At the same time, La Niña in the eastern
Pacific Ocean transports water east to west.
Not exact matches
Cold, polar waters constantly absorb CO2, sink as it becomes more dense, and is
transported to the equatorial waters via the ThermoHaline and outgases in the warmer waters of the Indian and
Pacific Oceans.
Dan H.: «Cold, polar waters constantly absorb CO2, sink as it becomes more dense, and is
transported to the equatorial waters via the ThermoHaline and outgases in the warmer waters of the Indian and
Pacific Oceans.»
At this time the E-W sea surface temperature gradients in both the
Pacific and Indian
Oceans increased [29], [31] intensifying the E-W moisture
transport in the tropics, which greatly increased rainfall variability both on a precession and an ENSO (El Niño Southern Oscillation) time - scales.
iBomber 3 will immediately
transport you into the thick of the action with multiple missions across the
Pacific Ocean, Europe, the Mediterranean and North Africa.
Other rides
transport you in different ways: Bayside Skyride offers a scenic ride above the bay — and be sure to take the elevator up the Skytower, with its panoramic view of Mission Bay, the
Pacific Ocean, downtown San Diego, and beyond.
This Breathtaking Oceanfront Villa includes; one - way
transport from airport to villa, daily maid service, cook upon request, AC, 4 superb suites, 5 plus bathrooms,
ocean view kitchen & living room, seated dining for 12, indoor & outdoor bar, tropical gardens, private outdoor terrace & palapa BBQ area next to a truly infinite infinity pool that flows into the
Pacific.
By analogy, a warmer world wouldn't be rainier (or cloudier); it's an imperfect analogy, because rain isn't absolutely correlated with cloudiness, and lateral
transport of energy by
ocean, air, and latent heat currents in and out of the E & W Pacific Ocean areas won't scale to global wa
ocean, air, and latent heat currents in and out of the E & W
Pacific Ocean areas won't scale to global wa
Ocean areas won't scale to global warming
Consenquently, the associated SST pattern is slightly cooler in the deep convection upwelling regions of the Equitorial
Pacific and the Indian
Ocean, strongly cooler in the nearest deep convection source region of the South Atlantic near Africa and the Equator, warm over the bulk of the North Atlantic, strongly warmer where the gulf stream loses the largest portion of its heat near 50N 25W, and strongly cooler near 45N 45W, which turns out to be a back - eddy of the Gulf Stream with increased
transport of cold water from the north whenever the Gulf Stream is running quickly.
On the other hand, the budgeting of salinity implicit in the
ocean model used by Hatun et al. may not properly account for river run - off (freshens the water),
transport from the
Pacific, the Canadian Archipelago, the East Greenland current, or melting processes.
There is a tremendous amount of
ocean heat
transport from both the
Pacific and the Atlantic going on in the Arctic.
In addition to the shallow La Niña — like patterns in the
Pacific that were the previous focus, we found that the slowdown is mainly caused by heat
transported to deeper layers in the Atlantic and the Southern
oceans, initiated by a recurrent salinity anomaly in the subpolar North Atlantic.
For the scenario representative of the years 2011 — 2013, the boundary conditions include anthropogenic sources of SO2 generated from Asia that are
transported across the
Pacific Ocean, emissions from ships in shipping lanes, along with sources from other states surrounding the SoCAB.
PACific Dust EXperiment «The long range transport of dust and anthropogenic aerosols (e.g, black carbon, organics and sulfates, and air pollution from Eurasia, across the Pacific Ocean, into North America is one of the most wide spread and major pollution events on the
PACific Dust EXperiment «The long range
transport of dust and anthropogenic aerosols (e.g, black carbon, organics and sulfates, and air pollution from Eurasia, across the
Pacific Ocean, into North America is one of the most wide spread and major pollution events on the
Pacific Ocean, into North America is one of the most wide spread and major pollution events on the planet.
What follows next depends on the winds — and factoring in Ekman
transport — driving the north and south
Pacific Ocean gyres.
Trade winds
transport some of this water vapor out of the Atlantic
Ocean basin, across the Isthmus of Panama, and into the
Pacific Ocean basin.
The evolution of global mean surface temperatures, zonal means and fields of sea surface temperatures, land surface temperatures, precipitation, outgoing longwave radiation, vertically integrated diabatic heating and divergence of atmospheric energy
transports, and
ocean heat content in the
Pacific is documented using correlation and regression analysis.
That's not to mention the madness of
transporting bottled water from the middle of the
Pacific Ocean around the world.
A negative SAM spins up the South
Pacific gyre
transporting cold Southern
Ocean water north and facilitating upwelling on the Peruvian coast.
It has been noted in a five - member multi-model ensemble analysis that, associated with the changes in temperature of the upper
ocean in Figure 10.7, the tropical Pacific Ocean heat transport remains nearly constant with increasing greenhouse gases due to the compensation of the subtropical cells and the horizontal gyre variations, even as the subtropical cells change in response to changes in the trade winds (Hazeleger, 2
ocean in Figure 10.7, the tropical
Pacific Ocean heat transport remains nearly constant with increasing greenhouse gases due to the compensation of the subtropical cells and the horizontal gyre variations, even as the subtropical cells change in response to changes in the trade winds (Hazeleger, 2
Ocean heat
transport remains nearly constant with increasing greenhouse gases due to the compensation of the subtropical cells and the horizontal gyre variations, even as the subtropical cells change in response to changes in the trade winds (Hazeleger, 2005).
Observations suggest that variability in oceanographic conditions in the Arctic is very largely driven by the consequences of the flows through open passages to both Atlantic and
Pacific Oceans, which themselves respond to the different and characteristic variability of the circulation patterns of each
ocean: each inflow is not only variable in volume of water
transported but also in the temperature of the water imported.
Jan - Erik Solheima, et al., tell us — e.g., water is
transported and spread throughout the Atlantic and exported to the Indian and
Pacific oceans before updwelling in Antarctic waters.
Zhang et al. (1997) estimated that about 800 Tg yr — 1 of Asian dust emissions are injected into the atmosphere annually, about 30 % of which is re-deposited onto the deserts and 20 % is
transported over regional scales, while the remaining approximately 50 % is subject to long - range
transport to the
Pacific Ocean and beyond.
Precipitation in the Desert Southwest correlates significantly with solar irradiance lagged 3 and 5 years, which suggests a link with
ocean - water temperature anomalies
transported by the Equatorial Countercurrent as well as the North
Pacific Gyre.
While Wyoming produces the most coal in the United States, long rail
transport distances, limited
Pacific Ocean coal export capacity, and the lower energy content of subbituminous coal place some limits on utilization.
The AMF2 was deployed on a research vessel offshore and provided critical measurements to quantify the moisture budget and cloud and precipitation processes associated with ARs and to characterize aerosols and aerosol - cloud - precipitation interactions associated with aerosols from long - range
transport in the
Pacific Ocean.
«The differences between sea water temperature reported in the Log of Ship's Weather Observations and specially observed sea surface temperature were studied for 6826 pairs of observations taken in the
Pacific Ocean from 3 Military Sea
Transport Service ships and 9 U.S. Navy Radar Picket ships during 92 different trips.
For instance, if over 50 % of actual downwards heat
transport takes place in the West
Pacific / Southern Indian
Ocean (s), could differences in tropical cyclonic activity be driving the major differences in heat flow?
Whether you have a trailer that you use to
transport your boat to and from the
Pacific Ocean or one that you use to take lawn equipment to job sites, a suitable trailer insurance policy may come in handy.