Validating CloudSat-CPR retrievals for the estimation of snow accumulation in the Canadian Arctic

Snow is a critical contributor to our global water and energy budget, with profound impacts for water resource availability, snow albedo feedback and flooding in cold regions. The vast size and remote nature of the Arctic present serious logistical and financial challenges to measuring snow over ext...

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Bibliographic Details
Main Author: King, Fraser
Format: Master Thesis
Language:English
Published: University of Waterloo 2019
Subjects:
CPR
CSA
SWE
Online Access:http://hdl.handle.net/10012/14736
id ftunivwaterloo:oai:uwspace.uwaterloo.ca:10012/14736
record_format openpolar
spelling ftunivwaterloo:oai:uwspace.uwaterloo.ca:10012/14736 2023-05-15T13:11:14+02:00 Validating CloudSat-CPR retrievals for the estimation of snow accumulation in the Canadian Arctic King, Fraser 2019-05-29 http://hdl.handle.net/10012/14736 en eng University of Waterloo http://hdl.handle.net/10012/14736 CloudSat Arctic snow station in situ comparison CPR remote sensing reanalysis radar Canada NASA CSA satellite clouds SWE Master Thesis 2019 ftunivwaterloo 2022-06-18T23:02:24Z Snow is a critical contributor to our global water and energy budget, with profound impacts for water resource availability, snow albedo feedback and flooding in cold regions. The vast size and remote nature of the Arctic present serious logistical and financial challenges to measuring snow over extended time periods. Satellite observations provided by the Cloud Profiling Radar (CPR) instrument-installed on the NASA satellite CloudSat-allow the retrieval of snowfall rates in high latitude regions, which have been used to estimate surface snow accumulation. In this study, a validation of CloudSat-derived terrestrial snow estimates is presented at four Environment and Climate Change Canada (ECCC) weather stations situated in the Arctic for the common period 2007-2015. Comparisons of monthly climatological snow accumulation show mean biases of less than 1.5 mm SWE annually. Monthly time series exhibit correlations above 0.5 and RMSE below 10 mm SWE at the two highest latitude stations (Eureka and Resolute Bay) with correlations falling below 0.5 south of 70 degrees N. CloudSat was also found to underestimate annual mean snow accumulation at the majority of sites, suggesting a potential negative bias in CloudSat's snowfall estimates, or underestimation related to sampling. These results imply that CloudSat can provide reliable estimates of snow accumulation across similar high latitude regions above 70 degrees N. Accurate space-based snowfall measurements provide new important observational perspectives of Arctic snow accumulation, which is a critical region for environmental monitoring in an era of global change. Master Thesis albedo Arctic Climate change Resolute Bay University of Waterloo, Canada: Institutional Repository Arctic Canada Eureka ENVELOPE(-85.940,-85.940,79.990,79.990) Resolute Bay ENVELOPE(-94.842,-94.842,74.677,74.677)
institution Open Polar
collection University of Waterloo, Canada: Institutional Repository
op_collection_id ftunivwaterloo
language English
topic CloudSat
Arctic
snow
station
in situ
comparison
CPR
remote sensing
reanalysis
radar
Canada
NASA
CSA
satellite
clouds
SWE
spellingShingle CloudSat
Arctic
snow
station
in situ
comparison
CPR
remote sensing
reanalysis
radar
Canada
NASA
CSA
satellite
clouds
SWE
King, Fraser
Validating CloudSat-CPR retrievals for the estimation of snow accumulation in the Canadian Arctic
topic_facet CloudSat
Arctic
snow
station
in situ
comparison
CPR
remote sensing
reanalysis
radar
Canada
NASA
CSA
satellite
clouds
SWE
description Snow is a critical contributor to our global water and energy budget, with profound impacts for water resource availability, snow albedo feedback and flooding in cold regions. The vast size and remote nature of the Arctic present serious logistical and financial challenges to measuring snow over extended time periods. Satellite observations provided by the Cloud Profiling Radar (CPR) instrument-installed on the NASA satellite CloudSat-allow the retrieval of snowfall rates in high latitude regions, which have been used to estimate surface snow accumulation. In this study, a validation of CloudSat-derived terrestrial snow estimates is presented at four Environment and Climate Change Canada (ECCC) weather stations situated in the Arctic for the common period 2007-2015. Comparisons of monthly climatological snow accumulation show mean biases of less than 1.5 mm SWE annually. Monthly time series exhibit correlations above 0.5 and RMSE below 10 mm SWE at the two highest latitude stations (Eureka and Resolute Bay) with correlations falling below 0.5 south of 70 degrees N. CloudSat was also found to underestimate annual mean snow accumulation at the majority of sites, suggesting a potential negative bias in CloudSat's snowfall estimates, or underestimation related to sampling. These results imply that CloudSat can provide reliable estimates of snow accumulation across similar high latitude regions above 70 degrees N. Accurate space-based snowfall measurements provide new important observational perspectives of Arctic snow accumulation, which is a critical region for environmental monitoring in an era of global change.
format Master Thesis
author King, Fraser
author_facet King, Fraser
author_sort King, Fraser
title Validating CloudSat-CPR retrievals for the estimation of snow accumulation in the Canadian Arctic
title_short Validating CloudSat-CPR retrievals for the estimation of snow accumulation in the Canadian Arctic
title_full Validating CloudSat-CPR retrievals for the estimation of snow accumulation in the Canadian Arctic
title_fullStr Validating CloudSat-CPR retrievals for the estimation of snow accumulation in the Canadian Arctic
title_full_unstemmed Validating CloudSat-CPR retrievals for the estimation of snow accumulation in the Canadian Arctic
title_sort validating cloudsat-cpr retrievals for the estimation of snow accumulation in the canadian arctic
publisher University of Waterloo
publishDate 2019
url http://hdl.handle.net/10012/14736
long_lat ENVELOPE(-85.940,-85.940,79.990,79.990)
ENVELOPE(-94.842,-94.842,74.677,74.677)
geographic Arctic
Canada
Eureka
Resolute Bay
geographic_facet Arctic
Canada
Eureka
Resolute Bay
genre albedo
Arctic
Climate change
Resolute Bay
genre_facet albedo
Arctic
Climate change
Resolute Bay
op_relation http://hdl.handle.net/10012/14736
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