{"id":211462,"date":"2022-08-02T12:31:45","date_gmt":"2022-08-02T10:31:45","guid":{"rendered":"https:\/\/climatescience.press\/?p=211462"},"modified":"2022-08-02T12:31:46","modified_gmt":"2022-08-02T10:31:46","slug":"surplus-arctic-ice-july-2022","status":"publish","type":"post","link":"https:\/\/climatescience.press\/?p=211462","title":{"rendered":"Surplus Arctic Ice July 2022"},"content":{"rendered":"
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\"\"<\/figure>\n<\/div>\n\n\n

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The animation shows Arctic ice extents on day 212 (end of July) starting with 2007 and showing the lack of decline through yesterday.\u00a0 Years vary as to which regions retain more or less ice.\u00a0 For example, some years the Russian shelf seas (left side) are mostly open water on day 212.\u00a0 Kara and Barents seas (top side) fluctuate.\u00a0 The Northwest passage (bottom), melts early some years in Beaufort Sea, and CAA, but this year not so much. The graph below compares the July monthly ice extents 2007 to 2022 and compared to the SII 16-year average.<\/p>\n\n\n\n

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Clearly July ice appears as a plateau, and most years MASIE shows greater extents than SII, with differences of only a few 100k km2.\u00a0 The previous three years were in deficit to average, but July 2020 has returned to surplus years like 2018.\u00a0 More on MASIE dataset at the end.<\/p>\n\n\n\n

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The graph shows the melting pattern during July 2022 remained above average all month, and greatly exceeded 2007 and 2020, especially in the last 2 weeks.\u00a0 July 31, 2022, was 275k km2 in surplus, and exceeded 2020 by 1.2 Wadhams (M km2).<\/p>\n\n\n\n

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The table below shows ice extents by regions comparing 2022 with 16-year average (2007 to 2022 inclusive) and 2020.<\/p>\n\n\n\n

Region<\/strong><\/td>2022212<\/strong><\/td>Day 212 Average<\/strong><\/td>2022-Ave.<\/strong><\/td>2020212<\/strong><\/td>2022-2020<\/strong><\/td><\/tr>
 (0) Northern_Hemisphere<\/td>7124997<\/td>6849722<\/td>275275<\/td>5880746<\/td>1244251<\/td><\/tr>
 (1) Beaufort_Sea<\/td>884463<\/td>789512<\/td>94950<\/td>875454<\/td>9008<\/td><\/tr>
 (2) Chukchi_Sea<\/td>575245<\/td>525326<\/td>49919<\/td>533748<\/td>41498<\/td><\/tr>
 (3) East_Siberian_Sea<\/td>787982<\/td>740081<\/td>47901<\/td>329453<\/td>458529<\/td><\/tr>
 (4) Laptev_Sea<\/td>297339<\/td>365902<\/td>-68563<\/td>61979<\/td>235360<\/td><\/tr>
 (5) Kara_Sea<\/td>104430<\/td>161090<\/td>-56660<\/td>95539<\/td>8891<\/td><\/tr>
 (6) Barents_Sea<\/td>0<\/td>31433<\/td>-31433<\/td>23940<\/td>-23940<\/td><\/tr>
 (7) Greenland_Sea<\/td>292278<\/td>291488<\/td>790<\/td>282403<\/td>9875<\/td><\/tr>
 (8) Baffin_Bay_Gulf_of_St._Lawrence<\/td>281955<\/td>130715<\/td>151240<\/td>35368<\/td>246587<\/td><\/tr>
 (9) Canadian_Archipelago<\/td>633235<\/td>540268<\/td>92967<\/td>515499<\/td>117735<\/td><\/tr>
 (10) Hudson_Bay<\/td>169704<\/td>135947<\/td>33757<\/td>92861<\/td>76844<\/td><\/tr>
 (11) Central_Arctic<\/td>3096938<\/td>3136284<\/td>-39347<\/td>3033706<\/td>63232<\/td><\/tr><\/tbody><\/table><\/figure>\n\n\n\n

2020 is 275k km2 above average (4%). The main deficits are in Laptev and Kara seas. More than offset by 151k km2 surplus in Baffin Bay, along with additional ice in CAA, and an icy BCE (Beaufort, Chukchi, East Siberian seas).<\/p>\n\n\n\n

Footnote on MASIE Data Sources:<\/strong><\/p>\n\n\n\n

MASIE reports are based on data primarily from NIC\u2019s Interactive Multisensor Snow and Ice Mapping System (IMS). From the documentation, the multiple sources feeding IMS are:<\/p>\n\n\n\n

