Genesis Quiz Flashcards

1
Q

Why do more tc’S develop in the northern hemisphere

A

Two additional genesis regions

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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;

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3
Q

Falling surface pressure

A

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

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4
Q

Tropical waves

A

Cyclonically curved, produce 70% of Atlantic busin formations

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5
Q

Non-tropical lows and thunderstorm complexes

A

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

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6
Q

Eddy flow

A

Turbulent flows develop spinning or swirling structures

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7
Q

Cyclonic wind flow / circulation

A
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8
Q

North Eddy flow

A

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

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9
Q

Eddy flow + background =

A

Resultant / combined flow

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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

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11
Q

What can assist development

A

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

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12
Q

What direction does most favorable near-zero shear come from

A

Any direction

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13
Q

_ Tropical waves develop - than - lows due to _

A

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

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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

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15
Q

Unfavorable westerly shear

A

Greater than 25 kts

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16
Q

Favorable tropical wave shear

A

Less than 10 kts

17
Q

Most favorable shear

A

Okts

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
Q

Useful Tc genesis environmental info can be obtained from the

A

Model output

26
Q

Madden-julien oscillation

A

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
Q

Positive phase upper level divergence created

A

More moist and lower Vws environment

28
Q

Convectively coupled Kelvin waves

A

Moderate scale gravity wave generated by deep convective burst

29
Q

Where do cckw waves develop?

A

Mountainous, elevated heat regions of Asian subcontinent and tropics

30
Q

Tc genesis enhanced ahead of cckw due to

A

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
Q

Cckw is limited to

A

7 degrees of equator (do not affect Tc genesis at higher lat )

32
Q

Cckw propagate

A

Eastward at 15-25 kts

33
Q

Mjo waves move

A

Eastward at less than 10 Kts

34
Q

Since cckws con move slower than, equal to, or faster than the Mjo

A

Locally de-amplify/degrade or amplify the effects of mjo

35
Q

Ingredients

A

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)