><a href="/wiki/Gulf_Stream" title="Gulf Stream">Gulf Stream</a></li> <li><a href="/wiki/Irminger_Current" title="Irminger Current">Irminger</a></li> <li><a href="/wiki/Labrador_Current" title="Labrador Current">Labrador</a></li> <li><a href="/wiki/Lomonosov_Current" title="Lomonosov Current">Lomonosov</a></li> <li><a href="/wiki/Loop_Current" title="Loop Current">Loop</a></li> <li><a href="/wiki/North_Atlantic_Current" title="North Atlantic Current">North Atlantic</a></li> <li><a href="/wiki/North_Brazil_Current" title="North Brazil Current">North Brazil</a></li> <li><a href="/wiki/North_Equatorial_Current" title="North Equatorial Current">North Equatorial</a></li> <li><a href="/wiki/Norwegian_Current" title="Norwegian Current">Norwegian</a></li> <li><a href="/wiki/Portugal_Current" title="Portugal Current">Portugal</a></li> <li><a href="/wiki/South_Atlantic_Current" title="South Atlantic Current">South Atlantic</a></li> <li><a href="/wiki/South_Equatorial_Current" title="South Equatorial Current">South Equatorial</a></li> <li><a href="/wiki/West_Greenland_Current" title="West Greenland Current">West Greenland</a></li> <li><a href="/wiki/West_Spitsbergen_Current" title="West Spitsbergen Current">West Spitsbergen</a></li></ul> </div></td></tr><tr><th scope="row" class="navbox-group" style="width:1%">Indian Ocean</th><td class="navbox-list-with-group navbox-list navbox-odd" style="width:100%;padding:0"><div style="padding:0 0.25em"> <ul><li><a href="/wiki/Agulhas_Current" title="Agulhas Current">Agulhas</a></li> <li><a href="/wiki/Agulhas_Return_Current" title="Agulhas Return Current">Agulhas Return</a></li> <li><a href="/wiki/East_Madagascar_Current" title="East Madagascar Current">East Madagascar</a></li> <li><a href="/wiki/Equatorial_Counter_Current" title="Equatorial Counter Current">Equatorial Counter</a></li> <li><a href="/wiki/Indian_Monsoon_Current" title="Indian Monsoon Current">Indian Monsoon</a></li> <li><a href="/wiki/Indonesian_Throughflow" title="Indonesian Throughflow">Indonesian Throughflow</a></li> <li><a href="/wiki/Leeuwin_Current" title="Leeuwin Current">Leeuwin</a></li> <li><a href="/wiki/Madagascar_Current" title="Madagascar Current">Madagascar</a></li> <li><a href="/wiki/Mozambique_Current" title="Mozambique Current">Mozambique</a></li> <li><a href="/wiki/North_Madagascar_Current" title="North Madagascar Current">North Madagascar</a></li> <li><a href="/wiki/Somali_Current" title="Somali Current">Somali</a></li> <li><a href="/wiki/South_Equatorial_Current" title="South Equatorial Current">South Equatorial</a></li> <li><a href="/wiki/West_Australian_Current" title="West Australian Current">West Australian</a></li></ul> </div></td></tr><tr><th scope="row" class="navbox-group" style="width:1%">Pacific Ocean</th><td class="navbox-list-with-group navbox-list navbox-even" style="width:100%;padding:0"><div style="padding:0 0.25em"> <ul><li><a href="/wiki/Alaska_Current" title="Alaska Current">Alaska</a></li> <li><a href="/wiki/Aleutian_Current" title="Aleutian Current">Aleutian</a></li> <li><a href="/wiki/California_Current" title="California Current">California</a></li> <li><a href="/wiki/Cromwell_Current" title="Cromwell Current">Cromwell</a></li> <li><a href="/wiki/Davidson_Current" title="Davidson Current">Davidson</a></li> <li><a href="/wiki/East_Australian_Current" title="East Australian Current">East Australian</a></li> <li><a