{"id":240,"date":"2020-05-07T09:32:57","date_gmt":"2020-05-07T09:32:57","guid":{"rendered":"http:\/\/snow.geus.dk\/?p=240"},"modified":"2020-05-07T09:33:39","modified_gmt":"2020-05-07T09:33:39","slug":"web-story-snow-grain-size-it-matters","status":"publish","type":"post","link":"https:\/\/snow.geus.dk\/index.php\/2020\/05\/07\/web-story-snow-grain-size-it-matters\/","title":{"rendered":"Web Story: Snow grain size \u2013 it matters"},"content":{"rendered":"
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link<\/a> to 29 MAY 2019 Web Story<\/p>\n

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Snow grain size \u2013 it matters<\/a><\/h1>\n<\/header>\n
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. With both snow and albedo part of the climate system, scientists are applying a novel analytical theory to Copernicus Sentinel-3 data and shedding new light on Greenland\u2019s changing albedo.<\/div>\n
The amount of sunlight absorbed or reflected by Earth\u2019s surface drives our climate and weather.<\/div>\n
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About one-third of the sunlight that hits Earth is reflected back into space and the other two-thirds is absorbed by the land, oceans and atmosphere. This ratio is governed by the reflectivity, or albedo, of the surface that the sunlight hits.<\/p>\n

Surfaces with lighter colours reflect more sunlight than darker surfaces. An everyday example of this is the difference we feel on a hot sunny day when wearing black clothes compared to wearing white. Earth is affected in the same way.<\/p>\n

So hypothetically, if the planet were completely covered in ice, it would reflect over 80% of incident sunlight back into space. On the other hand, if it were covered by dark green forest, it would only reflect about 10%.<\/p>\n

The albedo of Earth\u2019s surface varies naturally according to the changing colours of the season, but long-term trends in changing snow and ice cover, as well as changing vegetation cover and air pollution, are having an impact on the overall balance of Earth\u2019s albedo \u2013 and, hence, on how much heat it absorbs.<\/p>\n<\/div>\n

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\"Grainy<\/a>
Grainy nature of snow<\/figcaption><\/figure>\n

The Global Climate Observing System lists both albedo and snow as essential climate variables, which when measured and studied over time are used to understand, monitor and predict climate change.<\/p>\n

Ice and snow are often cited as the first causalities of climate change, and are measured and monitored from space in a variety of ways. However, while ice and snow may be present, the melting process affects its albedo.<\/p>\n

Snow grain size is a fundamental property of snow and is directly proportional to its surface area. Fresh dry snow tends to have a small grain size (under 0.5 mm in diameter), but as it melts the grain size grows and the larger grains reflect less sunlight.<\/p>\n

Thanks to Alex Kokhanovsky from Vitrociset who, along with several authors, published an elegant analytical\u00a0theory<\/a>, scientists have a fast new way of retrieving snow grain size from satellite images.<\/p>\n

Scientists from the Geological Survey of Denmark and Greenland (GEUS) in Copenhagen are coupling this theory with data from the Copernicus Sentinel-3 satellites\u2019 Ocean Land and Colour Instruments \u2013 as the animation above shows.<\/p>\n

Jason Box, from GEUS, explains, \u201cOne way of measuring the albedo of snow is to monitor how the surface colour changes because of pollution such as from wildfire soot. But this doesn\u2019t give us the whole story. Remarkably, this exciting new theory allows us to retrieve snow grain size from satellite optical images.<\/p>\n<\/div>\n

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\"Polluted<\/a>
Polluted snow and ice on Greenland<\/figcaption><\/figure>\n

\u201cThrough ESA\u2019s Earth Observation Science for Society programme, we have been able to demonstrate this over Greenland. We have found that pulses of warm air cause dark blemishes far inland on the ice sheet, contributing to increased climate sensitivity.\u201d<\/p>\n

In fact, the Copernicus Sentinel-3 satellite constellation can now take the relay in maintaining the climate record on snow albedo, which was first provided by the Advanced Very High Resolution Radiometer instruments on the US NOAA and Europe\u2019s MetOp satellites, and then the Moderate Resolution Imaging Spectroradiometer on the US Terra and Aqua satellites.<\/p>\n

In the future, the method will be extended and applied to areas with more complex terrain than Greenland. Furthermore, grain size data is now on the horizon for being used operationally to improve weather, hydrological and hazards forecasts, in service to society.<\/p>\n<\/div>\n<\/div>\n

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

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. With both snow and albedo part of the … Continue reading “Web Story: Snow grain size \u2013 it matters”<\/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":true,"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-3S","jetpack-related-posts":[{"id":27,"url":"https:\/\/snow.geus.dk\/index.php\/2017\/04\/03\/optical-remote-sensing-to-improve-snow-models\/","url_meta":{"origin":240,"position":0},"title":"Optical remote sensing to improve snow models – Copenhagen Workshop Session","date":"April 3, 2017","format":false,"excerpt":"This ESA SEOM Sentinel-3 for Science Land Study: Snow \"S-3-Snow\"\u00a0includes an element to gather and prioritise snow modeller interest and requirements about optical remotely sensed snow parameters (snow extent, albedo, grain size, impurity content). The ESA contract is to engage\u00a0users of Sentinel-3 snow optical retrievals in 1.) model comparison and\/or\u2026","rel":"","context":"In "meeting"","img":{"alt_text":"","src":"","width":0,"height":0},"classes":[]},{"id":111,"url":"https:\/\/snow.geus.dk\/index.php\/2017\/11\/01\/snow-albedo-validation-publications\/","url_meta":{"origin":240,"position":1},"title":"snow albedo validation publications","date":"November 1, 2017","format":false,"excerpt":"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). 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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":85,"url":"https:\/\/snow.geus.dk\/index.php\/2017\/09\/24\/daily-greenland-arctic-canada-and-iceland-land-ice-albedo-grids\/","url_meta":{"origin":240,"position":3},"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). 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