Sentences with phrase «where ocean cooling»

The largest effects of volcanic dimming should be evident in the tropics where ocean cooling should be taking place.

Not exact matches

The Temecula Valley Wine Country is a pristine area where the air is swept clean by cooling ocean breezes and rolling hills are covered with vineyards.

River Road Vineyard is located at the northern end of Santa Lucia Highlands classified as cold Region I, where ocean breezes create superior cool - climate Burgundian varieties Chardonnay and Pinot Noir.

Places where the Pacific was cooler than normal are blue, places where temperatures were average are white, and places where the ocean was warmer than normal are red.

But a few billion years ago a slightly fainter sun might have allowed for a relatively cool Venus, one where liquid water could have pooled in vast oceans that were friendly to life.

If the water remained in the channel, the water would eventually cool to a point where it was not melting much ice, but the channels allow the water to flow out to the open ocean and warmer water to flow in, again melting the ice shelf from beneath.

Compared to seasonal norms, the coldest place in Earth's atmosphere in May was over the northern Pacific Ocean, where temperatures were as much as 2.08 C (about 3.74 degrees Fahrenheit) cooler than seasonal norms.

«The wide swath of ocean that is cooled by hurricanes is much larger in area than the narrow swath where damage occurs on reefs,» Manzello notes.

The study, according to Valley, strengthens the theory of a «cool early Earth,» where temperatures were low enough for liquid water, oceans and a hydrosphere not long after the planet's crust congealed from a sea of molten rock.

After cooling briefly in July, ocean temperatures in the Niño 3.4 region — the area where ENSO conditions are monitored — began warming once again.

Now it's the turn of the Indian Ocean, where pollution from the subcontinent has been wafting over the Bay of Bengal, cooling the sea surface and weakening the annual monsoon.

While the stratosphere recovers from volcanic events quite quickly, the troposphere takes longer as some heat is transferred into the oceans, where cooling - down and heating back up take time.

The cool skin behaves quite differently to the water below, because it is the boundary where the ocean and air meet, and therefore turbulence (the transfer of energy / heat via large - scale motion) falls away as it approaches this boundary.

The warming of the oceans by sunlight, makes the daytime surface waters more bouyant than the cooler waters below and this leads to stratification - a situation where the warmer water floats atop cooler waters underneath, and is less inclined to mix.

It's where my dad grew up, where my grandparents live and all around a great little town filled with unique shops, beaches, a marina and a cool ocean breeze.

Aziz Ansari looked as though he stepped out of a scene from Ocean's Eleven in New York, where his shirt screamed cool and his pants screamed chill.

One of my favorite things about summer are those evenings where the heat breaks and there is a cool ocean breeze.

The mountains are my next favorite, and when it's hot and I can't make it to a lake or the ocean, then a cool mountain river is where I want to be.

Take a boat cruise down Cooper Creek looking for salt water crocodiles, birds, butterflies and lots of other interesting rainforest dwellers, take a walk on beautiful beaches where the rainforest grows to the edge of the sand, walk along trails to reach the peak so you can gaze out over the ocean and mountains beyond and then begin your journey back to Port Douglas but not before calling into Mossman Gorge to explore this new interactive Aboriginal cultural centre and maybe even have a swim in the cool river.

Mariner's Walk Villas, located in the gated community of Wild Dunes on the northeastern tip of the Isle of Palms, offers a place where guests can catch a cool breeze from a screened porch or open deck with an ocean view.

This is truly where time stands still with the sounds of the waves crashing beneath your views and the cool ocean breezes blowing through your hair.

We pride ourselves with the fact that we have the only swimming pool in town where our guests, those not brave enough to face the cold waters of the ocean, can cool down.

With 1,500 miles of coast, where both Atlantic and the Indian Ocean meet together, unbelievable miscellaneous topography from the coolest winery of the southwest to the hot Kalahari Desert in the north, from magnificent beaches to the kingdom of wilderness, South Africa now greets more than 9 million tourists every year.

Sunset Oceanfront Lodging takes you away to the beautiful coast of Oregon, where you can breathe in crisp natural air, enjoy the cool ocean breeze in... more

The abundant waters off the coast of Cabo San Lucas — located at the southern tip of the Baja Peninsula, where the calm and warm waters of the Sea of Cortez mixes with the unfathomable cool currents of the Pacific Ocean — offer the ideal conditions for plenty of sport - fish species, including (among others) Rooster Fish, Mahi Mahi (known locally as Dorado), varieties of Tuna, Sharks, Jacks, Groupers, and Billfish such as Sailfish, Swordfish, Black Marlin, Blue Marlin and Striped Marlin.

«For several years now, scientists have had evidence that dust from storms across the vast expanse of the Sahara Desert drifts out over the Atlantic where it reflects some solar radiation back into space, thus cooling the ocean waters that fuel hurricanes.

And just as increased algal productivity at sea increases the emission of sulfur gases to the atmosphere, ultimately leading to more and brighter clouds over the world's oceans, so too do CO2 - induced increases in terrestrial plant productivity lead to enhanced emissions of various sulfur gases over land, where they likewise ultimately cool the planet.

