{"id":639,"date":"2024-03-19T17:17:12","date_gmt":"2024-03-19T17:17:12","guid":{"rendered":"https:\/\/ubwp.buffalo.edu\/glyremotesensinglab\/?p=639"},"modified":"2024-03-19T17:19:10","modified_gmt":"2024-03-19T17:19:10","slug":"surface-velocities-of-a-greenland-outlet-glacier-from-high-resolution-visible-satellite-imagery","status":"publish","type":"post","link":"https:\/\/ubwp.buffalo.edu\/glyremotesensinglab\/2024\/03\/19\/surface-velocities-of-a-greenland-outlet-glacier-from-high-resolution-visible-satellite-imagery\/","title":{"rendered":"Surface velocities of a Greenland outlet glacier from high-resolution visible satellite imagery"},"content":{"rendered":"\n<p><em>Abstract:<\/em>&nbsp;A multidisciplinary team of researchers reports the results of a study of the feasibility of utilizing high-resolution Declassified Intelligence Satellite Photographs (DISP) to derive surface speeds of fast-moving Greenland outlet glaciers from tracking surface features on sequential DISP images. The images provide coverage of the entire Greenland Ice Sheet for most of the 1960s and their value as a resource for establishing a baseline for assessing ongoing and future changes in the ice sheet is demonstrated.<\/p>\n\n\n\n<figure class=\"wp-block-gallery has-nested-images columns-default is-cropped wp-block-gallery-1 is-layout-flex wp-block-gallery-is-layout-flex\">\n<figure class=\"wp-block-image size-large\"><img fetchpriority=\"high\" decoding=\"async\" width=\"344\" height=\"352\" data-id=\"642\" src=\"https:\/\/ubwp.buffalo.edu\/glyremotesensinglab\/wp-content\/uploads\/sites\/201\/2024\/03\/kvdisp1_kl.gif\" alt=\"DISP Image of Kangerdlugssuaq Glacier, east Greenland\n\" class=\"wp-image-642\" \/><figcaption class=\"wp-element-caption\">DISP Image of Kangerdlugssuaq Glacier, east Greenland<\/figcaption><\/figure>\n\n\n\n<figure class=\"wp-block-image size-large\"><img decoding=\"async\" width=\"238\" height=\"361\" data-id=\"643\" src=\"https:\/\/ubwp.buffalo.edu\/glyremotesensinglab\/wp-content\/uploads\/sites\/201\/2024\/03\/green_kl.gif\" alt=\"Location map\t\" class=\"wp-image-643\" \/><figcaption class=\"wp-element-caption\">Location map<\/figcaption><\/figure>\n\n\n\n<figure class=\"wp-block-image size-large\"><img decoding=\"async\" width=\"254\" height=\"479\" data-id=\"644\" src=\"https:\/\/ubwp.buffalo.edu\/glyremotesensinglab\/wp-content\/uploads\/sites\/201\/2024\/03\/kv218a-kl.jpg\" alt=\"Glacier changes 1933 - 1966\" class=\"wp-image-644\" srcset=\"https:\/\/ubwp.buffalo.edu\/glyremotesensinglab\/wp-content\/uploads\/sites\/201\/2024\/03\/kv218a-kl.jpg 254w, https:\/\/ubwp.buffalo.edu\/glyremotesensinglab\/wp-content\/uploads\/sites\/201\/2024\/03\/kv218a-kl-159x300.jpg 159w\" sizes=\"(max-width: 254px) 100vw, 254px\" \/><figcaption class=\"wp-element-caption\">Glacier changes 1933 &#8211; 1966<\/figcaption><\/figure>\n\n\n\n<figure class=\"wp-block-image size-large\"><img loading=\"lazy\" decoding=\"async\" width=\"323\" height=\"351\" data-id=\"645\" src=\"https:\/\/ubwp.buffalo.edu\/glyremotesensinglab\/wp-content\/uploads\/sites\/201\/2024\/03\/kvd2b-kl.gif\" alt=\"Magnified view of the two features labeled A and B in the DISP Image on the June 23 and September 24, 1966 images.\" class=\"wp-image-645\" \/><figcaption class=\"wp-element-caption\">Magnified view of the two features labeled A and B in the DISP Image on the June 23 and September 24, 1966 images.<\/figcaption><\/figure>\n<\/figure>\n\n\n\n<div class=\"wp-block-group has-background\" style=\"background:linear-gradient(135deg,rgb(247,242,255) 0%,rgb(232,240,255) 100%)\"><div class=\"wp-block-group__inner-container is-layout-constrained wp-block-group-is-layout-constrained\">\n<p><strong>REFERENCE<\/strong><\/p>\n\n\n\n<p>Csatho, B. M., J. F. Bolzan, C. J. van der Veen, A. F. Schenk, D-C. Lee, &#8220;Surface Velocities of a Greenland outlet glacier from high-resolution visible satellite imagery,&#8221;\u00a0<em>Polar Geography<\/em>, 1999,<strong>23<\/strong>, No.1, pp.71-82. (<a href=\"https:\/\/ubwp.buffalo.edu\/glyremotesensinglab\/wp-content\/uploads\/sites\/201\/2024\/03\/csatho_polar_geography_1999.pdf\">pdf<\/a>)<\/p>\n<\/div><\/div>\n","protected":false},"excerpt":{"rendered":"<p>Abstract:&nbsp;A multidisciplinary team of researchers reports the results of a study of the feasibility of utilizing high-resolution Declassified Intelligence Satellite Photographs (DISP) to derive surface speeds of fast-moving Greenland outlet &hellip; <a href=\"https:\/\/ubwp.buffalo.edu\/glyremotesensinglab\/2024\/03\/19\/surface-velocities-of-a-greenland-outlet-glacier-from-high-resolution-visible-satellite-imagery\/\" class=\"more-link\">Continue reading <span class=\"screen-reader-text\">Surface velocities of a Greenland outlet glacier from high-resolution visible satellite imagery<\/span> <span class=\"meta-nav\">&rarr;<\/span><\/a><\/p>\n","protected":false},"author":580,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[11],"tags":[],"class_list":["post-639","post","type-post","status-publish","format-standard","hentry","category-research"],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v27.3 - 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