Pre-ABoVE: Remotely Sensed Active Layer Thickness, Barrow, Alaska, 2006-2011

Active layer thickness (ALT) is a critical parameter for monitoring the status of permafrost that is typically measured at specific locations using probing, in situ temperature sensors, or other ground-based observations. The thickness of the active layer is the average annual thaw depth, in permafr...

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Language:unknown
Published: ORNL DAAC
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Online Access:https://search.dataone.org/view/scimeta_1266.xml
id dataone:scimeta_1266.xml
record_format openpolar
spelling dataone:scimeta_1266.xml 2023-11-08T14:14:08+01:00 Pre-ABoVE: Remotely Sensed Active Layer Thickness, Barrow, Alaska, 2006-2011 ENVELOPE(-156.89,-156.39,71.35,71.2) BEGINDATE: 2006-01-01T00:00:00Z ENDDATE: 2011-12-31T00:00:00Z 2015-01-23T00:00:00Z https://search.dataone.org/view/scimeta_1266.xml unknown ORNL DAAC ACTIVE LAYER|Advanced Land Observation Satellite (ALOS)|Interferometric Synthetic Aperture Radar (InSAR) TERRAIN ELEVATION|Advanced Land Observation Satellite (ALOS)|Interferometric Synthetic Aperture Radar (InSAR) ACTIVE LAYER Interferometric Synthetic Aperture Radar (InSAR) Advanced Land Observation Satellite (ALOS) Dataset dataone:urn:node:ORNLDAAC 2023-11-08T13:37:20Z Active layer thickness (ALT) is a critical parameter for monitoring the status of permafrost that is typically measured at specific locations using probing, in situ temperature sensors, or other ground-based observations. The thickness of the active layer is the average annual thaw depth, in permafrost areas, due to solar heating of the surface. This data set includes the mean Remotely Sensed Active Layer Thickness (ReSALT) over years 2006 to 2011 for the region near Barrow, Alaska. The data were produced by an Interferometric Synthetic Aperture Radar (InSAR) technique that measures seasonal surface subsidence and infers ALT. ReSALT estimates were validated by comparison with ground-based ALT obtained using probing and Ground Penetrating Radar at multiple sites. These results indicate remote sensing techniques based on InSAR could be an effective way to measure and monitor ALT over large areas on the Arctic coastal plain. These data provide gridded (30-m) estimates of active layer thickness (cm; ALT) and seasonal subsidence (cm), as well as calculated uncertainty in each of these parameters. This data set was developed in support of NASA's Arctic-Boreal Vulnerability Experiment (ABoVE) field campaign. The data are presented in one netCDF (*.nc) file. Dataset Active layer thickness Arctic Barrow permafrost Alaska ORNL DAAC (via DataONE) Arctic ENVELOPE(-156.89,-156.39,71.35,71.2)
institution Open Polar
collection ORNL DAAC (via DataONE)
op_collection_id dataone:urn:node:ORNLDAAC
language unknown
topic ACTIVE LAYER|Advanced Land Observation Satellite (ALOS)|Interferometric Synthetic Aperture Radar (InSAR)
TERRAIN ELEVATION|Advanced Land Observation Satellite (ALOS)|Interferometric Synthetic Aperture Radar (InSAR)
ACTIVE LAYER
Interferometric Synthetic Aperture Radar (InSAR)
Advanced Land Observation Satellite (ALOS)
spellingShingle ACTIVE LAYER|Advanced Land Observation Satellite (ALOS)|Interferometric Synthetic Aperture Radar (InSAR)
TERRAIN ELEVATION|Advanced Land Observation Satellite (ALOS)|Interferometric Synthetic Aperture Radar (InSAR)
ACTIVE LAYER
Interferometric Synthetic Aperture Radar (InSAR)
Advanced Land Observation Satellite (ALOS)
Pre-ABoVE: Remotely Sensed Active Layer Thickness, Barrow, Alaska, 2006-2011
topic_facet ACTIVE LAYER|Advanced Land Observation Satellite (ALOS)|Interferometric Synthetic Aperture Radar (InSAR)
TERRAIN ELEVATION|Advanced Land Observation Satellite (ALOS)|Interferometric Synthetic Aperture Radar (InSAR)
ACTIVE LAYER
Interferometric Synthetic Aperture Radar (InSAR)
Advanced Land Observation Satellite (ALOS)
description Active layer thickness (ALT) is a critical parameter for monitoring the status of permafrost that is typically measured at specific locations using probing, in situ temperature sensors, or other ground-based observations. The thickness of the active layer is the average annual thaw depth, in permafrost areas, due to solar heating of the surface. This data set includes the mean Remotely Sensed Active Layer Thickness (ReSALT) over years 2006 to 2011 for the region near Barrow, Alaska. The data were produced by an Interferometric Synthetic Aperture Radar (InSAR) technique that measures seasonal surface subsidence and infers ALT. ReSALT estimates were validated by comparison with ground-based ALT obtained using probing and Ground Penetrating Radar at multiple sites. These results indicate remote sensing techniques based on InSAR could be an effective way to measure and monitor ALT over large areas on the Arctic coastal plain. These data provide gridded (30-m) estimates of active layer thickness (cm; ALT) and seasonal subsidence (cm), as well as calculated uncertainty in each of these parameters. This data set was developed in support of NASA's Arctic-Boreal Vulnerability Experiment (ABoVE) field campaign. The data are presented in one netCDF (*.nc) file.
format Dataset
title Pre-ABoVE: Remotely Sensed Active Layer Thickness, Barrow, Alaska, 2006-2011
title_short Pre-ABoVE: Remotely Sensed Active Layer Thickness, Barrow, Alaska, 2006-2011
title_full Pre-ABoVE: Remotely Sensed Active Layer Thickness, Barrow, Alaska, 2006-2011
title_fullStr Pre-ABoVE: Remotely Sensed Active Layer Thickness, Barrow, Alaska, 2006-2011
title_full_unstemmed Pre-ABoVE: Remotely Sensed Active Layer Thickness, Barrow, Alaska, 2006-2011
title_sort pre-above: remotely sensed active layer thickness, barrow, alaska, 2006-2011
publisher ORNL DAAC
publishDate
url https://search.dataone.org/view/scimeta_1266.xml
op_coverage ENVELOPE(-156.89,-156.39,71.35,71.2)
BEGINDATE: 2006-01-01T00:00:00Z ENDDATE: 2011-12-31T00:00:00Z
long_lat ENVELOPE(-156.89,-156.39,71.35,71.2)
geographic Arctic
geographic_facet Arctic
genre Active layer thickness
Arctic
Barrow
permafrost
Alaska
genre_facet Active layer thickness
Arctic
Barrow
permafrost
Alaska
_version_ 1782011952341450752