a half of the earth,usually divided into northern and southern halves by the equator
weather
the condition of the earths atmosphere at a particular time and place.
climate
The average (expected) weather conditions in an area based on data collected over 30 years or more.
troposphere
he area of the atmosphere from the Earth's surface to a height of 10-15km in which the weather takes place
climate zone
divisions of the Earth's climates into belts or zones, according to average temperature and average rainfall. The three major zones are polar, temperate and tropical.
latitude
he imaginary lines that surround the earth ranging from 0° at the equator to 90° at the pole
atmospheric air pressure
The force exerted on the Earth's surface by the weight of the air, measured in millibars.
low pressure
caused when air is rising, so less air is pressing down on the ground; air rises as it warms, leading to low pressure at the surface.
high pressure
when there is more air pressing down on the ground, caused by air sinking; air descends as it cools, leading to high pressure at the surface.
condensation
the process by which rising water vapour becomes a liquid.
precipitation
he collective term for moisture that falls from the atmosphere; this could be in the form of rain, snow, sleet or hail
hadley cell
a system of vertical and horizontal air circulation that creates major weather patterns, predominantly in tropical and subtropical regions
ferrel cell
air circulation cell found at midlatitudes (between 30° and 60°) between Hadley and Polar cells.
polar cell
air circulation cell found between 60° and 90°, air rises at lower latitude and sinks at poles.
front
a boundary separating two masses of air with different densities, usually heavier cold air and lighter warm air.
trade winds
the prevailing pattern of easterly surface winds found in the tropics within the lower section of the Earth's atmosphere.
prevailing wind
the most frequent, or common, wind direction
rain shadow
an area or region behind a hill that has little rainfall because it is sheltered from rain bearing winds.
monsoon
heavy rainfall that arrives as a result of seasonal wind, notably in southern Asia and India between May and September.
Katabatic wind
movements of cold dense air that flow downhill and along valley floors; in Antarctica, most winds blow towards the coast from the centre.