Platform(s) AQUA, DMSP, DMSP 5D-3\/F17, GOES-10, GOES-11, GOES-13, GOES-9, METEOSAT, MSG, MTSAT-1R, MTSAT-2, NOAA-14, NOAA-15, NOAA-16, NOAA-17, NOAA-18, NOAA-N, RADARSAT-2, SUOMI-NPP, TERRA<\/p>\n\n\n\n

Sensor(s): AMSU-A, ATMS, AVHRR, GOES I-M IMAGER, MODIS, MTSAT 1R Imager, MTSAT 2 Imager, MVIRI, SAR, SEVIRI, SSM\/I, SSMIS, VIIRS<\/p>\n\n\n\n

Summary: IMS Daily Northern Hemisphere Snow and Ice Analysis<\/strong><\/p>\n\n\n\n

The National Oceanic and Atmospheric Administration \/ National Environmental Satellite, Data, and Information Service (NOAA\/NESDIS) has an extensive history of monitoring snow and ice coverage.Accurate monitoring of global snow\/ice cover is a key component in the study of climate and global change as well as daily weather forecasting.<\/p>\n\n\n\n

The Polar and Geostationary Operational Environmental Satellite programs (POES\/GOES) operated by NESDIS provide invaluable visible and infrared spectral data in support of these efforts. Clear-sky imagery from both the POES and the GOES sensors show snow\/ice boundaries very well; however, the visible and infrared techniques may suffer from persistent cloud cover near the snowline, making observations difficult (Ramsay, 1995). The microwave products (DMSP and AMSR-E) are unobstructed by clouds and thus can be used as another observational platform in most regions. Synthetic Aperture Radar (SAR) imagery also provides all-weather, near daily capacities to discriminate sea and lake ice. With several other derived snow\/ice products of varying accuracy, such as those from NCEP and the NWS NOHRSC, it is highly desirable for analysts to be able to interactively compare and contrast the products so that a more accurate composite map can be produced.<\/p>\n\n\n\n

The Satellite Analysis Branch (SAB) of NESDIS first began generating Northern Hemisphere Weekly Snow and Ice Cover analysis charts derived from the visible satellite imagery in November, 1966. The spatial and temporal resolutions of the analysis (190 km and 7 days, respectively) remained unchanged for the product\u2019s 33-year lifespan.<\/p>\n\n\n\n

As a result of increasing customer needs and expectations, it was decided that an efficient, interactive workstation application should be constructed which would enable SAB to produce snow\/ice analyses at a higher resolution and on a daily basis (~25 km \/ 1024 x 1024 grid and once per day) using a consolidated array of new as well as existing satellite and surface imagery products. The Daily Northern Hemisphere Snow and Ice Cover chart has been produced since February, 1997 by SAB meteorologists on the IMS.<\/p>\n\n\n\n

Another large resolution improvement began in early 2004, when improved technology allowed the SAB to begin creation of a daily ~4 km (6144\u00d76144) grid. At this time, both the ~4 km and ~24 km products are available from NSIDC with a slight delay. Near real-time gridded data is available in ASCII format by request.<\/p>\n\n\n\n

In March 2008, the product was migrated from SAB to the National Ice Center (NIC) of NESDIS. The production system and methodology were preserved during the migration. Improved access to DMSP, SAR, and modeled data sources is expected as a short-term from the migration, with longer term plans of twice daily production, GRIB2 output format, a Southern Hemisphere analysis, and an expanded suite of integrated snow and ice variable on horizon. <\/p>\n\n\n\n

Source:\u00a0\u00a0Interactive Multisensor Snow and Ice Mapping System (IMS)<\/strong><\/a><\/p>\n\n\n\n

<\/p>\n\n\n

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\"\"<\/figure>\n<\/div>\n\n\n

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<\/p>\n\n\n\n

via Science Matters<\/mark><\/em><\/strong><\/p>\n\n\n\n

August 1, 2022<\/p>\n\n\n\n

Surplus Arctic Ice July 2022 | Science Matters (rclutz.com)<\/a><\/p>\n\n\n\n

<\/p>\n","protected":false},"excerpt":{"rendered":"

