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An irregularly periodic variation in winds and sea surface temperatures over the tropical eastern Pacific Ocean, affecting the climate of much of the tropics and subtropics.

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A coupled ocean-atmosphere phenomenon that is the counterpart of El Niño as part of the broader El Niño–Southern Oscillation climate pattern.

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The warm phase of the El Niño–Southern Oscillation and is associated with a band of warm ocean water that develops in the central and east-central equatorial Pacific, including the area off the Pacific coast of South America.

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The local name given a chinook wind in southern California.

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Unseasonably warm winds that can cause extreme increases in temperatures within a few hours.

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The nightly downslope winds commonly encountered in a mountain valley.

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The daily upslope winds commonly encountered in a mountain valley.

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A breeze blowing toward the sea from the land, especially at night, owing to the relative warmth of the sea.

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A breeze blowing toward the land from the sea, especially during the day owing to the relative warmth of the land.

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Sea breezes and land breezes are two familiar categories of local winds that are driven by differences in temperature and in air pressure, which is the pressure exerted by air on a given area.

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Areas of high atmospheric pressure around the north and south poles; the north polar high being the stronger one because land gains and loses heat more effectively than sea.

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The boundary between the polar cell and the Ferrell cell around the 60° latitude in each hemisphere.

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Low pressure located at about the latitudes of the Arctic and Antarctic Circles.

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The dry, cold prevailing winds that blow from the high-pressure areas of the polar highs at the north and south poles towards low-pressure areas within the Westerlies at high latitudes.

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Prevailing winds from the west toward the east in the middle latitudes between 30 and 60 degrees latitude.

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The prevailing pattern of surface winds from the east toward the west found in the tropics, within the lower portion of the Earth's atmosphere, in the lower part of the troposphere near the Earth's equator.

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The subtropical latitudes between 30 and 35 degrees both north and south where Earth's atmosphere is dominated by the subtropical high, an area of high pressure, which suppresses precipitation and cloud formation, and has variable winds mixed with calm winds.

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The area encircling Earth near the Equator, where the northeast and southeast trade winds converge.

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The rise of air in the equatorial region reduces surface air pressure, creating an equatorial low pressure zone (Equatorial Low).

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The character and amount of atmospheric pressure change during a specified period of time, often a three-hour period preceding an observation.

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The condition that exists when the distribution of winds in a given area results in a net horizontal outflow of air into the area.

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The condition that exists when the distribution of winds in a given area results in a net horizontal inflow of air into the area.

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A high-pressure center characterized by a clockwise flow of air in the Northern Hemisphere. Also known as a anticyclone.

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A large scale air mass that rotates around a strong center of low atmospheric pressure.

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Fast flowing, narrow, meandering air currents in the atmospheres of some planets, including Earth.

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The theoretical winds that would result from an exact balance between the Coriolis force and the pressure gradient force.

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An effect whereby a mass moving in a rotating system experiences a force acting perpendicular to the direction of motion and to the axis of rotation.

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The force which results when there is a difference in pressure across a surface.

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A line on a map connecting points having the same atmospheric pressure at a given time or on average over a given period.

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The flow of gases on a large scale. On the surface of the Earth, wind consists of the bulk movement of air.

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A barometer that records its readings on a moving chart.

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An instrument for measuring pressure as a method that does not involve liquid.

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A barometer in which the weight of a column of mercury in a glass tube with a sealed top is balanced against that of the atmosphere pressing on an exposed cistern of mercury at the base of the mercury column, the height of the column varying with atmospheric pressure.

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The weight of the atmosphere pressing down on the earth.