Genesis Quiz Flashcards

1
Q

Why do more tc’S develop in the northern hemisphere

A

Two additional genesis regions

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

Large -scale conditions associated with Tc formation

A

Upper-tropospheric anticyclone outflow; enhanced lower tropospheric relative vorticity; appearance of curved banding features in deep connection;

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

Falling surface pressure

A

Greater than or equal to 3mb in a 24 hr period

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

Tropical waves

A

Cyclonically curved, produce 70% of Atlantic busin formations

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

Non-tropical lows and thunderstorm complexes

A

Frequent precursor of subtropical cyclones which can evolve into Tc, strong upper level divergence

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

Eddy flow

A

Turbulent flows develop spinning or swirling structures

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

Cyclonic wind flow / circulation

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

North Eddy flow

A

Superimposed onto the easterly background flow, an open wave instead of closed cyclonic circulation System

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

Eddy flow + background =

A

Resultant / combined flow

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

Why do open tropical waves develop slower than closed lows?

A

Asymmetrical low-level convergence and convection, convection displaced from lowest pressure axis

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

What can assist development

A

Light to moderate easterly deep-layer vertical wind shear, pushes convection/latent heat over wave axis

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

What direction does most favorable near-zero shear come from

A

Any direction

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

_ Tropical waves develop - than - lows due to _

A

Open; slower; close; asymmetrical low level convergence and convection

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

What does low / no vertical wind shear do?

A

Allows vortex column to remain vertical, creating ideal conditions for latent heat released to be concentrated near surface pressure minimum

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
15
Q

Unfavorable westerly shear

A

Greater than 25 kts

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

Favorable tropical wave shear

A

Less than 10 kts

17
Q

Most favorable shear

18
Q

Why is a most mid level > 70 % Rh so important in order for Tc genesis to occur

A

Prevent the development of cold downdrafts created by rain evaporating into dry mid-level air

19
Q

Entrainment of moist mid level air

A

Feed convective updrafts with nigh theta -E air, enhances updrafts

20
Q

Entrainment of dry mid-level air

A

Creates evaporatively cooled downdrafts, which spread out at the ocean surface, disrupting or even destroying the surface wind field

21
Q

Dry slot penetration of inner core will

A

Erode central deep connection & slow down the genesis process

22
Q

Why do early development of Dolly support Tc genesis?

A

Merger of mult lower to middle troposphere mesoscale

23
Q

Ships

A

Statistical hurricane intensity precipitation scheme

24
Q

What is the ships model

A

Statistical - dynamical model that was developed for forecasting the intensity existing tropical cyclones not tropical disturbances

25
Useful Tc genesis environmental info can be obtained from the
Model output
26
Madden-julien oscillation
Large scale global gravity wave generated by deep connection that develops and persist over mountainous, elevated heat regions of Asian subcontinent and Asian tropics
27
Positive phase upper level divergence created
More moist and lower Vws environment
28
Convectively coupled Kelvin waves
Moderate scale gravity wave generated by deep convective burst
29
Where do cckw waves develop?
Mountainous, elevated heat regions of Asian subcontinent and tropics
30
Tc genesis enhanced ahead of cckw due to
Increased upper-level divergence E weakening of low-level easterlies and/or an increase in low level westerlies which increases low level cyclonic vorticity
31
Cckw is limited to
7 degrees of equator (do not affect Tc genesis at higher lat )
32
Cckw propagate
Eastward at 15-25 kts
33
Mjo waves move
Eastward at less than 10 Kts
34
Since cckws con move slower than, equal to, or faster than the Mjo
Locally de-amplify/degrade or amplify the effects of mjo
35
Ingredients
Pre existing disturbance, warm sea surface temps, little change in the wind speed and/or direction with height, nigh values of tropospheric moisture, unstable atmosphere, location several degrees latitude away from the equator (coriolisspin)