Lecture 1 - Energy Balance Flashcards

1
Q

What is the synonym for light

A

Electromagnectic radiation

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2
Q

What is a perfect blackbody?

A

A perfect blackbody is one that absorbs all incoming light (i.e. all wavelengths) and does not reflect any. At room temperature, such an object would appear to be perfectly black.

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3
Q

What does the Plankโ€™s Radiation Law mean?

A

It means that with a perfect blackbodyโ€™s temperature has a specific spectrum and intensity.

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4
Q

What are the five atmospheric absorption band?

A
  • Solar radiation transmitted (70-75%)
  • Infrared atmospheric window at 10 micrometer
  • Most terrestrial radiation is absorbed (15-30% emitted)
  • GHGs only absorb at specific wavelengths
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5
Q

Which are the most important greenhouse gases?

A

CO2 and H2O

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6
Q

What is forcing?

A

A forcing of 1 W/m2 means that at the top of the atmosphere the incoming SWR exceeds the outgoing
LWR by 1 W/m2.

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7
Q

What are positive forces?

A
  • GHG
  • Ozone
  • Solar irradiation
  • Albedo
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8
Q

What are negative forces?

A
  • Aerosol effects
  • Albedo
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9
Q

Where does a large proportion of the radiative imbalance goes to?

A

Oceans take of 93% and accumulates it as heat in the ocean.

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10
Q

What are the three most important positive feedbacks?

A
  • Water vapor feedback: H2O is a strong greenhouse gas. Warming leads to more water vapor
    in the atmosphere
  • Albedo feedback: melting ice reduces surface albedo, more SWR absorbed and thus
    enhanced warming
  • Cloud feedback: Clouds affect both short wave radiation (reflectivity) and long wave
    radiation (absorption/emission).
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11
Q

What is the most important negative feedback?

A

Stefan-Boltzmann law: The amount of heat removed from the earth changes with the fourth power of temperature. ๐น = ๐œŽ๐‘‡^4.

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12
Q

Why do clouds form differently in the tropics compared to the extra-tropics?

A

The tropics is characterized by deep convection, while extra-tropics is characterized by frontal systems.

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13
Q

What are the characteristics of High clouds?

A

Cold due to high altitude. Absorbed LWR is re-emitted at low temperatures and thus little LWR emitted to space, relatively transparant for sunlight: Warming effect.

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14
Q

What are the characteristics of Low clouds?

A

Very white, reflecting lots of SWR, relative warm so emit relatively much LWR: cooling effect

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15
Q

On average? What is the cloud effect? Cooling or warming? And how will this change with further global warming?

A

On average a cooling effect:
* Warming effect of high clouds expected to increase as high clouds will rise as the troposphere deepens. This results in an increase of cloud top and reface temperature.
* Cooling effect of low clouds expected to decrease. Reduction in mid- and low-level clouds. Shift of cloudy storm tracks poleward to regions with less sunlight meaning that less sunlight is reflected by clouds.

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16
Q

Why are there big uncertainties to do with cloud feedbacks?

A
  1. Clouds are a multi-scale problem
    - Cloud effect temperature distribution -> which affects winds patterns, which impact the impact of clouds on solar radiation.
  2. Clouds are tightly linked to heat balance & wind fields
17
Q

Explain the concept of arctic amplification.

A
  • Melting of sea ice -> lowered albedo -> increase of absorbed sunlight
18
Q
A