Sentences with phrase «warm surface water into»

It is apparently driven by the acceleration and slowing of the great ocean conveyor that carries warm surface water into the northern North Atlantic (Science, 1 July 2005, p. 41).

They flush the cooled surface waters down into the ocean depths, part of a giant conveyor belt that brings more warm surface water into the far north.

Not exact matches

1) Sift the flour into a mixing bowl 2) Add the salt to the flour, mixing together 3) Add the olive oil, mixing as you add to ensure the flour envelopes the oil 4) Add warm water bit by bit until dough reaches the right consistency 5) One the dough ready, roll it into a ball, and knead well on a cool, flat surface 6) Flatten the dough with a wooden rolling pin 7) Cut into 10 cm pieces and roll them long enough and evenly 8) Place the pin - shaped dough on a well - greased baking tray 9) Bake in oven at 175 deg cel (medium heat for gas ovens) for 20 -30 minutes or until the sticks are ready (test by breaking off a small piece to check that the inside is well cooked) 10) Allow to cool for 5 minutes before serving

Dip a rice paper wrapper into warm water and immediately pull it out of the water, letting the excess moisture drip off before placing on a clean surface.

1) Mix flour, butter and icing sugar in a bowl using two knives to cut the butter until the mixture resembles fine breadcrumbs 2) Add in the egg yolks and vanilla extracts and mix well, then add iced water until the dough starts to come together 3) Shape the dough into a ball on a cool, flat, floured surface 4) Flatten dough into a disc and then wrap in plastic wrap, and chill in the refrigerator for at least 30 minutes 5) Meanwhile, peel, core and slice the apples into as thin slices as possible 6) Mix sugar and ground cinnamon powder with sliced apples and let it rest for a while 7) Pre-heat oven to 180 deg cel 8) Once dough has chilled, roll pastry dough on a sheet of parchment paper until it has expanded to the size of the tart mold (I used a rough mold the size of a large pizza) 9) Leaving at least an inch of dough free, arrange apple slices by overlapping them slightly in the shape of a circle, starting from the outermost part of the circle, until you reach the inside 10) Fold the edges of dough over the filling and then sprinkle the dough with a bit of sugar 11) Bake for about 40 - 45 minutes, or until the crust is golden brown and the apples are soft 12) Serve warm, with a side of whipped cream or ice cream (optional)

So, for example, a big part of what drives a hurricane is the fact that you've got a lot of warm water near the surface of the ocean that is transferring heat into the air, and that's what's moving up, and that is a big part of then what's propelling the entire bigger storm system.

With an El Niño now under way — meaning warm surface waters in the Pacific are releasing heat into the atmosphere — and predicted to intensify, it looks as if the global average surface temperature could jump by around 0.1 °C in just one year.

Instead of dissipating into space, the infrared radiation that is absorbed by atmospheric water vapor or carbon dioxide produces heating, which in turn makes the earths surface warmer.

Without the periodic upwelling of cold water associated with La Niña, warm water would cover most of the surface of the Pacific, releasing its heat into an atmosphere already warming because of climate change.

Warm and saline water transported poleward cools at the surface when it reaches high latitudes and becomes denser and subsequently sinks into the deep ocean.

They mix warm equatorial surface water into greater depths, and help bring cooler waters to the surface.

With lots of warm surface water releasing heat into the atmosphere, in addition to ever - rising levels of greenhouse gases, 2015 is likely to surpass the warmest year on record, and 2016 will be similarly hot.

As the Earth continued to cool from Years 0.1 to 0.3 billion, a torrential rain fell that turned to steam upon hitting the still hot surface, then superheated water, and finally collected into hot or warm seas and oceans above and around cooling crustal rock leaving sediments.

Note that Ekman pumping does not penetrate deep into the oceanic interior, but since the trades advect the surface waters westward, the upper layer of warm sea water is deeper in the west than in the east.

Because the temperature of Ceres is relatively warm (between -93 ℃ and -33 ℃), water - ice exposed at the surface would rapidly convert into a gas in such a low - pressure environment.

The penetration of LWIR into water is immaterial, as by warming the surface, one also warms whatever water the surface layer then mixes with.

Cassini discovered a liquid - water ocean under the icy surface of the moon Enceladus and, perhaps a victim of its own success, must die to prevent any chance that its warm electric generators might melt their way down into those life - friendly waters.

Oats have anti-oxidant and anti-inflammatory compounds such as avenanthramides (a polyphenol) and vitamin E. Oat powder mixed with warm water turns oats into a colloidal mixture that deposits onto the skin's surface to create a protective barrier to soothe the skin.

For global warming scenarios, additional forcing comes into play: surface warming and enhanced high - latitude precipitation, which will also reduce density of northern surface waters (an effect which alone has shut down deep water formation in some model experiments, e.g. Manabe and Stouffer 1993, 1994).

Geoengineering proposals fall into at least three broad categories: 1) managing atmospheric greenhouse gases (e.g., ocean fertilization and atmospheric carbon capture and sequestration), 2) cooling the Earth by reflecting sunlight (e.g., putting reflective particles into the atmosphere, putting mirrors in space to reflect the sun's energy, increasing surface reflectivity and altering the amount or characteristics of clouds), and 3) moderating specific impacts of global warming (e.g., efforts to limit sea level rise by increasing land storage of water, protecting ice sheets or artificially enhancing mountain glaciers).

If as a result of physical processes (such as El Nino) warmer water reaches the surface of the ocean, so less heat is conducted from the atmosphere into the ocean and the atmopsheric temperature will therefore increase — on a much shorter — comparatively instantaneous — timescale.

