Daily Area of Snow Melt Onset on Arctic Sea Ice from Passive Microwave Satellite Observations 1979–2012

Variability in snow melt onset (MO) on Arctic sea ice since 1979 is examined by determining the area of sea ice experiencing the onset of melting during the melt season on a daily basis. The daily MO area of the snow and ice surface is determined from passive microwave satellite-derived MO dates for...

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Published in:Remote Sensing
Main Authors: Angela Bliss, Mark Anderson
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2014
Subjects:
Online Access:https://doi.org/10.3390/rs61111283
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spelling ftmdpi:oai:mdpi.com:/2072-4292/6/11/11283/ 2023-09-26T15:13:07+02:00 Daily Area of Snow Melt Onset on Arctic Sea Ice from Passive Microwave Satellite Observations 1979–2012 Angela Bliss Mark Anderson agris 2014-11-13 application/pdf https://doi.org/10.3390/rs61111283 EN eng Multidisciplinary Digital Publishing Institute https://dx.doi.org/10.3390/rs61111283 https://creativecommons.org/licenses/by/4.0/ Remote Sensing; Volume 6; Issue 11; Pages: 11283-11314 Arctic sea ice melt onset snow melt passive microwave remote sensing Text 2014 ftmdpi https://doi.org/10.3390/rs61111283 2023-08-27T23:52:26Z Variability in snow melt onset (MO) on Arctic sea ice since 1979 is examined by determining the area of sea ice experiencing the onset of melting during the melt season on a daily basis. The daily MO area of the snow and ice surface is determined from passive microwave satellite-derived MO dates for the Arctic Ocean and sub-regions. Annual accumulations of MO area are determined by summing the time series of daily MO area through the melt season. Daily areas and annual accumulations of MO area highlight inter-annual and regional variability in the timing of MO area, which is sensitive to day-to-day variations in spring weather conditions. Two distinct spatial patterns in MO area accumulations including an intense, fast accumulating melt area pattern and a slow accumulating melt pattern are examined for two melting events in the Kara Sea. In comparing the 34 years of MO dates for the Arctic Ocean and sub-regions, melt accumulations have changed during the period. In the earlier years, 1979–1987, the MO generally was later in the year than the mean, while in more recent years, the MO accumulations have been occurring earlier in the melt season. The sub-regions of the Arctic Ocean also exhibit greater annual variability than the Arctic Ocean. Text Arctic Arctic Ocean Kara Sea Sea ice MDPI Open Access Publishing Arctic Arctic Ocean Kara Sea Remote Sensing 6 11 11283 11314
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic Arctic
sea ice
melt onset
snow melt
passive microwave
remote sensing
spellingShingle Arctic
sea ice
melt onset
snow melt
passive microwave
remote sensing
Angela Bliss
Mark Anderson
Daily Area of Snow Melt Onset on Arctic Sea Ice from Passive Microwave Satellite Observations 1979–2012
topic_facet Arctic
sea ice
melt onset
snow melt
passive microwave
remote sensing
description Variability in snow melt onset (MO) on Arctic sea ice since 1979 is examined by determining the area of sea ice experiencing the onset of melting during the melt season on a daily basis. The daily MO area of the snow and ice surface is determined from passive microwave satellite-derived MO dates for the Arctic Ocean and sub-regions. Annual accumulations of MO area are determined by summing the time series of daily MO area through the melt season. Daily areas and annual accumulations of MO area highlight inter-annual and regional variability in the timing of MO area, which is sensitive to day-to-day variations in spring weather conditions. Two distinct spatial patterns in MO area accumulations including an intense, fast accumulating melt area pattern and a slow accumulating melt pattern are examined for two melting events in the Kara Sea. In comparing the 34 years of MO dates for the Arctic Ocean and sub-regions, melt accumulations have changed during the period. In the earlier years, 1979–1987, the MO generally was later in the year than the mean, while in more recent years, the MO accumulations have been occurring earlier in the melt season. The sub-regions of the Arctic Ocean also exhibit greater annual variability than the Arctic Ocean.
format Text
author Angela Bliss
Mark Anderson
author_facet Angela Bliss
Mark Anderson
author_sort Angela Bliss
title Daily Area of Snow Melt Onset on Arctic Sea Ice from Passive Microwave Satellite Observations 1979–2012
title_short Daily Area of Snow Melt Onset on Arctic Sea Ice from Passive Microwave Satellite Observations 1979–2012
title_full Daily Area of Snow Melt Onset on Arctic Sea Ice from Passive Microwave Satellite Observations 1979–2012
title_fullStr Daily Area of Snow Melt Onset on Arctic Sea Ice from Passive Microwave Satellite Observations 1979–2012
title_full_unstemmed Daily Area of Snow Melt Onset on Arctic Sea Ice from Passive Microwave Satellite Observations 1979–2012
title_sort daily area of snow melt onset on arctic sea ice from passive microwave satellite observations 1979–2012
publisher Multidisciplinary Digital Publishing Institute
publishDate 2014
url https://doi.org/10.3390/rs61111283
op_coverage agris
geographic Arctic
Arctic Ocean
Kara Sea
geographic_facet Arctic
Arctic Ocean
Kara Sea
genre Arctic
Arctic Ocean
Kara Sea
Sea ice
genre_facet Arctic
Arctic Ocean
Kara Sea
Sea ice
op_source Remote Sensing; Volume 6; Issue 11; Pages: 11283-11314
op_relation https://dx.doi.org/10.3390/rs61111283
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/rs61111283
container_title Remote Sensing
container_volume 6
container_issue 11
container_start_page 11283
op_container_end_page 11314
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