{"id":10641,"date":"1970-01-01T00:00:00","date_gmt":"1970-01-01T00:00:00","guid":{"rendered":"https:\/\/www.mercator-ocean.eu\/sea-ice-bulletin-2\/"},"modified":"1970-01-01T00:00:00","modified_gmt":"1970-01-01T00:00:00","slug":"sea-ice-bulletin-2","status":"publish","type":"post","link":"https:\/\/www.mercator-ocean.eu\/fr\/sea-ice-bulletin-2\/","title":{"rendered":"Sea Ice Bulletin (2)"},"content":{"rendered":"<div style=\"margin-top: 0px; margin-bottom: 0px;\" class=\"sharethis-inline-share-buttons\" ><\/div>\n<div class=\"wp-block-cover aligncenter has-background-dim-20 has-background-dim\" style=\"background-image:url(https:\/\/www.mercator-ocean.eu\/wp-content\/uploads\/2024\/02\/BG-4-min.png)\"><div class=\"wp-block-cover__inner-container is-layout-flow wp-block-cover-is-layout-flow\">\n<div class=\"wp-block-columns is-layout-flex wp-container-core-columns-is-layout-28f84493 wp-block-columns-is-layout-flex\">\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:100%\">\n<div style=\"height:30px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n\n<div class=\"wp-block-image\"><figure class=\"aligncenter size-large is-resized\"><img fetchpriority=\"high\" decoding=\"async\" src=\"https:\/\/www.mercator-ocean.eu\/wp-content\/uploads\/2024\/02\/Sea-Ice-Bulletin-compressed-700x700.png\" alt=\"\" class=\"wp-image-32998\" width=\"227\" height=\"227\"\/><\/figure><\/div>\n<\/div>\n<\/div>\n\n\n\n<p class=\"has-text-align-center\" style=\"font-size:18px\">&nbsp;<\/p>\n<\/div><\/div>\n\n\n\n<div style=\"height:50px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n\n<div class=\"wp-block-columns has-text-color is-layout-flex wp-container-core-columns-is-layout-28f84493 wp-block-columns-is-layout-flex\" style=\"color:#000000\">\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:100%\">\n<div class=\"wp-block-columns has-background is-layout-flex wp-container-core-columns-is-layout-28f84493 wp-block-columns-is-layout-flex\" style=\"background-color:#d2ebf9\">\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:2%\"><\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:96%\">\n<div style=\"height:10px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n\n<h3 class=\"wp-block-heading\"><strong>Key take-aways<\/strong><\/h3>\n\n\n\n<ul class=\"wp-block-list\"><li>Sea ice cover in the Antarctic has reached its annual minimum extent on the 19th of February, <strong>20%&nbsp;<\/strong>below the long-term average (1993-2010).<\/li><li>Sea Ice volume is currently at <strong>1.18 thousand km\u00b3<\/strong>, <strong>47%<\/strong> lower the long-term average (1993-2010).<\/li><li>February 2024 remains another year of low sea ice extent and volume for the Antarctic.<\/li><\/ul>\n\n\n\n<p><\/p>\n\n\n\n<div style=\"height:10px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n<\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:2%\"><\/div>\n<\/div>\n<\/div>\n<\/div>\n\n\n\n<h2 class=\"has-text-align-center wp-block-heading\"><strong>Sea Ice Extent<\/strong><\/h2>\n\n\n\n<div style=\"height:20px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n\n<div class=\"wp-block-columns is-layout-flex wp-container-core-columns-is-layout-28f84493 wp-block-columns-is-layout-flex\">\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\">\n<div class=\"wp-block-image\"><figure class=\"aligncenter size-large\"><img decoding=\"async\" src=\"https:\/\/www.mercator-ocean.eu\/wp-content\/uploads\/2024\/02\/image-4-1.png\" alt=\"\" class=\"wp-image-33411\"\/><figcaption><em>Figure 1: The 1993-2024 Antarctic daily sea ice extent. Global 1\/12\u00b0 forecasting and reanalysis systems. Source:&nbsp;European Union, Copernicus Marine Service Data (20\/02\/2024) I \u00a9 Mercator Ocean<\/em><\/figcaption><\/figure><\/div>\n<\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\">\n<div class=\"wp-block-image\"><figure class=\"aligncenter size-large\"><img decoding=\"async\" src=\"https:\/\/www.mercator-ocean.eu\/wp-content\/uploads\/2024\/02\/image-5.png\" alt=\"\" class=\"wp-image-33413\"\/><figcaption><em>Figure 2: The 1993-2024 Antarctic Sea ice extent daily anomaly (using 1993-2010 climatology). Global 1\/12\u00b0 forecasting and reanalysis systems. Source:&nbsp;<\/em>European Union, Copernicus Marine Service Data (date) I \u00a9 Mercator Ocean&nbsp;<\/figcaption><\/figure><\/div>\n<\/div>\n<\/div>\n\n\n\n<p>Antarctic sea ice cover has reached its annual minimum extent of 1.86 million km\u00b2 on the <a rel=\"noreferrer noopener\" target=\"_blank\">19<em>th<\/em><\/a>&nbsp; of February 2024.