Lecture 13 & 14 Flashcards

1
Q

Does water or land have a greater heat capacity

A

Water

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2
Q

Can solar radiation penetrate further into land or water, therefore spreading energy at a greater depth

A

Water

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3
Q

Is latent or sensible heat dominant for water

A

Latent

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4
Q

Is Q* larger over water or land?

A

Water- has a lower albedo

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5
Q

Effectiveness of QE and QS mean that Qh …

A

is small

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6
Q

During the day, is land or sea warmer?

A

Land

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7
Q

At night, is land or sea warmer?

A

Sea

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8
Q

What is the marine thermal characteristics similar to?

A

The soil temperature profile

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8
Q

What is the marine thermal characteristics similar to?

A

The soil temperature profile

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9
Q

Why is there no sea breeze in the morning?

A

Sun still rising, no temperature differences between land and water, so no pressure differences mean no circulation

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10
Q

What breeze develops during the day?

A

The sea breeze

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11
Q

What breeze develops at night?

A

The land breeze

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12
Q

What kind of conditions are conducive to SB-LB occurrence?

A

Strong thermal difference between land and sea
high SW radiation input (little clouds), weak synoptic scale winds

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12
Q

What kind of conditions are conducive to SB-LB occurrence?

A

Strong thermal difference between land and sea
high SW radiation input (little clouds), weak synoptic scale winds

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13
Q

Characteristics of sea breezes - temperate climates eg South Island

A

typical windspeeds of 2 to 5 ms-1
typical inland extent of 30-50 km

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14
Q

characteristics of sea breezes - tropical climates

A

> 300 km inland extent

15
Q

the sea breeze front

A

associated with the development of cumulus cloud, may be sufficient uplift to lead to precipitation

16
Q

direction of breeze

A

initially perpendicular, but influenced by Earth’s rotation / Coriolis force so may become parallel with coast by late afternoon

17
Q

Implications of sea breezes

A

Relief from high temperatures, disperse pollution

18
Q

Lake breeze cause

A

Land will warm faster than the lake during the day so onshore lake breezes may result

19
Q

Generally, the active surface is elevated so that zero plane displacement =

20
Q

Does albedo of a stand decrease higher or lower in the canopy?

A

Decreases with height

21
Q

Effects on SW radiation in vegetation

A

Albedo, shading, skyview factor

22
Q

Effects on LW radiation in vegetation

A

the larger skyview factor, the more LW radiation is retained.

23
Effects of vegetation on energy balance
Q*=QH+QE+QS+QP+QA
24
What is Qp
biochemical energy storage due to photosynthesis
25
The energy balance of vegetated surfaces- QE
most dominant flux
26
The energy balance of vegetated surfaces- QH
flux is reversed because high evaporation keeps the crop cool
27
The energy balance of vegetated surfaces- QG
no QG - ground is shaded so heat storage is soil is small
28
The energy balance of vegetated surfaces- QS
relatively small heat stored inside crop
29
Is the forest a heat sink at day or night
Day
30
Is the forest a heat source at day or night
Night
31
Why is it not always possible to generalise vegetation effects on energy balance?
Diversity of vegetation species and vegetation structures Stand architecture Vertical differences Orientation of principal exchange surfaces
32
Precipitation in forests: stem flow
Water drained along leaves, branches to tree stem
33
Precipitation in forests: canopy drip
Water directed to the edge of tree
34
Precipitation in forests: interception
Water held in the canopy
35
Precipitation in forest: water extracted from...
the atmosphere
36
Vegetation effects on wind speed
Wind speed approaches zero well above the ground surface
37
Why are wind and turbulence in canopies important?
Momentum transfer - wind load & wind throw Land atmosphere interactions - global biogeochemical cycles, energy balance, water use and evapotranspiration Dispersion - dispersion of pollen, forest fires, air pollution