Sentences with phrase «more warm surface water»

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

2/3 cup warm water 1/2 teaspoon dry active yeast 1/2 teaspoon granulated sugar 1 teaspoon olive oil plus more for bowl and brushing pizza 1-1/2 cups bread flour plus more for work surface 1/2 teaspoon kosher salt 3/4 cup tomato sauce 4 ounces fresh mozzarella, torn 6 squash blossoms, de-stemmed and petals separated

Ingredients 3 1/2 to 3 3/4 cups unbleached all - purpose flour, plus more for dusting the work surface 2 teaspoons salt 1 cup warm whole milk (about 110 degrees) 1/3 cup warm water (about 110 degrees) 2 tablespoons unsalted butter, melted 3 tablespoons honey 2 1/4 tsp (1 envelope) rapid rise yeast

Ingredients: 1 1/2 tsp dry active yeast 1 cup warm water, (105 degrees to 110 degrees) 1 tbsp agave nectar 1 1/4 cups rye flour 1 1/2 cups whole wheat flour 3/4 cup all - purpose flour, plus more for work surface 2 tablespoons caraway seeds 2 teaspoons salt 6 tbsp canola or olive oil 1/4 c soy yogurt

2/3 cup warm water 1/2 teaspoon dry active yeast 1/2 teaspoon granulated sugar 1 teaspoon olive oil plus more for bowl and brushing dough 1-1/2 cups bread flour plus more for work surface 1/2 teaspoon kosher salt 1/2 cups tomato sauce plus more for serving 1/2 cup pesto plus more for serving 1/4 cup shredded Italian cheese blend 1/4 cup finely grated Parmesan 1/4 teaspoon dried thyme 1/4 teaspoon garlic powder

1 cup plus 1 tablespoon old - fashioned oats 1/2 cup honey 2 tablespoons butter 1-1/2 teaspoons kosher salt 2 cups boiling water 1 package dry active yeast (about 2-1/4 teaspoons) 1/3 cup warm water 1/4 cup flaxseed meal 3 cups whole wheat flour 1-1/2 cups all - purpose flour plus more for work surface Vegetable oil for greasing 2 teaspoons poppy seeds 2 teaspoons sesame seeds 1 teaspoon garlic flakes 1 teaspoon onion flakes 1 teaspoon coarse salt 1 teaspoon water 1 large egg

«It may be that the cooler, deeper water in MCEs could be more hospitable to many species than the warmer surface water,» she said.

The cycle of Pacific Ocean surface water warming and cooling has become more variable in recent decades, suggesting El Niño may strengthen under climate change

Higher sea surface temperatures led to a huge patch of warm water, dubbed «The Blob,» that appeared in the northern Pacific Ocean more than two years ago.

Driven by stronger winds resulting from climate change, ocean waters in the Southern Ocean are mixing more powerfully, so that relatively warm deep water rises to the surface and eats away at the underside of the ice.

The more heat in the Pacific, the bigger the El Niño, and right now, 150 metres below the surface, a ball of warm water is crossing that ocean.

So this effect could either be the result of natural variability in Earth's climate, or yet another effect of carbon dioxide and other greenhouse gases like water vapor trapping more heat and thus warming sea - surface temperatures.

Heat that stays at the surface will ultimately result in greater sea - level rise as warmer water expands more readily as it heats up.

A rather straightforward calculation showed that doubling the level of carbon dioxide in the atmosphere... which would arrive in the late 21st century if no steps were taken to curb emissions... should raise the temperature of the surface roughly one degree C. However, a warmer atmosphere would hold more water vapor, which ought to cause another degree or so of warming.

As La Nia ends, the surface water flows back and the coast is hit with unusually warm water, which results in more rainfall.

They pointed to a warmer atmosphere, which carries more water vapor to worsen rainstorms, as well as to higher ocean surface temperatures, which intensify hurricanes.

As the planet warms from climate change, there is more evaporation from both land and water surfaces.

The research published in Nature Communications found that in the past, when ocean temperatures around Antarctica became more layered - with a warm layer of water below a cold surface layer - ice sheets and glaciers melted much faster than when the cool and warm layers mixed more easily.

However, the surface warming caused by human - produced increases in carbon dioxide, methane, and other greenhouse gases leads to a large increase in water vapor, since a warmer atmosphere holds more moisture.

CO2 is more soluble in colder than in warmer waters; therefore, changes in surface and deep ocean temperature have the potential to alter atmospheric CO2.

UHI effects have been documented in city environments worldwide and show that as cities become increasingly urbanised, increasing energy use, reductions in surface water (and evaporation) and increased concrete etc. tend to lead to warmer conditions than in nearby more rural areas.

As a general matter, yes, but AIUI the increasing height (depth) of the ice face is the key factor for accelerating retreat of these glaciers since it creates more surface area for the warm water to work on.

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.

At the same time, the warm surface waters collect more heat from the atmosphere as they move further westward, and form a warm pool near New Guinea, Australia and the Philippines.

Manta Point and Crystal Bay can be more challenging due to the currents and cold water, and Nusa Lembongan is the relaxing, warmer, shallower dive usually done after a long lunch break and surface interval.

Other factors would include: — albedo shifts (both from ice > water, and from increased biological activity, and from edge melt revealing more land, and from more old dust coming to the surface...); — direct effect of CO2 on ice (the former weakens the latter); — increasing, and increasingly warm, rain fall on ice; — «stuck» weather systems bringing more and more warm tropical air ever further toward the poles; — melting of sea ice shelf increasing mobility of glaciers; — sea water getting under parts of the ice sheets where the base is below sea level; — melt water lubricating the ice sheet base; — changes in ocean currents -LRB-?)

