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You are watching: The principal controls and influences of temperature patterns include


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The 4 controls that atmospheric temperature space (1) differential heater of land and also water; (2) s currents; (3) altitude and also geographic position; and also (4) cloud cover and also albedo (Pearson, The setting ). Atmospheric temperature is defined as the temperature tape-recorded on a thermometer inserted in Earth"s air wherein sheltered from...


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The four controls that atmospheric temperature space (1) differential heating of land and water; (2) ocean currents; (3) altitude and also geographic position; and also (4) cloud cover and albedo (Pearson, The Atmosphere). Atmospheric temperature is characterized as the temperature videotaped on a thermometer inserted in Earth"s air where sheltered from straight solar radiation.

(1) Differential heater of land and water: The oceans and also the land warmth up and retain heat at different rates, at differential rates. This heating and cooling differential affects regional temperatures leading to varying inland and oceanside temperatures in relatively closely related vicinities. Contrasted to oceans, land heats and cools easily while oceans heat and also cool slowly. As a result, ocean waters deserve to cool summer atmospheric warmth and, conversely, heat winter atmospheric cold. This is due to the fact that of the differential prices of easily or gradually accumulating or releasing existing levels that solar heat.

(2) s currents: Directional movements of ocean currents affects land temperatures. An international current motions are facility patterns the are influenced by number of things: s bottom topography; earth"s rotation; s salinity; ocean heat content; and also wind (Smithsonian, s Planet). Together these fads move throughout the oceans, floor masses space either warmed or cooled. A change to any kind of factors affecting surface (surface circulation) or deep currents (thermoline circulation) can change the effects of s currents top top atmospheric temperatures.

(3) Altitude: miscellaneous altitudes have corresponding air pressure and also air density that affect atmospheric temperature. As altitude increases from sea level, waiting pressure and also air thickness inversely decrease. Correspondingly, atmospheric temperature also decreases together altitude increases. Over there is a direct correlation between air pressure, wait density and temperature while there is the inverse, one indirect correlation in between altitude and also temperature.

Geographic position: Atmospheric temperatures have tendency to be comparable on geographic circulation from east to west if temperatures tend to vary considerably in geographic circulation from north to south. Temperature reduce in a pole-ward direction if staying reasonably equal in one east-west direction. In various other words, the temperature in Singapore and Washington D.C. Will tend to be more similar than the temperature in Buenos Aries and also Nuuk.

(4) Cloud cover: Clouds influence temperature because they space a arsenal of frozen particles that have actually a cooling effect; lock drop precipitation i beg your pardon cools; and they reflect and also radiate heat into the space, external Earth"s atmosphere. By mirroring heat, clouds insure a security of temperature so planet doesn"t overheat. By dropping precipitation, clouds cool the warmth accumulation.

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Albedo: The fractional amount of solar power reflected ago into space, as in when warmth is reflected off clouds and radiated earlier into space. Listed below clouds, Earth"s surfaces create various amounts of albedo. Because that example, ice has actually a high albedo when water has a low albedo.