&nbsp; This represents a loss of 0.49 million km\u00b2 compared to the 1993-2010 long term average (2.36 million km\u00b2), or 20% less the same period. February 2024 shows another exceptional low extent (after the record-low in February 2023, since satellite record).<\/p>\n\n\n\n<p><\/p>\n\n\n\n<hr class=\"wp-block-separator is-style-dots\"\/>\n\n\n\n<h2 class=\"has-text-align-center wp-block-heading\"><strong>Sea Ice Concentration<\/strong><\/h2>\n\n\n\n<p>On the 20<em>th<\/em> of February 2024, the Antarctic Sea ice concentration (figure 2 red line) was noticeably below the long-term average between 1993 and 2010 (figure 2 black line) for the same date in the year. Compared to the 1993-2010 period, large areas of sea ice cover are missing in the Atlantic and Pacific sectors (figure 1).<\/p>\n\n\n\n<div class=\"wp-block-image\"><figure class=\"aligncenter size-large\"><img decoding=\"async\" src=\"https:\/\/www.mercator-ocean.eu\/wp-content\/uploads\/2024\/02\/image-6-1.png\" alt=\"\" class=\"wp-image-33427\"\/><figcaption><em>Figure 3: Antarctic Sea ice concentration (red) for 20th February 2024. The black line represents the 1993-2010 average (climatology) for the same date in the year. Global 1\/12\u00b0 forecasting (Lellouche, 2018) and reanalysis (Lellouche, 2022). Source:&nbsp;European Union, Copernicus Marine Service DataI \u00a9 Mercator Ocean<\/em><\/figcaption><\/figure><\/div>\n\n\n\n<div style=\"height:70px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n\n<h2 class=\"has-text-align-center wp-block-heading\"><strong>Sea Ice Volume<\/strong><\/h2>\n\n\n\n<div style=\"height:20px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n\n<div class=\"wp-block-columns is-layout-flex wp-container-core-columns-is-layout-28f84493 wp-block-columns-is-layout-flex\">\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\">\n<figure class=\"wp-block-image size-large\"><img decoding=\"async\" src=\"https:\/\/www.mercator-ocean.eu\/wp-content\/uploads\/2024\/02\/Image1.png\" alt=\"\" class=\"wp-image-33432\"\/><figcaption><em><em>Figure 4: The 1993-2024 Antarctic daily Sea ice volume. Global 1\/12\u00b0 forecasting and reanalysis systems. Source: Mercator Ocean International, Copernicus Marine Service.<\/em>&nbsp;<\/em><\/figcaption><\/figure>\n<\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\">\n<figure class=\"wp-block-image size-large\"><img decoding=\"async\" src=\"https:\/\/www.mercator-ocean.eu\/wp-content\/uploads\/2024\/02\/Image2.png\" alt=\"\" class=\"wp-image-33434\"\/><figcaption><em>Figure 5: The 1993-2024 Antarctic Sea ice volume daily anomaly (using 1993-2010 climatology). Global 1\/12\u00b0 forecasting and reanalysis systems. <\/em>European Union, Copernicus Marine Service Data I \u00a9 Mercator Ocean\u202f&nbsp;<\/figcaption><\/figure>\n<\/div>\n<\/div>\n\n\n\n<p>The Antarctic sea ice volume has reached its minimum volume of 1.18 thousand km\u00b3 on the 20th of February 2024.&nbsp; This represents a loss of 1.05 thousand km\u00b3 compared to the 1993-2010 long term average (2.24 thousand km3), or the equivalent to a 47% loss in sea ice volume. In the last two years, minimum sea ice volume in the Antarctic was 50% below the 1993-2020 yearly minimum average.&nbsp;<\/p>\n\n\n\n<h2 class=\"has-text-align-center wp-block-heading\"><strong>Antarctic Sea Ice Volume trend&nbsp;&nbsp;<\/strong><\/h2>\n\n\n\n<div class=\"wp-block-image\"><figure class=\"aligncenter size-large\"><img decoding=\"async\" src=\"https:\/\/www.mercator-ocean.eu\/wp-content\/uploads\/2024\/02\/Image3-700x700.png\" alt=\"\" class=\"wp-image-33439\"\/><figcaption><em>Figure 6: Antarctic sea ice volume yearly minimums in the Southern Hemisphere for the 1993-2024 period. The white dashed line represents the long-term trend.