Radiation and Energy Balance, Pt.2 Flashcards

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1
Q

What is Sensible Heat?

A

When we measure the temperature of something with a thermometer, we are measuring its sensible heat

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2
Q

Sensible heat is a form of __________ energy.

A

Kinetic

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3
Q

Why is sensible heat a form of kinetic energy?

A

Since the temperature of a system is really a measure of how fast its atoms or molecules are moving/vibrating, on average.

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4
Q

True or False: Sensible heat can’t be felt.

A

False, it can be sensed.

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5
Q

Define Sensible Heat Transfer:

A

When two bodies of different temperatures are in contact with each other, the sensible heat will flow from the hotter body to the colder body, by the process of conduction.

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6
Q

Give an example of Sensible heat transfer:

A

Ex, our skin with the air, if the air around us is warm, sensible heat flowing from the air to our skin, through conduction.

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7
Q

In the process of Sensible Heat Transfer, one body will ______ and the other will ______, until they reach ____________ __________.

A

cool, warm, and thermal equilibrium.

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8
Q

_____________: transfers heat vertically (up or down) in turbulent eddies.

A

Convection

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9
Q

_____________: transfers heat horizontally (advective process)

A

Advection

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10
Q

What are the three forms of Latent Heat?

A

Liquid
Gas
Solid

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11
Q

Define Latent Heat:

A

Latent heat is the energy gained or lost when a substance changes phases. Energy that is added or removed to change the state of the substance, without changing its temperature.

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12
Q

True or False: Latent Heat can be sensed.

A

False, it cannot be sensed.

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13
Q

What physical change occurs when latent heat is released or absorbed?

A

Between ice and water vapour.

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14
Q

With latent heat, when heat is released from the water, the environment around it is ________.

A

warmed

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15
Q

With latent heat, When heat is absorbed by the water, the environment around it is _________.

A

cooled

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16
Q

Why does temperature not increase during the phase of melting ice to liquid?

A

That is because the energy is being used to break the bonds, once they’re broken, then temperature begins to rise, this is latent heat. Latent heat is the process of changing form.

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17
Q

What is the latent heat for melting and freezing?

A

334 joules/gram

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18
Q

What is the latent heat for vaporization and condensation?

A

2260 joules/gram

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19
Q

__________ is the process of skipping all phases and moving from gas to solid.

A

Deposition

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20
Q

___________ is the process of skipping all phases and moving from solid to a gas.

A

Sublimation

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21
Q

Quiz or Exam will include a question like this: To test your knowledge of this concept, try to think about what happens when we blow on a bowl of soup. Why might this work to cool it down? What processes are at play here?

A

more complicated than we think. What is going on at the surface of the liquid, what is floating above the bowl of soup. Where does evaporation, latent heat of evaporation, condensation (if applicable), convection/advection, play a role??

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22
Q

Q: If the boiling point of water is 100o C, why do puddles disappear when it is not that hot outside? Why do your bath towels dry when you hang them up? And why does snow/ice disappear when it is well below 0oC?

A

The temperature of a system is an indication of the average kinetic energy of all molecules in that system. Individual molecules can get enough energy to change the phase (even if the whole system is not at that temperature), by sensible heat transfer from adjacent molecules, or by absorption of radiation. When we measure the temp, it is an average kinetic energy.

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23
Q

What are the three processes of heat transfer?

A

Sensible heat transfer
Latent heat transfer
Radiative heat transfer

24
Q

________________: energy moves by conduction from cold masses to warm masses, and perhaps by convection/advection.

A

Sensible heat transfer

25
Q

_______________: the water that turned to gas escapes, taking its latent heat of vaporization with it. Wherever the gas later condenses, the latent heat is liberated to cause warming.

A

Latent heat transfer

26
Q

______________: radiation is emitted to cause cooling, or it is absorbed to cause warming. Incoming solar radiation warms things up, while the earth emits its longwave radiation to cool it.

A

Radiative heat transfer

27
Q

True or False: Greenhouse gases are important for earth to regulate temperature, a delicate balance.

