climate 1.1-1.4 Flashcards
what is weather
the state of atmosphere at a particular place and time.
what is climate
the average state of the atmosphere at a particular place over a log period of time, typically 25 years
climate types
tropical equatorial climate
tropical monsoon climate
cool temperature climate
tropical equatorial climate ?
generally high temperature while year, abt 27 degree c
small annual temp range abt 2-3 degree c
high annual precipitation , more than 2000mm
precipitation falls evenly throughout every year
10 degree N and 10 degree S of equator
eg singapore
tropical monsoon climate
generally high temp whole year, abt 25 degree c
small annual temp range abt 3-4 degree c
high annual precipitation abt 1500mm
distinct wet and dry seasons
5 degree N/S and 30 degree N/S of equator
eg kochi, india
cool temperature climate
4 distinct seasons
large annual temp range of abt 21 degree c
annual ppt between 300-900mm
ppt falls evenly throughout the year
between 45 degree N/S and 60 degree N/S of the equator
eg London, UK
relative humidity
ratio of amt of water vapour present in air to the max amt of water vapour the air can hold at a given temp
formula : (amt of water vapour present / max amt of water vapour air can hold) X 100%
convectional rain
heat from the sun is absorb by land and air above it gains heat .
the warm air rises and cools, and condenses on condensation nuclei at dew point temperature , clouds are form
water droplets in the clouds collide and coalesce , when they are large enough , they fall rain
e.g. frequent afternoon thunderstorm in SG
relief rain
prevailing winds pick up moisture over the sea , push the moist air up the windward side of the mountain
rising moist air cools and condenses on condensation nuclei at dew point temperature, clouds are formed
water droplets in the clouds collides and coalesce, when they become large and heavy enough, they fall as rain on the windward side.
most of the moisture has fallen on the windward side , the leeward side experiences dry and descending air, thus it is dry .
eg. wws of sierra Nevada mountain ranges , USA, receives higher rainfall thus has lush forests
lws is hot and dry creating death vally dessert
latitude
is the distance of any point of the earth measured .
how latitude affects temp
low lat , solar angle is higher ( 90dc), sunray / solar radiation is more concentrated on a smaller area , higher temp
high lat, solar angle is lower (10dc) sunray / solar radiation less concentrated is spread / diffuse over a wider area, lower temp
eg. beijing,china (40dc N of equator) average temp is 12dc . sg(10dc n) of equator average temp is 29dc
how altitude affect temp
high alt, air is less dense & air pressure >less able/ lower ability to absorb heat and radiate hear > low temp
low alt , high air density and air pressure > higher ability to absorb and radiate heat >higher temp
eg. genting highlands (alt 1700m above sea lvl) average temp of 21dc
at sea lvl average temp of 32dc
how types of surface affect temp
more dark surface which absorb more solar radiation and radiate more heat
skyscrapers have glass reflects sunlight to ground surface , increases absorption of solar radiation.> high temp
eg urban areas, raffles place sg
light coloured surface reflect more solar radiation and radiate less heat > low temp
eg. ski resort greenland.
how distance from sea affect temp
sea heats up and cools down more slowly than land . hence during winter, sea is warmer than land , warming the air along coastal area. During summer, sea is cooler the land, cooling the air along coastal area.
coastal area : experience cool summer, warm winter due to maritime effect > low temp [ eg. Anchorage , USA annual temp range of 23 dc ]
inland are : warm summers , cold winters due to continental effect > high temp [ eg. Fairbanks, USA annual temp of 40 dc ]
how are clouds formed
air rises up the atmosphere, it cools , reducing the amt of water vapour it can hold.
the amt of water vapour in the air will exceeds the max amt of water vapour the air can hold
at this temp[ dew pt temp] air condenses into water droplets at condensation nuclei
condensation nuclei provide surfaces where water vapour can change into water droplets /solid ice crystal and form clouds.