&nbsp;<\/em><\/figcaption><\/figure><\/div>\n\n\n\n<p>After nearly 30 years of a highly variable sea ice cover in the Antarctic region throughout the year, and therefore no clear trend, the last few years have shown a slight negative trend, particularly when considering the annual minimum value (measured in February). The 1993-2024 trend (figure 6) represents a loss of 0.25 thousand km\u00b3 per decade.&nbsp;<\/p>\n\n\n\n<p>Monitoring the sea ice cover in this period of the year is crucial because it represents the annual minimum sea ice coverage in the Antarctic. These measurements provide a vital indicator on the changes happening every year, as they serve as a reference for seasonal contrasts in sea ice cover.&nbsp;<\/p>\n\n\n\n<p><\/p>\n\n\n\n<p>Recent changes in the Antarctic Sea ice extent trend are, according to scientists, a probable consequence of a decades-long ocean warming trend and atmospheric circulation changes (Eayrs et al, 2019). Other processes may be contributing to the acceleration in sea ice loss in the Antarctic, including marine heat wave events. No scientific study has demonstrated that Antarctic Sea ice loss can be attributed to the occurrence of marine heat waves. However, the study of Zhang et al., 2022 shows that the warming of subsurface water masses in the Southern Ocean could play a role in sea ice melting.&nbsp;<\/p>\n\n\n\n<div style=\"height:70px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n\n<h3 class=\"wp-block-heading\">Antarctic Sea Ice Extent<\/h3>\n\n\n\n<hr class=\"wp-block-separator is-style-wide\"\/>\n\n\n\n<div style=\"height:20px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n\n<div class=\"wp-block-columns is-layout-flex wp-container-core-columns-is-layout-28f84493 wp-block-columns-is-layout-flex\">\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\">\n<p>Since the beginning of May, which is generally the beginning of a time when sea ice grows during the austral autumn and winter, Antarctic Sea ice is at a record-low. It sits at approximately 1.8 million km<sup>2<\/sup>&nbsp;below the long-term average (1993-2010). This year 2023, Antarctic Sea ice has reached its maximum annual extent on the 7<sup>th<\/sup>&nbsp;of September, extending to 16.8 million km<sup>2<\/sup>, which is 1.9 million of km<sup>2<\/sup>&nbsp;less compared to the 1993-2010 average for the same date.&nbsp;<strong>This corresponds to a sea ice loss of 3 times the size of France (all regions).<\/strong>&nbsp;Last year, 2022, was already at a low with 18.4 million km<sup>2<\/sup>&nbsp;of sea ice. This is the first time since the beginning of the satellite record (1979) that Antarctic sea ice extent is below 17 million km<sup>2<\/sup>.<\/p>\n<\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\">\n<p>The September 2023 maximum is at an unprecedented low and indicates that sea ice has not well been reformed in the cold season of the southern hemisphere. Figure 1 illustrates the Antarctic Sea ice concentration for the 7<sup>th<\/sup>&nbsp;of September 2023 in dark red well below the previous record-low in 2022 (orange line). These are both far below the sea ice concentration for the long-term average between1993-2010 (grey line) for the same date in the year. Compared to the 1993-2010 period, large areas of sea ice cover are missing in the Atlantic and Pacific sectors while it is slightly compensated in Bellingshausen Sea (figure 1).<\/p>\n<\/div>\n<\/div>\n\n\n\n<div style=\"height:70px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n\n<h3 class=\"wp-block-heading\">Subtitle 2<\/h3>\n\n\n\n<hr class=\"wp-block-separator is-style-wide\"\/>\n\n\n\n<div style=\"height:20px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n\n<div class=\"wp-block-columns is-layout-flex wp-container-core-columns-is-layout-28f84493 wp-block-columns-is-layout-flex\">\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\">\n<p>Since the beginning of May, which is generally the beginning of a time when sea ice grows during the austral autumn and winter, Antarctic Sea ice is at a record-low. It sits at approximately 1.8 million km<sup>2<\/sup>&nbsp;below the long-term average (1993-2010). This year 2023, Antarctic Sea ice has reached its maximum annual extent on the 7<sup>th<\/sup>&nbsp;of September, extending to 16.8 million km<sup>2<\/sup>, which is 1.9 million of km<sup>2<\/sup>&nbsp;less compared to the 1993-2010 average for the same date.