Evaluation of the CloudSat surface snowfall product over Antarctica using ground-based precipitation radars
<p>In situ observations of snowfall over the Antarctic Ice Sheet are scarce. Currently, continent-wide assessments of snowfall are limited to information from the Cloud Profiling Radar on board the CloudSat satellite, which has not been evaluated up to now. In this study, snowfall derived from...
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doaj-9fb63e1da2a844d684e579c4ad20fcc62020-11-24T20:42:27ZengCopernicus PublicationsThe Cryosphere1994-04161994-04242018-11-01123775378910.5194/tc-12-3775-2018Evaluation of the CloudSat surface snowfall product over Antarctica using ground-based precipitation radarsN. Souverijns0A. Gossart1S. Lhermitte2I. V. Gorodetskaya3J. Grazioli4J. Grazioli5A. Berne6C. Duran-Alarcon7B. Boudevillain8C. Genthon9C. Scarchilli10N. P. M. van Lipzig11Department of Earth and Environmental Sciences, KU Leuven, Leuven, BelgiumDepartment of Earth and Environmental Sciences, KU Leuven, Leuven, BelgiumDepartment of Geoscience and Remote Sensing, Delft University of Technology, Delft, the NetherlandsCESAM – Centre for Environmental and Marine Studies, Department of Physics, University of Aveiro, Aveiro, PortugalEnvironmental Remote Sensing Laboratory, Ecole Polytechnique Fédérale de Lausanne, Lausanne, SwitzerlandFederal Office of Meteorology and Climatology, MeteoSwiss, Locarno-Monti, SwitzerlandEnvironmental Remote Sensing Laboratory, Ecole Polytechnique Fédérale de Lausanne, Lausanne, SwitzerlandUniversité Grenoble Alpes, CNRS, IRD, Grenoble INP, IGE, Grenoble, FranceUniversité Grenoble Alpes, CNRS, IRD, Grenoble INP, IGE, Grenoble, FranceUniversité Grenoble Alpes, CNRS, IRD, Grenoble INP, IGE, Grenoble, FranceTechnical Unit for Energy and Environmental Modeling UTMEA, ENEA, Rome, ItalyDepartment of Earth and Environmental Sciences, KU Leuven, Leuven, Belgium<p>In situ observations of snowfall over the Antarctic Ice Sheet are scarce. Currently, continent-wide assessments of snowfall are limited to information from the Cloud Profiling Radar on board the CloudSat satellite, which has not been evaluated up to now. In this study, snowfall derived from CloudSat is evaluated using three ground-based vertically profiling 24 GHz precipitation radars (Micro Rain Radars: MRRs). Firstly, using the MRR long-term measurement records, an assessment of the uncertainty caused by the low temporal sampling rate of CloudSat (one revisit per 2.1 to 4.5 days) is performed. The 10–90th-percentile temporal sampling uncertainty in the snowfall climatology varies between 30 % and 40 % depending on the latitudinal location and revisit time of CloudSat. Secondly, an evaluation of the snowfall climatology indicates that the CloudSat product, derived at a resolution of 1<span class="inline-formula"><sup>∘</sup></span> latitude by 2<span class="inline-formula"><sup>∘</sup></span> longitude, is able to accurately represent the snowfall climatology at the three MRR sites (biases <span class="inline-formula"><</span> 15 %), outperforming ERA-Interim. For coarser and finer resolutions, the performance drops as a result of higher omission errors by CloudSat. Moreover, the CloudSat product does not perform well in simulating individual snowfall events. Since the difference between the MRRs and the CloudSat climatology are limited and the temporal uncertainty is lower than current Climate Model Intercomparison Project Phase 5 (CMIP5) snowfall variability, our results imply that the CloudSat product is valuable for climate model evaluation purposes.</p>https://www.the-cryosphere.net/12/3775/2018/tc-12-3775-2018.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
N. Souverijns A. Gossart S. Lhermitte I. V. Gorodetskaya J. Grazioli J. Grazioli A. Berne C. Duran-Alarcon B. Boudevillain C. Genthon C. Scarchilli N. P. M. van Lipzig |
spellingShingle |
N. Souverijns A. Gossart S. Lhermitte I. V. Gorodetskaya J. Grazioli J. Grazioli A. Berne C. Duran-Alarcon B. Boudevillain C. Genthon C. Scarchilli N. P. M. van Lipzig Evaluation of the CloudSat surface snowfall product over Antarctica using ground-based precipitation radars The Cryosphere |
author_facet |
N. Souverijns A. Gossart S. Lhermitte I. V. Gorodetskaya J. Grazioli J. Grazioli A. Berne C. Duran-Alarcon B. Boudevillain C. Genthon C. Scarchilli N. P. M. van Lipzig |
author_sort |
N. Souverijns |
title |
Evaluation of the CloudSat surface snowfall product over Antarctica using ground-based precipitation radars |
title_short |
Evaluation of the CloudSat surface snowfall product over Antarctica using ground-based precipitation radars |
title_full |
Evaluation of the CloudSat surface snowfall product over Antarctica using ground-based precipitation radars |
title_fullStr |
Evaluation of the CloudSat surface snowfall product over Antarctica using ground-based precipitation radars |
title_full_unstemmed |
Evaluation of the CloudSat surface snowfall product over Antarctica using ground-based precipitation radars |
title_sort |
evaluation of the cloudsat surface snowfall product over antarctica using ground-based precipitation radars |
publisher |
Copernicus Publications |
series |
The Cryosphere |
issn |
1994-0416 1994-0424 |
publishDate |
2018-11-01 |
description |
<p>In situ observations of snowfall over the Antarctic Ice Sheet are scarce.
Currently, continent-wide assessments of snowfall are limited to information
from the Cloud Profiling Radar on board the CloudSat satellite, which has not been evaluated up to now. In this study,
snowfall derived from CloudSat is evaluated using three ground-based
vertically profiling 24 GHz precipitation radars (Micro Rain Radars: MRRs).
Firstly, using the MRR long-term measurement records, an assessment of the
uncertainty caused by the low temporal sampling rate of CloudSat (one revisit
per 2.1 to 4.5 days) is performed. The 10–90th-percentile temporal sampling
uncertainty in the snowfall climatology varies between 30 % and 40 %
depending on the latitudinal location and revisit time of CloudSat. Secondly,
an evaluation of the snowfall climatology indicates that the CloudSat
product, derived at a resolution of 1<span class="inline-formula"><sup>∘</sup></span> latitude by 2<span class="inline-formula"><sup>∘</sup></span>
longitude, is able to accurately represent the snowfall climatology at the
three MRR sites (biases <span class="inline-formula"><</span> 15 %), outperforming ERA-Interim. For coarser
and finer resolutions, the performance drops as a result of higher omission
errors by CloudSat. Moreover, the CloudSat product does not perform well in
simulating individual snowfall events. Since the difference between the MRRs
and the CloudSat climatology are limited and the temporal uncertainty is
lower than current Climate Model Intercomparison Project Phase 5 (CMIP5)
snowfall variability, our results imply that the CloudSat product is valuable
for climate model evaluation purposes.</p> |
url |
https://www.the-cryosphere.net/12/3775/2018/tc-12-3775-2018.pdf |
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