Sea, ice and surface water circulation, Alaskan continental shelf

The author has identified the following significant results. Salinity and temperature measurements in the Bering Sea indicate that the Yukon River outflow extends as far as 200 km from its mouth. The fresh water flow from the Yukon River flows north and east into Norton Sound. Various levels of susp...

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Bibliographic Details
Main Authors: Wright, F. F., Burns, J. J., Sharma, G. D.
Format: Other/Unknown Material
Language:unknown
Published: 1973
Subjects:
Online Access:http://hdl.handle.net/2060/19730023494
id ftnasantrs:oai:casi.ntrs.nasa.gov:19730023494
record_format openpolar
spelling ftnasantrs:oai:casi.ntrs.nasa.gov:19730023494 2023-05-15T15:43:33+02:00 Sea, ice and surface water circulation, Alaskan continental shelf Wright, F. F. Burns, J. J. Sharma, G. D. Unclassified, Unlimited, Publicly available Sep 30, 1973 application/pdf http://hdl.handle.net/2060/19730023494 unknown Document ID: 19730023494 Accession ID: 73N32226 http://hdl.handle.net/2060/19730023494 No Copyright CASI GEOPHYSICS E73-11050 NASA-CR-133871 BMPR-7 1973 ftnasantrs 2019-07-21T11:28:04Z The author has identified the following significant results. Salinity and temperature measurements in the Bering Sea indicate that the Yukon River outflow extends as far as 200 km from its mouth. The fresh water flow from the Yukon River flows north and east into Norton Sound. Various levels of suspended sediment concentration in waters have been successfully color coded using a VP-8 color density slicing image analyzer. The 70 mm negative transparencies have provided the best fit for the ground truth observations. Other/Unknown Material Bering Sea Sea ice Yukon river Yukon NASA Technical Reports Server (NTRS) Bering Sea Norton Sound ENVELOPE(69.507,69.507,-49.202,-49.202) Yukon
institution Open Polar
collection NASA Technical Reports Server (NTRS)
op_collection_id ftnasantrs
language unknown
topic GEOPHYSICS
spellingShingle GEOPHYSICS
Wright, F. F.
Burns, J. J.
Sharma, G. D.
Sea, ice and surface water circulation, Alaskan continental shelf
topic_facet GEOPHYSICS
description The author has identified the following significant results. Salinity and temperature measurements in the Bering Sea indicate that the Yukon River outflow extends as far as 200 km from its mouth. The fresh water flow from the Yukon River flows north and east into Norton Sound. Various levels of suspended sediment concentration in waters have been successfully color coded using a VP-8 color density slicing image analyzer. The 70 mm negative transparencies have provided the best fit for the ground truth observations.
format Other/Unknown Material
author Wright, F. F.
Burns, J. J.
Sharma, G. D.
author_facet Wright, F. F.
Burns, J. J.
Sharma, G. D.
author_sort Wright, F. F.
title Sea, ice and surface water circulation, Alaskan continental shelf
title_short Sea, ice and surface water circulation, Alaskan continental shelf
title_full Sea, ice and surface water circulation, Alaskan continental shelf
title_fullStr Sea, ice and surface water circulation, Alaskan continental shelf
title_full_unstemmed Sea, ice and surface water circulation, Alaskan continental shelf
title_sort sea, ice and surface water circulation, alaskan continental shelf
publishDate 1973
url http://hdl.handle.net/2060/19730023494
op_coverage Unclassified, Unlimited, Publicly available
long_lat ENVELOPE(69.507,69.507,-49.202,-49.202)
geographic Bering Sea
Norton Sound
Yukon
geographic_facet Bering Sea
Norton Sound
Yukon
genre Bering Sea
Sea ice
Yukon river
Yukon
genre_facet Bering Sea
Sea ice
Yukon river
Yukon
op_source CASI
op_relation Document ID: 19730023494
Accession ID: 73N32226
http://hdl.handle.net/2060/19730023494
op_rights No Copyright
_version_ 1766377729469448192