Sea Ice Melt Ponds: Snow, SSL, and Pond Depths
Snow, surface scattering layer (SSL), or melt pond depths are measured by inserting a metal probe with centimeter gradations into the surface until it struck hard ice. Positive (+) measurements reflect snow or loose decaying ice crystals known as the surface scattering layer, while negative (-) meas...
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dataone:doi:10.5065/D6XW4GXP 2024-11-03T19:45:00+00:00 Sea Ice Melt Ponds: Snow, SSL, and Pond Depths Chris Polashenski Kerry Claffey Zoe Courville Chris Petrich Donald Perovich No geographic description provided. ENVELOPE(-156.54417,-156.507,71.37114,71.37078) BEGINDATE: 2008-05-28T00:00:00Z ENDDATE: 2010-06-21T00:00:00Z 2016-04-02T10:54:57.245Z https://doi.org/10.5065/D6XW4GXP unknown Arctic Data Center High Latitude Transects Arctic Ice Physics climatologyMeteorologyAtmosphere Dataset dataone:urn:node:ARCTIC https://doi.org/10.5065/D6XW4GXP 2024-11-03T19:08:09Z Snow, surface scattering layer (SSL), or melt pond depths are measured by inserting a metal probe with centimeter gradations into the surface until it struck hard ice. Positive (+) measurements reflect snow or loose decaying ice crystals known as the surface scattering layer, while negative (-) measurements indicate melt pond depths. Measurements were made every 0.5m, along the transect lines. Dataset Arctic Sea ice Arctic Data Center (via DataONE) Arctic ENVELOPE(-156.54417,-156.507,71.37114,71.37078) |
institution |
Open Polar |
collection |
Arctic Data Center (via DataONE) |
op_collection_id |
dataone:urn:node:ARCTIC |
language |
unknown |
topic |
High Latitude Transects Arctic Ice Physics climatologyMeteorologyAtmosphere |
spellingShingle |
High Latitude Transects Arctic Ice Physics climatologyMeteorologyAtmosphere Chris Polashenski Kerry Claffey Zoe Courville Chris Petrich Donald Perovich Sea Ice Melt Ponds: Snow, SSL, and Pond Depths |
topic_facet |
High Latitude Transects Arctic Ice Physics climatologyMeteorologyAtmosphere |
description |
Snow, surface scattering layer (SSL), or melt pond depths are measured by inserting a metal probe with centimeter gradations into the surface until it struck hard ice. Positive (+) measurements reflect snow or loose decaying ice crystals known as the surface scattering layer, while negative (-) measurements indicate melt pond depths. Measurements were made every 0.5m, along the transect lines. |
format |
Dataset |
author |
Chris Polashenski Kerry Claffey Zoe Courville Chris Petrich Donald Perovich |
author_facet |
Chris Polashenski Kerry Claffey Zoe Courville Chris Petrich Donald Perovich |
author_sort |
Chris Polashenski |
title |
Sea Ice Melt Ponds: Snow, SSL, and Pond Depths |
title_short |
Sea Ice Melt Ponds: Snow, SSL, and Pond Depths |
title_full |
Sea Ice Melt Ponds: Snow, SSL, and Pond Depths |
title_fullStr |
Sea Ice Melt Ponds: Snow, SSL, and Pond Depths |
title_full_unstemmed |
Sea Ice Melt Ponds: Snow, SSL, and Pond Depths |
title_sort |
sea ice melt ponds: snow, ssl, and pond depths |
publisher |
Arctic Data Center |
publishDate |
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url |
https://doi.org/10.5065/D6XW4GXP |
op_coverage |
No geographic description provided. ENVELOPE(-156.54417,-156.507,71.37114,71.37078) BEGINDATE: 2008-05-28T00:00:00Z ENDDATE: 2010-06-21T00:00:00Z |
long_lat |
ENVELOPE(-156.54417,-156.507,71.37114,71.37078) |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic Sea ice |
genre_facet |
Arctic Sea ice |
op_doi |
https://doi.org/10.5065/D6XW4GXP |
_version_ |
1814733476733124608 |