{"id":824,"date":"2024-05-22T17:01:44","date_gmt":"2024-05-22T21:01:44","guid":{"rendered":"https:\/\/ubwp.buffalo.edu\/glyremotesensinglab\/?p=824"},"modified":"2024-05-22T17:01:46","modified_gmt":"2024-05-22T21:01:46","slug":"mass-balance-and-velocity-data-for-greenlands-ice-sheets-at-high-elevations","status":"publish","type":"post","link":"https:\/\/ubwp.buffalo.edu\/glyremotesensinglab\/2024\/05\/22\/mass-balance-and-velocity-data-for-greenlands-ice-sheets-at-high-elevations\/","title":{"rendered":"Mass Balance and Velocity Data for Greenland&#8217;s Ice Sheets at High Elevations"},"content":{"rendered":"<div class=\"wp-block-image\">\n<figure class=\"aligncenter size-full is-resized\"><img fetchpriority=\"high\" decoding=\"async\" width=\"562\" height=\"152\" src=\"https:\/\/ubwp.buffalo.edu\/glyremotesensinglab\/wp-content\/uploads\/sites\/201\/2024\/05\/Greenland_MB_Header.gif\" alt=\"Greenland Mass Balance\" class=\"wp-image-825\" style=\"width:642px;height:auto\" \/><\/figure><\/div>\n\n\n<div class=\"wp-block-group\"><div class=\"wp-block-group__inner-container is-layout-constrained wp-block-group-is-layout-constrained\">\n<div class=\"wp-block-group\"><div class=\"wp-block-group__inner-container is-layout-constrained wp-block-group-is-layout-constrained\">\n<div class=\"wp-block-columns is-layout-flex wp-container-core-columns-is-layout-9d6595d7 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-buttons is-content-justification-center is-layout-flex wp-container-core-buttons-is-layout-16018d1d wp-block-buttons-is-layout-flex\">\n<div class=\"wp-block-button has-custom-width wp-block-button__width-75\"><a class=\"wp-block-button__link has-background wp-element-button\" href=\"https:\/\/ubwp.buffalo.edu\/glyremotesensinglab\/2024\/05\/22\/mass-balance-and-velocity-data-for-greenlands-ice-sheets-at-high-elevations-data\/\" style=\"background:linear-gradient(135deg,rgb(12,149,228) 0%,rgb(212,176,242) 100%)\">Data<\/a><\/div>\n<\/div>\n<\/div>\n<\/div>\n<\/div><\/div>\n<\/div><\/div>\n\n\n\n<h2 class=\"wp-block-heading\">Goal<\/h2>\n\n\n\n<p>Estimation of mass balance of the Greenland Ice Sheet at higher elevations by using a mass budget method<\/p>\n\n\n\n<h2 class=\"wp-block-heading\">Procedure &amp; Methodology<\/h2>\n\n\n\n<p>Mass balance was computed as the difference between the estimated annual total snow accumulation and ice discharge<\/p>\n\n\n\n<p>Outgoing flux is estimated from ice sheet velocity and ice thickness measured around the central part of the Greenland Ice Sheet<\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li>Ice velocity and thickness measurements at 161 stations located 30 km apart, at 2000 m elevation that circumnavigates Greenland<\/li>\n\n\n\n<li>Stations are numbered counter-clockwise starting in the northwest corner<\/li>\n\n\n\n<li>Ice velocities were determined from repeat, differential carrier-phase GPS data collected in 1-2 years intervals between 1993 to 1997<\/li>\n\n\n\n<li>Ice thickness was measured by using ice-penetrating radar<\/li>\n<\/ul>\n\n\n\n<p>Annual snow accumulation is estimated from an observational analysis of ice core and pit data.<\/p>\n\n\n\n<p>Results are presented as mass balance estimates in single gates:<\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li>Data from two adjacent stations were combined to form 161 single gate<\/li>\n<\/ul>\n\n\n\n<p>Mass balance estimates at medium-sized regions:<\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li>Adjacent single gates were combined to form 130 medium gates each with a minimum area of 30,000 km2.