Validation of CloudSat-CPR Derived Precipitation Occurrence and Phase Estimates across Canada

Snowfall affects the terrestrial climate system at high latitudes through its impacts on local meteorology, freshwater resources and energy balance. Precise snowfall monitoring is essential for cold countries such as Canada, and particularly in temperature-sensitive regions such as the Arctic; howev...

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Published in:Atmosphere
Main Authors: Rithwik Kodamana, Christopher G. Fletcher
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2021
Subjects:
Online Access:https://doi.org/10.3390/atmos12030295
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spelling ftmdpi:oai:mdpi.com:/2073-4433/12/3/295/ 2023-08-20T04:04:15+02:00 Validation of CloudSat-CPR Derived Precipitation Occurrence and Phase Estimates across Canada Rithwik Kodamana Christopher G. Fletcher agris 2021-02-25 application/pdf https://doi.org/10.3390/atmos12030295 EN eng Multidisciplinary Digital Publishing Institute Meteorology https://dx.doi.org/10.3390/atmos12030295 https://creativecommons.org/licenses/by/4.0/ Atmosphere; Volume 12; Issue 3; Pages: 295 remote sensing CloudSat POSS snowfall arctic precipitation phase ground validation Text 2021 ftmdpi https://doi.org/10.3390/atmos12030295 2023-08-01T01:08:35Z Snowfall affects the terrestrial climate system at high latitudes through its impacts on local meteorology, freshwater resources and energy balance. Precise snowfall monitoring is essential for cold countries such as Canada, and particularly in temperature-sensitive regions such as the Arctic; however, its size and remote location means the precipitation gauge network there is sparse. While satellite remote sensing of snowfall from instruments such as CloudSat-CPR offers a potential solution, satellite detection of precipitation phase has not been systematically evaluated across Canada. In this study, CloudSat-based precipitation occurrence and phase retrievals were validated at 26 stations across Canada maintained by Environment and Climate Change Canada (ECCC). Probability of Detection (POD), defined as the percentage agreement between coincident CloudSat and human-observed present weather information for precipitation (solid, liquid or no precipitation), and False Alarm Ratio (FAR) were used as the primary metrics for validation. The mean POD (FAR) for precipitation occurrence across Canada is 65.5% ± 4.3 (31.4% ± 5.1) and for no precipitation is 90.6% ± 1.4 (11% ± 2.5). The results show lower rates of detection under cloudier skies, in the presence of (freezing) drizzle and for lighter snowfall, which may be explained by a large number of false-positives due to CloudSat-CPR’s high instrumental sensitivity. When CloudSat correctly detects the occurrence of precipitation, it shows uniformly high POD (>80%) and low FAR (<10%) for classifying the phase of precipitation. Large databases of coincident ground and satellite measurements allow us to provide a new estimate of around 9% for the frequency of virga events, a factor of two smaller than a previous estimate for the Arctic. The results from this study show that CloudSat has useful accuracy in detecting precipitation occurrence and very high accuracy at classifying precipitation phase, over diverse climate zones across Canada. As such, there is ... Text Arctic Climate change MDPI Open Access Publishing Arctic Canada Atmosphere 12 3 295
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic remote sensing
CloudSat
POSS
snowfall
arctic
precipitation phase
ground validation
spellingShingle remote sensing
CloudSat
POSS
snowfall
arctic
precipitation phase
ground validation
Rithwik Kodamana
Christopher G. Fletcher
Validation of CloudSat-CPR Derived Precipitation Occurrence and Phase Estimates across Canada
topic_facet remote sensing
CloudSat
POSS
snowfall
arctic
precipitation phase
ground validation
description Snowfall affects the terrestrial climate system at high latitudes through its impacts on local meteorology, freshwater resources and energy balance. Precise snowfall monitoring is essential for cold countries such as Canada, and particularly in temperature-sensitive regions such as the Arctic; however, its size and remote location means the precipitation gauge network there is sparse. While satellite remote sensing of snowfall from instruments such as CloudSat-CPR offers a potential solution, satellite detection of precipitation phase has not been systematically evaluated across Canada. In this study, CloudSat-based precipitation occurrence and phase retrievals were validated at 26 stations across Canada maintained by Environment and Climate Change Canada (ECCC). Probability of Detection (POD), defined as the percentage agreement between coincident CloudSat and human-observed present weather information for precipitation (solid, liquid or no precipitation), and False Alarm Ratio (FAR) were used as the primary metrics for validation. The mean POD (FAR) for precipitation occurrence across Canada is 65.5% ± 4.3 (31.4% ± 5.1) and for no precipitation is 90.6% ± 1.4 (11% ± 2.5). The results show lower rates of detection under cloudier skies, in the presence of (freezing) drizzle and for lighter snowfall, which may be explained by a large number of false-positives due to CloudSat-CPR’s high instrumental sensitivity. When CloudSat correctly detects the occurrence of precipitation, it shows uniformly high POD (>80%) and low FAR (<10%) for classifying the phase of precipitation. Large databases of coincident ground and satellite measurements allow us to provide a new estimate of around 9% for the frequency of virga events, a factor of two smaller than a previous estimate for the Arctic. The results from this study show that CloudSat has useful accuracy in detecting precipitation occurrence and very high accuracy at classifying precipitation phase, over diverse climate zones across Canada. As such, there is ...
format Text
author Rithwik Kodamana
Christopher G. Fletcher
author_facet Rithwik Kodamana
Christopher G. Fletcher
author_sort Rithwik Kodamana
title Validation of CloudSat-CPR Derived Precipitation Occurrence and Phase Estimates across Canada
title_short Validation of CloudSat-CPR Derived Precipitation Occurrence and Phase Estimates across Canada
title_full Validation of CloudSat-CPR Derived Precipitation Occurrence and Phase Estimates across Canada
title_fullStr Validation of CloudSat-CPR Derived Precipitation Occurrence and Phase Estimates across Canada
title_full_unstemmed Validation of CloudSat-CPR Derived Precipitation Occurrence and Phase Estimates across Canada
title_sort validation of cloudsat-cpr derived precipitation occurrence and phase estimates across canada
publisher Multidisciplinary Digital Publishing Institute
publishDate 2021
url https://doi.org/10.3390/atmos12030295
op_coverage agris
geographic Arctic
Canada
geographic_facet Arctic
Canada
genre Arctic
Climate change
genre_facet Arctic
Climate change
op_source Atmosphere; Volume 12; Issue 3; Pages: 295
op_relation Meteorology
https://dx.doi.org/10.3390/atmos12030295
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/atmos12030295
container_title Atmosphere
container_volume 12
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