href="/wiki/East_Korea_Warm_Current" title="East Korea Warm Current">East Korea Warm</a></li> <li><a href="/wiki/Equatorial_Counter_Current" title="Equatorial Counter Current">Equatorial Counter</a></li> <li><a href="/wiki/Humboldt_Current" title="Humboldt Current">Humboldt</a></li> <li><a href="/wiki/Indonesian_Throughflow" title="Indonesian Throughflow">Indonesian Throughflow</a></li> <li><a href="/wiki/Kamchatka_Current" title="Kamchatka Current">Kamchatka</a></li> <li><a href="/wiki/Kuroshio_Current" title="Kuroshio Current">Kuroshio</a></li> <li><a href="/wiki/Mindanao_Current" title="Mindanao Current">Mindanao</a></li> <li><a href="/wiki/North_Equatorial_Current" title="North Equatorial Current">North Equatorial</a></li> <li><a href="/wiki/North_Korea_Cold_Current" title="North Korea Cold Current">North Korea Cold</a></li> <li><a href="/wiki/North_Pacific_Current" title="North Pacific Current">North Pacific</a></li> <li><a href="/wiki/Oyashio_Current" title="Oyashio Current">Oyashio</a></li> <li><a href="/wiki/South_Equatorial_Current" title="South Equatorial Current">South Equatorial</a></li> <li><a href="/wiki/Tasman_Front" title="Tasman Front">Tasman Front</a></li></ul> </div></td></tr><tr><th scope="row" class="navbox-group" style="width:1%">Southern Ocean</th><td class="navbox-list-with-group navbox-list navbox-odd" style="width:100%;padding:0"><div style="padding:0 0.25em"> <ul><li><a class="mw-selflink selflink">Antarctic Circumpolar</a></li> <li><a href="/wiki/Tasman_Outflow" title="Tasman Outflow">Tasman Outflow</a></li></ul> </div></td></tr></tbody></table><div></div></td></tr><tr><th scope="row" class="navbox-group" style="width:1%"><a href="/wiki/Ocean_gyre" title="Ocean gyre">Gyres</a></th><td class="navbox-list-with-group navbox-list navbox-odd hlist" style="width:100%;padding:0"><div style="padding:0 0.25em"></div><table class="nowraplinks navbox-subgroup" style="border-spacing:0"><tbody><tr><th scope="row" class="navbox-group" style="width:1%">Major gyres</th><td class="navbox-list-with-group navbox-list navbox-even" style="width:100%;padding:0"><div style="padding:0 0.25em"> <ul><li><a href="/wiki/Indian_Ocean_Gyre" title="Indian Ocean Gyre">Indian Ocean Gyre</a></li> <li><a href="/wiki/North_Atlantic_Gyre" title="North Atlantic Gyre">North Atlantic Gyre</a></li> <li><a href="/wiki/South_Atlantic_Gyre" title="South Atlantic Gyre">South Atlantic Gyre</a></li> <li><a href="/wiki/North_Pacific_Gyre" title="North Pacific Gyre">North Pacific Gyre</a></li> <li><a href="/wiki/South_Pacific_Gyre" title="South Pacific Gyre">South Pacific Gyre</a></li></ul> </div></td></tr><tr><th scope="row" class="navbox-group" style="width:1%">Other gyres</th><td class="navbox-list-with-group navbox-list navbox-odd" style="width:100%;padding:0"><div style="padding:0 0.25em"> <ul><li><a href="/wiki/Beaufort_Gyre" title="Beaufort Gyre">Beaufort Gyre</a></li> <li><a href="/wiki/Ross_Gyre" title="Ross Gyre">Ross Gyre</a></li> <li><a href="/wiki/Weddell_Gyre" title="Weddell Gyre">Weddell Gyre</a></li></ul> </div></td></tr></tbody></table><div></div></td></tr><tr><th scope="row" class="navbox-group" style="width:1%">Related</th><td class="navbox-list-with-group navbox-list navbox-even hlist" style="width:100%;padding:0"><div style="padding:0 0.25em"> <ul><li><a href="/wiki/Atmospheric_circulation" title="Atmospheric circulation">Atmospheric