Midterm Unit Two Flashcards

1
Q

Why are we interested in finding the value of ρ for moist air?

A

To assess if it is buoyant or not

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
2
Q

What is the law of partial pressure?

A

Partial pressure: pressure a gas would exert if it were alone in the same volume at the same temperature.

It states that the total pressure is the some of each partial pressure in a gas.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
3
Q

Suppose you have a hurricane. What does convergence/divergence of flow tell you about the vorticity and thus sense of rotation at each level.

A

Divergence generates vorticity.

Convergence->negative divergence->positive vorticity-> ccw : this is at low level so generation of cyclonic vorticity

Divergence->positive divergence->negative vorticity->cw

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
4
Q

What does pressure tendency at the surface’s equation state?

A

It states that the pressure tendency at the surface is the total convergence of mass into the atmospheric column

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
5
Q

What is T_v

A

It is the virtual temperature which is the temperature that the parcel would need for its density to be maintained if all moisture were removed with the pressure held constant

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
6
Q

Does a sample of dry air @ given T and p need to cool or warm to become as light as sample of moist air @ given T and p?

A

It need to have its temperature raise

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
7
Q

What is the saturation vapour pressure?

A

It is the pressure at which there is equilibrium between liquid water that evaporates from a water surface into the air layer and water vapour that condenses into liquid water.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
8
Q

How can we estimate the density of a saturated air mass?

A

For any pair of p,T values we can estimate the corresponding Tv and thus the density ρ_saturated in the above condition.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
9
Q

What is Td?

A

It is the temperature dew point. The temperature to which an airmass must be cooled @ constant pressure so that it becomes saturated

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
10
Q

What happens when we lower T to Td?

A

The air mass becomes saturated but w has not changed until saturation. RH does.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
11
Q

What is Tw?

A

It is the temperature of the air around an evaporative raindrop. It is the temperature that the air mass will acquire if water vapour is evaporated until the air mass reaches saturation.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
12
Q

What is the difference between cooling from T to Tw

and from T to Td

A

T -> Tw: Saturation through addition of water vapour. It is the absorption of latent heat by process of evaporation. Saturation achieved faster (1. External addition of water vapour 2. evaporative cooling)

T-Td: Saturation through cooling. It is externally imposed.

Td

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
13
Q

What are the conditions for a dry adiabatic lapse rate?

A

Hydrostatic atmosphere
No exchange of heat with the air surrounding it
Without reaching saturation at any point

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
14
Q

What is the internal energy of an air-mass?

A

It is the microscopic energy that an air mass has due to the potential E and KE of its molecules/atoms.

T increases:

  • increase of KE so U
  • change in phase so PE so U
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
15
Q

What is cv?

A

It is the specific heat cv: the amount of heat dq required to be given to 1kg of air for its T to increase by amount dT with its volume kept constant.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
16
Q

what is cp?

A

It is the amount of heat dq required to be given to 1kg of air for its temperature to increase by amount dT with pressure kept constant

17
Q

What is enthalpy?

A

It is the sum of the internal energy of a system and the product of the pressure times the volume.

18
Q

What is the Static energy?

A

It is the sum of enthalpy and geopotential of an air mass.

19
Q

What does conservation of static energy implies

A

It implies that the airmass moves without exchanging heat with the environment. The atmospheric column is in hydrostatic balance and there is no change of phase as it is moving.

20
Q

What is an adiabatic displacement ?

A

It is when the Static energy is kept constant so no exchange of heat between the air mass and the environment.

21
Q

What is an adiabatic transformation ?

A

It refers to the changes in the properties p,V,T during an adiabatic displacement.

22
Q

What is an air parcel?

A

It is when an air mass moves and conserves its static energy.

23
Q

Compare the dry adiabatic lapse rate to the mean environmental lapse rate.

A

A parcel displaced in a dry adiabatic manner has its temperature T falling at a faster rate than the environment. The parcel quickly becomes colder so it is more dense and heavier than the air surrounding it: it sinks down to the surface.

24
Q

What is the potential temperature associated with?

A

It is associated with dry adiabatic motion.

25
Q

What is the potential temperature?

A

It is the temperature T that an unsaturated parcel would have it if were moved (compressed/expanded) adiabatically from its present p to the reference pressure (1000hPa) in a hydrostatic atmosphere.

26
Q

What insights does the potential temperature give?

A

Knowing θ we can generate (p,T) pairs which can be compared to temperature of environmental air @ the different pressure layers. Will tell if the parcel is lighter/buoyant->can assess the stability of the air-mass with respect to the air above/below.

27
Q

How does θ vary with height in the atmosphere?

A

It increases with height.

  • gradient of θ from poles towards Equator
  • meridional θ gradient can be seen @ all altitudes.
28
Q

What is adiabatic heating?

A

When there is no change in the static energy of the parcel. I.e. when the parcel is heated (internal energy increased) it results in the redistribution of energy within the parcel.

29
Q

What is diabatic heating?

Give the three types of heating.

A

When there is exchange of energy between air parcel and the environment. (Gain/loss of dq).
Hr = Radiative heating. heat transmission through electromagnetic waves (IR)
Sh = Sensible heating. Heating due to conduction (through contact with adjacent warmer/cooler surface).
LHR = Latent heat release. Heat release/absorbed due to change of phase of water vapour
-LHR>0:condensation.
-LHR<0:evaporation.

30
Q

What happens when assumed that all LHR stays in the parcel:

  • condensation?
  • evaporation?
A

condensation: decrease in mixing ratio because of condensation and increase in the temperature
evaporation: increase in mixing ration because of evaporation and decrease in the temperature.

31
Q

What is the moist static energy Se?

How is it conserved?

A

It is the sum of a parcels enthalpy (associated with U and work done), the potential energy and the latent energy.

It is conserved if the parcel is not subjected to radiation heating/cooling due to convection.

32
Q

Implication of Se conservation.

  • before saturation as it is ascending?
  • after saturation as it is ascending?

Conclusion?

A
  • Mixing ratio doesn’t change so dw=0. Increase of z leads to cooling.
  • Condensation occurs so dw<0. The parcel is heated since LHR by amount dT. Heating makes it more buoyant so it moves upwards: dz>0
  • > the increase of z leads to adiabatic expansion which cools the parcel so more condensation so dw<0.
  • > dT and dw compensate for increase in dz.

Energy is continuously redistributed between cpT, geopotential and Lw.

33
Q

What is moist/saturated adiabatic displacement?

A

The parcel does not exchange energy with the environment as it moves in the hydrostatic atmosphere, even as saturation/evaporation happens

34
Q

What does pseudoadiabatic refers to?

A

It refers to saturated adiabatic displacement because the last is an approximation (there is always some energy exchange with the environment and condensed water falls out as precipitation.