author_facet Webster, Melinda A.
Rigor, Ignatius G.
Perovich, Donald K.
Richter‐Menge, Jacqueline A.
Polashenski, Christopher M.
Light, Bonnie
Webster, Melinda A.
Rigor, Ignatius G.
Perovich, Donald K.
Richter‐Menge, Jacqueline A.
Polashenski, Christopher M.
Light, Bonnie
author Webster, Melinda A.
Rigor, Ignatius G.
Perovich, Donald K.
Richter‐Menge, Jacqueline A.
Polashenski, Christopher M.
Light, Bonnie
spellingShingle Webster, Melinda A.
Rigor, Ignatius G.
Perovich, Donald K.
Richter‐Menge, Jacqueline A.
Polashenski, Christopher M.
Light, Bonnie
Journal of Geophysical Research: Oceans
Seasonal evolution of melt ponds on Arctic sea ice
Earth and Planetary Sciences (miscellaneous)
Space and Planetary Science
Geochemistry and Petrology
Geophysics
Oceanography
author_sort webster, melinda a.
spelling Webster, Melinda A. Rigor, Ignatius G. Perovich, Donald K. Richter‐Menge, Jacqueline A. Polashenski, Christopher M. Light, Bonnie 2169-9275 2169-9291 American Geophysical Union (AGU) Earth and Planetary Sciences (miscellaneous) Space and Planetary Science Geochemistry and Petrology Geophysics Oceanography http://dx.doi.org/10.1002/2015jc011030 <jats:title>Abstract</jats:title><jats:p>The seasonal evolution of melt ponds has been well documented on multiyear and landfast first‐year sea ice, but is critically lacking on drifting, first‐year sea ice, which is becoming increasingly prevalent in the Arctic. Using 1 m resolution panchromatic satellite imagery paired with airborne and in situ data, we evaluated melt pond evolution for an entire melt season on drifting first‐year and multiyear sea ice near the 2011 Applied Physics Laboratory Ice Station (APLIS) site in the Beaufort and Chukchi seas. A new algorithm was developed to classify the imagery into sea ice, thin ice, melt pond, and open water classes on two contrasting ice types: first‐year and multiyear sea ice. Surprisingly, melt ponds formed ∼3 weeks earlier on multiyear ice. Both ice types had comparable mean snow depths, but multiyear ice had 0–5 cm deep snow covering ∼37% of its surveyed area, which may have facilitated earlier melt due to its low surface albedo compared to thicker snow. Maximum pond fractions were 53 ± 3% and 38 ± 3% on first‐year and multiyear ice, respectively. APLIS pond fractions were compared with those from the Surface Heat Budget of the Arctic Ocean (SHEBA) field campaign. APLIS exhibited earlier melt and double the maximum pond fraction, which was in part due to the greater presence of thin snow and first‐year ice at APLIS. These results reveal considerable differences in pond formation between ice types, and underscore the importance of snow depth distributions in the timing and progression of melt pond formation.</jats:p> Seasonal evolution of melt ponds on Arctic sea ice Journal of Geophysical Research: Oceans
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title Seasonal evolution of melt ponds on Arctic sea ice
title_unstemmed Seasonal evolution of melt ponds on Arctic sea ice
title_full Seasonal evolution of melt ponds on Arctic sea ice
title_fullStr Seasonal evolution of melt ponds on Arctic sea ice
title_full_unstemmed Seasonal evolution of melt ponds on Arctic sea ice
title_short Seasonal evolution of melt ponds on Arctic sea ice
title_sort seasonal evolution of melt ponds on arctic sea ice
topic Earth and Planetary Sciences (miscellaneous)
Space and Planetary Science
Geochemistry and Petrology
Geophysics
Oceanography
url http://dx.doi.org/10.1002/2015jc011030
publishDate 2015
physical 5968-5982
description <jats:title>Abstract</jats:title><jats:p>The seasonal evolution of melt ponds has been well documented on multiyear and landfast first‐year sea ice, but is critically lacking on drifting, first‐year sea ice, which is becoming increasingly prevalent in the Arctic. Using 1 m resolution panchromatic satellite imagery paired with airborne and in situ data, we evaluated melt pond evolution for an entire melt season on drifting first‐year and multiyear sea ice near the 2011 Applied Physics Laboratory Ice Station (APLIS) site in the Beaufort and Chukchi seas. A new algorithm was developed to classify the imagery into sea ice, thin ice, melt pond, and open water classes on two contrasting ice types: first‐year and multiyear sea ice. Surprisingly, melt ponds formed ∼3 weeks earlier on multiyear ice. Both ice types had comparable mean snow depths, but multiyear ice had 0–5 cm deep snow covering ∼37% of its surveyed area, which may have facilitated earlier melt due to its low surface albedo compared to thicker snow. Maximum pond fractions were 53 ± 3% and 38 ± 3% on first‐year and multiyear ice, respectively. APLIS pond fractions were compared with those from the Surface Heat Budget of the Arctic Ocean (SHEBA) field campaign. APLIS exhibited earlier melt and double the maximum pond fraction, which was in part due to the greater presence of thin snow and first‐year ice at APLIS. These results reveal considerable differences in pond formation between ice types, and underscore the importance of snow depth distributions in the timing and progression of melt pond formation.</jats:p>