Note that Ekman pumping does not penetrate deep into the oceanic interior, but since the trades advect the surface waters westward, the upper layer of warm sea water is deeper in the west than in the east.

I recall mention that Katrina was unusual because while crossing the Gulf «Ring Current» the deeper water pulled up by the hurricane was almost as warm as the sea surface, so the deeper water fed almost as much heat energy into the storm as the surface.

The surface waters of the tropical Atlantic are then transported, via the Gulf Stream, towards the high latitudes where they warm the atmosphere before plunging into the abysses in the convection zones situated in the seas of Norway, Greenland and Labrador.

eadler2 January 10, 2015 at 5:54 pm ... When ocean surface temperatures cool, due to a La Nina, the warmer surface water is mixed deeper into the ocean and cooler ocean water flows along the surface of the Pacific.

The researchers found that Mount Pinatubo's eruption still kept much of the world dry, even after taking into consideration the drying effects of El Niño an abnormal warming of surface ocean waters in the eastern tropical Pacific.

When ocean surface temperatures cool, due to a La Nina, the warmer surface water is mixed deeper into the ocean and cooler ocean water flows along the surface of the Pacific.

The increased area of warm water on the surface allows the tropical Pacific Ocean to discharge more heat than normal into the atmosphere through evaporation.

Due to the predominance of La Nina's in the last 15 years, the warmer surface water has been mixed into the deeper ocean.

East Coast winter storms, known as «nor» easters» because of the unusual northeasterly direction of the winds as the storm spirals in from the south, are unusual in that they derive their energy not just from large contrasts in temperature that drive most extratropical storm systems, but also from the energy released when water evaporates from the (relatively warm) ocean surface into the atmosphere.

But again, I have to ask a question that you have not answered: How does the heat trapped by CO2 at the surface skin warm the subsurface ocean waters since it is widely acknowledged that the infrared heat from CO2 can't penetrate into the ocean itself?

The results suggest that warm Atlantic water never ceased to flow into the Nordic seas during the glacial period; inflow at the surface during the Holocene and warm interstadials changed to subsurface and intermediate inflow during cold stadials.

That water vapor that turned into snow clouds causing snow was generated from a warmer surface, from when the snow landed back on it.

The warmth is eventually diluted into the frigid (3C) abyss by a factor of 10 to 1 (the ratio of cold abyssal water to warm surface water).

IF we had say, a bowl of frigid ocean water — and we immersed a sun warmed rock into that bowl of frigid ocean water, till 70 % of it was covered — then whipped the exposed surface of the rock with air that was many degrees colder than the exposed rock surface --

According to fluid modelling, at one point the accumulation of OCAPE was released abruptly (~ 1 month) into kinetic energy of thermobaric cabbeling convection (TCC), resulting in the warmer salty waters getting to the surface and subsequently warming of ca. 2 °C sea surface warming.

The main mechanism for wind - driven mixing into the deep ocean (down to around 2000 metres) is via convergence of warm tropical surface water in the subtropical ocean gyres.

Most of the deep ocean warming is occurring in the subtropical ocean gyres - vast rotating masses of water in each ocean basin where near - surface currents converge and are forced downward into the ocean interior.

It can not account for the huge volume of leftover warm water that's below the surface and returned to the West Pacific and into the eastern tropical Indian Ocean via off - equatorial slow - moving Rossby waves.

So warmer - than - normal surface waters in the South Atlantic created by the changes in atmospheric circulation during an El Niño should be transported northward into the North Atlantic (and vice versa for a La Niña).

Global surface temperatures in the last few years have received a bump in recent years because of a large El Niñ0 event, which brought warm water up from the depths of the Pacific ocean and released the energy into the atmosphere.

AGW climate scientists seem to ignore that while the earth's surface may be warming, our atmosphere above 10,000 ft. above MSL is a refrigerator that can take water vapor scavenged from the vast oceans on earth (which are also a formidable heat sink), lift it to cold zones in the atmosphere by convective physical processes, chill it (removing vast amounts of heat from the atmosphere) or freeze it, (removing even more vast amounts of heat from the atmosphere) drop it on land and oceans as rain, sleet or snow, moisturizing and cooling the soil, cooling the oceans and building polar ice caps and even more importantly, increasing the albedo of the earth, with a critical negative feedback determining how much of the sun's energy is reflected back into space, changing the moment of inertia of the earth by removing water mass from equatorial latitudes and transporting this water vapor mass to the poles, reducing the earth's spin axis moment of inertia and speeding up its spin rate, etc..

This resulted from the combined effects of high sea surface temperatures in open water areas and the effects of atmospheric circulation drawing warm air into the region.

Global warming affects evapotranspiration — the movement of water into the atmosphere from land and water surfaces and plants due to evaporation and transpiration — which is expected to lead to:

The warmed surface water is then transferred downward into the water column by conduction and convection.

The warming reached a depth of about 10,000 feet (4,000 meters), interfering with the normal circulation process in which colder surface water descends, taking oxygen and nutrients deep into the ocean.

The extra boost from the warmer water is adding even more energy into this storm system, increasing the availability and transport of moisture toward land and producing more efficient wind gusts to the surface.

The unusually high sea ice surface temperatures reflect a shift in ocean circulation, enhancing the import of warm, Atlantic - derived waters into the Arctic Ocean.

The deep waters, being warmer than such surface waters, rise to the surface, as the upper layers sink slowly into the dark ocean depths.

So, it is not surprising that those modellers who «need» to get warm surface waters to move into the depths of the oceans, and remain sequestered there for long periods of time, would turn to the physical mechanism of this vertical circulation system.