The animation shows Arctic ice extents on day 212 (end of July) starting with 2007 and showing the lack of decline through yesterday.\u00a0 Years vary as to which regions retain more or less ice.\u00a0 For example, some years the Russian shelf seas (left side) are mostly open water on day 212.\u00a0 Kara and Barents seas […]<\/p>\n","protected":false},"author":121246920,"featured_media":211464,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_coblocks_attr":"","_coblocks_dimensions":"","_coblocks_responsive_height":"","_coblocks_accordion_ie_support":"","_crdt_document":"","advanced_seo_description":"","jetpack_seo_html_title":"","jetpack_seo_noindex":false,"jetpack_post_was_ever_published":false,"_jetpack_newsletter_access":"","_jetpack_dont_email_post_to_subs":false,"_jetpack_newsletter_tier_id":0,"_jetpack_memberships_contains_paywalled_content":false,"_jetpack_memberships_contains_paid_content":false,"footnotes":"","jetpack_publicize_message":"","jetpack_publicize_feature_enabled":true,"jetpack_social_post_already_shared":true,"jetpack_social_options":{"image_generator_settings":{"template":"highway","default_image_id":0,"font":"","enabled":false},"version":2}},"categories":[1],"tags":[],"class_list":{"0":"post-211462","1":"post","2":"type-post","3":"status-publish","4":"format-standard","5":"has-post-thumbnail","6":"hentry","7":"category-uncategorized","9":"fallback-thumbnail"},"jetpack_publicize_connections":[],"jetpack_featured_media_url":"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2022\/08\/0arcticjuly-day212-2007-to-2022.gif?fit=1000%2C562&ssl=1","jetpack_likes_enabled":true,"jetpack_sharing_enabled":true,"jetpack_shortlink":"https:\/\/wp.me\/paxLW1-T0G","jetpack-related-posts":[{"id":271056,"url":"https:\/\/climatescience.press\/?p=271056","url_meta":{"origin":211462,"position":0},"title":"Arctic Ice Surplus End July\u00a02023","author":"uwe.roland.gross","date":"02\/08\/2023","format":false,"excerpt":"The graph for the last 30 days shows the normal melt is 2.7M km2 down to 6.9M km2.\u00a0 2023 was tracking average for 2 weeks, and well above average after that.\u00a0 SII tracked the MASIE average throughout, and slightly lower the second half. 2007 was average mid-July, but dropped much\u2026","rel":"","context":"In \"Beaufort and East Siberian seas\"","block_context":{"text":"Beaufort and East Siberian seas","link":"https:\/\/climatescience.press\/?tag=beaufort-and-east-siberian-seas"},"img":{"alt_text":"","src":"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2023\/08\/image-59.png?fit=1200%2C795&ssl=1&resize=350%2C200","width":350,"height":200,"srcset":"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2023\/08\/image-59.png?fit=1200%2C795&ssl=1&resize=350%2C200 1x, 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Ice","link":"https:\/\/climatescience.press\/?tag=arctic-ice"},"img":{"alt_text":"","src":"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/09\/AQMdvRrPd8AapbqS598oXlkKL8lNU7wsJBLh3lBQbLXWVp8gPxPHVJ-c7_IyaJq2InhtPF4rh1Pm1Nr0yWAI8PFpn_cmf8Qs4FqzCtKq9vyhUnJ2IkdmpVNu6ZbDUspvvyl6vBhZ_OaycAK7i7JQcb1lXNUVlA.jpeg?fit=1200%2C1200&ssl=1&resize=350%2C200","width":350,"height":200,"srcset":"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/09\/AQMdvRrPd8AapbqS598oXlkKL8lNU7wsJBLh3lBQbLXWVp8gPxPHVJ-c7_IyaJq2InhtPF4rh1Pm1Nr0yWAI8PFpn_cmf8Qs4FqzCtKq9vyhUnJ2IkdmpVNu6ZbDUspvvyl6vBhZ_OaycAK7i7JQcb1lXNUVlA.jpeg?fit=1200%2C1200&ssl=1&resize=350%2C200 1x, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2025\/09\/AQMdvRrPd8AapbqS598oXlkKL8lNU7wsJBLh3lBQbLXWVp8gPxPHVJ-c7_IyaJq2InhtPF4rh1Pm1Nr0yWAI8PFpn_cmf8Qs4FqzCtKq9vyhUnJ2IkdmpVNu6ZbDUspvvyl6vBhZ_OaycAK7i7JQcb1lXNUVlA.jpeg?fit=1200%2C1200&ssl=1&resize=525%2C300 1.5x, 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Outlook and Results Not\u00a0Scary","author":"uwe.roland.gross","date":"10\/10\/2023","format":false,"excerpt":"From Science Matters By\u00a0Ron Clutz The graph above shows the monthly averages for September Arctic ice extents including 2023 compared to previous years back to 2007.\u00a0 This year is slightly below the 17 year average of 4.63M km2;\u00a0 MASIE shows 4.43M and SII shows 4.37.