Labrador Sea (French: mer du Labrador) is an arm of the North Atlantic Ocean between Labrador and Greenland. Water depths in the center of Labrador Sea are around 3.

Past sunset at Labrador Sea, off the coast of Paamiut, Greenland One of the world's largest turbidite channels runs N-S in the middle of Labrador Sea.

The Labrador Sea probably formed by sea-floor spreading that started around 61 million years ago and stopped about 40 million years ago. There is an earlier history of basin formation on all margins.

Labrador Sea (French: mer du Labrador) (60°00'N, 55°00'W) is an arm of the North Atlantic Ocean between Labrador and Greenland.

Labrador Sea changed in more recent times.

The Labrador Sea Experiment and air-sea interaction - sea ice engine During 1995-1998 I worked at the University of Toronto, Canada with Prof.

My Labrador Sea work has resulted in a series of papers on air-sea interaction during cold, atmospherically unstable conditions.

Labrador Sea Convection Experiment An experiment whose purpose is to improve the understanding of the

It underlies the Labrador Sea as well as most of the Irminger Sea.

The Labrador Sea is part of the pathway through which the low salinity outflows of the Arctic Ocean move

Back from the Labrador Sea, the team continues to work on docking.

mooring in the Labrador Sea appeared as e-mail on colleagues' computers. Satellites relayed e-mail from scientists back to the mooring.

This vertical mixing of the Labrador Sea - a critical part of the thermohaline cycle - delivers cold water to the deep ocean as part of a larger circulation process transferring heat from warm tropical

Water in the Labrador Sea are part of a continuum of overflows at different densities from the Norwegian-Greenland Sea region.

classical Labrador Sea water which persist further equatorward.

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).

Labrador Sea water (from the central Labrador Sea) but is significantly fresher and hence lighter.

Labrador Sea in 1966 by Thomas C Wolford (Paperback - Jan. 18, 2010)Buy new: $20.00 7 new from $19.771 used from $20.

Newfoundland and the Labrador Sea in 1970 by Robert Erwin Ettle (Paperback - Jan. 18, 2010)Buy new: $21.70 7 new from $21.481 used from $22.

Labrador sea located on which continent? Read answer...

The Labrador Sea is the source of the North Atlantic Deep Water, a cold, highly saline water that forms in the Labrador Sea and flows at great depth

* Labrador sea located on which continent? * How big is Labrador Sea? * Can a labrador? »

Links between Labrador Sea convection and subtropical middepth warming/cooling patterns. This volume. J Geophys. Res., 101, 8749 - 8758. Deser, C., and M.L.Blackmon. 1993.

the Labrador Sea (LS) can be well described forward in time from World War II (WWII), with a few pre - WWII observations also available.

Introduction: The warming and cooling of Labrador Sea Water in the western subpolar North Atlantic.

Labrador Sea to the east and the Gulf of St. Lawrence to the south.

Labrador Sea were captured on film by the crewmembers of the Space Shuttle Atlantis during STS-110.

Sea ice drifts in the Labrador Sea in this photograph taken from the International Space Station.

across the Northern Hemisphere to the Labrador Sea off the coast of Newfoundland, Canada. The smoke appears as gray swirls in the bottom right quadrant of the image.

Oceanography of the Labrador Sea in the vicinity of Hudson Strait in 1965 - Kollmeyer, Ronald C Includes bibliographical references Keywords: Oceanography - Labrador Sea; Oceanography -

waters from the Labrador Sea to the south begin to encroach into the Bay as spring progresses, eventually freeing the Bay of its winter ice. Sensor: Terra/MODIS. Data Start Date: 4/19/02.

the meteorological component of the Labrador Sea Ocean Convection Experiment. This experiment is aimed at observing deep ocean convection: an important component in the earth's climate system.

Labrador Sea are of particular importance because: 1.

Labrador Sea in search of the Northwest Passage, a presumed sea route between the Atlantic and Pacific oceans.

LINKS External Web Sites The topic Labrador Sea is discussed at the following external Web sites.

intermediate water, in the Labrador Sea, started at ca. 7 ka BP (Hillaire-Marcel et al.

Labrador Sea, near Orphan Knoll and on the Greenland rise, respectively, whereas core MD99-2254 (56º47,78' N, 30º39,86' W; 2240 m) was raised from the Bight Fracture zone area, east of the

Labrador Sea sites suggests a lesser variability of the North Atlantic Drift (NAD), that governs sea-surface conditions there, than of the cold East Greenland and Labrador currents, that influence

The Labrador Sea is an arm of the North Atlantic Ocean between Labrador and Greenland. Water depths in the center of Labrador Sea are around 3.

geology of the seabed in the Labrador Sea on board of the research vessel Maria S. Merian.

Labrador Sea Water (the result of convection activity) and the interior circulation (see also Project A4).

vertical velocity and temperature at 400 m in the Labrador Sea in winter 1997. (a)... (b) Color-coded by mean T of each time series, .