Temperature tends to respond so that, depending on optical properties, LW emission will tend to reduce the vertical differential heating by cooling warmer parts more than cooler parts (for the surface and atmosphere); also (not significant within the atmosphere and ocean in general, but significant at the interface betwen the surface and the air, and also significant (in part due to the small heat fluxes involved, viscosity in the crust and somewhat in the mantle (where there are thick boundary layers with superadiabatic lapse rates) and thermal conductivity of the core) in parts of the Earth's interior) temperature changes will cause conduction / diffusion of heat that partly balances the differential heating.

When upwelling brings cold water to the ocean's surface, cooling the atmosphere, where is that heat lost from the atmosphere «hiding»?

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.

Depending on where the powerful winds cross the Atlantic, the jet stream can have a cooling or warming effect on sea surface temperatures in the North Atlantic Ocean, according to the study, published (May 27 2015) in the journal Nature.

La Nina / PDO is a perfect example where changes in ocean currents / ocean upwelling affect heat transfer between the phases of the system (and cool the air)-- on a human time scale.

But as cogently interpreted by the physicist and climate expert Dr. Joseph Romm of the liberal Center for American Progress, «Latif has NOT predicted a cooling trend — or a «decades - long deep freeze» — but rather a short - time span where human - caused warming might be partly offset by ocean cycles, staying at current record levels, but then followed by «accelerated» warming where you catch up to the long - term human - caused trend.

It's because both land and ocean surfaces are heated by shortwave solar radiation and where aerosols reflect SWR equally well over land or water and where greenhouse gases work by retarding the rate of radiative cooling which is not equal over land and water.

I also suspect that a good portion of the additional warming shown in the hybrid version of the Cowtan and Way (2013) data (versus their Krig data) comes from the Southern Ocean surrounding Antarctica, where sea surface temperatures are cooling and lower troposphere temperatures are warming.

They still think that the Antarctic surface is warming, not cooling like you now believe because of this Hansen paper: «In contrast, the Southern Ocean (specifically the region where Antarctic sea ice forms) has been warming at 0.17 °C per decade.»

The high SSTs provide ample moisture to the atmosphere and the resulting evaporative cooling of the ocean dropped the subsequent SST values down, but meanwhile heavy rains, often record breaking in intensity, occurred nearby to where the winds carried the moisture.

However, there is also the expansion of the Hadley Cells where water vapor from tropical ocean evaporation rises, water in the form of rain falls out as the air cools with increased altitude, then dry air descends at poleward edge of the cells in the dry subtropics.

And that's where I'm heading now, to take a look at what happens in the oceans near Greenland's eastern and southwestern coastlines, the processes that make worldwide climate flip so abruptly from warm - and - wet into cool - dry - dusty - windy.

Net energy into the ocean either means somewhere else is cooling (where?)

(The Los Angeles figure is low because the weather station where it was taken is at the airport, which is cooled by the nearby ocean; temperatures downtown and in the valleys are higher.)

RE: # 423 — The only case I know of where these mild sorts of winds would have any sort of cooling effect at all would be where they are coming off of a cold ocean — and that impact would only affect the first couple of miles inland.

Where clouds are absent, darker surfaces like the ocean or vegetated land absorb heat, but where clouds occur their white tops reflect incoming sunlight away, which can cause a cooling effect on Earth's surWhere clouds are absent, darker surfaces like the ocean or vegetated land absorb heat, but where clouds occur their white tops reflect incoming sunlight away, which can cause a cooling effect on Earth's surwhere clouds occur their white tops reflect incoming sunlight away, which can cause a cooling effect on Earth's surface.

Additional cooling to that shown in runs 2 — 5 has developed almost everywhere, apart from in the ocean around Antarctica, where some areas have warmed strongly and others cooled strongly.

As part of the planet's reciprocal relationship between ocean circulation and climate, this conveyor belt transports warm surface water to high latitudes where the water warms the air, then cools, sinks, and returns towards the equator as a deep flow.»

Currents that move through the upper ocean then dive down to depth may move some of the surface heat to the deeper waters, especially where the currents have dived not just from cooling water (hot water would tend to go up, cold water would tend to go down) but because it is driven in «conveyor» systems which may run counter to expectations of where water should go when considering only local conditions, and especially, if the water is dropping because of an increase in salinity.

Global surface temperatures were the 8th or 9th highest recorded, partly because the first two months were cool - ish thanks to a La Nina in the Pacific, where cooler waters sit on the top of the ocean and suck up heat from the atmosphere.

The second is a temperature driven process where cold water sinks at the poles cooling the deep ocean.

The storms gather their energy from warm seas, and so, as oceans heat up, fiercer ones occur and threaten areas where at present the seas are too cool for such weather.

In the Atlantic Ocean, the Gulf Stream is part of what's called the Atlantic Meridional Overturning Circulation, a conveyor belt of ocean water that carries warm water from Florida to Greenland where it cools and sinks to 1000 meters or more before traveling back down the coast to the troOcean, the Gulf Stream is part of what's called the Atlantic Meridional Overturning Circulation, a conveyor belt of ocean water that carries warm water from Florida to Greenland where it cools and sinks to 1000 meters or more before traveling back down the coast to the troocean water that carries warm water from Florida to Greenland where it cools and sinks to 1000 meters or more before traveling back down the coast to the tropics.