Weather Flashcards
4 basic types of cumuliform clouds
Cumulus (CU)
Towering cumulus (TCU)
Cumulonimbus (CB)
Altocumulus castellanus (ACC)
CU
Cumulus
Develop vertically
Bulging upper part
Appear detached from other clouds
White at the tp and relatively dark bases
TCU
Towering cumulus
Rapidly growing cumulus
Height exceeds the width
CB
Cumulonimbus
Contain thunderstorm activity
Upper portion is smooth/ fibrous & always flattened
ACC
Altocumulus castellanus
White/ gray/ both
Composed of rounded masses & rolls, may/ may not be merged
Pressure gradient
Rate of change of pressure with horizontal distance measure in km
Calculated by 4 hPa in ‘x’ km (distance between isobars is always 4 hPa)
Buys Ballot’s Law
In N. hemisphere: wind at your back = area of low pressure lies to your left
Veering
Wind makes a clockwise change in direction
Backing
Wind makes a counter-clockwise change in direction
Arrows on surface maps indicate the direction wind is ____
Blowing from
Full barb on arrow represent ___ knots
10
5 lifting agents
Convection
Orographic lift
Frontal lift
Mechanical turbulence
Convergence
Convection
Air is heated from below by contact with Earth’s surface
Orographic lift
Air is force up sloping terrain by the wind
Frontal lift
Air is forced to rise by a wedge of colder/ denser air
Mechanical turbulence
Friction between the air and ground cause the air to be stirred up into series of swirling motion known as eddies
Convergence
Air converges at the centre of low-pressure systems and is force to rise, resulting in cloud & precipitation