The Energetics of Extensive Melt Water Flooding of Level Arctic Sea Ice

During the spring-to-summer transition, the snow cover on Arctic sea ice melts and meltwater pools on the surface to form melt ponds; however, the timing and extent of the ponding varies between years. In Dease Strait (Nunavut), this transition was particularly dramatic in 2014 when on 18 June meltw...

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Format: Dataset
Language:unknown
Published: Canadian Watershed Information Network (CanWIN) 2023
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Online Access:https://search.dataone.org/view/sha256:a014502d4ca277edabbe311183587f892df32a4222bb39290c76a965d78ac780
id dataone:sha256:a014502d4ca277edabbe311183587f892df32a4222bb39290c76a965d78ac780
record_format openpolar
spelling dataone:sha256:a014502d4ca277edabbe311183587f892df32a4222bb39290c76a965d78ac780 2024-11-03T19:44:44+00:00 The Energetics of Extensive Melt Water Flooding of Level Arctic Sea Ice BEGINDATE: 2014-04-25T00:00:00Z ENDDATE: 2014-06-27T00:00:00Z 2023-01-01T00:00:00Z https://search.dataone.org/view/sha256:a014502d4ca277edabbe311183587f892df32a4222bb39290c76a965d78ac780 unknown Canadian Watershed Information Network (CanWIN) Salinity Meteorological Landfast ice Snow Air temperature Wind speed CTD profiles Albedo Sea ice Sea ice melt Dataset 2023 dataone:urn:node:CANWIN 2024-11-03T19:19:05Z During the spring-to-summer transition, the snow cover on Arctic sea ice melts and meltwater pools on the surface to form melt ponds; however, the timing and extent of the ponding varies between years. In Dease Strait (Nunavut), this transition was particularly dramatic in 2014 when on 18 June meltwater had flooded >95% of the surface. In this study, continuous surface energy balance measurements throughout the transition highlight how the timing of transient weather events influenced seasonal shifts in distinct ice melt stages. The keys to the extensive flooding were 1) the level ice cover, 2) a strong low-pressure system on 24 May that deposited ~10 cm of snow, and 3) freeze-thaw cycling and a subsequent return to sub-zero air temperatures on 30 May that led to superimposed and interposed ice formation. Without these, melt ponds would have likely developed within days from an initial melt onset on 28 May. After a 2-week delay, snow-melt resumed and lead to near-complete flooding of the surface for four days. The albedo of the flooded ice remained high (0.35-0.40), as a result of the bubble-laden superimposed ice layer. Once this layer eroded, the albedo over melt ponds decreased to a more typical level (~0.20). Our observations suggest that the formation of superimposed and interposed ice prevented the vertical drainage of meltwater to the ocean. Future challenges remain to measure the presence of these layers and understand their effect on sea ice permeability and pond evolution while sea ice temperatures are near the melting point. We present a time series of the full surface energy budget of the landfast sea ice cover in Dease Strait, Nunavut (Canada), over the spring to summer transition in 2014. Time-series of hourly means of vertical temperature in the snow, sea ice, and seawater. This is the metadata template associated with the data files. Contains site locations for atmospheric, ice, snow and seawater data. Dataset albedo Arctic Nunavut Sea ice Canadian Watershed Information Network (CanWIN) (via DataONE) Arctic Canada Dease Strait ENVELOPE(-107.502,-107.502,68.834,68.834) Nunavut
institution Open Polar
collection Canadian Watershed Information Network (CanWIN) (via DataONE)
op_collection_id dataone:urn:node:CANWIN
language unknown
topic Salinity
Meteorological
Landfast ice
Snow
Air temperature
Wind speed
CTD profiles
Albedo
Sea ice
Sea ice melt
spellingShingle Salinity
Meteorological
Landfast ice
Snow
Air temperature
Wind speed
CTD profiles
Albedo
Sea ice
Sea ice melt
The Energetics of Extensive Melt Water Flooding of Level Arctic Sea Ice
topic_facet Salinity
Meteorological
Landfast ice
Snow
Air temperature
Wind speed
CTD profiles
Albedo
Sea ice
Sea ice melt
description During the spring-to-summer transition, the snow cover on Arctic sea ice melts and meltwater pools on the surface to form melt ponds; however, the timing and extent of the ponding varies between years. In Dease Strait (Nunavut), this transition was particularly dramatic in 2014 when on 18 June meltwater had flooded >95% of the surface. In this study, continuous surface energy balance measurements throughout the transition highlight how the timing of transient weather events influenced seasonal shifts in distinct ice melt stages. The keys to the extensive flooding were 1) the level ice cover, 2) a strong low-pressure system on 24 May that deposited ~10 cm of snow, and 3) freeze-thaw cycling and a subsequent return to sub-zero air temperatures on 30 May that led to superimposed and interposed ice formation. Without these, melt ponds would have likely developed within days from an initial melt onset on 28 May. After a 2-week delay, snow-melt resumed and lead to near-complete flooding of the surface for four days. The albedo of the flooded ice remained high (0.35-0.40), as a result of the bubble-laden superimposed ice layer. Once this layer eroded, the albedo over melt ponds decreased to a more typical level (~0.20). Our observations suggest that the formation of superimposed and interposed ice prevented the vertical drainage of meltwater to the ocean. Future challenges remain to measure the presence of these layers and understand their effect on sea ice permeability and pond evolution while sea ice temperatures are near the melting point. We present a time series of the full surface energy budget of the landfast sea ice cover in Dease Strait, Nunavut (Canada), over the spring to summer transition in 2014. Time-series of hourly means of vertical temperature in the snow, sea ice, and seawater. This is the metadata template associated with the data files. Contains site locations for atmospheric, ice, snow and seawater data.
format Dataset
title The Energetics of Extensive Melt Water Flooding of Level Arctic Sea Ice
title_short The Energetics of Extensive Melt Water Flooding of Level Arctic Sea Ice
title_full The Energetics of Extensive Melt Water Flooding of Level Arctic Sea Ice
title_fullStr The Energetics of Extensive Melt Water Flooding of Level Arctic Sea Ice
title_full_unstemmed The Energetics of Extensive Melt Water Flooding of Level Arctic Sea Ice
title_sort energetics of extensive melt water flooding of level arctic sea ice
publisher Canadian Watershed Information Network (CanWIN)
publishDate 2023
url https://search.dataone.org/view/sha256:a014502d4ca277edabbe311183587f892df32a4222bb39290c76a965d78ac780
op_coverage BEGINDATE: 2014-04-25T00:00:00Z ENDDATE: 2014-06-27T00:00:00Z
long_lat ENVELOPE(-107.502,-107.502,68.834,68.834)
geographic Arctic
Canada
Dease Strait
Nunavut
geographic_facet Arctic
Canada
Dease Strait
Nunavut
genre albedo
Arctic
Nunavut
Sea ice
genre_facet albedo
Arctic
Nunavut
Sea ice
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