{"id":111,"date":"2017-11-01T12:50:12","date_gmt":"2017-11-01T12:50:12","guid":{"rendered":"http:\/\/snow.geus.dk\/?p=111"},"modified":"2017-11-01T12:50:12","modified_gmt":"2017-11-01T12:50:12","slug":"snow-albedo-validation-publications","status":"publish","type":"post","link":"https:\/\/snow.geus.dk\/index.php\/2017\/11\/01\/snow-albedo-validation-publications\/","title":{"rendered":"snow albedo validation publications"},"content":{"rendered":"

Box, J.E., D. van As, K. Steffen, 2017. Greenland, Canadian and Icelandic land ice albedo grids (2000-2016), Geological Survey of Denmark and Greenland Bulletin, 38, 53-56.\u00a0http:\/\/www.geus.dk\/DK\/publications\/geol-survey-dk-gl-bull\/38\/Documents\/nr38_p53-56.pdf<\/a><\/span><\/p>\n

Hall, D. K., G. A. Riggs, and V.V. Salomonson (1995). Development of Methods for Mapping Global Snow Cover Using Moderate Resolution Imaging Spectroradiometer Data. Remote Sensing of Environment, 54(2), 127-140. <\/span><\/p>\n

Hall, D. K., Riggs, G. A., and Salomonson, V. V.: MODIS\/Terra Snow Cover Daily L3 Global 500m Grid V004, January to March 2003, Digital media, updated daily. National Snow and Ice Data Center, Boulder, CO, USA, 2011. <\/span><\/p>\n

Hall, D. K. and G. A. Riggs. 2016. MODIS\/Terra Snow Cover Daily L3 Global 500m Grid, Version 6. Greenland coverage. Boulder, Colorado USA. NASA National Snow and Ice Data Center Distributed Active Archive Center. doi: <\/span>http:\/\/dx.doi.org\/10.5067\/MODIS\/MOD10A1.006<\/span><\/a>. Accessed December, 2016. <\/span><\/p>\n

Lyapustin, A., et al. (2014), Science impact of MODIS C5 calibration degradation and C6+ improvements, Atmos. Meas. Tech. Discuss., 7, 7281\u20137319.<\/span><\/p>\n

Riggs, G.A. and D.K. Hall. 2015. MODIS Snow Products Collection 6 User Guide, 11 December 2015 <\/span>https:\/\/nsidc.org\/sites\/nsidc.org\/files\/files\/MODIS-snow-user-guide-C6.pdf<\/span><\/a><\/p>\n

Stroeve, J.: Assessment of Greenland albedo variability from the advanced very high resolution radiometer Polar Pathfinder data set, J. Geophys. Res.-Atmos., 106, 33989\u201334006, doi:10.1029\/2001jd900072, 2001.<\/span><\/p>\n

Stroeve, J.C., Box, J.E., Haran, T., 2006: Evaluation of the MODIS (MOD10A1) daily snow albedo product over the Greenland ice sheet, Remote Sensing of Environment, 105(2), 155-171 doi:10.1016\/j.rse.2006.06.009<\/span><\/p>\n

Stroeve, J.C., J.E. Box, Z. Wang,\u00a0C. Schaaf,\u00a0A. Barrett. 2013.\u00a0Re-evaluation of MODIS MCD43 Greenland albedo accuracy and trends,\u00a0Remote Sensing of Environment, 138, 199\u2013214.\u00a0<\/span>doi:10.1016\/j.rse.2013.07.023<\/span><\/a><\/p>\n","protected":false},"excerpt":{"rendered":"

Box, J.E., D. van As, K. Steffen, 2017. Greenland, Canadian and Icelandic land ice albedo grids (2000-2016), Geological Survey of Denmark and Greenland Bulletin, 38, 53-56.\u00a0http:\/\/www.geus.dk\/DK\/publications\/geol-survey-dk-gl-bull\/38\/Documents\/nr38_p53-56.pdf Hall, D. K., G. A. Riggs, and V.V. Salomonson (1995). Development of Methods for Mapping Global Snow Cover Using Moderate Resolution Imaging Spectroradiometer Data. Remote Sensing of Environment, 54(2), … Continue reading “snow albedo validation publications”<\/span><\/a><\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"jetpack_post_was_ever_published":false,"jetpack_publicize_message":"","jetpack_is_tweetstorm":false,"jetpack_publicize_feature_enabled":true,"jetpack_social_post_already_shared":false,"jetpack_social_options":{"image_generator_settings":{"template":"highway","enabled":false}}},"categories":[1],"tags":[],"jetpack_publicize_connections":[],"aioseo_notices":[],"jetpack_featured_media_url":"","jetpack_sharing_enabled":true,"jetpack_shortlink":"https:\/\/wp.me\/paxG8S-1N","jetpack-related-posts":[{"id":85,"url":"https:\/\/snow.geus.dk\/index.php\/2017\/09\/24\/daily-greenland-arctic-canada-and-iceland-land-ice-albedo-grids\/","url_meta":{"origin":111,"position":0},"title":"daily Greenland, Arctic Canada and Iceland land ice albedo grids","date":"September 24, 2017","format":false,"excerpt":"Daily 0.5 km, 1 km and 5 km resolution Greenland, Arctic Canada and Iceland glaciated area albedo grids are available beginning April 2000 and (currently ending) September, 2017. The data are\u00a0based on NASA MOD10A1 Collection 6 data\u00a0with de-noising, gap filling, and bias correction after\u00a0Box et al. (2017). The grids are\u2026","rel":"","context":"In "data"","img":{"alt_text":"","src":"https:\/\/i0.wp.com\/snow.geus.dk\/wp-content\/uploads\/Fig-1-albedo-product-787x1024.png?resize=350%2C200","width":350,"height":200},"classes":[]},{"id":240,"url":"https:\/\/snow.geus.dk\/index.php\/2020\/05\/07\/web-story-snow-grain-size-it-matters\/","url_meta":{"origin":111,"position":1},"title":"Web Story: Snow grain size \u2013 it matters","date":"May 7, 2020","format":false,"excerpt":"link to 29 MAY 2019 Web Story Snow grain size \u2013 it matters Most of us probably wouldn\u2019t think of describing snow in terms of its grain size. However, grain size is fundamental to the amount of sunlight that snow reflects back into space \u2013 its albedo. 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Snow has a major influence on\u2026","rel":"","context":"Similar post","img":{"alt_text":"","src":"","width":0,"height":0},"classes":[]},{"id":82,"url":"https:\/\/snow.geus.dk\/index.php\/2017\/09\/01\/workshop-including-model-uses-of-optical-remotely-sensed-data\/","url_meta":{"origin":111,"position":4},"title":"workshop including Model uses of Optical Remotely Sensed Data","date":"September 1, 2017","format":false,"excerpt":"\u00a0 see session 4 in the following that is designed to resonate with this ESA contract... Workshop:\u00a0Modeling Meltwater in Snow and Firn: Processes, Validation, Intercomparison and Model uses of Optical Remotely Sensed Data 20-22 September 2017, Copenhagen. The\u00a0workshop\u00a0starts\u00a0Wednesday Sep 20 at 12.00, and ends\u00a0Friday Sep 22 at 12.00. 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