Zobrazeno 1 - 10
of 52
pro vyhledávání: '"Ronald K. Reed"'
Autor:
Ronald K. Reed
Publikováno v:
Continental Shelf Research. 23:1255-1263
The eastern Bering Sea shelf is a vast area with weak net circulation. As a result, heat exchange with the atmosphere mainly accounts for changes in heat content of the water column. This region also has marked changes in atmospheric and water proper
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9a5c267d714b1786216e15b4fdaab629
https://doi.org/10.1016/s0278-4343(03)00128-6
https://doi.org/10.1016/s0278-4343(03)00128-6
Publikováno v:
Deep Sea Research Part II: Topical Studies in Oceanography. 49:5919-5930
We examined inflow through Unimak Pass (
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::54acec08011446344ed6c28b940fcc5e
https://doi.org/10.1016/s0967-0645(02)00326-0
https://doi.org/10.1016/s0967-0645(02)00326-0
Autor:
Ronald K. Reed, Phyllis J. Stabeno
Publikováno v:
Deep Sea Research Part II: Topical Studies in Oceanography. 49:5911-5917
Observations from a surface mooring, in a weak-flow regime over the southeastern Bering Sea shelf, were used to derive surface heat fluxes for the period May–July 1996. Changes in heat content of the water column also were determined from subsurfac
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1b33a301bfcfba6b8dd18aa7075ef02d
https://doi.org/10.1016/s0967-0645(02)00325-9
https://doi.org/10.1016/s0967-0645(02)00325-9
Autor:
Calvin W. Mordy, Ronald K. Reed
Publikováno v:
Journal of Marine Research. 57:763-773
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1212ec19e4e070f9cfac0b6c9327f24f
https://doi.org/10.1357/002224099321560564
https://doi.org/10.1357/002224099321560564
Autor:
Phyllis J. Stabeno, Ronald K. Reed
Publikováno v:
Journal of Oceanography. 55:79-85
We examine results from a cruise in May 1997. CTD casts to near the bottom were made south of the Aleutian Islands, across Amchitka Pass, and north of the islands. We computed a westward geostrophic speed of 123 cm s−1 at 173.5°W in the Alaskan St
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::22b1953f31a9de0b7360fa8b02b6f36e
https://doi.org/10.1023/a:1007813206897
https://doi.org/10.1023/a:1007813206897
Autor:
Ronald K. Reed
Publikováno v:
Continental Shelf Research. 18:99-103
Data from 16 CTD sections during spring 1979–1981 were used to derive mean geopotential topography and geostrophic flow (and its variability). Inshore of 100 m, there was a weak (∼1.5 cm s -1 ) but quite stable southeastward flow, with a horizont
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::94501e1bf9aab35d0652903ddbb46e2e
https://doi.org/10.1016/s0278-4343(97)00069-1
https://doi.org/10.1016/s0278-4343(97)00069-1
Autor:
Ronald K. Reed, Phyllis J. Stabeno
Publikováno v:
Journal of Marine Research. 55:565-575
In summer 1995, the Alaskan Stream at 173.5W was very intense; the peak geostrophic speed was ∼ 125 cm s -1 , and the computed volume transport above 1000 db, referred to 1000 db, was 9 × 10 6 m 3 s -1 . Flow north of the central Aleutians was sha
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::87338d59cc103a4763483c06662d0f3b
https://doi.org/10.1357/0022240973224328
https://doi.org/10.1357/0022240973224328
Autor:
Ronald K. Reed, Phyllis J. Stabeno
Publikováno v:
Continental Shelf Research. 16:1297-1305
We derive climatological mean summer circulation over the eastern Bering Sea shelf. Geostrophic flow (from CTD data, 1975–1989) and drifter velocities (from satellite-tracked buoys, 1986–1994) were used. The following features are shown: (1) in d
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::93b124509f29d946317a8702c2395e4f
https://doi.org/10.1016/0278-4343(95)00067-4
https://doi.org/10.1016/0278-4343(95)00067-4
Autor:
Ronald K. Reed
Publikováno v:
Fisheries Oceanography. 4:317-323
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e132d47337515db111e3aad4b98eefa5
https://doi.org/10.1111/j.1365-2419.1995.tb00076.x
https://doi.org/10.1111/j.1365-2419.1995.tb00076.x
Autor:
Ronald K. Reed
Publikováno v:
Journal of Oceanography. 51:489-498
Various data sets in the deep Bering Sea are examined in an effort to find suitable reference levels for geostrophic transport computations. Because of the lack of other data, classical methods are used: mainly vertical structure of differences in ge
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4e2211f281f63e4a4f5663aff9c1acda
https://doi.org/10.1007/bf02286394
https://doi.org/10.1007/bf02286394