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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1973
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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 |