The Climate of Earth and Other Planets Flashcards

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1
Q

How do you calculate the temperature of planets and moons?

A

A box model.

The model balances incoming solar energy against outgoing infrared energy.

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2
Q

What are the shortcomings of the box model?

A

The box model only works for mars and the moon.
It fails to predict the temperature of Venus and earth.
This is because the box model does not account for atmosphere.

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3
Q

How far up in infrared radiation emitted?

A

Up to 5.5km up

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4
Q

Oceans -

Where is most of the heat absorbed?

A

20m down

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5
Q

Oceans -

What is the length of the mixed layer in the ocean?

A

From 20 to 100km

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6
Q

What is heal flow?

A

the rate of energy transfer between an object

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7
Q

What is the unit of measurement for heal flow?

A

jewels per second/ kilo watts

often talked about through unit per area

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8
Q

What factors affect temperature?

A
  1. Distance from sun
  2. Albedo
  3. Atmosphere
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9
Q

Which planet is an example of how albedo impacts temperature?

A

Venus - close to sun yet reflects 90% of infa-red energy

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10
Q

What is solar irradiance?

A

The power per unit area received from the sun in the form of electromagnetic radiation.

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11
Q

What is the solar irradiance when the sun shines directly on the earth?

A

Solar irradiance = 1361 W m-2

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12
Q

What factor is the solar irradiance divided by?

A

4

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13
Q

Why is solar irradiance divided by 4?

A
  • Half of the earth is in shadow

- most of the day surface is obliquely lit

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14
Q

What is the actual solar irradiance?

A

340 W m-2

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15
Q

What percentage of incoming energy does the earth reflect?

A

30%

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16
Q

How do you work out planetary temperature?

A
  1. Caluculate solar heating using distance from the sun
  2. Multiply by (1-albedo) to get flux into planet’s climate system
  3. Find the temperature that gives a matching flux out using
    - Const. x (t+273C) 4
17
Q

What is the troposphere?

4 points

A
  • lowest layer of earth’s atmosphere (0-18km)
  • where weather takes place
  • 99% of water vapour stored here
18
Q

What is the stratosphere?

A
  • layer above the troposphere
  • stratified in temperature,
  • warmer layers higher and cooler layers closer to the Earth
  • increase of temperature with altitude is a result of the absorption of the Sun’s ultraviolet radiation by the ozone layer
19
Q

As you go higher into the troposphere, what is the temperature gradient?

A
  • 6 to 10 degrees C per km of altitude
20
Q

Why can thermal radiation increase quickly as temperature increases?

A
  • is to the power of 4 in equation

- if temperature increases by 1%, radiation increases by 4%

21
Q

What kind of heat flow happens in the ocean?

A

Vertical flows of heat

22
Q

Why does vertical exchanges happen?

A
  • mixing in the top 100m is wind driven
23
Q

Where does ocean mixing happen?

A

in the top 100m