{"id":592,"date":"2024-08-13T13:56:47","date_gmt":"2024-08-13T04:56:47","guid":{"rendered":"https:\/\/ocean.hanyang.ac.kr\/?post_type=labs&#038;p=592"},"modified":"2025-10-24T19:01:13","modified_gmt":"2025-10-24T10:01:13","slug":"%ea%b8%b0%ed%9b%84%eb%aa%a8%eb%8d%b8%eb%a7%81-%ec%97%b0%ea%b5%ac%ec%8b%a4","status":"publish","type":"labs","link":"https:\/\/ocean.hanyang.ac.kr\/en\/labs\/%ea%b8%b0%ed%9b%84%eb%aa%a8%eb%8d%b8%eb%a7%81-%ec%97%b0%ea%b5%ac%ec%8b%a4\/","title":{"rendered":"Ocean-Climate Dynamics Lab"},"content":{"rendered":"<h5>introduction<\/h5>\n<p>Hanyang University&#039;s ERICA Climate Modeling Laboratory is studying polar sea ice dynamics and changes in polar sea ice-ocean circulation due to climate change.<\/p>\n<ol>\n<li>Interactions between Arctic and Antarctic sea ice and ocean circulation:\n<ul>\n<li>Atlantic Meridional Overturning Circulation<\/li>\n<li>Antarctic Bottom Water formation<\/li>\n<\/ul>\n<\/li>\n<li>Ocean circulation changes due to reduction in Arctic and Antarctic sea ice<\/li>\n<\/ol>\n<h5>Field of study<\/h5>\n<h6>sea ice dynamics<\/h6>\n<p><img fetchpriority=\"high\" decoding=\"async\" class=\"alignnone size-full wp-image-1607\" src=\"https:\/\/ocean.hanyang.ac.kr\/wp-content\/uploads\/2024\/08\/Wind-Ice_angle.png\" alt=\"\" width=\"521\" height=\"409\" srcset=\"https:\/\/ocean.hanyang.ac.kr\/wp-content\/uploads\/2024\/08\/Wind-Ice_angle.png 521w, https:\/\/ocean.hanyang.ac.kr\/wp-content\/uploads\/2024\/08\/Wind-Ice_angle-300x236.png 300w, https:\/\/ocean.hanyang.ac.kr\/wp-content\/uploads\/2024\/08\/Wind-Ice_angle-200x157.png 200w\" sizes=\"(max-width: 521px) 100vw, 521px\" \/><\/p>\n<p>* Park, H.-S. and AL Stewart, 2016: An analytical model for wind-driven Arctic summer sea ice drift, The Cryosphere, 10, 227-244.<\/p>\n<p>&nbsp;<\/p>\n<h6>Antarctic Bottom water formation<\/h6>\n<p><img decoding=\"async\" class=\"alignnone size-full wp-image-1608\" src=\"https:\/\/ocean.hanyang.ac.kr\/wp-content\/uploads\/2024\/08\/123.png\" alt=\"\" width=\"574\" height=\"766\" srcset=\"https:\/\/ocean.hanyang.ac.kr\/wp-content\/uploads\/2024\/08\/123.png 574w, https:\/\/ocean.hanyang.ac.kr\/wp-content\/uploads\/2024\/08\/123-225x300.png 225w, https:\/\/ocean.hanyang.ac.kr\/wp-content\/uploads\/2024\/08\/123-200x267.png 200w, https:\/\/ocean.hanyang.ac.kr\/wp-content\/uploads\/2024\/08\/123-487x650.png 487w\" sizes=\"(max-width: 574px) 100vw, 574px\" \/><\/p>\n<p>Jeong. H., S.-S. Lee, *H.-S. Park, and AL Stewart, 2023: Future changes in Antarctic coastal polynyas and bottom water formation simulated by a high-resolution coupled model. Communications Earth &amp; Environment. 4(490).<\/p>","protected":false},"template":"","meta":{"_acf_changed":false},"class_list":["post-592","labs","type-labs","status-publish","hentry"],"acf":[],"_links":{"self":[{"href":"https:\/\/ocean.hanyang.ac.kr\/en\/wp-json\/wp\/v2\/labs\/592","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/ocean.hanyang.ac.kr\/en\/wp-json\/wp\/v2\/labs"}],"about":[{"href":"https:\/\/ocean.hanyang.ac.kr\/en\/wp-json\/wp\/v2\/types\/labs"}],"wp:attachment":[{"href":"https:\/\/ocean.hanyang.ac.kr\/en\/wp-json\/wp\/v2\/media?parent=592"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}