Zobrazeno 1 - 10
of 18
pro vyhledávání: '"John R. N. Lazier"'
Autor:
Jonathan M. Lilly, Uwe Send, John R. N. Lazier, Eric A. D'Asaro, Peter B. Rhines, Friedrich Schott, Kara L. Lavender
Publikováno v:
Progress in Oceanography. 59:75-176
This paper is an observational study of small-scale coherent eddies in the Labrador Sea, a region of dense water formation thought to be of considerable importance to the North Atlantic overturning circulation. Numerical studies of deep convection em
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::49e4f08b3b62d277d9a0ddad9296d163
https://doi.org/10.1016/j.pocean.2003.08.013
https://doi.org/10.1016/j.pocean.2003.08.013
Publikováno v:
Deep Sea Research Part I: Oceanographic Research Papers. 49:1819-1835
Temperature, salinity and other property distributions observed across the central Labrador Sea in the early summers between 1990 and 2000 reveal a 4-year period of exceptionally intense convection followed by 5 years of restratification. The intense
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b9ca335b705c576f3ee4377ab8cf0337
https://doi.org/10.1016/s0967-0637(02)00064-x
https://doi.org/10.1016/s0967-0637(02)00064-x
Publikováno v:
Deep Sea Research Part I: Oceanographic Research Papers. 44:1025-1054
Two processes are investigated that result in the rapid (order of months) export of newly-ventilated water from the sub-polar north Atlantic. Both mechanisms involve mid-depth water mass formation within the western boundary current system, which lea
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ed22e9cb73bb7646fd256f2b614d7f2d
https://doi.org/10.1016/s0967-0637(96)00122-7
https://doi.org/10.1016/s0967-0637(96)00122-7
Autor:
Alfred Putzka, Klaus Peter Koltermann, Alexander Sy, John R. N. Lazier, Jens Meincke, Manfred Bersch, Monika Rhein
Publikováno v:
Scopus-Elsevier
Ocean temperature, salinity and chlorofluorocarbon concentration data are used to track the recent spreading of cold intermediate-depth water masses from the Labrador Sea across the northern North Atlantic Ocean. These water masses, which are formed
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::82c0a20564462c579b371c58aa1e142c
https://doi.org/10.1038/386675a0
https://doi.org/10.1038/386675a0
Publikováno v:
Journal of Geophysical Research: Oceans. 101:20711-20726
A new type of submesoscale eddy has been observed south of the Labrador Sea during late winter, embedded in equatorward flow along the western boundary. The eddy radius is 20 km, with a weak dynamic signature (swirl speed of 0.5 cm/s). The center of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::76c53aac51009dde5a7c7baa0d123942
https://doi.org/10.1029/96jc01453
https://doi.org/10.1029/96jc01453
Publikováno v:
Progress in Oceanography. 38:241-295
The North Atlantic is a peculiarly convective ocean. The convective renewal of intermediate and deep waters in the Labrador Sea and Greenland/Iceland Sea both contribute significantly to the production and export of North Atlantic Deep Water, thus he
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::be3ef39354bda8a3709a930836dd3f9c
https://doi.org/10.1016/s0079-6611(97)00002-5
https://doi.org/10.1016/s0079-6611(97)00002-5
Autor:
John R. N. Lazier
Publikováno v:
Journal of Physical Oceanography. 24:1449-1463
The North Atlantic Current, a northern branch of the Gulf Stream, flows in a northerly direction to the east of the Grand Banks of Newfoundland and turns sharply to the right north of Flemish Cap in the “Northwest Corner.” The currents and water
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::05adf5794fcb4af66389c77c708831c0
https://doi.org/10.1175/1520-0485(1994)024<1449:oitnco>2.0.co
https://doi.org/10.1175/1520-0485(1994)024<1449:oitnco>2.0.co
Autor:
John R. N. Lazier, Daniel G. Wright
Publikováno v:
Journal of Physical Oceanography. 23:659-678
Analyses of CTD and current meter data obtained between 1978 and 1988 off southern Labrador reveal two distinct regimes in the Labrador Current. The first lies over the shelf and upper slope and is the traditional Labrador Current transporting cold l
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::75371c355b02959a3e0422b9f95954cd
https://doi.org/10.1175/1520-0485(1993)023<0659:avvitl>2.0.co
https://doi.org/10.1175/1520-0485(1993)023<0659:avvitl>2.0.co
Publikováno v:
Journal of Physical Oceanography, 35 (4). pp. 489-511.
The Labrador Sea is one of the few regions of the World Ocean where deep convection takes place. Several moorings across the Labrador continental slope just north of Hamilton Bank show that convection does take place within the Labrador Current. Mixi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6ef050bc1e39b28085f7bc667e55b259
http://www.vliz.be/nl/open-marien-archief?module=ref&refid=211156
http://www.vliz.be/nl/open-marien-archief?module=ref&refid=211156
Autor:
Russ E. Davis, Ian A. Renfrew, Gerd Krahmann, Mark D. Prater, John R. N. Lazier, Eric A. D'Asaro, G. W. Kent Moore, W. Brechner Owens, Pearn P. Niiler, Jens Meincke, Peter B. Rhines, Martin Visbeck, Robert S. Pickart, William M. Smethie, Peter S. Guest, R. Allyn Clarke, Friedrich Schott
Publikováno v:
Geochemistry, Geophysics, Geosystems. 4
Between 1996 and 1998, a concerted effort was made to study the deep open ocean convection in the Labrador Sea. Both in situ observations and numerical models were employed with close collaboration between the researchers in the fields of physical oc
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e0af95d50f63394c4c9eb087b9727012
https://doi.org/10.1029/2003gc000536
https://doi.org/10.1029/2003gc000536