{"id":468,"date":"2021-04-07T22:56:21","date_gmt":"2021-04-07T22:56:21","guid":{"rendered":"http:\/\/sites.rutgers.edu\/kyle-mattingly\/?page_id=468"},"modified":"2021-04-10T06:36:38","modified_gmt":"2021-04-10T06:36:38","slug":"antarctica","status":"publish","type":"page","link":"https:\/\/sites.rutgers.edu\/kyle-mattingly\/research\/antarctica\/","title":{"rendered":"Antarctica"},"content":{"rendered":"<h3>Antarctic coupled ocean-atmosphere-cryosphere extremes<\/h3>\n<p>Like the Arctic, the Southern Hemisphere high latitudes are home to a major land ice mass and seasonally varying sea ice cover. The Antarctic Ice Sheet is the world\u2019s largest and is buttressed by numerous floating ice shelves, while the sea ice cover of the Southern Ocean changes more dramatically between the winter and summer than in the Arctic. My colleagues and I have been researching the interactions between atmospheric extreme events and these components of the land and ocean cryosphere. We have found that repeated atmospheric river events in 2017 triggered the opening of a rare polynya in an area of the Southern Ocean preconditioned by oceanic conditions in previous years, and that a series of extreme cyclones contributed to the 2019 calving of a massive iceberg from the Amery Ice Shelf through their impact on sea surface slope. Future studies will further examine interactions between ocean-atmosphere coupled extreme events and the Antarctic cryosphere.<\/p>\n<p>&nbsp;<\/p>\n<figure id=\"attachment_499\" aria-describedby=\"caption-attachment-499\" style=\"width: 708px\" class=\"wp-caption aligncenter\"><a href=\"http:\/\/sites.rutgers.edu\/kyle-mattingly\/wp-content\/uploads\/sites\/656\/2021\/04\/F20_Sci_Adv_fig_1.jpg\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-499\" src=\"http:\/\/sites.rutgers.edu\/kyle-mattingly\/wp-content\/uploads\/sites\/656\/2021\/04\/F20_Sci_Adv_fig_1-1024x869.jpg\" alt=\"Weddell polynya\" width=\"708\" height=\"601\" srcset=\"https:\/\/sites.rutgers.edu\/kyle-mattingly\/wp-content\/uploads\/sites\/656\/2021\/04\/F20_Sci_Adv_fig_1-1024x869.jpg 1024w, https:\/\/sites.rutgers.edu\/kyle-mattingly\/wp-content\/uploads\/sites\/656\/2021\/04\/F20_Sci_Adv_fig_1-300x255.jpg 300w, https:\/\/sites.rutgers.edu\/kyle-mattingly\/wp-content\/uploads\/sites\/656\/2021\/04\/F20_Sci_Adv_fig_1-768x652.jpg 768w, https:\/\/sites.rutgers.edu\/kyle-mattingly\/wp-content\/uploads\/sites\/656\/2021\/04\/F20_Sci_Adv_fig_1.jpg 1050w\" sizes=\"(max-width: 708px) 100vw, 708px\" \/><\/a><figcaption id=\"caption-attachment-499\" class=\"wp-caption-text\">Satellite imagery of atmospheric rivers during development of the 2017 Weddell Sea polynya, along with images of the 1974 and 2017 polynyas.<br \/>From <a href=\"https:\/\/advances.sciencemag.org\/content\/6\/46\/eabc2695\">Francis et al. 2020<\/a>, <em>Science Advances<\/em>, reproduced under a <a href=\"https:\/\/creativecommons.org\/licenses\/by-nc\/4.0\/\">Creative Commons Attribution NonCommercial License 4.0<\/a> (CC BY-NC).<\/figcaption><\/figure>\n<p>&nbsp;<\/p>\n<div style=\"text-align: center\">\n<figure style=\"width: 550px\" class=\"wp-caption alignnone\"><iframe loading=\"lazy\" title=\"Weddell Polynya IVT animation, Aug-Sept 2017\" width=\"500\" height=\"375\" src=\"https:\/\/www.youtube.com\/embed\/Bh-RUAgnpzw?feature=oembed\" frameborder=\"0\" allow=\"accelerometer; autoplay; clipboard-write; encrypted-media; gyroscope; picture-in-picture; web-share\" referrerpolicy=\"strict-origin-when-cross-origin\" allowfullscreen><\/iframe><figcaption class=\"wp-caption-text\">Animation of atmospheric rivers accompanying Weddell Sea polynya opening in September 2017. <em>Note: If video appears blurred, trying changing quality to 720p<\/em>.