Climate 1 Flashcards

(38 cards)

1
Q

Weather definition, what it involves

A

State of atmosphere, particular place, short time
- air temperature
- cloud cover
- precipitation
- wind speed, direction

day-to-day changes
more spontaneous changes

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2
Q

Climate defintion, what it involves

A

Average state, atmospheres, particular place, >25yrs
- tropical equatorial
- tropical monsoon
- cool temperate

longer term
more consistent

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3
Q

tropical equatorial climate characteristics

equator

A
  • generally high temp (27deg)
  • small annual temp range, 2-3deg
  • > 2000m annual precipitation, even rainfall

singapore got no season

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4
Q

tropical monsoon climate characteristics

A
  • 25deg
  • 3-4deg
  • 1500mm
  • distinct wet, dry seasons

all other points same as tropical equatorial
these countries have seasons

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5
Q

cool temperature climate

all seasons

A
  • 4 distinct seasons
  • 21deg annual temp range
  • 300-900mm annual precipitation
  • even rainfall
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6
Q

location tropical equatorial climate

A

10deg North
10deg South
equator

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7
Q

location tropical monsoon climate

A

5deg North
30deg North

5deg South
30deg South
equator

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8
Q

location cool temperate climate

A

45deg North
60deg South

45deg South
60deg North
equator

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9
Q

what does climograph show

A

avg monthly temp, rainfall (1yr)

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10
Q

wat cause climatic hazards
their impact

A
  • natural, human induce
  • weather patterns, predictable -> unpredictable (many places)
  • extreme weather event

Natural, human system significant

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11
Q

how does air temp vary

A

in a day / in a year

in a day
day/night

in a year
seasons

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12
Q

air temp variation in 1 day

more minute changes,
usually occur day/night

A

Earth’s rotation on own axis

1 complete rotation = about 24h

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13
Q

Different tropics/regions, Earth

https://docs.google.com/document/d/12rAwkWXiw5RGFDGpRY3RhY_ab2Cs2ZpI7u36Bog2OvM/edit?tab=t.0 page 9

A

https://docs.google.com/document/d/12rAwkWXiw5RGFDGpRY3RhY_ab2Cs2ZpI7u36Bog2OvM/edit?tab=t.0 page 10

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14
Q

How does air temp work in relation 2 rotation of Earth?

A
  1. earth rotate, side face Sun, day, recieve solar radiation, experience higher temp
  2. side eventually face away, rotation, dosent recieve solar radiation experience night time, experience lower temp
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15
Q

3 diff times of day

A
  • midday
  • before, after midday
  • before sunrise

https://docs.google.com/document/d/12rAwkWXiw5RGFDGpRY3RhY_ab2Cs2ZpI7u36Bog2OvM/edit?tab=t.0 page 11

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16
Q

Midday
1. sun position
2. solar radiation
3. temperature

over year
revolutions + seasons

A
  1. directly overhead
  2. smaller surface area hit, more concentrated
  3. highest of whole day

SG

23-25-31-33

17
Q

before, after midday
1. sun position
2. solar radiation
3. temperature

A
  1. not directly overhead
  2. larger surface area hit, less concentrated
  3. lower than midday

SG

23-25-31-33

18
Q

before sunrise
1. sun position
2. solar radiation
3. temperature

aka night

A
  1. does not recieve solar radiation, loses heat for longest time, form of longwave radiation
  2. lowest

SG

23-25-31-33
longwave radiation emitted from ground

19
Q

air temp variations (year) cause

aka seasons

A
  • earth revolution arnd sun
  • 23.5deg Earth axis tilt
  • hemispheres recieve diff amt solar radiation across yr
20
Q

Template for Temperature at different seasons.

A
  1. At month, N/S/Neither Hemisphere
    leans towards Sun
  2. higher/lower direct solar radiation
  3. experience hotter/colder/moderate temp
  4. NH (spring/autumn), SH (autumn/spring)
  5. tropics near equator, direct solar radiation, high temperatures throughout year
  6. temp variations more significant, places outside tropics

Step 2 if Summer/Winter
Step 4 if Autumn/Spring

June: NH lean towards Sun
Dec: SH learn towards Sun
Rest months (Sept, March) Neither

21
Q

relative humidity calculation

A

Amt water vapor (g)/(max water (g) air can hold at that temp) * 100%

22
Q

1 type of cloud in syllabus

A

Culmulonimbus clouds

23
Q

describe how diff latitude -> diff temp

A

Global scale, higher latitude, temp lower
1. Earth spherical shape, solar angle, varies, different parts, Earth
2. higher latitude, smaller solar angle, solar radiation less direct, spread over large area, lower temp

solar angle -> angle in which Sun rays strike Earth surface

24
Q

desc different altitude -> different temp

A

local scale, higher altitude lower temp
1. gravity pull most air molecules -> ground surface
2. lower air density, pressure at higher altitude
3. less air molecules absorb, radiate heat

