Beaufort Sea environmental data: U.S.C.G.C. Northwind 1968
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Beaufort Sea environmental data: U.S.C.G.C. Northwind 1968 U.S.C.G.C. Staten Island 1968 and 1969. by University of Alaska (College). Institute of Marine Science.

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Published in College .
Written in English

Subjects:

Places:

  • Beaufort Sea.

Subjects:

  • Oceanography -- Beaufort Sea.

Book details:

Edition Notes

StatementReport compiled by D. C. Burrell [and others]
SeriesUniversity of Alaska. Institute of Marine Science. Report R70-20
ContributionsBurrell, David C., comp.
Classifications
LC ClassificationsGC1 .A497 R70-20, GC411 .A497 R70-20
The Physical Object
Pagination274 p.
Number of Pages274
ID Numbers
Open LibraryOL5741188M
LC Control Number70635729

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[63] As in the central Beaufort Sea, the small eddies detected near the Northwind Ridge are associated with a lack of internal waves (Figures 21 and 22). Although the rotation rates (and relative vorticities) of these eddies are comparable to their larger Beaufort Sea cousins (Halle and Pinkel, manuscript in preparation, ), they are Cited by: elsewhere in the Beaufort Sea during this cruise (Frame, ). In 24 days as the icebreaker passed through statute miles of ice-covered seas, I recorded 13 polar bears (Table 1 and Fig. 1). One was sighted in the Chukchi Sea, about miles west of Point Barrow. The other 12 bears occurred at six different locations in the Beaufort Sea. Here, we use (a) legacy seismic data that constrain upper slope gas hydrate distributions on the U.S. Beaufort Sea margin, (b) Alaskan North Slope borehole data and offshore thermal gradients. USCGC Northwind, July–August ; USCGC Staten Island, July–August , pp. College, Alaska: University of Alaska Institute of Marine Science (Data Rep. Inst. mar. Sci. Univ. Alaska No. R) Google Scholar.

Characteristics of wateborne industrial noise, Pp. in Behavior, disturbance responses and distribution of bowhead whales Balaena mysticetus in the eastern Beaufort Sea, , W.J. Richardson, editor., ed. LGL Ecological Research Associates, Inc. pp. This study addresses an important knowledge gap in the distribution of lead (Pb) in the Arctic Ocean, by presenting dissolved Pb concentrations from samples collected during the GEOTRACES Canadian cruise in Dissolved Pb showed an increase in concentration from the Canada Basin toward Baffin Bay and the Labrador Sea. Canada Basin was the most isolated region from anthropogenic Pb inputs. Ahlnäs, K. and G. Wendler Sea ice conditions in the Chukchi, Beaufort, East Siberian and Northern Bering seas during March , , and as seen from the NOAA 2, 3 and 4 satellites, Proceedings of Third International Conference on Port and Ocean Engineering under Arctic Conditions (POAC ), Fairbanks, Alaska, August ,   mnxinE mKROpflLEonroLOcv ELSEVIER Marine Micropaleontology 26 () Biostratisraphic and paleoclimatic significance of a iiSQilAMEr '94 new Pliocene foraminiferal fauna from the central Arctic Ocean Michael W. Müllen a, David H. McNeilb "U.S. Geological Survey, Middlefield Road, Menio Park California, , USA ^'Institute (if Sedimentary and Petroleum Geology, .

'This book is an accessible and thorough analysis of the current state of play in the Central Arctic Ocean and its five bordering coastal states, an area where the combination of melting sea-ice and the growing demand for oil and gas has increased international interest in resource exploration, shipping rights and environmental protection. The stations labeled by station numbers, i.e., St. (East Siberian Sea shelf slope), St. (western Chukchi Sea shelf slope), St. (Chukchi Plateau), St. (eastern Chukchi Sea shelf. Audio Books & Poetry Community Audio Computers, Technology and Science Music, Arts & Culture News & Public Affairs Non-English Audio Spirituality & Religion. Librivox Free Audiobook. Skye Talks Jignesh Arthur Better Health, Best In Health Care Pots And Pans Productions Jack Gadd All In Pod.   A similar assemblage was found in sea-ice sediments sampled from an ice floe in the Beaufort Sea (Reimnitz et al., ). As shown by Reimnitz et al., , Reimnitz et al., , the inner and middle shelf (10 to 30–40 m water depth) is the main area where benthic organisms can be easily entrained into ice, mainly through the mechanism of.