atmosphere and weathering Flashcards
atmosphere
area of transparent gases surrounding earth
weather
short term conditions of the atmosphere
climate
long term average conditions in atmosphere
incoming solar radiation
main energy input strongly influenced by cloud cover and latitude
reflected solar radiation
albedo of a surface, proportion of sunlight reflected
surface absorption
energy arriving has potential to heat up surface
latent heat
liquid-water vapour, consumes considerable amount of energy
sensible heat transfer
transfer of parcels of air to or from point at which energy budget is being assessed
long wave radiation
1.emitted by earths surface - atmosphere
mist
cloud at ground level, collection of water droplets
fog
when visibility below 1000m, thicker cloud cover
advection fog
warm moist air passes over cold surface = chilled, condensation happens = dew
radiation fog
ground looses gear at night by LW radiation and so air above = cooled = condensation and fog
dew
condensation of water on a surface
temperature inversions
normally air temp drops with altitude BUT sometimes abnormal layer of warmer air above colder
temp inversions - why happen?
during day, ground heated, heats air above it - emits LW radiation. at night, ground looses heat so just above ground = very cold as cools quicker
sea breeze
differential heating of land and sea
land breeze
occurs at night when land cools faster than sea
net radiation
amount of sun received by an area
insolation
radiation concentrated near equator , dispersed at poles