Met 421 Exam 1 Flashcards

1
Q

Scale Analysis

A
W = 10 ^-2 m/s
U = 10 m/s
L = 10 ^ 6 m
F = 10 ^ -4
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
2
Q

3 characteristics for Potential Temp

A
  • Temp parcel would have if it was compressed or expanded to 1000mb
  • Vertical temp profile related to static stability
  • Helps locate fronts especially over uneven terrains
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
3
Q

Potential Temp and Stability

A

Change in Pot. Temp over time
> 0 : Stable
= 0 : Neutral
< 0 : Unstable

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

Why does geostrophic veering wind require waa?

A

A veering geostrophic wind requires flow from warmer to colder thickness.

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

Veering

A
  • Clockwise

- WAA

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

Backing

A
  • Counter Clockwise

- CAA

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

Competing Effects of Rossby Waves

A
  • Advection of relative vorticity moving system eastward

- Advection of planetary vorticity moving system westward.

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

What Causes Rossby Waves?

A
  • Terrain
  • Latent heat
  • Advection
  • Downstream development
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
9
Q

Forecast Process

A
  • Observe
  • Analyze
  • Diagnosis
  • Prognosis
  • Communicate
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
10
Q

Why is subjective analysis important?

A
  • Station data is very valuable in assessing current conditions
  • Better locate locations of fronts and systems
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
11
Q

Ingredient based forecasting for winter weather

A
  • Forcing for ascent
  • Moisture
  • Instability
  • Temperature
  • Precipitation Efficiency
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
12
Q

Methods of estimating vertical motion

A
  • Divergence aloft

- Vertical temperature profile

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

What does QG theory do?

A
  • Helps understand the 3-D synoptic scale weather systems
  • Reveals how hydrostatic and geostrophic balance constrain and simplify atmospheric motions
  • Physical insight into forcing of vertical motions
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
14
Q

Assumptions for QG theory

A
  • Rossby number less than 0.10
  • Hydrostatic balance
  • Horizaontally uniform static stability
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
15
Q

Q-G Omega Equation Term A

A
  • 3-D Laplacian of vertical motion
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
16
Q

Q-G Omega Equation Term B

A
  • Differential geostrophic vorticity advection by geostrophic wind
17
Q

Q-G Omega Equation Term C

A
  • Laplacian of temperature advection by geostrophic wind
18
Q

What is the Q-G Omega equation telling us?

A

Vertical motion is a result of vorticity advection and thermal advection

19
Q

Q-G Omega Upward Motion

A

Upward Motion

  • Increasing PVA
  • WAA
20
Q

Q-G Omega Downward Motion

A

Downward Motion

  • Increasing NVA
  • CAA
21
Q

Q-G Geopotential Tendency Equation: HEIGHT FALLS

A

Height Falls

  • PVA
  • Increasing WAA
22
Q

Q-G Geopotential Tendency Equation HEIGHT RISES

A

Height Rises

  • NVA
  • Increasing CAA
23
Q

Prognostic vs Diagnostic

A

Diagnostic

  • Spatial distribution at a given time
  • Vertical motion field

Prognostic

  • Local rate of change with time
  • Vorticity and Temperature advection
24
Q

Vertical Motion (Rising air vs Sinking air)

A

Rising Air
- Clouds and Precip

Sinking Air
- Clear skies

25
Q

Q Vectors

A
  • Converging: Rising motion
  • Diverging: Sinking motion
  • Points toward warm air: Frontogenesis
  • Parallel to isotherms/thickness: Thermal advection