Labrador Sea is the most active convection region in the North Atlantic, which forms a distinctive water mass of the thermohaline system named the Labrador Sea Water

time of expected Labrador Sea Water formation by deep convection to follow the newly formed water masses.

* Labrador Sea: Definition from Answers. Labrador Sea: Definition from Answers.

Labrador Sea (French: mer du Labrador) is an arm of the North Atlantic Ocean between Labrador and Greenland.

The Labrador Sea is the source of the North Atlantic Deep Water, a cold, ...

Characteristics of the Labrador Sea water in potential temperature - salinity coordinates. Figure 2.1.

the Labrador Sea were at their warmest and saltiest since the 1930s.

Characteristics of the Labrador Sea water in potential temperature - salinity coordinates. 2. WOCE Section AR7W: the 1990s under a Magnifying Glass imageg.

* Labrador Sea Deep Convection Experiment * Characteristics of the Model Run * Convection

here between a Labrador Sea MIT general circulation model run with 14 kilometer resolution and 1) TOPEX/POSEIDON altimetry, 2) WOCE hydrography, 3) current meters, and 4) PALACE floats.

the Labrador Sea deep convection cycle? = Geoffrey Gebbie Advisor: Carl Wunsch Collaborators: Julio Sheinbaum (CICESE), Detlef Stammer (SIO)

Deep convective ventilation in the Labrador Sea is partly controlled by mechanisms other than local surface forcing and local density gradients.

for the ONR Labrador Sea Convection Experiment.

Labrador Sea Convection Experiment Page Oceanic Planetary Boundary Layer (OPBL) home page - e-mail:

in the Labrador Sea (tectonic activity) ended about 45 million years ago. The discovery of the seamount indicates that the seabed at the exit of the Labrador Sea changed in more recent times.

Labrador Sea in the Irminger Sea.

The Labrador Sea and the Mediterranean have been thought to be the only locations where open-ocean convection leads to formation of deep water in the North Atlantic to depths of 1500-2000 meters.

Central Labrador Sea during the winters of 1997 and 1998 as part of the Labrador Sea Deep Convection Experiment.

Hydrography of the Labrador Sea During Active Convection 25 JUN 2002 Authors: Robert S. Pickart; Daniel J. Torres; R.

Labrador Sea - Convection Data CD-Rom JAN 2003 10 pages Authors: Gerd Krahmann; Martin Visbeck; LAMONT-DOHERTY EARTH OBSERVATORY

Labrador Sea is the body of water between Greenland and the coast of Labrador.

the axis of the Labrador Sea, some 3800 km from the mouth of HUDSON STRAIT southward into the North Atlantic.

A water mass, the Labrador Sea water is formed in the western Labrador Sea by wintertime cooling and spreads into the northwest Atlantic at depths of 1500-2000 m.

Labrador Sea An arm of the northern Atlantic Ocean between eastern Canada and southwest Greenland.

Labrador SeaLabrador Sea - an arm of the northern Atlantic between Labrador and southern GreenlandAtlantic, Atlantic Ocean - the 2nd largest ocean; separates North and South America on the west from

northwest Labrador Sea in the summer of 2007.

Labrador Sea Deep Convection Experiment meteorology research program . Here you can find links to some plots of surface meteorology variables and descriptions of available data sets.

Labrador Sea Deep Convection Experiment: = - The 1997 and 1998 cruises of the R/V Knorr - =

Welcome to the Labrador Sea Deep Convection Experiment Knorr meteorology pages.

* Main Labrador Sea Deep Convection Experiment Home Page * Peter Guest's Home Page Acknowledgements

Guest's Labrador Sea deep convection studies and the preparation of these web sites were sponsored by the Office of Naval Research grant number N0001497WR30058.

Labrador Sea Deep Convection Experiment: = - The 1997 cruise of the R/V Knorr - =

contrasting the Labrador Sea Water temperature in its cool period before World War II (1935), the peak of warming (1971), and at its coldest point (1993).

Enlarge ImageTime series of Labrador Sea Water properties in its source region. Thickness is the vertical distance (meters) between two density surfaces that bracket the Labrador Sea Water.

Labrador Sea Water layer (blue curve) in its formation area, and temperature of the LSW core (green curve).

before the ship heads toward the Labrador Sea on Sept. 19, 2007.

We’re steaming toward Greenland, through the Labrador Sea in the North Atlantic, to deploy a mooring in a part of the ocean where something interesting happens.

Field work in support of the Labrador Sea Convection Experiment - The field work for this experiment had four components: * floats and drifter, which provide

Labrador Sea Deep Convection Experiment Data Collection = assembled by Gerd Krahmann and Martin Visbeck Lamont-Doherty Earth Observatory of Columbia

The purpose of the Labrador Sea convection experiment is, by a combination of field observations, laboratory studies, theory and modeling, to improve our understanding of the convective process and