weather studies Flashcards
factors influencing weather
temperature
relative humidity
rainfall
pressure and wind
temperature is
the degree of hotness or coldness of a place
factors influencing temperature
latitude
altitude
distance from sea
cloud cover
format- how does temperature vary in a year
at a degree of 23.5 which hemisphere sun is over where days and nights solar angle path length effect on temperature
march and september
exposed to sun for equal timing to cool and heat up
diff temps at diff latitudes- solar angle
at lower latitudes- angle of the sun rays reach the earth’s surface vertically
concentrated heating-smaller surface area
intense heating-higher temperature
conversely,
scattered heating-large surface area
less intense heating- lower temperature
diff temps at diff latitudes- path length
lower latitudes- rays past thru shorter distance of atmosphere- lose less heat
conversely,
higher latitudes- rays past thru longer distance of atmosphere- lose more heat
temperature-altitude[radiation]
solar energy reaches earth through radiation
energy absorbed and radiated from ground
high altitude- less heat
temperature-altitude[density of air]
higher altitudes- lower air pressure
less water vapour and dust at higher altitudes
cannot absorb a lot of heat
allows heat to escape
maritime effect
summer- temp rises= land heats up faster
cool air over sea is brought to the coast= cool coastal areas
winter- temp drops= land cools faster
warmer air over sea is brought to the coast= warmer coastal areas
experience cool summer and warmer winters
coastal effect
summer- land heats up faster than sea
air is warmer- warm summers
winter- land loses heat faster than sea
air is colder- cool winters
night- cloud cover
little clouds- cold- heat radiating into space isn’t blocked
many clouds- heat radiated from ground is limited by clouds
it absorbs and deflects radiated heat from ground-heat is trapped
day-cloud cover
little clouds-warm- huge amounts of sun energy reach earth, absorbed by land
many clouds-cool-reflects large amount of suns energy back into space.
how is conventional rain formed?
- air is heated. It expands and rises
- cools to dew point temperature, further cooling results in condensation on condensation nuclei
- droplets merge to form large and heavy droplets- cumulonimbus clouds.
- when they become too heavy and large, they may fall to the ground as conventional rain
how is relief rain formed?
- air passes over the sea and arrives at the coast.
- moist air is forced to rise up the windward side of the mountain
- as air rises, it cools. the air becomes saturated with water vapour when dew point temperature is reached. further cooling results in condensation on condensation nuclei amend cloud formation.
- rain falls on the windward side when water droplets merge and become large and heavy enough. this is known as relief rainfall.