<\/li>\n\n\n\n<li>The gates were grouped by shifting one traverse station at a time.<\/li>\n<\/ul>\n\n\n\n<p>Mass balance estimates at large regions:<\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li>The single gates were combined to form 12 large gates (A-L) with an average area of approximately 100,000 km2 each.<\/li>\n\n\n\n<li>The maximum numbers of single gates were in gate D with 23 single gates, from station F069 to F096.<\/li>\n\n\n\n<li>The minimum numbers of single gates were in gate C with 6 single gates, from station F096 to F101.<\/li>\n<\/ul>\n\n\n\n<h2 class=\"wp-block-heading\">Results<\/h2>\n\n\n\n<ul class=\"wp-block-list\">\n<li>Overall the ice sheets in Greenland are in balance within 10mm\/yr; thickening and thinning in different regions.<\/li>\n\n\n\n<li>In the northwest the ice sheet thinned 5 cm\/yr, and thickened 2 cm\/yr in the northeast.<\/li>\n\n\n\n<li>In the southwest the ice sheet thickened 21 cm\/yr, and thinned 30 cm\/yr in the southeast<\/li>\n<\/ul>\n\n\n\n<h2 class=\"wp-block-heading\">People<\/h2>\n\n\n\n<h4 class=\"wp-block-heading\">University at Buffalo<\/h4>\n\n\n\n<ul class=\"wp-block-list\">\n<li>Dr. Beata Csatho\u00a0&#8211; Point of Contact:\u00a0<a href=\"mailto:bcsatho@buffalo.edu\">E-Mail<\/a><\/li>\n\n\n\n<li>Melissa Zelazny<\/li>\n\n\n\n<li>Justin L. Rich<\/li>\n\n\n\n<li>Taehun Yoon<\/li>\n<\/ul>\n\n\n\n<h4 class=\"wp-block-heading\">EG&amp;G Services<\/h4>\n\n\n\n<ul class=\"wp-block-list\">\n<li>Robert Thomas<\/li>\n<\/ul>\n\n\n\n<h4 class=\"wp-block-heading\">University of Kansas<\/h4>\n\n\n\n<ul class=\"wp-block-list\">\n<li>Prasad Gogineni: Electrical Engineering &amp; Computer Science.\u00a0<a href=\"mailto:gogineni@eecs.ku.edu\">E-Mail<\/a><\/li>\n<\/ul>\n\n\n\n<h2 class=\"wp-block-heading\">Publications<\/h2>\n\n\n\n<ul class=\"wp-block-list\">\n<li>Thomas, R., T. Akins, B. Csatho, M. Fahnestock, P. Gogineni, C. Kim, and J. Sonntag. 2000. Mass balance of the Greenland Ice Sheet at high elevations. Science 289: 426-427.<\/li>\n\n\n\n<li>Thomas, R., B. Csatho, C. Davis, C. Kim, W. Krabill, S. Manizade, J. McConnell and J. Sonntag. 2001. Mass balance of higher-elevation parts of the Greenland Ice Sheet. Journal of Geophysical Research &#8211; Atmosphere 106 (D24) (December): 33707-33716.<\/li>\n\n\n\n<li>Thomas, R., B. Csatho, S. Gogineni, K. Jezek, and K. Kuivinen. 1998. Thickening of the western part of the Greenland Ice Sheet. Journal of Glaciology 44: 653-658.<\/li>\n<\/ul>\n","protected":false},"excerpt":{"rendered":"<p>Goal Estimation of mass balance of the Greenland Ice Sheet at higher elevations by using a mass budget method Procedure &amp; Methodology Mass balance was computed as the difference between &hellip; <a href=\"https:\/\/ubwp.buffalo.edu\/glyremotesensinglab\/2024\/05\/22\/mass-balance-and-velocity-data-for-greenlands-ice-sheets-at-high-elevations\/\" class=\"more-link\">Continue reading <span class=\"screen-reader-text\">Mass Balance and Velocity Data for Greenland&#8217;s Ice Sheets at High Elevations<\/span> <span class=\"meta-nav\">&rarr;<\/span><\/a><\/p>\n","protected":false},"author":580,"featured_media":0,"comment_status":"closed","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[16,18],"tags":[],"class_list":["post-824","post","type-post","status-publish","format-standard","hentry","category-data","category-greenland"],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v27.3 - 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