&nbsp;<strong>This corresponds to a sea ice loss of 3 times the size of France (all regions).<\/strong>&nbsp;Last year, 2022, was already at a low with 18.4 million km<sup>2<\/sup>&nbsp;of sea ice. This is the first time since the beginning of the satellite record (1979) that Antarctic sea ice extent is below 17 million km<sup>2<\/sup>.<\/p>\n<\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\">\n<p>The September 2023 maximum is at an unprecedented low and indicates that sea ice has not well been reformed in the cold season of the southern hemisphere. Figure 1 illustrates the Antarctic Sea ice concentration for the 7<sup>th<\/sup>&nbsp;of September 2023 in dark red well below the previous record-low in 2022 (orange line). These are both far below the sea ice concentration for the long-term average between1993-2010 (grey line) for the same date in the year. Compared to the 1993-2010 period, large areas of sea ice cover are missing in the Atlantic and Pacific sectors while it is slightly compensated in Bellingshausen Sea (figure 1).<\/p>\n<\/div>\n<\/div>\n\n\n\n<div style=\"height:50px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n\n<hr class=\"wp-block-separator is-style-dots\"\/>\n\n\n\n<div style=\"height:50px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n\n<h2 class=\"has-text-align-center wp-block-heading\"><strong>Title 2<\/strong><\/h2>\n\n\n\n<div class=\"wp-block-image\"><figure class=\"aligncenter size-large is-resized\"><img decoding=\"async\" src=\"https:\/\/www.mercator-ocean.eu\/wp-content\/uploads\/2023\/12\/iStock-1475285952-1024x424.jpg\" alt=\"\" class=\"wp-image-32530\" width=\"1024\" height=\"424\"\/><figcaption>1475285952<\/figcaption><\/figure><\/div>\n\n\n\n<p>Since the beginning of May, which is generally the beginning of a time when sea ice grows during the austral autumn and winter, Antarctic Sea ice is at a record-low. It sits at approximately 1.8 million km<sup>2<\/sup>&nbsp;below the long-term average (1993-2010). This year 2023, Antarctic Sea ice has reached its maximum annual extent on the 7<sup>th<\/sup>&nbsp;of September, extending to 16.8 million km<sup>2<\/sup>, which is 1.9 million of km<sup>2<\/sup>&nbsp;less compared to the 1993-2010 average for the same date.&nbsp;<strong>This corresponds to a sea ice loss of 3 times the size of France (all regions).<\/strong>&nbsp;Last year, 2022, was already at a low with 18.4 million km<sup>2<\/sup>&nbsp;of sea ice. This is the first time since the beginning of the satellite record (1979) that Antarctic sea ice extent is below 17 million km<sup>2<\/sup>.<\/p>\n\n\n\n<div style=\"height:70px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n\n<h3 class=\"wp-block-heading\">Subtitle 1<\/h3>\n\n\n\n<hr class=\"wp-block-separator is-style-wide\"\/>\n\n\n\n<div style=\"height:20px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n\n<div class=\"wp-block-columns is-layout-flex wp-container-core-columns-is-layout-28f84493 wp-block-columns-is-layout-flex\">\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:66.66%\">\n<figure class=\"wp-block-image size-large\"><img decoding=\"async\" src=\"https:\/\/www.mercator-ocean.eu\/wp-content\/uploads\/2024\/02\/MicrosoftTeams-image-35-1-875x700.png\" alt=\"\" class=\"wp-image-33123\"\/><figcaption>jhgjhhv<\/figcaption><\/figure>\n<\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:33.33%\">\n<p>Since the beginning of May, which is generally the beginning of a time when sea ice grows during the austral autumn and winter, Antarctic Sea ice is at a record-low. It sits at approximately 1.8 million km<sup>2<\/sup>&nbsp;below the long-term average (1993-2010). This year 2023, Antarctic Sea ice has reached its maximum annual extent on the 7<sup>th<\/sup>&nbsp;of September, extending to 16.8 million km<sup>2<\/sup>, which is 1.9 million of km<sup>2<\/sup>&nbsp;less compared to the 1993-2010 average for the same date.