atmosphere and weathering Flashcards

(52 cards)

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
Hadley cell
30 degree latitude - responsible for trade winds in the tropics and control low-latitude weather
26
Polar cell
60-70 degrees N&S - air sinks over highest latitudes and flows out towards the lower latitudes
27
Ferrell cell
mid-latitude - warm air from tropics get fed north by the surface winds of this cell
28
Rossby waves
large-scale fast 'rivers of air' formed by westerly winds
29
throughs
low pressure systems
30
ridges
high pressure systems
31
jet streams
strong and regular winds which blow in upper atmosphere as part of Rossby waves
32
air rising
low pressure
33
air descending
high pressure
34
corriolos effect
deflection of moving objects caused by rotation of earth. deflects objects to left in NH and left in SH
35
difference in climate due to : latitude
decrease in temp between equator and poles, shine concentrated at equator
36
difference in climate due to : altitude
for every 100m temp drops by 1 degree, pressure dries as altitude increase = less dense and cooler
37
difference in climate due to : prevailing winds
air at equator = rises, when cooled = sinks
38
difference in climate due to : ocean currents
warm from hot areas = rise temp cool areas = cool temp flow in same direction SO affect same places
39
difference in climate due to : distance from sea
land heats up and cools more quickly than the sea
40
condensation nuclei
tiny particles where vapour can condense on e.g. dust
41
absolute humidity
amount of water vapour in atmosphere
42
relative humidity
amount of water vapour in atmosphere expressed as a % of max. amount of water air can hold at that temp
43
cloud
visible mass of condensed water vapour/ice particles floating in the atmosphere
44
cloud classicised according to : altitude
below 2,000m = low between 2000-20000m = ALTO above 6000m = CIRRO
45
cloud classicised according to : shape
cumulus - heavy/lumpy/fluffy cirrus - wispy starts - vast sheets
46
cloud classicised according to : bring precipitation ?
``` nimbus = yes nimbostratus = flat/wide rain clouds cumulonimbus = taller/denser clouds , thunderstorms ```
47
Orographic rainfall
air forced to rise over barrier, as rises cools/condenses = rain, rain shadow effect where reward slope = v. little rain
48
convection rainfall
when land = v. hot = heats air above it, air expands and rises, cools and condenses, continues to rise = rainfall TROPICAL AREAS
49
frontal rainfall
warm air meets cool air at a front, warm air lighter = rises above condenser. as rises cools and condenses = rain MID - LATITUDES
50
hail
frozen pellets of rain formed by raindrops being carried up/down in vertical air
51
snow and sleet
form when temp. below freezing and sublimation occurs
52
frost
occurs on cloud free nights when radiation cooling to below freezing