L2 - Radiation balance and greenhouse Flashcards

1
Q

Planck function

A

relates intensity of radiation from a blackbody to its wavelength (radiation curve)

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2
Q

Radiation

A

Travels as waves of photos which release energy when absorbed
Emitted energy increases to the 4th power of its blackbody temperature

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3
Q

Why does radiation decrease when it penetrates the atmosphere?

A

This is due to absorption (20%) and reflection e.g. by clouds

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4
Q

In what form can radiation reach the ground?

A

Direct radiation or diffuse radiation

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5
Q

Diffuse radiation

A

beam of radiation broken into weaker rays redirected in other direcctions by gases in the atmosphere

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6
Q

Albedo

A

measure of amount of reflected shortwave radiation (can be considered as %)

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7
Q

What type of radiation does the atmosphere absorb?

A

Longwave

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8
Q

What is excess radiative energy used for?

A

80% used for evaporation (latent heat) and 20% for rising warm air and sinking cold air (sensible heat transfer)

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9
Q

Inverse square law

A

intensity of the radiation goes down by the square of the distance from the source

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10
Q

There is more outgoing radiation than incoming at the poles. Does this mean they are cooling down?

A

No. Energy is transferred to the poles via wind, ocean currents and moisture from the tropics

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11
Q

Radiative forcing (RF)

A

The difference between:
- Incoming solar radiation
- Outgoing LW radiation
- Incoming LW radiation from stratosphere

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12
Q

Instantaneous radiative forcing

A

without temperature adjustment of the stratosphere

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13
Q

(Adjusted) Radiative forcing

A

Including temperature adjustment of stratosphere. Reduces RF due to LW flux from stratosphere to troposphere

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14
Q

To what extent is radiation from the lower atmosphere layers absorbed by higher layers and vice versa?

A

Constant absorption between layers - this is why more complex models are used

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