Session 3 (Earths Energy Balance (cont.)) Flashcards

1
Q

Greenhouse gasses

A

Water Vapor, CO2, Nitrous Oxide, Methane, Ozone =.

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2
Q

Non Greenhouse Gasses.

A

nitrogen, oxygen

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3
Q

How does a GHG absorb the radiaiton?

A

If the gas vibrates on the same wavelength as the Radiation.

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4
Q

Once
Band Saturation has been reached, it does
not matter if we put any more of this GHG into
the atmosphere.

A

False, adding more GHG’s will lead to more warming since the scattering effect still transports heat out to space, the transport only decreases.

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5
Q

Gases with
lower band
saturation can
have a much
bigger impact
as gases with
high band because….

A

they have yet to be saturated and have more potential to trap more.

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6
Q

Why is water vapor the most important GHG on earth?

A

It captures the most radiation. Increases its lifetime depending on how warm it is.

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7
Q

Water Vapor Feedback loop

A

Global air increase -> Increased water vapor -> Increased GHG warming from water vapor

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8
Q

3 ways to analyze the global warming potential of a GHG

A

Ability to absorb IR radiation, Saturation, Lifetime

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9
Q

PM10

A

Larger droplets, shorter life, more precipitation (WARMING)

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10
Q

PM2.5

A

Smaller droplets, longer life, less precipitation (COOLING)

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11
Q

Do anthropogenic aerosol clouds
have a warming or a cooling effect?

A

Cooling due to reflectivity

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12
Q

Anthropogenic aerosols

A

Biomass burning, Industrial emissions

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13
Q

Natural Aerosols

A

Volcanic, marine, wind blown dust

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14
Q

If aerosols have a net cooling effect, are they a good thing then?

A

No, There ares still effects like lung damage, rain reduction, and altercation of wind circulation

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15
Q

More Higher Clouds leads to…

A

Warming

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16
Q

Less lower clouds leads to….

A

Warming

17
Q

more small water droplets in clouds leads to….

A

Cooling