Valley Climates Flashcards

(22 cards)

1
Q

Aspect

A

The direction of hill slopes in relation to the suns rays

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
2
Q

Shadow zone

A

The area where there is no direct warming from the sun (faces poles)

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
3
Q

Anabatic winds

A

Winds that blow upslope (during the day)

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
4
Q

Katabatic winds

A

Winds that blow downslope (at night)

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
5
Q

Valley winds

A

Winds that blow up valley (during the day)

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
6
Q

Mountain winds

A

Winds that blow down valley (at night)

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
7
Q

Temperature inversion

A

When air temperature increases with increasing altitude

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
8
Q

Frost pocket

A

The bottom of a valley where cold air collects and causes frost to form

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
9
Q

Radiation fog

A

Fog formed due to terrestrial radiation

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
10
Q

Comment on aspect of slopes

A

Slopes facing the equator are warmer than those facing the poles

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
11
Q

Aspect affect on vegetation and human settlement (north facing)

A

Soils are dryer
Grasses and shrubs
Houses built on these slopes because they are warmer.
Crops like grapes which like hot, sunny conditions

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
12
Q

Aspect affect on vegetation and human settlement (south facing)

A

Soils are wetter
Shade-loving plants such as trees, ferns and mosses.
Not popular
Suited to forestry
Winter wheat in SW Cape

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
13
Q

Valley winds during the day

A

Slopes and air above heat them.

Warm, less dense air above the slopes rises (anabatic winds)

Winds also blow up the valley during the day (valley winds)

Warm, less dense air above the slopes rises

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
14
Q

Valley winds at night

A

Slopes and air above them are cooled

Cold, dense air on slopes sinks (katabatic winds)

Winds also blow down the valley at night (mountain winds)

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
15
Q

Normal temperature lapse rate

A

Where temperature decreases with increasing altitude

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
16
Q

Temperature inversion

A

NTLR reversed, when temperature increases with increasing altitude

17
Q

Frost

A

Still, clear winter night the land cools quickly.

No clouds prevent terrestrial radiation from escaping
No wind to mix the air

The cold air drains down to the valley floor, displacing the warm air upwards. This causes a temperature inversion where temperature increases with an increase in altitude.

If dew point is below freezing, then water vapour changes into ice crystals and frost is formed on the valley floor (frost pocket)

18
Q

Effects of temperature inversions on settlement and farming

A

People will build their houses halfway up the slope of a valley to be in the warmer thermal belt

Crops which need warm, frost-free condition will be planted in the thermal belt, e,g. Sugar cane

19
Q

Thermal belt

A

The zine where warm air is trapped between colder air masses (usually middle part of slope)

20
Q

Why are settlements in SH usually halfway up north facing slopes where it is warmest?

A

Gets direct perpendicular rays of sun (faces equator)
Avoids the top (temp decreases with increased altitude)
Avoids valley floor (cold pocket of air)

21
Q

Effects of frost pockets on settlement and farming

A

Crops which can withstand cold conditions can be planted at the bottom of the valley e.g. potatoes

Pollution is trapped in the cold air below the temperature inversion at night

22
Q

Radiation fog

A

Forms in valley on cold, clear, windless nights.

Rapid cooling to dew point (>0) through a great vertical depth causes condensation

Water droplets are so small that they are suspended in the air.

This is known as radiation fog because it forms as a result of cooling due to terrestrial radiation .

The densest fog forms in the lowest part of the valley where air is coldest

As the earths surface starts to heat up during the morning, the fog evaporates from below and appears to “lift”.