By Adrian E. Gill
During this paintings, Dr. Gill appears to be like on the research of oceanic and atmospheric circulations. He explains how atmospheric and oceanic circulations are eventually pushed by means of solar power, and covers the learn of saw distributions of actual amounts, together with temperature.
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Additional info for Atmosphere-Ocean Dynamics
The second is by viscous stresses. The irregularities on which forces are exerted may vary in size from mountain ranges like the Andes down to trees, blades of grass, and ocean surface waves. 1 Fig. 2. The spacing of latitudes is such that the distance between two nearby latitudes is proportional to the square of the cosine of the latitude. With this scale the area under the curve would be zero if the average rate of transfer of momentum from the atmosphere were the same over the land as over the sea at each latitude.
Such a circulation in the meridional plane is now known to exist in the tropics (see Fig. 7)and Halley’s explanation of the circulation is essentially correct. However, this meridional circulation is now called the Hadley circulation. This appears to be because Halley’s explanation of the easterly component of the trade winds was incorrect, whereas Hadley (1735) gave an explanation that is much closer to the truth. 5’ latitude) by some 2083 miles per day. 5” would, in the absence of friction, acquire a westward velocity of 2083 miles per day at the equator.
The heat transferred by this means is, on average, about 75% of the convective transport (see Fig. 6). The release of latent heat in clouds also affects the conditions under which convection can take place. The amount of water vapor a parcel of air rising adiabatically can hold decreases with height. Thus if the parcel is already saturated with water vapor, latent heat will be released as the parcel rises, so the rate of decrease of temperature with height will be less than for dry air. The rate of decrease with height is called the moist adiabatic lapse rate and has a value that depends on the temperature and pressure.