25
define relative humidity
1. ratio amt water vapor in air to maximum amt of water vapor air can hold in certain temp 2. temp increases, amt water vapor, air can hold increase, Rh decrease 3. evaporation -> more water vapor added 4. Rh 100%, max amt water vapor attained, air saturated -> condensation ## Footnote Amt water vapor (g)/(max water (g) air can hold at that temp) * 100% Rh affected by temp.
26
how are clouds formed
1. air rises up atmosphere, cools, reduce amt water vapor, can hold 2. amt water vapor air, exceed max amt water vapor air, hold, saturated air, 100% Rh 3. **dew point temp**, air condense, water droplets, condensation nuclei (i.e. ash particles from volcano) 4. water vapor -> solid ice crystals, form clouds
27
water cycle
recycle water btwn atmosphere, Earth surface - Sun's heat, water, water bodies evaporate - plants -> water vapor, transpiration - water vapor rise, atmosphere, cool, condense, condensation nuclei, dew pt temp -> clouds - water droplets, clouds, big, heavy enf, fall ground -> precipitation (i.e. snow) - water, ground surface inflitrates subsurface soil - water flows over ground surface, surface runoff, enter bodies of water - below earth surface, groundwater moves horizontally above impermeable rock ## Footnote https://docs.google.com/document/d/12rAwkWXiw5RGFDGpRY3RhY_ab2Cs2ZpI7u36Bog2OvM/edit?tab=t.0 page 11
28
rate of water movement what changes it
1. type soil - more water infiltrate in large pore soil (sandey v clayey soil) 2. built-up area - concrete, tiny pores 3. presence natural vegetation - roots, plants loosen soil, more open space, faster groundwater movement, infiltration - surface runoff slower, stems, roots, plants, act, obstruction, increase surface roughness
29
relief rain formation
1. prevailing winds pick up moisture, sea, push moist air up windward side mountain 2. rising moist air cools, condenses, condensation nuclei, dew pt temp, clouds 3. water droplets clouds coalasce, collide, when large, heavy enf, fall -> ground as rain, windward side 4. most moisture fall, windward side, leeward side, descending air, dry
30
convectional rain, sg
1. in day, heat from Sun, absorbed by land, air above it warm 2. warm air rises -> atmosphere, cools, condenses, dew pt temp, condensation nuclei 3. water droplets, clouds, collide, coalesce, large, heavy enf, fall -> ground 4. sometimes, rain drops break apart as they fall ## Footnote freq afternoon thunderstorms, sg
31
wind speed
depends on 1. strength, pressure gradient 2. friction - moving air, variations, Earth topography, increase frictional drag - uneven relief n rough surfaces on land, greatest frict. drag (**valleys, mountains**)
32
land breeze
1. night, sea, land lose heat, longwave radiation 2. sea n air above it lose heat slowly, warmer air less dense, rises, form lower pressure in air over sea 3. land n air above it lose heat quickly, colder air denser, sinks, form higher pressure in air over land 4. air move down pressure gradient, land -> sea ## Footnote water has high heat cap., hence need more effort to change temp of water BOTH LAND AND SEA BREEZES ARE **LOCAL** WINDS!
33
wind formation
1. horizontal movement, air across Earth surface 2. occurs due 2 unequal distribution, air temp -> unequal distribution, air pressure 3. place w/ lower temperature, air cools, sinks, result area, high air pressure 4. place w/ higher temperature, air heats up, rises, result area, low air pressure 5. air move, higher pressure region -> lower pressure region, **fill void** ## Footnote https://docs.google.com/document/d/12rAwkWXiw5RGFDGpRY3RhY_ab2Cs2ZpI7u36Bog2OvM/edit?tab=t.0 page 14
34
oct-Feb winds
1. Oct-Feb, NH winter, cooler temp, SH summer, higher temp 2. in winter, air over central Asia, cold, sinks, create area, high pressure 3. summer, air over Australia, hot, rises, create area, low pressure 4. air move, Central Asia (high pressure) -> Australia (lower pressure) 5. deflected, right, as travel -> India, Coriollis effect, North-East monsoon, India, SG ## Footnote https://docs.google.com/document/d/12rAwkWXiw5RGFDGpRY3RhY_ab2Cs2ZpI7u36Bog2OvM/edit?tab=t.0 page 16 central asia -> NH australia -> SH
35
North-East monsoon
1. dry, cool, little moisture picked up, Central Asia 2. India experience little rain 3. Winds blow over South China Sea, pick up moisture, form of water vapor, bring heavy rain, areas like SG 4. winds cross over -> SH, deflect, left, continue pick up moisture, Indian Ocean, bring rain, countries, Australia
36
Corolis force NH and SH deflection direction
Winds originating from NH: deflect left Winds originating from SH: deflect right
37
Southwest Monsoon
1. June-Sept, NH experiences summer, higher temp, SH experiences winter, cooler temp 2. NH, warmer air expand, lower pressure over Central Asia 3. SH, cooler air contract, highe pressure over Australia 4. Air, Australia (higher pressure) -> Central Asia (lower pressure) 5. Wind cross into NH, deflect, right, Coriollis effect, South-West Monsoon, India, SG 6. winds move over Indian Ocean, pick moisture, Indian Ocean, bring heavy rain India
38
why varied wind directions in Earth?
1. unequal distribution, air temp, unequal distribution, air pressure 2. air move across Earth regions, high pressure -> low pressure 3. wind travel over long distances, deflect, Corillis force, occurs due 2 Earth rotation