Sentences with phrase «ocean boundary current»

Eventually they flow into the Agulhas Current, the Indian Ocean boundary current that flows around southern Africa.

This is the highest volumetric inflow to the Arctic Ocean, equalling about 10 times that of the Pacific inflow, and it creates the Arctic Ocean Boundary Current.

Not exact matches

Earth System Threshold Measure Boundary Current Level Preindustrial Climate Change CO2 Concentration 350 ppm 387 ppm 280 ppm Biodiversity Loss Extinction Rate 10 pm > 100 pm * 0.1 - one pm Nitrogen Cycle N2 Tonnage 35 mmt ** 121 mmt 0 Phosphorous Cycle Level in Ocean 11 mmt 8.5 - 9.5 mmt — 1 mmt Ozone Layer O3 Concentration 276 DU # 283 DU 290 DU Ocean Acidification Aragonite ^ ^ Levels 2.75 2.90 3.44 Freshwater Usage Consumption 4,000 km3 ^ 2,600 km3 415 km3 Land Use Change Cropland Conversion 15 km3 11.7 km3 Low Aerosols Soot Concentration TBD TBD TBD Chemical Pollution TBD TBD TBD TBD * pm = per million ** mmt = millions of metric tons #DU = dobson unit ^ km3 = cubic kilometers ^ ^ Aragonite is a form of calcium carbonate.

MHW intensity between 1982 — 1998 and 2000 — 2016 increased in over 65 % of the global ocean, most notably in all five western boundary current regions, where the mean warming has been considerably faster than the global average39, and most mid-latitude ocean basins (Fig. 1e).

Hotspots of high intensity occurred in regions of large SST variability including the five western boundary current extension regions (+2 — 5 °C), the central and eastern equatorial Pacific Ocean (+1 — 4 °C) and eastern boundary current regions (+1 — 3 °C).

As may be expected from the positions of ocean currents, most mixing in the upper layers of the ocean takes place on the western boundaries of ocean gyres where the current speeds are greatest.

Coastal and boundary current systems with a focus on processes that link the nearshore and continental shelf to the open ocean, such as along - and across - shore transport processes, stirring and mixing of water masses, and the coastal response to larger - scale forcing events; long - duration, high - resolution observations using autonomous underwater gliders.

Ocean currents that may carry large amounts of heat are not calculated into the GCM, and thus we do not have a good estimate of the rate of energy transfer at the boundaries of specific sea - floor methane systems.

The oceans are a difficult part of the system for a number of reasons (mainly that the scale at which important things happen (bottom currents, eddies, western boundary currents) is quite small relative to similar processes in the atmosphere.

Because of the Earth's rotation, the poleward flow in the western Atlantic is constrained to a narrow current on the western boundary of the ocean basin.

While western boundary currents exist in all the major ocean basins, the two in the Northern Hemisphere (including the Kuroshio Current in the Pacific) are better developed and more intense than their Southern Hemisphere counterparts.»

Cronin, M. F., N. Bond, J. Booth, H. Ichikawa, T. M. Joyce, K. Kelly, M. Kubota, B. Qiu, C. Reason, M. Rouault, C. Sabine, T. Saino, J. Small, T. Suga, L. D. Talley, L. Thompson, and R. A. Weller, 2010: Monitoring ocean - atmosphere interactions in western boundary current extensions.

Kathryn A.Kelly at U. Wash has done a lot of great work on ocean - heat flux from western boundary currents in relation to the winds related to AO.

The US CLIVAR Western Boundary Current Working Group was charged with identifying shortcomings in the atmosphere, ocean, and coupled models that need to be addressed to accurately model western boundary current atmosphere - ocean inteBoundary Current Working Group was charged with identifying shortcomings in the atmosphere, ocean, and coupled models that need to be addressed to accurately model western boundary current atmosphere - ocean interCurrent Working Group was charged with identifying shortcomings in the atmosphere, ocean, and coupled models that need to be addressed to accurately model western boundary current atmosphere - ocean inteboundary current atmosphere - ocean intercurrent atmosphere - ocean interaction.

Note that there is also poleward transport in the shallow currents at the western edge of each subtropical ocean gyre - known as western boundary currents.

They are largest in regions of high sea surface temperature variability such as the western boundary currents and along the northern boundary of the Southern Ocean.

The two gyres share the eastward extension of western boundary currents, such as the Gulf Stream or Kuroshio, and are induced by the shear in the winds that cross the respective ocean basins.

Tidal variability in more complex regional models that include sea ice, ice shelves, and ocean currents that vary with depth, is obtained by using global models to set tides at the regional model's open boundaries.

The thing is, Lindzen was right and Nye was wrong - nothing short of freezing the ocean or boiling it off, or stopping the rotation of the earth, will literally stop the western boundary currents.

Consequently, surface ocean currents are stronger, narrower, and deeper in all western boundary regions.

For example, the Agulhas Current, the Indian Ocean's western boundary current, is a source ofCurrent, the Indian Ocean's western boundary current, is a source ofcurrent, is a source of rings.

These currents are weaker than those in the northern ocean basins, in part because western boundary currents require extended land barriers that are generally absent in the Southern Hemisphere.

Boundaries between water masses define major thermohaline fronts, which are generally synonymous with ocean currents.

Gyre - Basin - scale ocean horizontal circulation pattern with slow flow circulating around the ocean basin, closed by a strong and narrow (100 - 200 km wide) boundary current on the western side.

Recent studies have shown that western boundary currents have shifted position slightly over the course decades, leading to changes in wind, temperature and precipitation patterns around the globe more commonly associated with El Niño and the other ocean oscillations.

The zonal integral (east to west) of wind stress curl across an ocean basin is proportional to the western boundary current transport (i.e., the transport responsible for the dominant part of the poleward heat flux by the ocean).

Surface Ocean Currents - including the coriolis effect, trade winds, boundary currents and the Ekman spiral The Global Conveyor Belt - including thermohaline circulation, the global conveyor belt, and effects of climateCurrents - including the coriolis effect, trade winds, boundary currents and the Ekman spiral The Global Conveyor Belt - including thermohaline circulation, the global conveyor belt, and effects of climatecurrents and the Ekman spiral The Global Conveyor Belt - including thermohaline circulation, the global conveyor belt, and effects of climate change.

In this paper, it is shown that coherent large - scale low - frequency variabilities in the North Atlantic Ocean — that is, the variations of thermohaline circulation, deep western boundary current, northern recirculation gyre, and Gulf Stream path — are associated with high - latitude oceanic Great Salinity Anomaly events.

Bring together the KESS, CLIMODE and other western boundary current atmosphere - ocean interaction groups for a synthesis of results

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