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[PDF] Top 20 Antarctic intermediate water mass formation in ocean general circulation models

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Antarctic intermediate water mass formation in ocean general circulation models

Antarctic intermediate water mass formation in ocean general circulation models

... the ocean and atmosphere. Cooling of surface water advected southward in the South Pacific gyre circulation results in a large enough buoyancy loss for convection to occur in the western South ... See full document

33

The Role of diapycnal mixing in coupled atmosphere ocean general circulation models

The Role of diapycnal mixing in coupled atmosphere ocean general circulation models

... deep water formed in the North Atlantic is called the North Atlantic Deep Water (NADW) and flows to the south as a deep western boundary return current at a depth of 2000 m and upwells in the rest of the ... See full document

153

On deep convection events and Antarctic Bottom Water formation in ocean reanalysis products

On deep convection events and Antarctic Bottom Water formation in ocean reanalysis products

... Three ocean reanalysis products were evaluated in this ...coupled ocean reanalysis is based on the Massachusetts Institute of Technology General Cir- culation Model (MITgcm) with a cube-sphere grid, ... See full document

22

Antarctic sea ice control on ocean circulation in present and glacial climates

Antarctic sea ice control on ocean circulation in present and glacial climates

... as Antarctic Bottom Water (AABW) at the bottom of the Atlantic, Indian, and Pacific Oceans (blue ...deep water; that is, into NADW in the Atlantic (green ribbon), Indian Deep Water in the ... See full document

6

Diagnosing the relation between ocean circulation, mixing and water mass transformation from an ocean hydrography and air sea fluxes

Diagnosing the relation between ocean circulation, mixing and water mass transformation from an ocean hydrography and air sea fluxes

... interior ocean mixing was performed and lead to the understanding described in Chap- ter ...many ocean models, this re- quires ...in ocean models and in the study presented in this ... See full document

163

Frontal circulation and submesoscale variability during the formation of a Southern Ocean mesoscale eddy

Frontal circulation and submesoscale variability during the formation of a Southern Ocean mesoscale eddy

... the Antarctic Circumpolar Current (ACC) and formed a cyclonic eddy ∼ 120 km in ...mode water (SAMW) ...horizontal water velocity time ...of water mass properties in the upper 200 m over ... See full document

41

Intermediate water mass production controlled by southern hemisphere winds

Intermediate water mass production controlled by southern hemisphere winds

... of intermediate water in a coarse resolution ocean general circulation model is controlled by Southern Hemisphere ...for intermediate water is ...of intermediate ... See full document

9

Deglacial intermediate water reorganization: new evidence from the Indian Ocean

Deglacial intermediate water reorganization: new evidence from the Indian Ocean

... of intermediate water masses in climate change and ocean circulation has been emphasized ...Southern Ocean Intermediate Waters (SOIW), such as Antarctic ... See full document

11

On wind-driven mid-latitude convection in ocean general circulation models

On wind-driven mid-latitude convection in ocean general circulation models

... Ocean general circulation models (OGCMs) adequately represent the formation of Subantarctic Mode Water (SAMW) and Antarctic Intermediate Water (AAIW) in the ... See full document

16

Seasonal variability of intermediate water masses in the Gulf  of Cádiz: implications of the Antarctic and subarctic seesaw

Seasonal variability of intermediate water masses in the Gulf of Cádiz: implications of the Antarctic and subarctic seesaw

... ter mass circulation generating local and smaller features but are not relevant for large regional depositional or erosional feature formation along continental slopes (Rebesco et ...regional ... See full document

17

Regional impacts of the westerly winds on Southern Ocean mode and intermediate water subduction

Regional impacts of the westerly winds on Southern Ocean mode and intermediate water subduction

... Southern Ocean transfer oxygen, heat, and anthropogenic carbon into the ocean ...Mode Water (SAMW) and Antarctic Intermediate Water (AAIW) classes, is dependent on the evolution ... See full document

10

On convection and the formation of subantarctic mode water in the Fine Resolution Antarctic Model - FRAM

On convection and the formation of subantarctic mode water in the Fine Resolution Antarctic Model - FRAM

... surface water and introduced tracer quantities. In primitive equation models, the vertical component of the advection is diagnosed from the horizontal velocity ...vertical circulation in the ... See full document

21

Excitation of equatorial Kelvin and Yanai waves by tropical cyclones in an ocean general circulation model

Excitation of equatorial Kelvin and Yanai waves by tropical cyclones in an ocean general circulation model

... equatorial ocean, and they can influence near-surface energy dissipation rates, surface heat fluxes, and temperatures in the equatorial undercurrent and at the surface (Moum et ...sub-thermocline ocean, and ... See full document

10

Impact of variable seawater conductivity on motional induction simulated with an ocean general circulation model

Impact of variable seawater conductivity on motional induction simulated with an ocean general circulation model

... Indian Ocean, Aleutian Islands, mid-Pacific Ocean and South Atlantic Ocean, only few significant changes in the depth-mean conductivity are ...surface ocean flow velocities and their large ... See full document

8

Initiation of a Marinoan Snowball Earth in a state-of-the-art atmosphere-ocean general circulation model

Initiation of a Marinoan Snowball Earth in a state-of-the-art atmosphere-ocean general circulation model

... the models’ treatment of sea- ice, oceanic, and atmospheric processes, the albedo of land, sea ice, and snow, and the continental configuration, with the latter exerting strong influence on the Snowball Earth ... See full document

15

Decadal ocean water mass changes : global observations and interpretation

Decadal ocean water mass changes : global observations and interpretation

... of ocean water property changes, with some largely qualitative discussion of possible explanations for the observed ...oxygen, circulation pathways and renewal ...various ocean parameters is ... See full document

189

Variability of Antarctic intermediate Water properties in the South Pacific Ocean

Variability of Antarctic intermediate Water properties in the South Pacific Ocean

... World Ocean Atlas should not be accepted as representative of the long term mean situ- ation north east of New ...tic Intermediate Water that reached the area was about ... See full document

15

Bathymetric control of warm ocean water access along the East Antarctic Margin

Bathymetric control of warm ocean water access along the East Antarctic Margin

... East Antarctic Ice Sheet (EAIS) ...sheet models, based on this new sub-ice topography, suggests that grounded ice in these basins could retreat and contribute signi fi cantly to future sea level rise ... See full document

14

Hydrological Structure, Circulation and Water Mass Transport in the Gulf of Cadiz

Hydrological Structure, Circulation and Water Mass Transport in the Gulf of Cadiz

... Comparing the salinity and potential temperature dis- tributions with the L_ADCP sections, westward strong velocities are associated with the undercurrents on the Iberian continental slope, as expected. At the lower MW ... See full document

25

Freshening of Antarctic Intermediate Water in the South Atlantic Ocean in 2005–2014

Freshening of Antarctic Intermediate Water in the South Atlantic Ocean in 2005–2014

... of Antarctic Intermediate Water (AAIW) is reported to have occurred in the South At- lantic Ocean during the period from 2005 to 2014, as shown by the gridded monthly means of the Array for ... See full document

10

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