Sentences with phrase «equatorial east»

Of course with the extra heat teleporting into the ocean it is a bit hard to see how the equatorial East Pacific could be cooling down for decades.

The process begins when strong convective activity over equatorial East Asia and subsiding cool air off South America's west coast creates a wind pattern which pushes Pacific water westward and piles it up in the western Pacific.

159 Dirk Verschuren, Kathleen R. Laird, Brian F. Cumming, «Rainfall and drought in equatorial East Africa during the past 1,100 years,» Nature 403:410 - 414 (27 January 2000).

Not only are droughts in the Horn of Africa (and equatorial East Africa directly to the south) a typical result of La Niña episodes, strong El Niños on the other hand are correlated with high precipitation and floodings.

Furthermore, possible connections between the new transport time series of the North Brazil Undercurrent (NBUC) and the transport variability of the Equatorial Undercurrent (EUC) as well as the resulting consequences for the climate relevant surface temperatures of the equatorial East Atlantic will be analyzed.

The climate in equatorial east Africa has alternated between drier than today, and relatively wet.

The results indicate that glaciers in equatorial East Africa advanced between 24,000 and 20,000 years ago at the coldest time of the world's last ice age.

Not exact matches

Far East 42,005,000 China & Korea 42,000,000 Japan 5,000 Southeast Asia 79,180,000 Indonesia 74,200,000 Philippines 250,000 Malaya 3,300,000 Thailand 640,000 Pakistan - India 107,450,000 Pakistan 66,000,000 India 40,200,000 Burma 750,000 Ceylon 500,000 Turkish areas 64,250,000 Sinkiang 3,000,000 Afghanistan 12,000,000 Turkey 23,600,000 Soviet Union 22,000,000 Albania 700,000 Yugoslavia 1,900,000 Bulgaria 800,000 Greece 200,000 Romania 50,000 Iran 20,700,000 Arabic areas 64,200,000 Iraq 5,000,000 Arabian Peninsula 12,500,000 Syria, Lebanon, Jordan, Israel 5,000,000 Egypt 20,000,000 Libya 1,100,000 Tunisia 3,200,000 Algeria 8,000,000 Morocco 9,400,000 Africa 35,000,000 Somaliland 1,800,000 Ethiopia 3,200,000 Tanganyika 1,500,000 Sudan 7,000,000 French Equatorial Africa1, 500,000 French West Africa 6,300,000 Other African countries 13,700,000 Western countries 800,000 Total 413,585,000

The equatorial sea surface temperatures will continue to slowly increase causing the development of El Niño conditions in the east equatorial Pacific.

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The experienced striker, who now plays his club football in the Middle East, was admitted to hospital in Equatorial Guinea on Saturday night, but because the disease was diagnosed so early he was able to be released the next morning.

Winds gusting at speeds of up to 1,650 km / h blow from West to East in the equatorial atmosphere, thirteen times the strength of the most destructive hurricane force winds that form on Earth «s equator.

Record warmth was observed across much of the central and western equatorial Pacific along with sections scattered across the eastern Pacific and regions of the western Indian Ocean, particularly notable in the waters east of Madagascar.

Three of the four warmest years since 1900 have been years with El Niño — the phenomenon in which warm water from the western side of the equatorial Pacific sloshes east, increasing global temperatures.

According to a paper published this week in the biogeography journal Diversity and Distributions, the areas that underwent the greatest habitat loss were found in the centre and east of the Democratic Republic of the Congo, western Equatorial Africa and the upper Guinean forest in Liberia.

The heart borders darker equatorial terrains, and the mottled terrain to its east (right) are complex.

The El Niño Southern Oscillation is a natural fluctuation of ocean temperatures in the equatorial Pacific that can give rise to El Niño and La Niña, which drive droughts and floods from South East Asia and Australia to the Americas.

The higher sea level near the western ocean boundary creates a west - east pressure difference in the ocean, that results in the equatorial undercurrent flowing from west to east below the surface.

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A measure of the difference in sea level pressure between the western (e.g., Darwin, Australia) and central / eastern (e.g., Tahiti) equatorial Pacific, representative of the east - west changes in atmospheric circulation associated with the El Nino / Southern Oscillation phenomenon.

Paleo - proxy reconstructions indicate that a lower insolation due to volcanic aerosols (or else) leads to a lower east - west SST gradient / a higher eastern equatorial SST / a higher El Nino variability?