&nbsp;<strong>This corresponds to a sea ice loss of 3 times the size of France (all regions).<\/strong>&nbsp;Last year, 2022, was already at a low with 18.4 million km<sup>2<\/sup>&nbsp;of sea ice. This is the first time since the beginning of the satellite record (1979) that Antarctic sea ice extent is below 17 million km<sup>2<\/sup>.<\/p>\n<\/div>\n<\/div>\n\n\n\n<p>Since the beginning of May, which is generally the beginning of a time when sea ice grows during the austral autumn and winter, Antarctic Sea ice is at a record-low. It sits at approximately 1.8 million km<sup>2<\/sup>&nbsp;below the long-term average (1993-2010). This year 2023, Antarctic Sea ice has reached its maximum annual extent on the 7<sup>th<\/sup>&nbsp;of September, extending to 16.8 million km<sup>2<\/sup>, which is 1.9 million of km<sup>2<\/sup>&nbsp;less compared to the 1993-2010 average for the same date.&nbsp;<strong>This corresponds to a sea ice loss of 3 times the size of France (all regions).<\/strong>&nbsp;Last year, 2022, was already at a low with 18.4 million km<sup>2<\/sup>&nbsp;of sea ice. This is the first time since the beginning of the satellite record (1979) that Antarctic sea ice extent is below 17 million km<sup>2<\/sup>.<\/p>\n\n\n\n<div style=\"height:70px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n\n<h3 class=\"wp-block-heading\">Subtitle 2<\/h3>\n\n\n\n<hr class=\"wp-block-separator is-style-wide\"\/>\n\n\n\n<div class=\"wp-block-image\"><figure class=\"aligncenter size-large is-resized\"><img decoding=\"async\" src=\"https:\/\/www.mercator-ocean.eu\/wp-content\/uploads\/2024\/02\/MicrosoftTeams-image-35-2-875x700.png\" alt=\"\" class=\"wp-image-33146\" width=\"647\" height=\"518\"\/><\/figure><\/div>\n\n\n\n<div class=\"wp-block-columns is-layout-flex wp-container-core-columns-is-layout-28f84493 wp-block-columns-is-layout-flex\">\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\">\n<p>Since the beginning of May, which is generally the beginning of a time when sea ice grows during the austral autumn and winter, Antarctic Sea ice is at a record-low. It sits at approximately 1.8 million km<sup>2<\/sup>&nbsp;below the long-term average (1993-2010). This year 2023, Antarctic Sea ice has reached its maximum annual extent on the 7<sup>th<\/sup>&nbsp;of September, extending to 16.8 million km<sup>2<\/sup>, which is 1.9 million of km<sup>2<\/sup>&nbsp;less compared to the 1993-2010 average for the same date.&nbsp;<strong>This corresponds to a sea ice loss of 3 times the size of France (all regions).<\/strong>&nbsp;Last year, 2022, was already at a low with 18.4 million km<sup>2<\/sup>&nbsp;of sea ice. This is the first time since the beginning of the satellite record (1979) that Antarctic sea ice extent is below 17 million km<sup>2<\/sup>.<\/p>\n<\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\">\n<p>The September 2023 maximum is at an unprecedented low and indicates that sea ice has not well been reformed in the cold season of the southern hemisphere. Figure 1 illustrates the Antarctic Sea ice concentration for the 7<sup>th<\/sup>&nbsp;of September 2023 in dark red well below the previous record-low in 2022 (orange line). These are both far below the sea ice concentration for the long-term average between1993-2010 (grey line) for the same date in the year. Compared to the 1993-2010 period, large areas of sea ice cover are missing in the Atlantic and Pacific sectors while it is slightly compensated in Bellingshausen Sea (figure 1).