Greenhouse effect and climate sensitivity Flashcards

1
Q

Why is the sun unusual?

A

Sun has an incredibly high temperature (~6000oC), sending out intense radiation in the small wavelengths.

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2
Q

The earth (recieving sunlight) has a much lower surface temperature than the sun, but nevertheless…

A

It has a temperature and the Earth itself emits radiation, at a level coordinating with it’s temperature (~15oC)

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3
Q

If everything is in equilibrium (no change in heat from the sun, no change in distances)

A

The earth and the moon will reradiate an equivalent amount of radiation to maintain a constant temperature.

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4
Q

The earth is interestingly warmer than the moon, relationship between radiational heat and gases…

What gases do and don’t take up heat?

A

O2 and N2 by and large don’t take up heat but CO2 and H2O do.

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5
Q

Flexible vs non flexible bonds

A

Flexible can change the orientation of the atoms that make up the molecule
In doing so temporarily absorbing extra energy which is then remitted

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6
Q

Absorption capacity of atmosphere depends on:

A

Amount of each type of molecule present

Absorption spectrum of each type of molecule

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7
Q

Why are generalisations of absorption often inaccurate?

A

To assume everything is absorbed and reemitted is wrong- there are clear window where no absorption occurs.

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8
Q

Where is energy exchange usually measured?

A

The GHGs lose heat at the top of the troposhere.

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9
Q

What is lapse rate?

A

The rate at which air temperature falls with increasing altitude.

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10
Q

Currently on Earth the more molecules of GHG added…

A

The more interception and re-radiation.
Adding GHGs is an ongoing process there is currently a disequilibrium.
Heat loss from the upper troposphere is not keeping up with heat gain via increased GHGs.

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