A

True

28
Q

True or False: GHGs in the atmosphere are not reflecting longwave

A

True

29
Q

The presence or absence of clouds may make a __% difference in the amount of energy that reaches the surface

A

75

30
Q

What two way do clouds impact earth’s radiation budget?

A

By reflecting and absorbing

31
Q

How do clouds reflect?

A

Reflect incoming solar radiation from above (high albedo), can reflect shortwave insolation or absorb and reradiate long wave radiation back toward earth.

32
Q

Do clouds have a high or low albedo?

A

High

33
Q

How do clouds absorb?

A

Absorb and re-radiate outgoing longwave radiation back towards earth.
-Some longwave energy returns to space and some toward the surface.

34
Q

What types of energy fluxes must we examined when explaining the variation of climate across the earths surface?

A

Radiative Flux
Non-Radiative Flux

35
Q

What does Flux mean?

A

Flux = Flow of Energy, transfers of energy

36
Q

What does Net mean?

A

Net = incoming – outgoing

37
Q

What does it mean if a Net is negative or positive?

A

Negative = more going out than coming in. Positive = more coming in than going out.

38
Q

What does Annual Mean Insolation and Earth’s Surface consider?

A

Considers the effect of the atmosphere, including clouds
Note the relatively low values in the equatorial latitudes. Over the year, how much insolation the earth is receiving as a whole.

39
Q

How is Annual Mean Insolation of Earths surface measured?

A

Watts/m2

40
Q

Why is the Annual mean insolation of earths surface higher in desert areas?

A

little cloud cover, dry area, no water to work with

41
Q

What is the The average annual planetary albedo?

A

(the thing that drives outgoing shortwave radiation)

42
Q

Where is annual planetary albedo lower?

A

Clear skies, oceans, forest, and vegetation.

43
Q

Where is the average annual surface albedo generally higher?

A

ice, snow, and cloudy areas.

44
Q

________________ : longwave radiation emitted downwards to the surface by the atmosphere and clouds.

A

Incoming terrestrial radiation

45
Q

_________________: long wave radiation emitted upwards by the surface.

A

Outgoing terrestrial radiation

46
Q

Where is terrestrial radiation warmer?

A

It’s always positive in the low latitudes.

47
Q

Where does terrestrial radiation fluctuate?

A

In the midlatitudes and polar latitudes it’s positive in the summer and negative in the winter. `

48
Q

What does Energy Budget by Latitude mean?

A

In order to strike a balance, energy needs to flow (or be transferred) from the low latitudes to the high latitudes.

49
Q

How is Net Radiation at Surface calculated?

A

Net R = (SW ↓+LW ↓) − (SW ↑+LW ↑)

50
Q

What would happen if we didn’t have GHG’s?

A

Greenhouse gases regulating earth’s temperature, if they weren’t there, we would lose all outgoing terrestrial radiation, with huge temperature swings throughout the day. The earth would be too cold, inhabitable for life.

51
Q

_________________: is the back-and-forth transfer between air and surface in turbulent eddies through convection and conduction where T is the land surface temperature and Tair is the air temperature, way of moving energy.

A

Sensible Heat Flux (SE)

52
Q

________________: is the energy that is stored in water vapor as water evaporates. Water absorbs large quantities of this latent heat as it changes state to water vapor, thus removing this heat energy from the surface. As we saw, this energy is transported elsewhere and released when the water condenses once again.

A

Latent Heat Flux (LE)

53
Q

________________: is the energy that flows into or out of the ground or water surface by conduction where T is the surface temperature and Td is the deep soil temperature.

A

Ground Heat Flux (G)

54
Q

What is the urban heat island?

A

Urban areas may regularly reach temperatures as much as 6 degrees warmer than surrounding areas (urban heat island).

55
Q

What are some physical characteristics of an Urban Heat Island?

A

similar to a desert location, High sensible heat (warming the atmosphere), due to little vegetation (Low latent heat), dark surfaces, pollution, transportation (Heat byproducts), etc…