<\/p>\n<\/div>\n<\/div>\n\n\n\n<div style=\"height:20px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n\n<p>The September 2023 maximum is at an unprecedented low and indicates that sea ice has not well been reformed in the cold season of the southern hemisphere. Figure 1 illustrates the Antarctic Sea ice concentration for the 7<sup>th<\/sup>&nbsp;of September 2023 in dark red well below the previous record-low in 2022 (orange line). These are both far below the sea ice concentration for the long-term average between1993-2010 (grey line) for the same date in the year. Compared to the 1993-2010 period, large areas of sea ice cover are missing in the Atlantic and Pacific sectors while it is slightly compensated in Bellingshausen Sea (figure 1).<\/p>\n\n\n\n<div class=\"wp-block-columns has-text-color has-background is-layout-flex wp-container-core-columns-is-layout-28f84493 wp-block-columns-is-layout-flex\" style=\"background-color:#97c3dd;color:#000000\">\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:5%\"><\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:90%\">\n<div style=\"height:40px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n\n<div style=\"height:1px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n\n<div class=\"wp-block-columns has-content-bg-background-color has-background is-layout-flex wp-container-core-columns-is-layout-28f84493 wp-block-columns-is-layout-flex\">\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:100%\">\n<div style=\"height:5px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n\n<div class=\"wp-block-columns is-layout-flex wp-container-core-columns-is-layout-28f84493 wp-block-columns-is-layout-flex\">\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:90%\">\n<h2 class=\"wp-block-heading\">Forecasts for November 14<\/h2>\n\n\n\n<hr class=\"wp-block-separator is-style-wide\"\/>\n\n\n\n<figure class=\"wp-block-image alignwide size-large\"><img decoding=\"async\" src=\"https:\/\/www.mercator-ocean.eu\/wp-content\/uploads\/2023\/11\/categ_global_GLO12_ANA_2023-11-14-2-1024x561.jpg\" alt=\"\" class=\"wp-image-32250\"\/><figcaption>Figure 2:&nbsp;<em>Carte d\u2019anomalies hebdomadaires de temp\u00e9rature de surface pour la semaine du 07 au 14 Novembre 2023 pour l\u2019ensemble de l\u2019oc\u00e9an mondial. Analyse GLO12. Source: Mercator Ocean International.<\/em><\/figcaption><\/figure>\n\n\n\n<h4 class=\"wp-block-heading\">Global Ocean<\/h4>\n\n\n\n<hr class=\"wp-block-separator is-style-wide\"\/>\n\n\n\n<div class=\"wp-block-columns are-vertically-aligned-center is-layout-flex wp-container-core-columns-is-layout-28f84493 wp-block-columns-is-layout-flex\">\n<div class=\"wp-block-column is-vertically-aligned-center is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:50%\">\n<p>For November 14, MOi forecasts that the marine heatwave in the Tropical Atlantic will remain stable with moderate to strong categories. The marine heatwave in the Caribbean Sea is decreasing in intensity from strong to severe to moderate to strong. In the Southern Tropical Atlantic, a marine heatwave is appearing with moderate to strong levels.<br><br>In the Tropical Pacific, the situation remains stable. In the western tropical Pacific, the marine heatwave is becoming more intense, with locally extreme levels.<\/p>\n<\/div>\n\n\n\n<div class=\"wp-block-column is-vertically-aligned-center is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:50%\">\n<p>The marine heatwave in the North Pacific is diminishing in extent but remains at moderate to locally strong levels overall.<br><br>The marine heatwave in the south-west Indian Ocean is decreasing in extent in its eastern part. In the western part of the Indian Ocean, the marine heatwave is intensifying, reaching high levels over most of the area.<br><br>In the South-East Asian seas, the marine heatwave remains stable at strong to extreme levels.<\/p>\n<\/div>\n<\/div>\n\n\n\n<h4 class=\"wp-block-heading\">Europe Zone<\/h4>\n\n\n\n<hr class=\"wp-block-separator is-style-wide\"\/>\n\n\n\n<div class=\"wp-block-columns are-vertically-aligned-top is-layout-flex wp-container-core-columns-is-layout-28f84493 wp-block-columns-is-layout-flex\">\n<div class=\"wp-block-column is-vertically-aligned-top is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:50%\">\n<p>For November 14, the Mercator Ocean International (MOi) forecasting system predicts a slight re-intensification of the marine heatwave around the Iberian Peninsula and the Moroccan coast with moderate categories.