Zobrazeno 1 - 10
of 14
pro vyhledávání: '"D A Smeed"'
Publikováno v:
Environmental Research Letters, Vol 16, Iss 8, p 084019 (2021)
Labrador Slope Water (LSLW) is a relatively fresh and cool water mass that originates from the Labrador Current in the subarctic and is known to occur in the Eastern Slope Sea on the US-Canadian shelf-slope north of the Gulf Stream. It has potential
Externí odkaz:
https://doaj.org/article/c101ab1a7aa44921927d3efa99105b1c
Publikováno v:
Ocean Science, Vol 17, Pp 1321-1340 (2021)
The large-scale system of ocean currents that transport warm waters in the upper 1000 m northward and return deeper cooler waters southward is known as the Atlantic meridional overturning circulation (AMOC). Variations in the AMOC have significant re
Externí odkaz:
https://doaj.org/article/e45019febf97496a865c6e73103d4cf9
Publikováno v:
Ocean Science, Vol 17, Pp 285-299 (2021)
A decline in Atlantic meridional overturning circulation (AMOC) strength has been observed between 2004 and 2012 by the RAPID-MOCHA-WBTS (RAPID – Meridional Overturning Circulation and Heatflux Array – Western Boundary Time Series, hereafter RAPI
Externí odkaz:
https://doaj.org/article/89464c8b989b4dc6ba32952c461587dd
Autor:
B. I. Moat, D. A. Smeed, E. Frajka-Williams, D. G. Desbruyères, C. Beaulieu, W. E. Johns, D. Rayner, A. Sanchez-Franks, M. O. Baringer, D. Volkov, L. C. Jackson, H. L. Bryden
Publikováno v:
Ocean Science, Vol 16, Pp 863-874 (2020)
The strength of the Atlantic meridional overturning circulation (AMOC) at 26∘ N has now been continuously measured by the RAPID array over the period April 2004–September 2018. This record provides unique insight into the variability of the lar
Externí odkaz:
https://doaj.org/article/3ad7930db1a94d70a77a0cd8b24bb1dc
Autor:
E. Frajka-Williams, C. S. Meinen, W. E. Johns, D. A. Smeed, A. Duchez, A. J. Lawrence, D. A. Cuthbertson, G. D. McCarthy, H. L. Bryden, M. O. Baringer, B. I. Moat, D. Rayner
Publikováno v:
Ocean Science, Vol 12, Iss 2, Pp 481-493 (2016)
From ten years of observations of the Atlantic meridional overturning circulation (MOC) at 26° N (2004–2014), we revisit the question of flow compensation between components of the circulation. Contrasting with early results from the observations,
Externí odkaz:
https://doaj.org/article/74f7a90fd70d45de9f1a09f87e99d6ce
Autor:
D. A. Smeed, G. D. McCarthy, S. A. Cunningham, E. Frajka-Williams, D. Rayner, W. E. Johns, C. S. Meinen, M. O. Baringer, B. I. Moat, A. Duchez, H. L. Bryden
Publikováno v:
Ocean Science, Vol 10, Iss 1, Pp 29-38 (2014)
The Atlantic meridional overturning circulation (AMOC) has been observed continuously at 26° N since April 2004. The AMOC and its component parts are monitored by combining a transatlantic array of moored instruments with submarine-cable-based measu
Externí odkaz:
https://doaj.org/article/3071d9db54a84a27a8bfdcafbd9cfc31
Publikováno v:
Ocean Science, Vol 6, Iss 2, Pp 573-586 (2010)
We study the variability of hydrographic preconditioning defined as the heat and salt contents in the Ligurian Sea before convection. The stratification is found to reach a maximum in the intermediate layer in December, whose causes and consequences
Externí odkaz:
https://doaj.org/article/c3ac49a9538a446696a8c579c5016f62
Autor:
D. A. Smeed, G. McCarthy, S. A. Cunningham, E. Frajka-Williams, D. Rayner, W. E. Johns, C. S. Meinen, M. O. Baringer, B. I. Moat, A. Duchez, H. L. Bryden
The Atlantic Meridional Overturning Circulation (AMOC) has been observed continuously at 26° N since April 2004. The AMOC and its component parts are monitored by combining a transatlantic array of moored instruments with submarine-cable based measu
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e7e69d2dd1a90259d9bd097585d74803
https://zenodo.org/record/29223
https://zenodo.org/record/29223
Autor:
D. A. Smeed, J. T. Allen
Publikováno v:
Journal of Physical Oceanography. 26:2611-2634
Using data from high-resolution surveys of the Iceland- Faerœs Front, the authors have calculated synoptic maps of the geostrophic velocity, vorticity, and potential vorticity on isopycnal surfaces. The data have also been used to diagnose the verti
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3f1412659e786f0bb15e9fb425c147a9
https://doi.org/10.1175/1520-0485(1996)026<2611:pvavva>2.0.co
https://doi.org/10.1175/1520-0485(1996)026<2611:pvavva>2.0.co
Autor:
A. E. Hill, I. D. James, P. F. Linden, J. P. Matthews, D. Prandle, J. H. Simpson, E. M. Gmitrowicz, D. A. Smeed, K. M. M. Lwiza, R. Durazo, A. D. Fox, D. G. Bowers
Publikováno v:
Understanding the North Sea System ISBN: 9789401045407
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::31a3edc16cd16b0a1271d9410da88405
https://doi.org/10.1007/978-94-011-1236-9_5
https://doi.org/10.1007/978-94-011-1236-9_5