Zobrazeno 1 - 10
of 48
pro vyhledávání: '"Wilton Sturges"'
Autor:
Wilton Sturges
Publikováno v:
Journal of Physical Oceanography. 50:1983-1988
Ship-drift data in the Gulf of Mexico have led to a perplexing result, that the near-surface flow in the west has a north–south mean, of the east–west flow, ~5–10 cm s−1 into a closed basin. Ship-drift data have been used in the past hundred
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0af68b4424780b6a4220e3391b9d79bb
https://doi.org/10.1175/jpo-d-19-0260.1
https://doi.org/10.1175/jpo-d-19-0260.1
Autor:
Wilton Sturges
Publikováno v:
Journal of Physical Oceanography.
A previous study of currents in the Gulf of Mexico by the author used long-term means from three independent data sources. Ship-drift results are in good agreement with surface drifters, but these two do not agree with satellite sea-surface heights (
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1ddf773613a993bfae3cce34b0cb550f
https://doi.org/10.1175/jpo-d-20-0232.1
https://doi.org/10.1175/jpo-d-20-0232.1
Autor:
Wilton Sturges
Publikováno v:
Journal of Physical Oceanography. 46:2915-2924
Previous studies have found a puzzling disagreement between two large datasets and the results of numerical models in the central Gulf of Mexico. The observations suggest an upper-layer mean flow to the west of order 10 cm s−1, while the numerical
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2367d53703ffa13e441df02d7c7f2c70
https://doi.org/10.1175/jpo-d-16-0062.1
https://doi.org/10.1175/jpo-d-16-0062.1
Autor:
Alexandra Bozec, Wilton Sturges
Publikováno v:
Journal of Physical Oceanography. 43:2673-2681
Two large, independent sets of direct observations in the central Gulf of Mexico show a mean near-surface flow of ~10 cm s−1 to the west, concentrated in the northern and southern Gulf. Numerical models that the authors have examined do not produce
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0d12a7a905e93a5331fabba265854625
https://doi.org/10.1175/jpo-d-13-081.1
https://doi.org/10.1175/jpo-d-13-081.1
Publikováno v:
Journal of Physical Oceanography. 40:900-913
The Loop Current in the Gulf of Mexico sheds large anticyclonic rings on an irregular basis. The authors attempt to show what actually triggers the ring separations. Pulses of increased transport through the Florida Straits, as observed by the cable
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::eff921de0a8b78dfa012d639f492378a
https://doi.org/10.1175/2009jpo4245.1
https://doi.org/10.1175/2009jpo4245.1
Autor:
Wilton Sturges, Kern E. Kenyon
Publikováno v:
Journal of Physical Oceanography. 38:1501-1514
Several independent data sources suggest that there is a net upper-layer mass flux O(3 Sv) (Sv ≡ 106 m3 s−1) to the west in the central Gulf of Mexico, even though the western gulf is a closed basin. A plausible explanation is that this net flux
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7b679a92fbf25692321483dd88eff974
https://doi.org/10.1175/2007jpo3802.1
https://doi.org/10.1175/2007jpo3802.1
Autor:
Christopher J. DeHaan, Wilton Sturges
Publikováno v:
Journal of Physical Oceanography. 35:1801-1812
The anticyclonic Loop Current dominates the upper-layer flow in the eastern Gulf of Mexico, with a weaker mean anticyclonic pattern in the western gulf. There are reasons, however, to suspect that the deep mean flow should actually be cyclonic. Topog
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2cba1bafef1551c6007c6f57596a193f
https://doi.org/10.1175/jpo2790.1
https://doi.org/10.1175/jpo2790.1
Autor:
Wilton Sturges, B. G. Hong
Publikováno v:
Journal of Physical Oceanography. 31:1304-1312
Variability of sea level on the offshore side of the Gulf Stream has been estimated with a wind-forced numerical model. The difference in sea level between the model and coastal tide gauges therefore provides an estimate of variability of the Gulf St
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::40364403cb43d636236e3b8db84a377b
https://doi.org/10.1175/1520-0485(2001)031<1304:gstvap>2.0.co
https://doi.org/10.1175/1520-0485(2001)031<1304:gstvap>2.0.co
Publikováno v:
Journal of Physical Oceanography. 30:2088-2098
One of the puzzling features of sea level on the east coast of the United States is the decedal-scale variability; the fluctuations are 10‐15 cm, peak to peak, at periods longer than a few years. The authors find that this variability, in the frequ
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3dc62293ddd9799a05e93cfa477a4fb9
https://doi.org/10.1175/1520-0485(2000)030<2088:slotus>2.0.co
https://doi.org/10.1175/1520-0485(2000)030<2088:slotus>2.0.co
Autor:
Robert R. Leben, Wilton Sturges
Publikováno v:
Journal of Physical Oceanography. 30:1814-1819
The most energetic events in the circulation of the Gulf of Mexico are the separation of large anticyclonic rings from the Loop Current. Building on previous work, the authors examine all the apparent rings since July 1973. This new dataset includes
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d1b75d84e64539602e1c0aa6f079b2eb
https://doi.org/10.1175/1520-0485(2000)030<1814:forsft>2.0.co
https://doi.org/10.1175/1520-0485(2000)030<1814:forsft>2.0.co