atmosphere and weathering Flashcards

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1
Q

atmosphere

A

area of transparent gases surrounding earth

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2
Q

weather

A

short term conditions of the atmosphere

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3
Q

climate

A

long term average conditions in atmosphere

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4
Q

incoming solar radiation

A

main energy input strongly influenced by cloud cover and latitude

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5
Q

reflected solar radiation

A

albedo of a surface, proportion of sunlight reflected

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6
Q

surface absorption

A

energy arriving has potential to heat up surface

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7
Q

latent heat

A

liquid-water vapour, consumes considerable amount of energy

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8
Q

sensible heat transfer

A

transfer of parcels of air to or from point at which energy budget is being assessed

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9
Q

long wave radiation

A

1.emitted by earths surface - atmosphere

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10
Q

mist

A

cloud at ground level, collection of water droplets

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11
Q

fog

A

when visibility below 1000m, thicker cloud cover

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12
Q

advection fog

A

warm moist air passes over cold surface = chilled, condensation happens = dew

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13
Q

radiation fog

A

ground looses gear at night by LW radiation and so air above = cooled = condensation and fog

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14
Q

dew

A

condensation of water on a surface

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15
Q

temperature inversions

A

normally air temp drops with altitude BUT sometimes abnormal layer of warmer air above colder

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16
Q

temp inversions - why happen?

A

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

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17
Q

sea breeze

A

differential heating of land and sea

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18
Q

land breeze

A

occurs at night when land cools faster than sea

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19
Q

net radiation

A

amount of sun received by an area

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20
Q

insolation

A

radiation concentrated near equator , dispersed at poles

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21
Q

poles

A

negative budget - SHOULD be colder

22
Q

tropics

A

positive budget - SHOULD be warmer

23
Q

HIGH air pressure

A

air pushing down , little cloud formation = better weather

24
Q

LOW air pressure

A

air moving up, more cloud formation = wetter weather

25
Q

Hadley cell

A

30 degree latitude - responsible for trade winds in the tropics and control low-latitude weather

26
Q

Polar cell

A

60-70 degrees N&S - air sinks over highest latitudes and flows out towards the lower latitudes

27
Q

Ferrell cell

A

mid-latitude - warm air from tropics get fed north by the surface winds of this cell

28
Q

Rossby waves

A

large-scale fast ‘rivers of air’ formed by westerly winds

29
Q

throughs

A

low pressure systems

30
Q

ridges

A

high pressure systems

31
Q

jet streams

A

strong and regular winds which blow in upper atmosphere as part of Rossby waves

32
Q

air rising

A

low pressure

33
Q

air descending

A

high pressure

34
Q

corriolos effect

A

deflection of moving objects caused by rotation of earth. deflects objects to left in NH and left in SH

35
Q

difference in climate due to : latitude

A

decrease in temp between equator and poles, shine concentrated at equator

36
Q

difference in climate due to : altitude

A

for every 100m temp drops by 1 degree, pressure dries as altitude increase = less dense and cooler

37
Q

difference in climate due to : prevailing winds

A

air at equator = rises, when cooled = sinks

38
Q

difference in climate due to : ocean currents

A

warm from hot areas = rise temp
cool areas = cool temp
flow in same direction SO affect same places

39
Q

difference in climate due to : distance from sea

A

land heats up and cools more quickly than the sea

40
Q

condensation nuclei

A

tiny particles where vapour can condense on e.g. dust

41
Q

absolute humidity

A

amount of water vapour in atmosphere

42
Q

relative humidity

A

amount of water vapour in atmosphere expressed as a % of max. amount of water air can hold at that temp

43
Q

cloud

A

visible mass of condensed water vapour/ice particles floating in the atmosphere

44
Q

cloud classicised according to : altitude

A

below 2,000m = low
between 2000-20000m = ALTO
above 6000m = CIRRO

45
Q

cloud classicised according to : shape

A

cumulus - heavy/lumpy/fluffy
cirrus - wispy
starts - vast sheets

46
Q

cloud classicised according to : bring precipitation ?

A
nimbus = yes 
nimbostratus = flat/wide rain clouds
cumulonimbus = taller/denser clouds , thunderstorms
47
Q

Orographic rainfall

A

air forced to rise over barrier, as rises cools/condenses = rain, rain shadow effect where reward slope = v. little rain

48
Q

convection rainfall

A

when land = v. hot = heats air above it, air expands and rises, cools and condenses, continues to rise = rainfall
TROPICAL AREAS

49
Q

frontal rainfall

A

warm air meets cool air at a front, warm air lighter = rises above condenser. as rises cools and condenses = rain
MID - LATITUDES

50
Q

hail

A

frozen pellets of rain formed by raindrops being carried up/down in vertical air

51
Q

snow and sleet

A

form when temp. below freezing and sublimation occurs

52
Q

frost

A

occurs on cloud free nights when radiation cooling to below freezing