Lec 4 Flashcards

(14 cards)

1
Q

What is radiative forcing? Give example for the types.

A

It is the change in energy balance. This can be local or global.

Local: Urbanization changes the characteristics of the surface making local radiative forcing

Global: Greenhouse gasses altering the composition of the atmosphere making a global radiative forcing

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2
Q

In what form does the earth intercept solar radiation?

A

Using the area of a circle and the solar constant

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3
Q

How do you get energy budget of earth?

A

absorbed solar radiation - outgoing radiation = energy budget

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4
Q

Where is planetary albedo the lowest and highest?

A

Highest in the poles lowest at deep water oceans

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5
Q

What is OLR where is it the greatest?

A

Outgoing longwave radiation

Greater over warm deserts and tropical ocean.

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6
Q

What is meridional transport?

A

transport of energy from the tropics to the poles

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7
Q

What is net short wave radiation?

A

Difference between incoming radiation and the amount reflected

K* = K (in) - K (out)

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8
Q

What is net longwave radiation dependant on?
(know for midterm exam)(stefan boltzmann used here)

A

Differences in temperature and emissivity, where clouds and other obstructions can have an important role

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9
Q

What is the surface energy balance?

A

Q* = Qh + Qe + Qg

net radiative flux of energy into a surface (Q*)

Qh: sensible heat flux from the surface to the atmosphere
Qe: latent heaf flux from the surface to the atmosphere
Qg: Sensible heat flux from the surface to the ground

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10
Q

What is sensible heat flux (Qh)

A

energy transferred between the surface and air when there is a temperature gradient present. It can be felt as a rise or fall in the temperature of the air

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11
Q

What is latent heat flux (Qe)

A

Energy released or required for the change in state

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12
Q

what is ground heat flux (Qg)

A

heat transfered into the ground via conduction, is generally smaller than sensible and latent heat fluxes

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13
Q

Incoming solar radiation reaching the earths surface:
a) absorbed only by water bodies on Earth
b) represents about 50% of the amount that was at the top of the atmosphere
c) is unaffected by the surface albedo
d) none of the above

A

C

however outgoing solar radiation IS effected by surface albedo

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14
Q

Why is energy budget more complex at the surface compared to the atmosphere

A

at the surface you have to also consider the heat transfer from conduction and convection along with radiation.

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