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author Webster, Melinda A., Rigor, Ignatius G., Perovich, Donald K., Richter‐Menge, Jacqueline A., Polashenski, Christopher M., Light, Bonnie
author_facet Webster, Melinda A., Rigor, Ignatius G., Perovich, Donald K., Richter‐Menge, Jacqueline A., Polashenski, Christopher M., Light, Bonnie, Webster, Melinda A., Rigor, Ignatius G., Perovich, Donald K., Richter‐Menge, Jacqueline A., Polashenski, Christopher M., Light, Bonnie
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container_issue 9
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description <jats:title>Abstract</jats:title><jats:p>The seasonal evolution of melt ponds has been well documented on multiyear and landfast first‐year sea ice, but is critically lacking on drifting, first‐year sea ice, which is becoming increasingly prevalent in the Arctic. Using 1 m resolution panchromatic satellite imagery paired with airborne and in situ data, we evaluated melt pond evolution for an entire melt season on drifting first‐year and multiyear sea ice near the 2011 Applied Physics Laboratory Ice Station (APLIS) site in the Beaufort and Chukchi seas. A new algorithm was developed to classify the imagery into sea ice, thin ice, melt pond, and open water classes on two contrasting ice types: first‐year and multiyear sea ice. Surprisingly, melt ponds formed ∼3 weeks earlier on multiyear ice. Both ice types had comparable mean snow depths, but multiyear ice had 0–5 cm deep snow covering ∼37% of its surveyed area, which may have facilitated earlier melt due to its low surface albedo compared to thicker snow. Maximum pond fractions were 53 ± 3% and 38 ± 3% on first‐year and multiyear ice, respectively. APLIS pond fractions were compared with those from the Surface Heat Budget of the Arctic Ocean (SHEBA) field campaign. APLIS exhibited earlier melt and double the maximum pond fraction, which was in part due to the greater presence of thin snow and first‐year ice at APLIS. These results reveal considerable differences in pond formation between ice types, and underscore the importance of snow depth distributions in the timing and progression of melt pond formation.</jats:p>
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spelling Webster, Melinda A. Rigor, Ignatius G. Perovich, Donald K. Richter‐Menge, Jacqueline A. Polashenski, Christopher M. Light, Bonnie 2169-9275 2169-9291 American Geophysical Union (AGU) Earth and Planetary Sciences (miscellaneous) Space and Planetary Science Geochemistry and Petrology Geophysics Oceanography http://dx.doi.org/10.1002/2015jc011030 <jats:title>Abstract</jats:title><jats:p>The seasonal evolution of melt ponds has been well documented on multiyear and landfast first‐year sea ice, but is critically lacking on drifting, first‐year sea ice, which is becoming increasingly prevalent in the Arctic. Using 1 m resolution panchromatic satellite imagery paired with airborne and in situ data, we evaluated melt pond evolution for an entire melt season on drifting first‐year and multiyear sea ice near the 2011 Applied Physics Laboratory Ice Station (APLIS) site in the Beaufort and Chukchi seas. A new algorithm was developed to classify the imagery into sea ice, thin ice, melt pond, and open water classes on two contrasting ice types: first‐year and multiyear sea ice. Surprisingly, melt ponds formed ∼3 weeks earlier on multiyear ice. Both ice types had comparable mean snow depths, but multiyear ice had 0–5 cm deep snow covering ∼37% of its surveyed area, which may have facilitated earlier melt due to its low surface albedo compared to thicker snow. Maximum pond fractions were 53 ± 3% and 38 ± 3% on first‐year and multiyear ice, respectively. APLIS pond fractions were compared with those from the Surface Heat Budget of the Arctic Ocean (SHEBA) field campaign. APLIS exhibited earlier melt and double the maximum pond fraction, which was in part due to the greater presence of thin snow and first‐year ice at APLIS. These results reveal considerable differences in pond formation between ice types, and underscore the importance of snow depth distributions in the timing and progression of melt pond formation.</jats:p> Seasonal evolution of melt ponds on Arctic sea ice Journal of Geophysical Research: Oceans
spellingShingle Webster, Melinda A., Rigor, Ignatius G., Perovich, Donald K., Richter‐Menge, Jacqueline A., Polashenski, Christopher M., Light, Bonnie, Journal of Geophysical Research: Oceans, Seasonal evolution of melt ponds on Arctic sea ice, Earth and Planetary Sciences (miscellaneous), Space and Planetary Science, Geochemistry and Petrology, Geophysics, Oceanography
title Seasonal evolution of melt ponds on Arctic sea ice
title_full Seasonal evolution of melt ponds on Arctic sea ice
title_fullStr Seasonal evolution of melt ponds on Arctic sea ice
title_full_unstemmed Seasonal evolution of melt ponds on Arctic sea ice
title_short Seasonal evolution of melt ponds on Arctic sea ice
title_sort seasonal evolution of melt ponds on arctic sea ice
title_unstemmed Seasonal evolution of melt ponds on Arctic sea ice
topic Earth and Planetary Sciences (miscellaneous), Space and Planetary Science, Geochemistry and Petrology, Geophysics, Oceanography
url http://dx.doi.org/10.1002/2015jc011030