Term
|
Definition
The prevailing fundamental atmospheric circulation on a planetary scale which must exist in response to radiation differences with latitude, to the rotation of the earth, and to the particular distribution of land and oceans, and which is required from the viewpoint of conservation of energy. |
|
|
Term
|
Definition
circulation induced in a rotating system. |
|
|
Term
|
Definition
The generally small, localized atmospheric circulations, represented by such phenomena as local winds, thunderstorms, and tornadoes. |
|
|
Term
|
Definition
North and South circulation is unusually pronounced |
|
|
Term
|
Definition
|
|
Term
|
Definition
caused by motion, size and number of gas molecules in the air. Height in altitude decreases pressure. |
|
|
Term
|
Definition
An instrument for measuring wind velocity |
|
|
Term
|
Definition
Measures direction of wind |
|
|
Term
|
Definition
are a result of the pressure gradient force and the Coriolus force on air currents: only occur when the wind blows parallel to straight isobars, when there are no other forces acting on it. |
|
|
Term
|
Definition
Below tropics of cancer and above capricorn, North East and South East |
|
|
Term
Inter-Tropical Convergence Zone |
|
Definition
Low pressure moves back and forth due to insolation. Lots of clouds due to warm air rising. |
|
|
Term
|
Definition
Drives air from high-pressure areas to low-pressure areas. Acts in right angles to Isobars. Wants to balance wind pressure. |
|
|
Term
|
Definition
high pressure cell with a clockwise flow |
|
|
Term
|
Definition
An instrument that measures wind pressure |
|
|
Term
|
Definition
Air on a high plateau or polar ice sheet cools and pours off the edge of the plateau. "Gravity drainage" |
|
|
Term
|
Definition
Mostly caused by the ITCZ. Also, is accounted for by the varying of pressure and winds between summer and winter. |
|
|
Term
|
Definition
The general patterns of major ocean currents follow circulation systems around pressure cells. |
|
|
Term
|
Definition
Waving undulations in the westerly flow of geostrophic winds |
|
|
Term
|
Definition
he process by which water formed within Earth reaches the surface is an ongoing process |
|
|
Term
|
Definition
The process of changing H20 from liquid to gas. The Water gains Latent heat, because it needs energy (heat) to transform. |
|
|
Term
|
Definition
When water vapor turns into water: Latent heat is released (we take away the energy of h20) |
|
|
Term
|
Definition
Usually covers a wide area of land after the earth has begun cooling (sunset-sunrise). Never over water. |
|
|
Term
|
Definition
fog produced by air in motion or to fog formed in one place and transported to another. This type of fog is formed when warmer air is transported over colder land or water surfaces. Over Coast-lines |
|
|
Term
|
Definition
When air is confronted by a mountain, goes over the mountain and cools, then sinks back down. Forms clouds. |
|
|
Term
|
Definition
Mother of Tornadoes, they contract horizontally, causing winds to accelerate in an inward vortex. |
|
|
Term
|
Definition
Mother of Tornadoes, they contract horizontally, causing winds to accelerate in an inward vortex. |
|
|
Term
|
Definition
Air that returns to its original position after an initial vertical displacement |
|
|
Term
|
Definition
The transition from ice to water vapor |
|
|
Term
|
Definition
Changing of water vapor directly to solid ice |
|
|
Term
|
Definition
Depends on Altitude and Shape |
|
|
Term
|
Definition
occurs when air flows toward an area of low pressure. Results in heaver precipitation in tropical regions. |
|
|
Term
|
Definition
occurs when air flows toward an area of low pressure. Results in heaver precipitation in tropical regions. |
|
|
Term
|
Definition
Produced when cold front overtakes a warm front in a mid-latitudinal cyclone |
|
|