Planetary Energy Balance Flashcards

1
Q

What is the simplest equation for the Earth’s surface temperature, assuming no atmosphere?

A

T^4_s = \frac{S(1-A)}{4 sigma}

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2
Q

What does sigma represent?

A

The Stefan-Boltzmann constant, applicable in blackbody emission.

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3
Q

What is the blackbody emission equation for an object of temperature T?

A

sigma T^4

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4
Q

What assumption is made when we consider energy balance per square metre?

A

Divides every term by 4.

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5
Q

What does epsilon denote?

A

The emissivity of an object (how much of a black body an object is when emitting radiation). Ranges from 0 to 1 as it is a proportion.

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6
Q

What is the Leaky Greenhouse model?

A

A uniform atmospheric slab describing the energy balance, from incoming radiation and outgoing from the surface and to the TOA

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7
Q

What are the longwave emission terms in the Leaky Greenhouse?

A

Incoming: S/4, and outgoing is SA/4. These pass wholly through the atmosphere.

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8
Q

How does longwave behave in the atmosphere?

A

The atmosphere is fairly transparent to longwave radiation.

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9
Q

What are the surface terms of emission for shortwave radiation in the Leaky Greenhouse Model?

A

Outgoing from surface: sigma T^4_s.
Incoming from atmosphere: epsilon sigma T^4_A.

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10
Q

What is the TOA terms from the shortwave radiation (from the atmospheric slab)

A

(1- epsilon) sigma T^4_s (from surface via atmosphere)
epsilon sigma T^4_A.

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11
Q

How does adding a hydrological cycle (turbulent fluxes) alter the energy balance equations?

A

It cools the surface and warms the atmosphere.

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12
Q

What is sensible heat flux?

A

Dry heat transport from upward air motion.

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13
Q

What is latent heat flux?

A

Upward heat flux from surface water evaporation, increasing the atmospheric temperatures and decreasing the surface’s.

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