Lectures 5 & 6 Flashcards

1
Q

What is conditional instability?

A

When an air parcel cools faster than the atmosphere but then cools slowly after condensation

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2
Q

What does the depth of frictional influence depend on?

A

Surface roughness
Thermal forcing

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3
Q

What is the top of the boundary layer (Zg)?

A

Where ū (mean windspeed) becomes approximately constant with height

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4
Q

Are vertical gradients of windspeed greater or lesser over smooth terrain?

A

Greater over smooth terrain - less forced convection

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5
Q

Open country windspeed

A

Rapid change of windspeed with height

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6
Q

City centre windspeed

A

More effective mixing so less rapid change in windspeed

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7
Q

Forced convection (in the boundary layer wind field)

A

Turbulence due to the production of shear stress by surface roughness

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8
Q

Free convection (in the boundary layer wind field)

A

Turbulence due to sensible heat working against gravity (producing buoyancy)

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9
Q

Which convection has stronger vertical components in eddies?

A

Free convection (not constrained to ground surface)

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10
Q

Momentum flux

A

change in momentum

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11
Q

Will a downdraft cause an increase or decrease in velocity and momentum of windspeed?

A

an increase

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12
Q

Will an updraft cause an increase or decrease in velocity and momentum of windspeed?

A

A decrease

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13
Q

Stability

A

A measure of the tendency of air tto move vertically

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14
Q

How is free convections stability assessed?

A

Via changing temperature with height - the heat flux density

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15
Q

How is forced convections stability assessed?

A

Via changing horizontal windspeed with height - momentum flux density

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16
Q

What is combined stability

A

the ratio between difference in temperature with height vs difference in horizontal windspeed with height

17
Q

How is combined stability commonly compared

A

Richardson number

18
Q

What is the leading edge effect?

A

The boundary line between the 2 climatically different surface types

19
Q

The adjustments are not immediate, generated at the surface and diffusing upwards. What is the layer of the air whose properties have been affected by the new surface called?

A

Internal boundary layer

20
Q

Speed of leading edge

A

Slow - gains 100-300m fetch for every 1m increase in vertical.

21
Q

Speed of internal boundary layer

A

Fetch of 10-30m for every 1m increase in the vertical

22
Q

Advection fog

A

typically formed by advection of air across water of very different temperatures

23
Q

cold water advection fog

A

Warm air flows over cold water. if air temp cools to dew point temp, water vapour condenses and fog forms

24
Q

warm water advection fog

A

Forms when very cold dry air is transported across warmer water body. The very low layer of air warms and evaporates water from surface. Warm, moist air next to surface is unstable. convects moisture into cooler air and air quickly becomes condensated.

25
Q

Topographic features causing precipitation

A

orographic precipitation

26
Q

Night time topoclimate

A

Solar angle less important, LW radiation more important

27
Q

Cold air accumulation depends on

A

-catchment size from which cold air drains
-duration of drainage
-screening of horizon: sky view factor

28
Q

Radiation frost

A

radiation cooling leads to temperatures <0°C. can be significant in valleys

29
Q

advection frost

A

air is already cold, and transported in. enhanced by altitude

30
Q

which direction are succulents likely to face?

A

towards the equator

31
Q

Equator facing slope characteristics

A

higher SW radiation input, higher temps = more evaporation