The team measured trace elements and stable isotopes in stalagmites from the Indonesian island of Flores and used them to reconstruct ancient rainfall, comparing them to records from East Asia and the central - eastern equatorial Pacific.

Location of the stations used for the Southern Oscillation Index (Tahiti and Darwin, black dots), the Equatorial Southern Oscillation Index (eastern equatorial Pacific and Indonesia regions, outlined in blue), and the Niño3.4 region in the east - central tropical Pacific Ocean for sea surface temperature (red dasEquatorial Southern Oscillation Index (eastern equatorial Pacific and Indonesia regions, outlined in blue), and the Niño3.4 region in the east - central tropical Pacific Ocean for sea surface temperature (red dasequatorial Pacific and Indonesia regions, outlined in blue), and the Niño3.4 region in the east - central tropical Pacific Ocean for sea surface temperature (red dashed line).

Along the east coast, the warm Agulhas Current brings nutrient - poor, tropical waters southward from the equatorial Indian Ocean.

Only looking at the Niño 3.4 index hides the fact that this event is more typical of La Niña Modoki, where cool SST anomalies in the central equatorial Pacific are flanked by warm anomalies to the east and west.

Equatorial Kelvin waves propagate to the east in the Northern and Southern hemispheres, using the equator as a guide.

The East Australian Current (EAC) is the southward western boundary current that is formed from the South Equatorial Current (SEC) crossing the Coral Sea and reaching the eastern coast of Australia.

The raging El Niño Southern Oscillation, a band of warm ocean water in the central and east - central equatorial Pacific, is about to cause droughts in southern Asia — and to bring enough rain to boost California almond production after years of drought - induced decline.

X Anomaly says: «And for those interested, the -2 sub surface temperature anomalies in the east central equatorial pacific have expanded and risen towards the surface by around 60 meters in the last month.»

And for those interested, the -2 sub surface temperature anomalies in the east central equatorial pacific have expanded and risen towards the surface by around 60 meters in the last month.

Maybe an East - West temperature oscillation is a natural feature of any body of water with enough East - West equatorial size for it, and it just happens that under the current continental configuration only the Pacific is large enough.

The average annual SST difference between the east and west equatorial Pacific is about 4.5 deg C. Refer to the graph I prepared for an upcoming post.

What Willis has described in terms of the interaction of the trades blowing equatorial Pacific water westward, cloud cover and upwelling in the east Pacific is a concise description of the Bjerknes feedback, described here.

During an El Niño, Australia, Indonesia, the Philippines, South Africa and Northeast Brazil tend to experience drought while Southern California, the southern US East equatorial Africa, western South America and Southeastern South America tend to see flooding, McPhaden tells Carbon Brief.

When enough warm water has piled up gravity flow begins east along that equatorial counter-current.

They include alternating «pulses» of warm and cool waters that travel across the equatorial Pacific (from west to east) called Kelvin waves.

In the North Atlantic and the North Pacific heat transport is regulated by conflict of warm and cold currents: North Atlantic Drift and East Greenland Currents (NA) as drivers of the AMO, Kuroshio and Oyashio Currents (NP) driving the PDO, while in Central Pacific the South Equatorial Current is the key oscillator, the source of the ENSO.

The Pacific regimes are caused by changes in upwelling in the north - east and equatorial Pacific over 20 to 30 year regimes.

Tropical winds blow from east to west and in the North Atlantic create the flow labeled «North Equatorial».

Higher SSH in the west, manifested as a deeper thermocline and subsurface warming, contributed to an intensified west - east pressure gradient that drives the equatorial undercurrent (EUC).

In the Equatorial Pacific, we normally have equatorial upwelling in the east and downwelling in the west, aka the Western Pacific Equatorial Pacific, we normally have equatorial upwelling in the east and downwelling in the west, aka the Western Pacific equatorial upwelling in the east and downwelling in the west, aka the Western Pacific Warm Pool.

It is driven by changes equatorial trade winds, which are normally weakest in the spring and change direction when warmer SSTs starts moving east.

However, a contradictory theory postulates sustained La Niña conditions due to stronger warming of the West Equatorial Pacific than the East, causing enhanced easterly winds and reinforcing the up - welling of cold water in the EEP (56).

La Niña is the periodic cooling of ocean waters in the east - central equatorial Pacific, which can impact the typical alignment of weather patterns around the globe.

It also brought drought to east Africa, the central equatorial Pacific area and the American south, as well as flooding in southern Africa, Asia and eastern Australia.