Sentences with phrase «push warm surface»

The Pacific trade winds can't push the warm surface waters any farther.

[TD] La Nina: Trade winds push warm surface water to the west, which causes deeper, colder water to rise to replace it.

Stronger trade winds push warm surface water towards the west, and bring cold deeper waters to the surface to replace them.

A self sustaining upwelling in the central Pacific with twin Walker Cells pushing warm surface water both east and west.

In La Niña the Pacific trade winds intensify pushing warm surface water towards the western rim.

Not exact matches

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The opposite occurred in 1997 and 1998, when warm surface waters in the Pacific Ocean brought about by El Niño pushed rainfall systems north, leaving parts of the southern and eastern Amazon forest dry and prone to fires.

Even as the surface warms, the deeps remain cool, and this cold water will continue to periodically push the ocean out of the El Niño state.

Kevin Trenbeth, a climate scientist at the National Center for Atmospheric Research in Boulder, Colo., said the study didn't account for changes in sea surface temperatures, which are the main drivers of changes in the position of the rain belts (as is seen during an El Nino event, when Pacific warming pushes the subtropical jet over the Western U.S. southward).

An El Niño happens when warm water spreads across the surface of the Pacific, pushing rainfall to the east and causing floods in the Americas and drought in Australia.

The prevailing surface winds over the tropical Pacific blow from east - to - west (easterlies), and tend drive a surface current, pushing (advecting) the warm surface water westward.

These strong, constant winds push and drag the warm surface water westward, «piling» it up and holding it in the western Pacific Ocean basin.

They pull the surface water away from Antarctica and push the warmer water down.

Crucial to Hofmann's art and his teachings first in Germany and then in the U.S., where he settled in 1932, was his belief in relying on the overall perimeter of the painting's surface as a key compositional guide while working improvisationally and intensifying differences between warm and cool colors — known as «push and pull,» based on the colors» appearance of advancing or receding.

In Antarctica, there is only occasional surface melt in the West Antarctic ice Sheet but the warmer seas around the edges should help unstick ice that has already pushed into the oceans.

The prevailing surface winds over the tropical Pacific blow from east - to - west (easterlies), and tend drive a surface current, pushing (advecting) the warm surface water westward.

The resulting larger waves, which also seem to persist for longer because they move more slowly west to east, tend to push warm air into the Arctic (e.g., over Alaska) later and later into the year, leading to very warm conditions and the later and later freezing of the land surface and later accumulation of snow.

The study — «Possible Artifacts of Data Biases in the Recent Global Surface Warming Hiatus» — was published by Science magazine in June 2015 and pushed back against assertions from other research groups that found a pause in rising global temperatures from 1998 to 2012, which goes against climate change advocates» insistence that the earth's temperature has been on a steady incline for decades.

But the data released today confirm that human - induced global warming is pushing temperatures higher at an alarming rate: 2014 was the previous record holder for global average surface temperature, clocking in at 0.57 °C above the 1960 to 1990 average, but last year was 0.75 °C above that average.

Let's see — a negative SAM --(http://curriculum.pmartineau.webfactional.com/monitoring-southern-hemisphere-stratospheric-vortex-fluctuations-and-tropospheric-coupling/)-- pushes cold water along the Peruvian Current to the Nino1 +2 zone dissipating the warm surface mixed layer and allowing cold subsurface upwelling.

This is influenced by cold water pushing towards the equator in the Peruvian and Californian Currents respectively and displacing the warm surface layer.

Since the whole world does not appear to freeze during a ice age, the must be massive ice making going at the pole driven by heat lifting oceans of water to the sky from the equator where it is pushed by the expanding air and vapor to the poles areas where it returns to the surface and follows cold land like a culvert between warmer expanding ocean air back down to the equatoral region.

The impact of the meteorite that wiped out the dinosaurs released vast amounts of CO2 from vaporising carbonate - rich rocks, pushing atmospheric CO2 levels up to approx 2,300 ppm resulting in a climatic forcing of +12 W - m -LRB--) 2 that would have been sufficient to warm the Earth's surface by 7.5 °C, in the absence of counter forcing by sulfate aerosols.

Deep ocean currents occasionally push through the warm surface layer in the south eastern Pacific in one of the major areas for upwelling on the planet.

The overturning circulation pushes water through the Atlantic Basin, distributing heat as it moves warmer surface water from the tropics toward Greenland and the high northern latitudes and carries colder, deeper water from the North Atlantic southward.

23) A returning warm pulse will try to expand the tropical air masses as more energy is released and will try to push the air circulation systems poleward against whatever resistance is being supplied at the time by the then level of solar surface activity.

Currently, human warming by Greenhouse gasses has pushed global average surface temperatures into a range about 1 degree Celsius hotter than the 1880s.

In their Geophysical Research Letters publication the researchers also write that «aerosol invigoration effect occurs mainly in warmed - based convection with weak shear «-- as they could not find similar effects in frontal convection weather systems, which have higher wind shear and where air is forced up not by land surface warming, but by a pushing cold air wedge.

It is not that heat enters the oceans which could reduce an increase in GMST, it is that colder deeper water must rise to the surface if warmer surface waters are being pushed downwards.

This is the power stroke of the pump, when the trade winds strip the warm surface waters off and push them westwards.

Soon the eastern trade winds start pushing the warm tropical surface waters and their associated thunderstorms and clouds to the west across the Pacific and eventually poleward again.

This spins up sub-polar gyres pushing cold water into the Californian and Peruvian Currents — diluting warm surface water and biasing the system to more upwelling.

We have got stuck in the ice, because the ocean warm water sunk to the bottom, pushing the cold ice forming water to the surface??

And this, at least in certain areas, has pushed cold surface waters away from the continent, allowing slightly warmer water to rise to the surface and melt ice shelves, Rignot said.

Basically I see this as the result of convection (from the DSR warmed water below) which increases the temperature up to the last mm or so and then the cooling above that is as a result of energy loss at the surface and additional energy loss from evaporation which pushes the temperature down.

The upward motion comes from air rising over mountains, warm air riding over cooler air (warm front), colder air pushing under warmer air (cold front), convection from local heating of the surface, and other weather and cloud systems.

Warm water ceases to surge into the eastern Pacific from the west (it was «piled» by past easterly winds) since there is no longer a surface wind to push it into the area of the west pacific.

Or it might push the surface of the Earth down so much that it reaches warmer elevations where it is more likely to melt.

A returning warm pulse will try to expand the tropical air masses as more energy is released and will try to push the air circulation systems poleward against whatever resistance is being supplied at the time by the then level of solar surface turbulence.

Converging winds at the surface are colliding and pushing warm, moist air upward.

``... cold water does rise up from the depths in certain wind conditions, which push aside and cool warmer water on the surface.