<\/p>\n<\/div>\n\n\n\n<div class=\"wp-block-column is-vertically-aligned-top is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:50%\">\n<p>The marine heatwave in the western Mediterranean is easing. The eastern part of the basin remains stable with moderate to strong marine heatwaves.<br><br>In the South-East Asian seas, the marine heatwave remains stable at strong to extreme levels.<\/p>\n<\/div>\n<\/div>\n<\/div>\n<\/div>\n\n\n\n<div style=\"height:40px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n<\/div>\n<\/div>\n\n\n\n<div style=\"height:20px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n<\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:5%\"><\/div>\n<\/div>\n\n\n\n<div class=\"wp-block-columns are-vertically-aligned-center has-text-color has-background is-layout-flex wp-container-core-columns-is-layout-28f84493 wp-block-columns-is-layout-flex\" style=\"background-color:#f1f1f1;color:#2c2c2c\">\n<div class=\"wp-block-column is-vertically-aligned-center is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:10%\"><\/div>\n\n\n\n<div class=\"wp-block-column is-vertically-aligned-center is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:80%\">\n<div style=\"height:15px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n\n<div style=\"height:20px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n\n<p>\u21d2 Discover the <a href=\"https:\/\/www.mercator-ocean.eu\/en\/category\/mhw-bulletin\/\"><strong>Mercator Ocean Marine Heatwave Bulletin<\/strong><\/a>.<\/p>\n\n\n\n<div style=\"height:20px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n\n<h6 class=\"wp-block-heading\"><strong><em>Copernicus Marine products used:<\/em><\/strong><\/h6>\n\n\n\n<ul class=\"wp-block-list\"><li><em>GLORYS12V1 global ocean eddy-resolving (1\/12\u00b0 horizontal resolution, 50 vertical levels) reanalysis covering the altimetry (1993 onward).&nbsp;<a href=\"https:\/\/doi.org\/10.48670\/moi-00021\" target=\"_blank\" rel=\"noreferrer noopener\">https:\/\/doi.org\/10.48670\/moi-00021<\/a><\/em><\/li><li><em>The Operational Mercator global ocean analysis and forecast system at 1\/12 degree.&nbsp;<a href=\"https:\/\/doi.org\/10.48670\/moi-00016\" target=\"_blank\" rel=\"noreferrer noopener\">https:\/\/doi.org\/10.48670\/moi-00016<\/a><\/em><\/li><\/ul>\n\n\n\n<div style=\"height:30px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n\n<h6 class=\"wp-block-heading\"><strong><em>References:<\/em><\/strong><\/h6>\n\n\n\n<p><em>Zhang, L., Delworth, T.L., Yang, X.&nbsp;et al.&nbsp;The relative role of the subsurface Southern Ocean in driving negative Antarctic Sea ice extent anomalies in 2016\u20132021.&nbsp;Commun Earth Environ&nbsp;<strong>3<\/strong>, 302 (2022). https:\/\/doi.org\/10.1038\/s43247-022-00624-1<\/em><\/p>\n\n\n\n<p><em>Jean-Michel L, Eric G, Romain B\u00e9-B, Gilles G, Ang\u00e9lique M, Marie D, Cl\u00e9ment B, Mathieu H, Olivier LG, Charly R, Tony C, Charles-Emmanuel T, Florent G, Giovanni R, Mounir B, Yann D and Pierre-Yves LT (2021) The Copernicus Global 1\/12\u00b0 Oceanic and Sea Ice GLORYS12 Reanalysis. Front. Earth Sci. 9:698876. doi: 10.3389\/feart.2021.698876&nbsp;<\/em><\/p>\n\n\n\n<p><em>Lellouche, J.-M., Greiner, E., Le Galloudec, O., Garric, G., Regnier, C., Drevillon, M., Benkiran, M., Testut, C.-E., Bourdalle-Badie, R., Gasparin, F., Hernandez, O., Levier, B., Drillet, Y., Remy, E., and Le Traon, P.-Y.: Recent updates to the Copernicus Marine Service global ocean monitoring and forecasting real-time 1\u221512\u00b0 high-resolution system, Ocean Sci., 14, 1093\u20131126,&nbsp;<a href=\"https:\/\/doi.org\/10.5194\/os-14-1093-2018\" target=\"_blank\" rel=\"noreferrer noopener\">https:\/\/doi.org\/10.5194\/os-14-1093-2018<\/a>, 2018.