\u00a0 For comparison the 2007 September\u2026","rel":"","context":"In \"Artic sea ice\"","block_context":{"text":"Artic sea ice","link":"https:\/\/climatescience.press\/?tag=artic-sea-ice"},"img":{"alt_text":"","src":"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2023\/10\/00Arctic-sea.jpg?fit=1200%2C800&ssl=1&resize=350%2C200","width":350,"height":200,"srcset":"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2023\/10\/00Arctic-sea.jpg?fit=1200%2C800&ssl=1&resize=350%2C200 1x, 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From Science Matters By\u00a0Ron Clutz The animation shows the rapid refreezing of Arctic ice from September 30 to yesterday October 9.\u00a0 Despite much ado about September minimums, in fact the ice recovers quickly from its annual\u2026","rel":"","context":"In \"Arctic Ice\"","block_context":{"text":"Arctic Ice","link":"https:\/\/climatescience.press\/?tag=arctic-ice"},"img":{"alt_text":"","src":"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2023\/10\/image-272.png?fit=1024%2C1024&ssl=1&resize=350%2C200","width":350,"height":200,"srcset":"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2023\/10\/image-272.png?fit=1024%2C1024&ssl=1&resize=350%2C200 1x, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2023\/10\/image-272.png?fit=1024%2C1024&ssl=1&resize=525%2C300 1.5x, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2023\/10\/image-272.png?fit=1024%2C1024&ssl=1&resize=700%2C400 2x"},"classes":[]},{"id":278030,"url":"https:\/\/climatescience.press\/?p=278030","url_meta":{"origin":211462,"position":5},"title":"September Outlook Arctic Ice\u00a02023","author":"uwe.roland.gross","date":"09\/09\/2023","format":false,"excerpt":"The experts involved in SIPN are expecting SII 2023 September to be higher than 2007 and somewhat lower than 2022. \u00a0The way MASIE is going, this September looks to be nearly average unless some bad weather intervenes.\u00a0 While the daily minimum for the year occurs mid September, ice extent on\u2026","rel":"","context":"In \"Arctic Ice\"","block_context":{"text":"Arctic Ice","link":"https:\/\/climatescience.press\/?tag=arctic-ice"},"img":{"alt_text":"","src":"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2023\/09\/010_9_14_upton_Antarctic_sea_ice_NASA__1050_788_s_c1_c_c.jpg?fit=1050%2C788&ssl=1&resize=350%2C200","width":350,"height":200,"srcset":"https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2023\/09\/010_9_14_upton_Antarctic_sea_ice_NASA__1050_788_s_c1_c_c.jpg?fit=1050%2C788&ssl=1&resize=350%2C200 1x, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2023\/09\/010_9_14_upton_Antarctic_sea_ice_NASA__1050_788_s_c1_c_c.jpg?fit=1050%2C788&ssl=1&resize=525%2C300 1.5x, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2023\/09\/010_9_14_upton_Antarctic_sea_ice_NASA__1050_788_s_c1_c_c.jpg?fit=1050%2C788&ssl=1&resize=700%2C400 2x, https:\/\/i0.wp.com\/climatescience.press\/wp-content\/uploads\/2023\/09\/010_9_14_upton_Antarctic_sea_ice_NASA__1050_788_s_c1_c_c.jpg?fit=1050%2C788&ssl=1&resize=1050%2C600 3x"},"classes":[]}],"_links":{"self":[{"href":"https:\/\/climatescience.press\/index.php?rest_route=\/wp\/v2\/posts\/211462","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/climatescience.press\/index.php?rest_route=\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/climatescience.press\/index.php?rest_route=\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/climatescience.press\/index.php?rest_route=\/wp\/v2\/users\/121246920"}],"replies":[{"embeddable":true,"href":"https:\/\/climatescience.press\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=211462"}],"version-history":[{"count":6,"href":"https:\/\/climatescience.press\/index.php?rest_route=\/wp\/v2\/posts\/211462\/revisions"}],"predecessor-version":[{"id":211473,"href":"https:\/\/climatescience.press\/index.php?rest_route=\/wp\/v2\/posts\/211462\/revisions\/211473"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/climatescience.press\/index.php?rest_route=\/wp\/v2\/media\/211464"}],"wp:attachment":[{"href":"https:\/\/climatescience.press\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=211462"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/climatescience.press\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=211462"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/climatescience.press\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=211462"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}