<\/figcaption><\/figure>\n<\/div>\n<p>&nbsp;<\/p>\n<figure id=\"attachment_498\" aria-describedby=\"caption-attachment-498\" style=\"width: 810px\" class=\"wp-caption aligncenter\"><a href=\"http:\/\/sites.rutgers.edu\/kyle-mattingly\/wp-content\/uploads\/sites\/656\/2021\/04\/F21_TC_fig_1.png\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-498\" src=\"http:\/\/sites.rutgers.edu\/kyle-mattingly\/wp-content\/uploads\/sites\/656\/2021\/04\/F21_TC_fig_1-1024x633.png\" alt=\"Amery Ice Shelf calving\" width=\"810\" height=\"501\" srcset=\"https:\/\/sites.rutgers.edu\/kyle-mattingly\/wp-content\/uploads\/sites\/656\/2021\/04\/F21_TC_fig_1-1024x633.png 1024w, https:\/\/sites.rutgers.edu\/kyle-mattingly\/wp-content\/uploads\/sites\/656\/2021\/04\/F21_TC_fig_1-300x185.png 300w, https:\/\/sites.rutgers.edu\/kyle-mattingly\/wp-content\/uploads\/sites\/656\/2021\/04\/F21_TC_fig_1-768x475.png 768w, https:\/\/sites.rutgers.edu\/kyle-mattingly\/wp-content\/uploads\/sites\/656\/2021\/04\/F21_TC_fig_1.png 1053w\" sizes=\"(max-width: 810px) 100vw, 810px\" \/><\/a><figcaption id=\"caption-attachment-498\" class=\"wp-caption-text\">Satellite imagery of Amery Ice Shelf calving event in September 2019.<br \/>From <a href=\"https:\/\/tc.copernicus.org\/preprints\/tc-2020-219\/\">Francis et al. 2021<\/a>, <em>The Cryosphere<\/em>, reproduced under a <a href=\"https:\/\/creativecommons.org\/licenses\/by-nc\/4.0\/\">Creative Commons Attribution NonCommercial License 4.0<\/a> (CC BY-NC).<\/figcaption><\/figure>\n<p>&nbsp;<\/p>\n<div style=\"text-align: center\">\n<figure style=\"width: 550px\" class=\"wp-caption alignnone\"><iframe loading=\"lazy\" title=\"Wind animation September 2019 Amery Ice Shelf calving\" width=\"500\" height=\"375\" src=\"https:\/\/www.youtube.com\/embed\/tNGaAKU6OT4?feature=oembed\" frameborder=\"0\" allow=\"accelerometer; autoplay; clipboard-write; encrypted-media; gyroscope; picture-in-picture; web-share\" referrerpolicy=\"strict-origin-when-cross-origin\" allowfullscreen><\/iframe><figcaption class=\"wp-caption-text\">Animation of mean sea level pressure and 10-meter wind during Amery Ice Shelf calving in September 2019. <em>Note: If video appears blurred, trying changing quality to 720p<\/em>.<\/figcaption><\/figure>\n<\/div>\n<p>&nbsp;<\/p>\n<h4>Read more:<\/h4>\n<ul>\n<li><a href=\"https:\/\/advances.sciencemag.org\/content\/6\/46\/eabc2695\">Francis et al., 2020<\/a> (<em>Science Advances<\/em>): On the crucial role of atmospheric rivers in the two major Weddell Polynya events in 1973 and 2017 in Antarctica<\/li>\n<li><a href=\"https:\/\/tc.copernicus.org\/preprints\/tc-2020-219\/\">Francis et al., 2021<\/a> (<em>The Cryosphere<\/em>): Atmospheric extremes caused high oceanward sea-surface slope triggering the biggest calving event in more than 50 years at the Amery Ice shelf<\/li>\n<\/ul>\n","protected":false},"excerpt":{"rendered":"<p>Antarctic coupled ocean-atmosphere-cryosphere extremes Like the Arctic, the Southern Hemisphere high latitudes are home to a major land ice mass and seasonally varying sea ice cover. The Antarctic Ice Sheet &hellip; <a href=\"https:\/\/sites.rutgers.edu\/kyle-mattingly\/research\/antarctica\/\" class=\"\">Read More<\/a><\/p>\n","protected":false},"author":1641,"featured_media":0,"parent":365,"menu_order":1,"comment_status":"closed","ping_status":"closed","template":"template-custom.php","meta":{"_acf_changed":false,"footnotes":""},"class_list":["post-468","page","type-page","status-publish","hentry"],"acf":[],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v23.5 - https:\/\/yoast.com\/wordpress\/plugins\/seo\/ -->\n<title>Antarctica - Kyle Mattingly<\/title>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/sites.rutgers.edu\/kyle-mattingly\/research\/antarctica\/\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Antarctica - Kyle Mattingly\" \/>\n<meta property=\"og:description\" content=\"Antarctic coupled ocean-atmosphere-cryosphere extremes Like the Arctic, the Southern Hemisphere high latitudes are home to a major land ice mass and seasonally varying sea ice cover. 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