<\/em><\/p>\n\n\n\n<div style=\"height:15px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n<\/div>\n\n\n\n<div class=\"wp-block-column is-vertically-aligned-center is-layout-flow wp-block-column-is-layout-flow\" style=\"flex-basis:10%\"><\/div>\n<\/div>\n\n\n<p><\/p>","protected":false},"excerpt":{"rendered":"<p>Key take-aways Sea ice cover in the Antarctic has reached its annual minimum extent on the 19th of February, 20%&nbsp;below the long-term average (1993-2010). Sea Ice volume is currently at 1.18 thousand km\u00b3, 47% lower the long-term average (1993-2010). February 2024 remains another year of low sea ice extent and volume for the Antarctic. Sea [&hellip;]<\/p>\n","protected":false},"author":2,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[40],"tags":[],"translation-status":[],"class_list":["post-10641","post","type-post","status-publish","format-standard","hentry","category-non-classe"],"acf":[],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v27.3 - https:\/\/yoast.com\/product\/yoast-seo-wordpress\/ -->\n<title>Sea Ice Bulletin (2) - Mercator Ocean International<\/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:\/\/www.mercator-ocean.eu\/fr\/sea-ice-bulletin-2\/\" \/>\n<meta property=\"og:locale\" content=\"fr_FR\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Sea Ice Bulletin (2) - Mercator Ocean International\" \/>\n<meta property=\"og:description\" content=\"Key take-aways Sea ice cover in the Antarctic has reached its annual minimum extent on the 19th of February, 20%&nbsp;below the long-term average (1993-2010). Sea Ice volume is currently at 1.18 thousand km\u00b3, 47% lower the long-term average (1993-2010). February 2024 remains another year of low sea ice extent and volume for the Antarctic. Sea [&hellip;]\" \/>\n<meta property=\"og:url\" content=\"https:\/\/www.mercator-ocean.eu\/fr\/sea-ice-bulletin-2\/\" \/>\n<meta property=\"og:site_name\" content=\"Mercator Ocean International\" \/>\n<meta property=\"article:publisher\" content=\"https:\/\/www.facebook.com\/MercatorOcean\" \/>\n<meta property=\"article:published_time\" content=\"1970-01-01T00:00:00+00:00\" \/>\n<meta property=\"og:image\" content=\"https:\/\/www.mercator-ocean.eu\/wp-content\/uploads\/2024\/02\/Sea-Ice-Bulletin-compressed-700x700.png\" \/>\n<meta name=\"author\" content=\"Damien Goubeau\" \/>\n<meta name=\"twitter:card\" content=\"summary_large_image\" \/>\n<meta name=\"twitter:creator\" content=\"@MercatorOcean\" \/>\n<meta name=\"twitter:site\" content=\"@MercatorOcean\" \/>\n<meta name=\"twitter:label1\" content=\"\u00c9crit par\" \/>\n\t<meta name=\"twitter:data1\" content=\"Damien Goubeau\" \/>\n\t<meta name=\"twitter:label2\" content=\"Dur\u00e9e de lecture estim\u00e9e\" \/>\n\t<meta name=\"twitter:data2\" content=\"11 minutes\" \/>\n<script type=\"application\/ld+json\" class=\"yoast-schema-graph\">{\"@context\":\"https:\\\/\\\/schema.org\",\"@graph\":[{\"@type\":\"Article\",\"@id\":\"https:\\\/\\\/www.mercator-ocean.eu\\\/fr\\\/sea-ice-bulletin-2\\\/#article\",\"isPartOf\":{\"@id\":\"https:\\\/\\\/www.mercator-ocean.eu\\\/fr\\\/sea-ice-bulletin-2\\\/\"},\"author\":{\"name\":\"Damien Goubeau\",\"@id\":\"https:\\\/\\\/www.mercator-ocean.eu\\\/fr\\\/#\\\/schema\\\/person\\\/8707759d6e2641e91ea76ae3fc537134\"},\"headline\":\"Sea Ice Bulletin (2)\",\"datePublished\":\"1970-01-01T00:00:00+00:00\",\"mainEntityOfPage\":{\"@id\":\"https:\\\/\\\/www.mercator-ocean.eu\\\/fr\\\/sea-ice-bulletin-2\\\/\"},\"wordCount\":2269,\"commentCount\":0,\"publisher\":{\"@id\":\"https:\\\/\\\/www.mercator-ocean.eu\\\/fr\\\/#organization\"},\"image\":{\"@id\":\"https:\\\/\\\/www.mercator-ocean.eu\\\/fr\\\/sea-ice-bulletin-2\\\/#primaryimage\"},\"thumbnailUrl\":\"https:\\\/\\\/www.mercator-ocean.eu\\\/wp-content\\\/uploads\\\/2024\\\/02\\\/Sea-Ice-Bulletin-compressed-700x700.png\",\"inLanguage\":\"fr-FR\",\"potentialAction\":[{\"@type\":\"CommentAction\",\"name\":\"Comment\",\"target\":[\"https:\\\/\\\/www.mercator-ocean.eu\\\/fr\\\/sea-ice-bulletin-2\\\/#respond\"]}]},{\"@type\":\"WebPage\",\"@id\":\"https:\\\/\\\/www.mercator-ocean.eu\\\/fr\\\/sea-ice-bulletin-2\\\/\",\"url\":\"https:\\\/\\\/www.mercator-ocean.eu\\\/fr\\\/sea-ice-bulletin-2\\\/\",\"name\":\"Sea Ice Bulletin (2) - 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