Lecture 05 Flashcards

(36 cards)

1
Q

According to the energy law; the energy received and emitted should be 255 K, but it is 288 K

A

Missing Kelvins because of the atmosphere

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2
Q

The Earth’s energy received and emitted without its atmosphere

A

255 K (-18 Celsius)

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3
Q

The Earth’s energy received and emitted with its atmosphere

A

288 K (-15 Celsius)

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4
Q

Why is the Earth’s energy colder than it should be?

A

Because of the greenhouse effect: Greenhouse gases (H₂O vapor, CO₂, CH₄, etc.) and clouds absorb some of the infrared radiation the surface emits and re-radiate part of it back downward.
This slows the loss of heat to space, so the surface must warm until outgoing infrared at the top of the atmosphere balances incoming solar energy.

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5
Q

Not a single uniform structure; thin layer of gas (N2 O2 CO2) preventing all solar energy from directly hitting the surface of the planet

A

The atmosphere

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6
Q

What’s the first layer of the atmosphere (where weather takes place)

A

The troposphere

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7
Q

What’s the second layer of the atmosphere?

A

Stratosphere

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8
Q

What’s the third layer of the atmosphere?

A

Mesosphere

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9
Q

How many layers in total does the atmosphere have?

A

4 layers

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10
Q

Of what is the atmosphere composed of ?

A

Numerous gases (N2, O2, CO2)-Clouds-Dust-Microplastic, it has a lot of physical particles to interfere with wavelengths of energy moving from the sun to the surface of the planet

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11
Q

Processes which interact with heat transfer in the atmosphere help to create

A

Global energy balance

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12
Q

The solar light entering the atmosphere collide with air, dust and cloud particles, this deflects light in all directions (short wavelength is the most effective for this process–> that’s why the sky is blue)

A

Scattering

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13
Q

When is there more scattering and longer wavelengths of light that scatters as well (longest wavelengths appear red)

A

At the end or the beginning of the day during sunset or sunrise

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14
Q

How much solar radiation is impacted by scattering as shortwave radiation

A

23%

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15
Q

Solar light entering the atmosphere collide with clouds and the terrestrial surface, it goes back to the source to where the energy source came from, it doesn’t move in all direction

A

Reflection

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16
Q

Related to reflection, it is the reflectance of a surface and how much of a given energy source will be reflected back (instead of absorbed)

17
Q

The more visible light is absorbed (low albedo) when…

A

The object is darker

18
Q

The more visible light is reflected (high albedo) when…

A

The object is lighter

19
Q

Which of these two has a higher albedo : snow or water ?

20
Q

How much energy is directly reflected by surface albedo?

21
Q

Knowing that energy is sent back into space how much in percentage is sent back combining albedo and scattering?

22
Q

Process where kinetic energy in the form of electromagnetic radiation is soaked up by colder substances in the atmosphere and the terrestrial surface

23
Q

What is energy absorbed by?

A

Clouds, terrestrial surface and atmosphere

24
Q

What’s in percentage, the total energy absorbed by terrestrial surfaces?

25
What's the total energy solar absorbed by atmospheric reservoirs?
20%
26
Can energy be created or destroyed?
No it is only transformed
27
The energetic shortwave radiation released by the sun is absorbed by cooler objects on Earth, it depends on the object temperature
Emission
28
Objects that are better at absorbing some wavelengths over others
Selective absorbers
29
Longwave absorbing gases trap some of the heat that the planet would emit back into space, these gases are...
Greenhouse gases
30
Re-releasing energy into space or back to the planet's surface for multiple times as long as the cycle can continue, it is the recycling of energy through re-emission, GHGs are helpful in that case
Re-emission
31
What are low clouds practical for?
They are useful for planetary cooling by reflecting high levels of incoming shortwave radiation, they re-emit more infrared energy back into space
32
What are high clouds practical for?
They tend to be thin, they are useful for planetary warming, it allows shortwave radiation to be absorbed at the planet surface
33
The energy that moves directly from the molecules of the ground to molecules in the air directly touching the ground, it is the transfer of energy between two substances which are in direct contact
Conduction
34
Energy that moves through warming air in the atmosphere, the air is warmed through conduction from terrestrial surfaces (the lighter air rises)
Convection
35
The energy taken in and released by water as it transitions through different states of matter, this energy is taken with water to water vapor, it releases energy through "the magic of evaporation"
Latent heat transfer
36
Why is the solar energy distributed over a greater area at the bottom of the planet and more concentrated at the equator?
Because of its spheric shape; the energy then depends on where we are positioned on the planet