Blowing snow in East Antarctica: comparison of ground-based and space-borne retrievals

Continuous measurements of blowing snow are scarce, both in time and space. Satellites now provide the opportunity to derive blowing snow occurrences, transport and sublimation rates over Antarctica. However, little ground truth is available to validate these retrievals. The recent application of ce...

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Main Authors: Gossart, Alexandra, Palm, Stephen P., Souverijns, Niels, Lenaerts, Jan T. M., Gorodetskaya, Irina V., Lhermitte, Stef, Lipzig, Nicole P. M.
Format: Text
Language:English
Published: 2019
Subjects:
Online Access:https://doi.org/10.5194/tc-2019-25
https://tc.copernicus.org/preprints/tc-2019-25/
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spelling ftcopernicus:oai:publications.copernicus.org:tcd74299 2023-05-15T13:55:28+02:00 Blowing snow in East Antarctica: comparison of ground-based and space-borne retrievals Gossart, Alexandra Palm, Stephen P. Souverijns, Niels Lenaerts, Jan T. M. Gorodetskaya, Irina V. Lhermitte, Stef Lipzig, Nicole P. M. 2019-02-21 application/pdf https://doi.org/10.5194/tc-2019-25 https://tc.copernicus.org/preprints/tc-2019-25/ eng eng doi:10.5194/tc-2019-25 https://tc.copernicus.org/preprints/tc-2019-25/ eISSN: 1994-0424 Text 2019 ftcopernicus https://doi.org/10.5194/tc-2019-25 2020-07-20T16:22:55Z Continuous measurements of blowing snow are scarce, both in time and space. Satellites now provide the opportunity to derive blowing snow occurrences, transport and sublimation rates over Antarctica. However, little ground truth is available to validate these retrievals. The recent application of ceilometers for detection of blowing snow frequencies provides an opportunity to validate the satellite retrievals of blowing snow frequencies at the Princess Elisabeth and Neumayer stations, East Antarctica for the 2011–2016 time period. A routine to detect blowing snow occurrence from remote sensing ceilometers has been developed at those locations. Thanks to their ground-based location, ceilometers are able to detect blowing snow events in the presence of clouds and precipitation, which can be missed by the satellite, since optically thick clouds impede the penetration of the signal. This is important, since ≈ 90 % of blowing snow happens under cloudy conditions at Neumayer and Princess Elisabeth station and represent 30 % of all cloudy conditions at both stations. Although both detection methods have their limitations, 10 % (4 %) of the measurements at Princess Elisabeth (and Neumayer) are identified as blowing snow by the satellite but not by the ceilometer, likely due to differences in sensors, limitation of the surface identification by the satellite, or the spatial inhomogeneity of the blowing snow event. While the satellite blowing snow retrieval is a useful product, further investigation is needed to reduce the uncertainties on blowing snow frequencies associated with clouds. Text Antarc* Antarctica East Antarctica Copernicus Publications: E-Journals East Antarctica Neumayer
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description Continuous measurements of blowing snow are scarce, both in time and space. Satellites now provide the opportunity to derive blowing snow occurrences, transport and sublimation rates over Antarctica. However, little ground truth is available to validate these retrievals. The recent application of ceilometers for detection of blowing snow frequencies provides an opportunity to validate the satellite retrievals of blowing snow frequencies at the Princess Elisabeth and Neumayer stations, East Antarctica for the 2011–2016 time period. A routine to detect blowing snow occurrence from remote sensing ceilometers has been developed at those locations. Thanks to their ground-based location, ceilometers are able to detect blowing snow events in the presence of clouds and precipitation, which can be missed by the satellite, since optically thick clouds impede the penetration of the signal. This is important, since ≈ 90 % of blowing snow happens under cloudy conditions at Neumayer and Princess Elisabeth station and represent 30 % of all cloudy conditions at both stations. Although both detection methods have their limitations, 10 % (4 %) of the measurements at Princess Elisabeth (and Neumayer) are identified as blowing snow by the satellite but not by the ceilometer, likely due to differences in sensors, limitation of the surface identification by the satellite, or the spatial inhomogeneity of the blowing snow event. While the satellite blowing snow retrieval is a useful product, further investigation is needed to reduce the uncertainties on blowing snow frequencies associated with clouds.
format Text
author Gossart, Alexandra
Palm, Stephen P.
Souverijns, Niels
Lenaerts, Jan T. M.
Gorodetskaya, Irina V.
Lhermitte, Stef
Lipzig, Nicole P. M.
spellingShingle Gossart, Alexandra
Palm, Stephen P.
Souverijns, Niels
Lenaerts, Jan T. M.
Gorodetskaya, Irina V.
Lhermitte, Stef
Lipzig, Nicole P. M.
Blowing snow in East Antarctica: comparison of ground-based and space-borne retrievals
author_facet Gossart, Alexandra
Palm, Stephen P.
Souverijns, Niels
Lenaerts, Jan T. M.
Gorodetskaya, Irina V.
Lhermitte, Stef
Lipzig, Nicole P. M.
author_sort Gossart, Alexandra
title Blowing snow in East Antarctica: comparison of ground-based and space-borne retrievals
title_short Blowing snow in East Antarctica: comparison of ground-based and space-borne retrievals
title_full Blowing snow in East Antarctica: comparison of ground-based and space-borne retrievals
title_fullStr Blowing snow in East Antarctica: comparison of ground-based and space-borne retrievals
title_full_unstemmed Blowing snow in East Antarctica: comparison of ground-based and space-borne retrievals
title_sort blowing snow in east antarctica: comparison of ground-based and space-borne retrievals
publishDate 2019
url https://doi.org/10.5194/tc-2019-25
https://tc.copernicus.org/preprints/tc-2019-25/
geographic East Antarctica
Neumayer
geographic_facet East Antarctica
Neumayer
genre Antarc*
Antarctica
East Antarctica
genre_facet Antarc*
Antarctica
East Antarctica
op_source eISSN: 1994-0424
op_relation doi:10.5194/tc-2019-25
https://tc.copernicus.org/preprints/tc-2019-25/
op_doi https://doi.org/10.5194/tc-2019-25
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