Observation of Flooded Ice in Arctic Regions

The remote detection of flooding in the Arctic ice pack has been difficult to accomplish using conventional techniques. We have examined a case of Arctic flooding (8 June 1989) with NOAA and DMSP visible and infrared measurements supplemented by DMSP microwave imager (SSM/1) data. Analysis of visibl...

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Main Authors: Goroch, A. K., Fett, R. W.
Other Authors: NAVAL RESEARCH LAB MONTEREY CA
Format: Text
Language:English
Published: 1993
Subjects:
FOG
Ice
Online Access:http://www.dtic.mil/docs/citations/ADA267615
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA267615
id ftdtic:ADA267615
record_format openpolar
spelling ftdtic:ADA267615 2023-05-15T14:44:34+02:00 Observation of Flooded Ice in Arctic Regions Goroch, A. K. Fett, R. W. NAVAL RESEARCH LAB MONTEREY CA 1993 text/html http://www.dtic.mil/docs/citations/ADA267615 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA267615 en eng http://www.dtic.mil/docs/citations/ADA267615 Approved for public release; distribution is unlimited. DTIC AND NTIS Snow Ice and Permafrost Optical Detection and Detectors *FLOODING *REMOTE DETECTION *PACK ICE *ARCTIC REGIONS MEASUREMENT PREDICTIONS MODELS LAYERS RADIATIVE TRANSFER OPEN WATER CLOUD COVER MICROWAVES SURFACES CASE STUDIES FOG INFRARED MEASUREMENTS VISIBLE MEASUREMENTS MICROWAVE MEASUREMENTS Text 1993 ftdtic 2016-02-22T07:41:56Z The remote detection of flooding in the Arctic ice pack has been difficult to accomplish using conventional techniques. We have examined a case of Arctic flooding (8 June 1989) with NOAA and DMSP visible and infrared measurements supplemented by DMSP microwave imager (SSM/1) data. Analysis of visible and infrared data for a sunglint region was used to show the distribution of flooding at 72 deg N, 135 deg W. A simple model was developed for the radiative transfer at microwave wavelengths through a bring layer over ice. The predictions of the model were found to be consistent with the spatial behaviour of the SSM/I measurements. This case study demonstrates the usefulness of using combine visible, infrared, and microwave measurements to differentiate among flooded, broken ice, and open water regions, even in the presence of cloud cover or surface fog. Availability: Pub. in Int. Jnl. of Remote Sensing, v14 n7 p1305- 1324 1993. Text Arctic Ice permafrost Defense Technical Information Center: DTIC Technical Reports database Arctic
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Snow
Ice and Permafrost
Optical Detection and Detectors
*FLOODING
*REMOTE DETECTION
*PACK ICE
*ARCTIC REGIONS
MEASUREMENT
PREDICTIONS
MODELS
LAYERS
RADIATIVE TRANSFER
OPEN WATER
CLOUD COVER
MICROWAVES
SURFACES
CASE STUDIES
FOG
INFRARED MEASUREMENTS
VISIBLE MEASUREMENTS
MICROWAVE MEASUREMENTS
spellingShingle Snow
Ice and Permafrost
Optical Detection and Detectors
*FLOODING
*REMOTE DETECTION
*PACK ICE
*ARCTIC REGIONS
MEASUREMENT
PREDICTIONS
MODELS
LAYERS
RADIATIVE TRANSFER
OPEN WATER
CLOUD COVER
MICROWAVES
SURFACES
CASE STUDIES
FOG
INFRARED MEASUREMENTS
VISIBLE MEASUREMENTS
MICROWAVE MEASUREMENTS
Goroch, A. K.
Fett, R. W.
Observation of Flooded Ice in Arctic Regions
topic_facet Snow
Ice and Permafrost
Optical Detection and Detectors
*FLOODING
*REMOTE DETECTION
*PACK ICE
*ARCTIC REGIONS
MEASUREMENT
PREDICTIONS
MODELS
LAYERS
RADIATIVE TRANSFER
OPEN WATER
CLOUD COVER
MICROWAVES
SURFACES
CASE STUDIES
FOG
INFRARED MEASUREMENTS
VISIBLE MEASUREMENTS
MICROWAVE MEASUREMENTS
description The remote detection of flooding in the Arctic ice pack has been difficult to accomplish using conventional techniques. We have examined a case of Arctic flooding (8 June 1989) with NOAA and DMSP visible and infrared measurements supplemented by DMSP microwave imager (SSM/1) data. Analysis of visible and infrared data for a sunglint region was used to show the distribution of flooding at 72 deg N, 135 deg W. A simple model was developed for the radiative transfer at microwave wavelengths through a bring layer over ice. The predictions of the model were found to be consistent with the spatial behaviour of the SSM/I measurements. This case study demonstrates the usefulness of using combine visible, infrared, and microwave measurements to differentiate among flooded, broken ice, and open water regions, even in the presence of cloud cover or surface fog. Availability: Pub. in Int. Jnl. of Remote Sensing, v14 n7 p1305- 1324 1993.
author2 NAVAL RESEARCH LAB MONTEREY CA
format Text
author Goroch, A. K.
Fett, R. W.
author_facet Goroch, A. K.
Fett, R. W.
author_sort Goroch, A. K.
title Observation of Flooded Ice in Arctic Regions
title_short Observation of Flooded Ice in Arctic Regions
title_full Observation of Flooded Ice in Arctic Regions
title_fullStr Observation of Flooded Ice in Arctic Regions
title_full_unstemmed Observation of Flooded Ice in Arctic Regions
title_sort observation of flooded ice in arctic regions
publishDate 1993
url http://www.dtic.mil/docs/citations/ADA267615
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA267615
geographic Arctic
geographic_facet Arctic
genre Arctic
Ice
permafrost
genre_facet Arctic
Ice
permafrost
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/ADA267615
op_rights Approved for public release; distribution is unlimited.
_version_ 1766316069998297088