The warming being seen during the Autumn and Winter is mainly due to increased heat fluxes from the surface (Screen & Simmonds 2010) due to thinner ice and more open water, so represents a net heat loss to the atmosphere.

Independent computer models (about 23 or so world - wide, I believe), generally show a warming of the surface and even more in the tropsophere in the tropics due to increased water vapor (warm the air up and it has more available water vapor (a greenhouse gas)..

So, if each underwater artic volcano emitted 1 km3 a week (a rather large average flow) and did it for a year (about 52 weeks) you would need about 620 very active and extremely powerful volcanoes in order to warm the artic ocean by just 1 C (and that ignores surface cooling, in / out water flows and time rates that would require even more volcanoes.)

(I think that an anomalously warm ocean surface heated from below would lead to more evaporation, and the additional water vapor would give a positive greenhouse effect that would partially offset the effect of a drop in greenhouse gas concentrations.)

Re 9 wili — I know of a paper suggesting, as I recall, that enhanced «backradiation» (downward radiation reaching the surface emitted by the air / clouds) contributed more to Arctic amplification specifically in the cold part of the year (just to be clear, backradiation should generally increase with any warming (aside from greenhouse feedbacks) and more so with a warming due to an increase in the greenhouse effect (including feedbacks like water vapor and, if positive, clouds, though regional changes in water vapor and clouds can go against the global trend); otherwise it was always my understanding that the albedo feedback was key (while sea ice decreases so far have been more a summer phenomenon (when it would be warmer to begin with), the heat capacity of the sea prevents much temperature response, but there is a greater build up of heat from the albedo feedback, and this is released in the cold part of the year when ice forms later or would have formed or would have been thicker; the seasonal effect of reduced winter snow cover decreasing at those latitudes which still recieve sunlight in the winter would not be so delayed).

However, at the same time, there's been the steady increase in subtropical ocean surface temperatures in the Atlantic Warm Pool, leading to record water temperatures off the US east coast in winter, which tends to fuel more extreme storms (via the increase in water vapor pressure over the warmer ocean).

Seems to me the debate about AGHG global warming and increasing TC frequency / intensity / duration boils down to the fact that as sea surface temperatures, as well as deeper water temperatures rise, the wallop of any TC over warmer seas without mitigating circumstances like wind sheer and dry air off land masses entrained in the cyclone will likely be much more devastating.

As the Earth's surface warms — due to either manmade greenhouse gases or natural fluctuations in the climate system — more water evaporates from the surface.

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.

The soil thaws, the surface collapses, lakes form, water flows, land surfaces erode which in turn releases more carbon dioxide to create more warming, to make the tundra even more vulnerable to spring thaw, and of course to accelerated warming.

They then looked at the challenges that warmer oceans delivered for crustaceans, molluscs, sponges, deep sea invertebrates, the warm and cold water corals that provide habitat for one - fourth of the ocean's variety, the pelagic or surface - swimming fish, and the demersal or deep - sea denizens that live longer, reproduce more slowly and are thus less likely to evolve and adapt to changing conditions.

Warmer air holds more water vapour so that warmer air will extract more vapour from the ocean surface thereby cooling the ocean surWarmer air holds more water vapour so that warmer air will extract more vapour from the ocean surface thereby cooling the ocean surwarmer air will extract more vapour from the ocean surface thereby cooling the ocean surface..

Sea level on the West coast may begin to rise due to climate regime shift as warm surface waters return to the Pacific Read More

As atmosphere is warmed by the warmed surface, more water would become a gas and ocean ice would become liquid.

One would get some water vapor in the atmosphere, but liquid water on the surface would be rare - probably more due to volcanic activity rather than sunlight warming surface.

Their causes range from completely unpredictable events like volcanic eruptions (which have mainly local effects) to more regular phenomena such as «El Niño» (a warming of the surface waters of the tropical Pacific that occurs every three to five years, temporarily affecting weather world - wide).

Additionally, the less sea ice covers the surface of the ocean, the more sunlight is absorbed by the water, which scientists warn could accelerate the Arctic's warming.

Due to the Antarctic Refrigerator Effect, the deep oceans continued to cool, and the thermocline that separates warm surface water from cooler deep waters became increasingly more shallow.

As warm surface currents near the poles the water cools and its salinity increases due to ocean water freezing and leaving the water near the poles more salty.

(Demos) As warm surface currents near the poles the water cools and its salinity increases due to ocean water freezing and leaving the water near the poles more salty.

Climate Alchemy and probably most scientists not taught chemical thermodynamics don't realise that the main heat transfer term in the oceans is the partial molar enthalpy transferred when the fresh, cold water sinking from melting ice in the Antarctic and Arctic summers is made more saline when it mixes with the warmer, more saline surface water for which solar energy has partially unmixed the ions.

The paper discusses that melting ice will decrease the salinity of the ocean waters around Antarctica, which will cause decreased mixing with the relatively warmer deep ocean waters, reducing sea surface temperatures, causing more sea ice to form.

Cold water surfacing more strongly in the PDO can give the impression that the surface layer is not warming very fast relative to layers below.

El Ni o an irregular variation of ocean current that, from January to February, flows off the west coast of South America, carrying warm, low - salinity, nutrient - poor water to the south; does not usually extend farther than a few degrees south of the Equator, but occasionally it does penetrate beyond 12 S, displacing the relatively cold Peruvian current; usually short - lived effects, but sometimes last more than a year, raising sea - surface temperatures along the coast of Peru and in the equatorial eastern Pacific Ocean, having disastrous effects on marine life and fishing