Observations of sea ice melt from Operation IceBridge imagery

The summer albedo of Arctic sea ice is heavily dependent on the fraction and color of melt ponds that form on the ice surface. This work presents a new dataset of sea ice surface fractions along Operation IceBridge (OIB) flight tracks derived from the Digital Mapping System optical imagery set. This...

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Published in:The Cryosphere
Main Authors: N. C. Wright, C. M. Polashenski, S. T. McMichael, R. A. Beyer
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2020
Subjects:
Online Access:https://doi.org/10.5194/tc-14-3523-2020
https://doaj.org/article/3d5cb27a185f49b2983ee384fb7997d6
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spelling ftdoajarticles:oai:doaj.org/article:3d5cb27a185f49b2983ee384fb7997d6 2023-05-15T13:11:33+02:00 Observations of sea ice melt from Operation IceBridge imagery N. C. Wright C. M. Polashenski S. T. McMichael R. A. Beyer 2020-10-01T00:00:00Z https://doi.org/10.5194/tc-14-3523-2020 https://doaj.org/article/3d5cb27a185f49b2983ee384fb7997d6 EN eng Copernicus Publications https://tc.copernicus.org/articles/14/3523/2020/tc-14-3523-2020.pdf https://doaj.org/toc/1994-0416 https://doaj.org/toc/1994-0424 doi:10.5194/tc-14-3523-2020 1994-0416 1994-0424 https://doaj.org/article/3d5cb27a185f49b2983ee384fb7997d6 The Cryosphere, Vol 14, Pp 3523-3536 (2020) Environmental sciences GE1-350 Geology QE1-996.5 article 2020 ftdoajarticles https://doi.org/10.5194/tc-14-3523-2020 2022-12-31T01:29:48Z The summer albedo of Arctic sea ice is heavily dependent on the fraction and color of melt ponds that form on the ice surface. This work presents a new dataset of sea ice surface fractions along Operation IceBridge (OIB) flight tracks derived from the Digital Mapping System optical imagery set. This dataset was created by deploying version 2 of the Open Source Sea-ice Processing (OSSP) algorithm to NASA's Advanced Supercomputing Pleiades System. These new surface fraction results are then analyzed to investigate the behavior of meltwater on first-year ice in comparison to multiyear ice. Observations herein show that first-year ice does not ubiquitously have a higher melt pond fraction than multiyear ice under the same forcing conditions, contrary to established knowledge in the sea ice community. We discover and document a larger possible spread of pond fractions on first-year ice leading to both high and low pond coverage, in contrast to the uniform melt evolution that has been previously observed on multiyear ice floes. We also present a selection of optical images that capture both the typical and atypical ice types, as observed from the OIB dataset. The derived OIB data presented here will be key to explore the behavior of melt pond formation Arctic sea ice. Article in Journal/Newspaper albedo Arctic Sea ice The Cryosphere Directory of Open Access Journals: DOAJ Articles Arctic Pleiades ENVELOPE(165.533,165.533,-72.700,-72.700) The Cryosphere 14 10 3523 3536
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Environmental sciences
GE1-350
Geology
QE1-996.5
spellingShingle Environmental sciences
GE1-350
Geology
QE1-996.5
N. C. Wright
C. M. Polashenski
S. T. McMichael
R. A. Beyer
Observations of sea ice melt from Operation IceBridge imagery
topic_facet Environmental sciences
GE1-350
Geology
QE1-996.5
description The summer albedo of Arctic sea ice is heavily dependent on the fraction and color of melt ponds that form on the ice surface. This work presents a new dataset of sea ice surface fractions along Operation IceBridge (OIB) flight tracks derived from the Digital Mapping System optical imagery set. This dataset was created by deploying version 2 of the Open Source Sea-ice Processing (OSSP) algorithm to NASA's Advanced Supercomputing Pleiades System. These new surface fraction results are then analyzed to investigate the behavior of meltwater on first-year ice in comparison to multiyear ice. Observations herein show that first-year ice does not ubiquitously have a higher melt pond fraction than multiyear ice under the same forcing conditions, contrary to established knowledge in the sea ice community. We discover and document a larger possible spread of pond fractions on first-year ice leading to both high and low pond coverage, in contrast to the uniform melt evolution that has been previously observed on multiyear ice floes. We also present a selection of optical images that capture both the typical and atypical ice types, as observed from the OIB dataset. The derived OIB data presented here will be key to explore the behavior of melt pond formation Arctic sea ice.
format Article in Journal/Newspaper
author N. C. Wright
C. M. Polashenski
S. T. McMichael
R. A. Beyer
author_facet N. C. Wright
C. M. Polashenski
S. T. McMichael
R. A. Beyer
author_sort N. C. Wright
title Observations of sea ice melt from Operation IceBridge imagery
title_short Observations of sea ice melt from Operation IceBridge imagery
title_full Observations of sea ice melt from Operation IceBridge imagery
title_fullStr Observations of sea ice melt from Operation IceBridge imagery
title_full_unstemmed Observations of sea ice melt from Operation IceBridge imagery
title_sort observations of sea ice melt from operation icebridge imagery
publisher Copernicus Publications
publishDate 2020
url https://doi.org/10.5194/tc-14-3523-2020
https://doaj.org/article/3d5cb27a185f49b2983ee384fb7997d6
long_lat ENVELOPE(165.533,165.533,-72.700,-72.700)
geographic Arctic
Pleiades
geographic_facet Arctic
Pleiades
genre albedo
Arctic
Sea ice
The Cryosphere
genre_facet albedo
Arctic
Sea ice
The Cryosphere
op_source The Cryosphere, Vol 14, Pp 3523-3536 (2020)
op_relation https://tc.copernicus.org/articles/14/3523/2020/tc-14-3523-2020.pdf
https://doaj.org/toc/1994-0416
https://doaj.org/toc/1994-0424
doi:10.5194/tc-14-3523-2020
1994-0416
1994-0424
https://doaj.org/article/3d5cb27a185f49b2983ee384fb7997d6
op_doi https://doi.org/10.5194/tc-14-3523-2020
container_title The Cryosphere
container_volume 14
container_issue 10
container_start_page 3523
op_container_end_page 3536
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