Global and Regional Snow Cover Decline: 2000–2022

Snow cover affects the global surface energy balance and, with its high albedo, exerts a cooling effect on the Earth’s climate. Decreases in snow cover alter the flow of solar energy from being reflected away from Earth to being absorbed, increasing the Earth’s surface temperature. To gain a global...

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Published in:Climate
Main Author: Stephen S. Young
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2023
Subjects:
Online Access:https://doi.org/10.3390/cli11080162
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spelling ftmdpi:oai:mdpi.com:/2225-1154/11/8/162/ 2023-08-20T04:01:29+02:00 Global and Regional Snow Cover Decline: 2000–2022 Stephen S. Young agris 2023-07-29 application/pdf https://doi.org/10.3390/cli11080162 EN eng Multidisciplinary Digital Publishing Institute https://dx.doi.org/10.3390/cli11080162 https://creativecommons.org/licenses/by/4.0/ Climate; Volume 11; Issue 8; Pages: 162 snow cover extent MODIS Mann—Kendall test univariate differencing Text 2023 ftmdpi https://doi.org/10.3390/cli11080162 2023-08-01T11:04:31Z Snow cover affects the global surface energy balance and, with its high albedo, exerts a cooling effect on the Earth’s climate. Decreases in snow cover alter the flow of solar energy from being reflected away from Earth to being absorbed, increasing the Earth’s surface temperature. To gain a global understanding of snow cover change, in situ measurements are too few and far between, so remotely sensed data are needed. This research used the medium-resolution sensor MODIS on the Terra satellite, which has been observing global snow cover almost daily since the year 2000. Here, the MOD10C2 eight-day maximum value composite time series data from February 2000 to March 2023 were analyzed to detect global and regional trends in snow cover extent for the first 23 years of the 21st century. Trends in snow cover change during different time periods (seasons and snow-year) were examined using the Mann—Kendall test and the univariate differencing analysis. Both methods produced similar results. Globally, snow cover declined two to ten times as much as it increased, depending on the season of analysis, and annually, global snow cover decreased 5.12% (not including Antarctica or Greenland) based on the Mann—Kendall test at the 95th percentile (p < 0.05). Regionally, Asia had the greatest net area decline in snow cover, followed by Europe. Although North America has the second-largest extent of snow cover, it had the least amount of net decreasing snow cover relative to its size. South America had the greatest local decline in snow cover, decreasing 20.60% of its annual (snow-year) snow cover area. The Australia–New Zealand region, with just 0.34% of the global snow cover, was the only region to have a net increase in snow cover, increasing 3.61% of its annual snow cover area. Text Antarc* Antarctica Greenland MDPI Open Access Publishing Greenland Kendall ENVELOPE(-59.828,-59.828,-63.497,-63.497) New Zealand Climate 11 8 162
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic snow cover extent
MODIS
Mann—Kendall test
univariate differencing
spellingShingle snow cover extent
MODIS
Mann—Kendall test
univariate differencing
Stephen S. Young
Global and Regional Snow Cover Decline: 2000–2022
topic_facet snow cover extent
MODIS
Mann—Kendall test
univariate differencing
description Snow cover affects the global surface energy balance and, with its high albedo, exerts a cooling effect on the Earth’s climate. Decreases in snow cover alter the flow of solar energy from being reflected away from Earth to being absorbed, increasing the Earth’s surface temperature. To gain a global understanding of snow cover change, in situ measurements are too few and far between, so remotely sensed data are needed. This research used the medium-resolution sensor MODIS on the Terra satellite, which has been observing global snow cover almost daily since the year 2000. Here, the MOD10C2 eight-day maximum value composite time series data from February 2000 to March 2023 were analyzed to detect global and regional trends in snow cover extent for the first 23 years of the 21st century. Trends in snow cover change during different time periods (seasons and snow-year) were examined using the Mann—Kendall test and the univariate differencing analysis. Both methods produced similar results. Globally, snow cover declined two to ten times as much as it increased, depending on the season of analysis, and annually, global snow cover decreased 5.12% (not including Antarctica or Greenland) based on the Mann—Kendall test at the 95th percentile (p < 0.05). Regionally, Asia had the greatest net area decline in snow cover, followed by Europe. Although North America has the second-largest extent of snow cover, it had the least amount of net decreasing snow cover relative to its size. South America had the greatest local decline in snow cover, decreasing 20.60% of its annual (snow-year) snow cover area. The Australia–New Zealand region, with just 0.34% of the global snow cover, was the only region to have a net increase in snow cover, increasing 3.61% of its annual snow cover area.
format Text
author Stephen S. Young
author_facet Stephen S. Young
author_sort Stephen S. Young
title Global and Regional Snow Cover Decline: 2000–2022
title_short Global and Regional Snow Cover Decline: 2000–2022
title_full Global and Regional Snow Cover Decline: 2000–2022
title_fullStr Global and Regional Snow Cover Decline: 2000–2022
title_full_unstemmed Global and Regional Snow Cover Decline: 2000–2022
title_sort global and regional snow cover decline: 2000–2022
publisher Multidisciplinary Digital Publishing Institute
publishDate 2023
url https://doi.org/10.3390/cli11080162
op_coverage agris
long_lat ENVELOPE(-59.828,-59.828,-63.497,-63.497)
geographic Greenland
Kendall
New Zealand
geographic_facet Greenland
Kendall
New Zealand
genre Antarc*
Antarctica
Greenland
genre_facet Antarc*
Antarctica
Greenland
op_source Climate; Volume 11; Issue 8; Pages: 162
op_relation https://dx.doi.org/10.3390/cli11080162
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/cli11080162
container_title Climate
container_volume 11
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container_start_page 162
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