{"id":73,"date":"2019-04-22T10:17:45","date_gmt":"2019-04-22T10:17:45","guid":{"rendered":"http:\/\/erik-behrens.de\/?page_id=73"},"modified":"2023-02-19T21:41:52","modified_gmt":"2023-02-19T21:41:52","slug":"presentations","status":"publish","type":"page","link":"https:\/\/erik-behrens.de\/?page_id=73","title":{"rendered":"Presentations"},"content":{"rendered":"\n<p><strong> <font color=#A8A8A8>The response of the Subtropical Front to changes in the Southern Hemisphere Westerly Winds\u2013Evidence from models and observations, DRAKKAR 2023, online, 012\/2023<\/p>\n<p><strong> <font color=#A8A8A8>The response of the Subtropical Front to changes in the Southern Hemisphere Westerly Winds\u2013Evidence from models and observations, AMOS, Adelaide, AUS, 12\/2022<\/p>\n<p><strong> <font color=#A8A8A8>The Impact of Sea-Ice Drift and Ocean&nbsp;Circulation on Dispersal of Toothfish Eggs and Juveniles in the Ross Gyre and&nbsp;Amundsen Sea, ICSHMO, online, 06\/2022<\/p>\n<p><strong> <font color=#A8A8A8>The Impact of Sea-Ice Drift and Ocean&nbsp;Circulation on Dispersal of Toothfish Eggs and Juveniles in the Ross Gyre and&nbsp;Amundsen Sea, BAS polar seminar, online, 10\/2021<\/p>\n<p><b style=\"text-align: justify; font-family: var( --e-global-typography-text-font-family ), Sans-serif; font-size: 1rem;\">Projections of future marine heatwaves for the oceans around New Zealand and Australia using New Zealand\u2019s Earth System Model, CLEX meeting, online, 9\/2021<\/b><\/p>\n<p><b>The Impact of Sea-Ice Drift and Ocean Circulation on Dispersal of Toothfish Eggs and Juveniles in the Ross Gyre and Amundsen Sea, Antarctic New Zealand, ChCh, 4\/2021<\/b><em><strong><br><\/strong><\/em><\/p>\n<p><em><strong>Variability of the Subtropical Front around New Zealand linked to the meridional transports of heat and freshwater through the Tasman Sea , AMOS, Freemantle, Australia, 2\/2020<\/strong> <\/em><\/p>\n<p>\n\n\n<p><\/p>\n\n\n<\/p>\n<p><em><strong>Meridional Oceanic Heat Transport Influences Marine Heatwaves in the Tasman Sea on Interannual to Decadal Timescales , AMOS, Freemantle, Australia, 2\/2020 <\/strong><\/em><\/p>\n<p>\n\n\n<p><\/p>\n\n\n<\/p>\n<p><em><strong>Meridional Oceanic Heat Transport Influences Marine Heatwaves in the Tasman Sea on Interannual to Decadal Timescales , MetSOC, WLG, NZ, 11\/2019 <\/strong><\/em><\/p>\n<p>\n\n\n<p><\/p>\n\n\n<\/p>\n<p><em><strong>New Zealand Earth System Model, JMMP, MetOffice, Exter, UK 10\/2019<\/strong><\/em><\/p>\n<p>\n\n\n<p><\/p>\n\n\n<\/p>\n<p><strong>NIWA seminar, NIWA, WLG, NZ, 7\/2019<\/strong><\/p>\n<p>\n\n\n<p><\/p>\n\n\n<\/p>\n<p><strong>Meridional Oceanic Heat Transport Influences Marine Heatwaves in the Tasman Sea on Interannual to Decadal Timescales , NZMSS, Dunedin, NZ, 6\/2019<\/strong><\/p>\n<p>\n\n\n<p><\/p>\n\n\n<\/p>\n<p style=\"text-align: left;\"><strong>Meridional Oceanic Heat Transport Influences Marine Heatwaves in the Tasman Sea on Interannual to Decadal Timescales , EGU, Vienna, Austria 4\/2019<\/strong><\/p>\n<p>\n\n\n<p><\/p>\n\n\n<\/p>\n<p><strong>Ocean Modelling from the Ross to the Tasman Sea, BAS, Cambridge, UK, 10\/2018<\/strong><\/p>\n<p>\n\n\n<p><\/p>\n\n\n<\/p>\n<p><strong>Convection in the Southern Ocean \u2013 What controls it?, POLAR2018, Davos, Switzerland, 6\/2018<\/strong><\/p>\n<p>\n\n\n<p><\/p>\n\n\n<\/p>\n<p><strong>DSC seminar, NIWA, WLG, NZ, 6\/2018<\/strong><\/p>\n<p>\n\n\n<p><\/p>\n\n\n<\/p>\n<p><strong>Oceanic Heat Waves around New Zealand, GEWEX, Canmore, Canada, 5\/2018<\/strong><\/p>\n<p>\n\n\n<p><\/p>\n\n\n<\/p>\n<p><strong>Seasonal to interannual variability of the Subtropical Front around New Zealand, PCCC , Wellington, NZ, 2\/2018<\/strong><\/p>\n<p>\n\n\n<p><\/p>\n\n\n<\/p>\n<p><strong>Convection in the Southern Ocean \u2013 What controls it?, AMOS-ICSHMO, Sydney, Australia, 2\/2018<\/strong><\/p>\n<p>\n\n\n<p><\/p>\n\n\n<\/p>\n<p><strong>Seasonal to interannual variability of the Subtropical Front around New Zealand, AMOS-ICSHMO, Sydney, Australia, 2\/2018<\/strong><\/p>\n<p>\n\n\n<p><\/p>","protected":false},"excerpt":{"rendered":"<p>The response of the Subtropical Front to changes in the Southern Hemisphere Westerly Winds\u2013Evidence from models and observations, DRAKKAR 2023, online, 012\/2023 The response of the Subtropical Front to changes in the Southern Hemisphere Westerly Winds\u2013Evidence from models and observations, AMOS, Adelaide, AUS, 12\/2022 The Impact of Sea-Ice Drift and Ocean&nbsp;Circulation on Dispersal of Toothfish &hellip; <\/p>\n<p class=\"link-more\"><a href=\"https:\/\/erik-behrens.de\/?page_id=73\" class=\"more-link\">Continue reading<span class=\"screen-reader-text\"> &#8222;Presentations&#8220;<\/span><\/a><\/p>\n","protected":false},"author":1,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":[],"_links":{"self":[{"href":"https:\/\/erik-behrens.de\/index.php?rest_route=\/wp\/v2\/pages\/73"}],"collection":[{"href":"https:\/\/erik-behrens.de\/index.php?rest_route=\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/erik-behrens.de\/index.php?rest_route=\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/erik-behrens.de\/index.php?rest_route=\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/erik-behrens.de\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=73"}],"version-history":[{"count":24,"href":"https:\/\/erik-behrens.de\/index.php?rest_route=\/wp\/v2\/pages\/73\/revisions"}],"predecessor-version":[{"id":12769,"href":"https:\/\/erik-behrens.de\/index.php?rest_route=\/wp\/v2\/pages\/73\/revisions\/12769"}],"wp:attachment":[{"href":"https:\/\/erik-behrens.de\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=73"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}