circulation</a></li> <li><a href="/wiki/Boundary_current" title="Boundary current">Boundary current</a></li> <li><a href="/wiki/Coriolis_force" title="Coriolis force">Coriolis force</a></li> <li><a href="/wiki/Ekman_transport" title="Ekman transport">Ekman transport</a></li> <li><a href="/wiki/Marine_debris" title="Marine debris">Marine debris</a></li> <li><a href="/wiki/Garbage_patch" title="Garbage patch">Marine garbage patches</a> <ul><li><a href="/wiki/Great_Pacific_Garbage_Patch" title="Great Pacific Garbage Patch">Great Pacific</a></li> <li><a href="/wiki/Indian_Ocean_garbage_patch" title="Indian Ocean garbage patch">Indian Ocean</a></li> <li><a href="/wiki/North_Atlantic_garbage_patch" title="North Atlantic garbage patch">North Atlantic</a></li> <li><a href="/wiki/South_Pacific_garbage_patch" title="South Pacific garbage patch">South Pacific</a></li></ul></li> <li><a href="/wiki/Thermohaline_circulation" title="Thermohaline circulation">Thermohaline circulation</a></li></ul> </div></td></tr><tr><td class="navbox-abovebelow" colspan="2"><div><b><span class="nowrap"><span class="noviewer" typeof="mw:File"><a href="/wiki/File:Aegopodium_podagraria1_ies.jpg" class="mw-file-description"><img alt="icon" src="//upload.wikimedia.org/wikipedia/commons/thumb/b/bf/Aegopodium_podagraria1_ies.jpg/32px-Aegopodium_podagraria1_ies.jpg" decoding="async" width="32" height="28" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/b/bf/Aegopodium_podagraria1_ies.jpg/48px-Aegopodium_podagraria1_ies.jpg 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/b/bf/Aegopodium_podagraria1_ies.jpg/64px-Aegopodium_podagraria1_ies.jpg 2x" data-file-width="800" data-file-height="700" /></a></span> </span><a href="/wiki/Portal:Environment" title="Portal:Environment">Environment&#32;portal</a>&#160;&#160;<span class="nowrap"><span class="noviewer" typeof="mw:File"><a href="/wiki/File:Waves_in_pacifica_1.jpg" class="mw-file-description"><img alt="icon" src="//upload.wikimedia.org/wikipedia/commons/thumb/4/45/Waves_in_pacifica_1.jpg/32px-Waves_in_pacifica_1.jpg" decoding="async" width="32" height="22" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/4/45/Waves_in_pacifica_1.jpg/48px-Waves_in_pacifica_1.jpg 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/4/45/Waves_in_pacifica_1.jpg/64px-Waves_in_pacifica_1.jpg 2x" data-file-width="2000" data-file-height="1358" /></a></span> </span><a href="/wiki/Portal:Oceans" title="Portal:Oceans">Oceans&#32;portal</a></b></div></td></tr></tbody></table></div> <!-- NewPP limit report Parsed by mw‐web.codfw.main‐5857dfdcd6‐flfxn Cached time: 20241203071409 Cache expiry: 2592000 Reduced expiry: false Complications: [vary‐revision‐sha1, show‐toc] CPU time usage: 0.654 seconds Real time usage: 0.807 seconds Preprocessor visited node count: 2066/1000000 Post‐expand include size: 86727/2097152 bytes Template argument size: 1179/2097152 bytes Highest expansion depth: 12/100 Expensive parser function count: 4/500 Unstrip recursion depth: 1/20 Unstrip post‐expand size: 77967/5000000 bytes Lua time usage: 0.425/10.000 seconds Lua memory usage: 8713600/52428800 bytes Number of Wikibase entities loaded: 0/400 --> <!-- Transclusion expansion time report (%,ms,calls,template) 100.00% 697.592 1 -total 24.29% 169.451 10 Template:Cite_journal 23.73% 165.564 1 Template:Reflist 19.11% 133.305 3 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