Evaluation of the CloudSat surface snowfall product over Antarctica using ground-based precipitation radars

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...

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Published in:The Cryosphere
Main Author: Scarchilli, C.
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus GmbH 2018
Subjects:
Online Access:https://hdl.handle.net/20.500.12079/4787
https://doi.org/10.5194/tc-12-3775-2018
https://www.scopus.com/inward/record.uri?eid=2-s2.0-85057741258&doi=10.5194%2ftc-12-3775-2018&partnerID=40&md5=e4a223b24e196276e625422b6f45797a
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spelling ftenea:oai:iris.enea.it:20.500.12079/4787 2024-02-11T09:58:08+01:00 Evaluation of the CloudSat surface snowfall product over Antarctica using ground-based precipitation radars Scarchilli, C. Scarchilli, C. 2018 https://hdl.handle.net/20.500.12079/4787 https://doi.org/10.5194/tc-12-3775-2018 https://www.scopus.com/inward/record.uri?eid=2-s2.0-85057741258&doi=10.5194%2ftc-12-3775-2018&partnerID=40&md5=e4a223b24e196276e625422b6f45797a en eng Copernicus GmbH volume:12 issue:12 numberofpages:3775 - 3789 journal:THE CRYOSPHERE http://hdl.handle.net/20.500.12079/4787 doi:10.5194/tc-12-3775-2018 info:eu-repo/semantics/altIdentifier/scopus/Scopus ID: 2-s2.0-85057741258 https://www.scopus.com/inward/record.uri?eid=2-s2.0-85057741258&doi=10.5194%2ftc-12-3775-2018&partnerID=40&md5=e4a223b24e196276e625422b6f45797a info:eu-repo/semantics/article 2018 ftenea https://doi.org/20.500.12079/478710.5194/tc-12-3775-2018 2024-01-23T23:16:51Z 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° latitude by 2° longitude, is able to accurately represent the snowfall climatology at the three MRR sites (biases<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. © 2018 Author(s). Article in Journal/Newspaper Antarc* Antarctic Antarctica Ice Sheet ENEA-IRIS Open Archive (Agenzia nazionale per le nuove tecnologie, l'energia e lo sviluppo economico sostenibile) Antarctic The Antarctic The Cryosphere 12 12 3775 3789
institution Open Polar
collection ENEA-IRIS Open Archive (Agenzia nazionale per le nuove tecnologie, l'energia e lo sviluppo economico sostenibile)
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language English
description 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° latitude by 2° longitude, is able to accurately represent the snowfall climatology at the three MRR sites (biases<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. © 2018 Author(s).
author2 Scarchilli, C.
format Article in Journal/Newspaper
author Scarchilli, C.
spellingShingle Scarchilli, C.
Evaluation of the CloudSat surface snowfall product over Antarctica using ground-based precipitation radars
author_facet Scarchilli, C.
author_sort Scarchilli, C.
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 GmbH
publishDate 2018
url https://hdl.handle.net/20.500.12079/4787
https://doi.org/10.5194/tc-12-3775-2018
https://www.scopus.com/inward/record.uri?eid=2-s2.0-85057741258&doi=10.5194%2ftc-12-3775-2018&partnerID=40&md5=e4a223b24e196276e625422b6f45797a
geographic Antarctic
The Antarctic
geographic_facet Antarctic
The Antarctic
genre Antarc*
Antarctic
Antarctica
Ice Sheet
genre_facet Antarc*
Antarctic
Antarctica
Ice Sheet
op_relation volume:12
issue:12
numberofpages:3775 - 3789
journal:THE CRYOSPHERE
http://hdl.handle.net/20.500.12079/4787
doi:10.5194/tc-12-3775-2018
info:eu-repo/semantics/altIdentifier/scopus/Scopus ID: 2-s2.0-85057741258
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