Week 3 Flashcards

(43 cards)

1
Q

Why do extreme winds happen?

A

Temperature difference of the air above glaciers and surrounding air that leads to difference in densities

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2
Q

Specific heat

A

Energy required to raise the temp by 1 deg Celsius

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3
Q

Freezing point of water at sea level: Celsius

A

0

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4
Q

Freezing point of water at sea level: Farenheit

A

32

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5
Q

Freezing point of water at sea level: kelvin

A

273.15

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6
Q

Boiling point of water at sea level: Celsius

A

100

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7
Q

Boiling point of water at sea level: Fahrenheit

A

212

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8
Q

Boiling point of water at sea level: kelvin

A

373.15

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9
Q

Average sea level atmospheric pressure: kPa

A

101.325

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10
Q

Average sea level atmospheric pressure: mb

A

1013.25

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11
Q

Average sea level atmospheric pressure: hPa

A

1013.25

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12
Q

Atmospheric pressure above sea level

A

Decreasing pressure (effect of gravitational pull is less, less mass)

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13
Q

1 atmosphere

A

14.7 PSI

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14
Q

What happens to atmospheric pressure as you increase/decrease in height?

A

The higher in height the lower the density and pressure

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15
Q

Convection

A

Air moving vertically

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16
Q

Advection

A

Air moving horizontally

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17
Q

2 main forces acting on atmospheric particles

A

Gravity and pressure gradient force

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18
Q

Direction of air movement

A

High pressure to low pressure

Parallel to wind

19
Q

Isobars

A

Join areas of equal pressure

20
Q

Why do pressure differences exist at earths surface?

A

Surface heating

Adiabatic changes

21
Q

Surface heating- high albedo

A

100%, means high reflectivity surface

22
Q

Net amount of radiation absorbed and retained at Earth’s surface

A

0.8 watts/m^2

23
Q

Four differences in energy absorption between water and land

A
  1. Specific heat
  2. Transmission
  3. Mobility
  4. Evaporative cooling
24
Q

Surface heating- specific heat

A

The specific heat of water is 4-5x that of land

25
Transmission
Solar radiation pénétrâtes water more easily than land
26
Mobility
Water mixes and distributes energy more evenly than land
27
Evaporative cooling
The process of evaporation absorbs energy, cooling the surrounding environment
28
Adiabatic
Without the addition or subtraction of heat within a system
29
What happens when air mass expands
Density of air particles decrease Air pressure decrease Temperature decrease Opposite of air mass is compressed
30
Convection cell
Column of air expands over hot surface Air flow replacing rising air Where global winds are developed
31
Hadley cell
Stable convection cell centred over the tropics/ midlatitudes/ poles Rising air over ITCZ Defending air over 30 deg latitude Shifts North and south seasonally based on the thermal equator
32
Global pressure regions
Global circulation cells cause consistent zones of high and low pressure
33
Coriolis effect
The apparent deflection of loving objects (wind, oceans) from travelling in a straight path, in proportion to the speed of earth’s rotation at different latitudes
34
Impacts of Coriolis on Hadley cell
Winds in the northern hemisphere are pushed right Concentrated in tropical latitudes Trade winds antitrade winds
35
Trade winds
Consistent surface winds blowing from east to west (easterlies)
36
Antitrade winds
Consistent upper wings blowing west to east westerlies
37
The polar cell
Cold air descending over the poles
38
Polar easterlies
Consistent surface winds blowing east to west (easterlies)
39
The midlatitudes
Season variations in temp prevent significant convection cells from stabilizing Airflow fed by Hadley and polar cell
40
Labelling winds
From direction they are coming from
41
Jet stream
Concentrated band of high speed upper atmospheric wind | 300km/hr
42
Why do jet streaks form at edge of circulation cells?
A cross section of the atmosphere: - 2 air masses of different temp - pressure variations at altitude - pressure gradient forces airflow
43
Rossby waves
The méridional (North/south) movement of a jet stream