Sentences with phrase «where heat exchanges»

The amplification is due to the diminishing ice cover for the most part, being strongest in the lower atmosphere where heat exchanges with the ocean take place.

[71] The film previewed at Florida International University where a heated exchange with the Dominican diplomatic envoy resulted in police presence.

Not exact matches

After exchanging greetings the two old men, both suffering from diabetes and the afternoon heat, walked arm - in - arm past rug shops, falafel stands, vendors of rosaries and frankincense, into the massive Crusader - built Church of the Holy Sepulchre (constructed on the ruins of Constantine's Anastasis) where a Byzantine liturgy of thanksgiving was conducted to mark the event.

Assemblywoman Amy Paulin took the stand Tuesday as the prosecution's first witness in the corruption trial of former state Assembly speaker Sheldon Silver, where her description of Albany's inner workings was pointedly contested by Silver's defense lawyer, Steven Molo, in a series of heated exchanges.

«Afterwards, the heated fluid is taken upwards to the geothermal station, where it produces electricity, generally via a binary cycle (exchanging heat between the water and an organic liquid), and it is re-injected into the site in a closed cycle.»

The Iceland and Greenland Seas are among the only places worldwide where conditions are right and this heat exchange is able to change the ocean's density enough to cause the surface waters to sink.

As a result, there has been a reduction in the heat exchange over the locations where sinking occurs in the ocean.

The El Niño Southern Oscillation is an internal phenomenon where heat is exchanged between the atmosphere and ocean and can not explain an overall buildup of global ocean heat.

While raising a stake for the World Series of Poker, Huck falls for a new - to - town chanteuse (Drew Barrymore) and, in several mesmerizing, heated exchanges, butts heads with his estranged poker - champ dad (Robert Duvall, in the rare Zeroes role where he's not window - dressing).

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This is not the case with surface - to - air heat exchange (which involves evapo - transpiration, sensible heat flows, and radiation) or even within the troposphere where impacts of latent heating on atmospheric circulations are realized on scales ranging from hundreds of meters to thousands of kilometers.

He laments the heat around global warming and similar topics, telling her, «These issues are exactly where we need rational discourse, an unbiased exchange of ideas, and the evaluation of facts not colored by us yelling at each other.»

Where he explains they don't apply is in the OSBL, commonly called the surface layer or the mixed layer, identified as the region gas (and heat) exchange occurs.

Sea ice is an important component of the Earth system; it is highly reflective, altering the amount of solar radiation that is absorbed; it changes the salinity of the ocean where it forms and melts, and it acts as a barrier to the exchange of heat and momentum fluxes between the atmosphere and ocean.

That's only one part of the problem of the heat transfer at the Earth's surface, where the non-radiative exchange is dominant (evaporation + convection).

In contrast, an adiabatic process is where a system exchanges no heat with its surroundings»

In some way, that's the engine where all the other variations must be hanged (specially variations in albedo because of clouds - maybe connected with solar cycles as other authors are trying to prove -, variations in albedo because of sea ice extention, linked with the oceanic currents - as in the «stadium wave» that was presented by Curry and others, etc., variations in heat exchange between atmosphere and oceans, and so on.

The heat exchange at the other side of the layer will be given by h * (Ta - Tb) where Tb is the temperature of the next layer and so on.

Without atmosphere the surface of the ocean or land would lose o (T ^ 4 — Ts ^ 4)(1) where Ts is the temperature of the space (about 4K) while in the presence of the atmosphere the heat losses are hc * (T — Tl)(2) and o (T ^ 4 — Tl ^ 4)(3) where (2) represents the heat transfer by convection (inclusive conduction) through the air layer and (3) corresponds to the net flow due to the heat exchange by radiation, Tl being the mean temperature of the air layer.

In other words, instead of using the empiric relation h (T — Tl) where h, being experimentally determined, involves all the channels for the exchange of heat, one splits the problem into the detailed discussion on how the different channels contribute to the final results.

If surface radiation has been measured and does indeed average 390 W / m ² then either the stated «input wattage» (your 170 Watts / m ^ 2) is incorrect or the «Earth System», Globe + Atmosphere, must be looked at as one complete unit where internal heat exchange uses or looses 390 — 170 = 220 W / m ², or — Kirchhoff was wrong but nobody, as far as I know, advocates that.

You can see below another hierarchical «tree» structure from Adrian Bejan's earlier work on constructal trees as heat exchange - where a single contact draws heat from a rectangular area.

This is the crux of the matter, and why I say this is where AGW is confused, to the point where as above shortwave radiation is believed to «be thermal energy heating the Earth», because this is how the «statistical» has justified «its method `, by looking at energy exchange out of context of heat.

Most people don't have a daily blog where they share their thoughts, but what child from a broken marriage hasn't accidentally overheard a heated exchange between their parents, or an upset comment to a friend or family member?