Urban climate - lectures 16-19 Flashcards

1
Q

Landscapes modified by human agency, buildings

A

Urban environment

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2
Q

The localised warming exerted by an urban area

A

Urban Heat Island

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3
Q

Heat added to the atmosphere by human activities

A

Qf

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4
Q

Road transport, power generation, domestic heating, air conditioning

A

Examples of Qf

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5
Q

Heat stored within the urban canopy

A

Qs

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6
Q

Advection (from surrounding areas)

A

Qa

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7
Q

Is Qe important in UHI

A

less important - little surface water available for transpiration and evaporation. For local climate with parks or irrigated areas may cause oasis effect!

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8
Q

Is Qg important in urban areas

A

Yes, an enhanced role

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9
Q

Why is Qg more important in urban areas

A

Increased heat storage during the day caused by urban materials, increased heat emission in evening and night, low sky view factors

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10
Q

Where is Qg less important

A

Mediterranean settlements

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11
Q

What heat flux is most important in suburbs

A

Qh

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12
Q

Suburban Qh lags rural Qh

A

diurnal variation

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13
Q

Urban radiation & energy fluxes lead to the generation of…

A

urban boundary layer

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14
Q

Multiple reflective surfaces (urban canyon), changed albedo, particulate matter - reflects and absorbs incoming SW radiation

A

SW radiation

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15
Q

Particulate matter reflects and absorbs incoming SW radiation, as a result is a source of downwards LW radiation, reduced LW emission (sky view factor)

A

LW radiation

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16
Q

Additional source of energy Qf, reduced Qe, increased Qg and Qs, reduced Qa

A

Surface energy balance

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17
Q

High Qh and Qs, low Qe

A

City centre energy balance

18
Q

High Qe, low Qh and Qs

A

Rural energy balance

19
Q

Slower to warm up in mornings (Qg) and low sky view factors mean reduced receipt of SW radiation

A

Urban cool island

20
Q

Urban areas often have slower heating and cooling rates than rural areas

A

Diurnal evolution of UHI

21
Q

Why are warming & cooling rates different?

A

Qg, outgoing LW radiation

22
Q

How are parks different from urban surroundings?

A

colour - albedo
water availability

23
Q

High proportion of available water

A

possible oasis effect Qe > Q*

24
Q

Only occurs when synoptic-scale pressure gradients light, more common at night, can be of great significance for pollutant dispersal

A

Urban breeze

25
Increased drag and turbulence from urban surface results in a relatively deep zone of friction - reduced windspeeds in comparison to equivalent rural atmosphere
Urban Boundary Layer
26
if wind is oblique to street =
corkscrew effect
27
if wind is parallel =
no sheltering by buildings - channelling of wind may result in jetting effect so enhanced wind speed
28
Speed increases with height, so tall buildings will deflect faster moving upper air down to ground level, so can be up to 3 times windier than over open ground
Impacts of tall buildings
29
Weak synoptic flow / pressure gradient, clear skies, more prominent at night
Favourable synoptic conditions for UHI
30
City located on a high mountain ridge, prone to UHI development - UHI > 11°C recorded. Entrainment of warm urban air into katabatic flow makes some valleys warmer than valley heads.
Johannesburg, South Africa
31
Since mid 1970s, greater diurnal temp on _____ and ____ compared to rest of the week
Sunday and Monday
32
small town east of Chicago, downwind of steel mills, with increased annual precipitation from 990 mm to 1450 mm in 1930-1945. at nearby stations precipitation decreased from 990 to 900mm. rise in precipitation kinked to rise in steel production - but little investigation
The La Porte Anomaly
33
positive correlation between UHI intensity and vapour pressure - so warmer nights associated with more moisture in air, difference in vapour pressure
Urban moisture excess (UME)
34
Urban Plume - meso or micro?
Meso
35
Canopy Layer - meso or micro?
Micro
36
Line & point pollution sources
Canopy Layer/ microscale
37
Areal pollution source
Boundary layer/ mesoscale
38
Warm air overlying cold air
inversion
39
occurs in a stable atmosphere, vertical motion is suppressed causing a relatively thin, concentrated plume
fanning
40
occurs during the development of a surface radiation inversion
lofting
41
If turbulent eddies are smaller than the pollutant cloud / plume
Will diffuse it
42
if turbulent eddies are larger than the pollutant cloud / plume
Will transport it