Track & Intensity Forecasting Flashcards

1
Q

Tropical Cyclone Motion

A

“A cork in a stream”

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2
Q

Problem with Tropical Cyclone Motion

A

The “Stream Flow” or steering currents are not static, they are dynamic or always changing

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3
Q

To a first- order approximation TC motion is governed by

A

Conservation of relative vorticity

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4
Q

How does the vortex move

A

With the large-scale steering flow

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5
Q

If a circulation has positive absolute angular momentum and it converges or contracts (diverges or expands) the it________ (slower) in the __________(negative)_________, and it will _______(lose) __________ absolute_______.

A

Must spin faster, positive, direction, gain, cyclonic, vorticity

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6
Q

Do changes in TC inner-core structure have any influence on the future track?

A

No there’s little influence

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7
Q

The Beta Effect or Beta Drift……..

A

Induces steering of 2-4 kt to the northwest

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8
Q

The circulation of a TC, combined with the North-South variation of the Coriolis parameter, induces asymmetries know as Beta Gyres. These Beta Gyres produce a net steering current across the TC generally toward the northwest at a few knots

A

Beta Drift or Beta Effect

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9
Q

Climatology and Persistence Model (CLIPER)

A

No longer provides useful operational guidance, but is used as a benchmark for other models and the official forecast. If a model has a lower mean errors than CLIPER it is said to be ‘skillful’

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10
Q

The Beta and Advection Model (BAM): A class of simple _______ that utilize vertically averaged horizontal winds from the GFS to compute TC Trajectories. These trajectories include a ________ to account for the _____ of the earth’s __________(beta advection)

A

Trajectory models, correction term, impact

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11
Q

BAM medium or BAMM/TABM (840-400 mb)

A

Default track model in the SHIPS intensity forecast model

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12
Q

Global Models have _______________ to define the TC ___________ (eye and eye wall structure)
(Inner-core changes have virtually no effect on track)

A

Inadequate resolution, inner core

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13
Q

Global models have no ___________conditions an therefore should have better ________ at longer ranges than the limites-area models

A

Lateral boundary, performance

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14
Q

Limited-Area (Regional) models performance _________ at ________ ranges

A

Degrades, longer

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15
Q

There is a ________ difference between _________ and __________ forecasts

A

HUGE, landfall, non-landfall

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16
Q

The 2022 hurricane season was _____ than _____ to forecast at 96 and 120 h due ro the 2022 CLIPER5 errors being ________ than ______

A

Easier, average, lower, average

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17
Q

Since 2016, NHC track forecast track errors……..

A

Have not changed

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18
Q

Since 2016, NHC track forecast skill has basically

A

Not changed

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19
Q

The ______(weaker) the TC, the ______ (worse) are NHC’s track forecasts at _____________

A

Stronger, better, all forecast times

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20
Q

Often the _________ models are __________ formed from an ensemble of good performing _________ models

A

Most successful, consensus aids, individual

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21
Q

Dynamical model consensus is an excellent……

A

First guess

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22
Q

Continuity dictates that it must be considered in…….

A

The view of previous official forecasts

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23
Q

Try to asses what so that you can understand and perhaps evaluate the model solutions?

A

Steering influences

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24
Q

Compare the models’ ________ of the environments features, not just the __________

A

Forecast, TC tracks

25
Q

Evaluate the _________ of the ____ in the model fields. Unrealistic TC can affect the ______ of a successful forecast.

A

Initialization, TC, likelihood

26
Q

Spread of ______ can dictate forecaster ________

A

Models, confidence

27
Q

Sometimes the forecaster might want to exclude certain models from a “selective consensus”……. If _________ amoung the models can be ________

A

Discrepancies, resolved

28
Q

Previous official forecast exerts a strong _______ on the current forecast

A

Constraint

29
Q

NO_________(1)

A

Windshield Wipering

30
Q

NO…..(2)

A

Tromboning

31
Q

‘Smart’ models have to _______ during the course of a new seasons and, thus, can be _________early

A

Re-learn, unreliable

32
Q

Accurate estimate of ________ and _____ is extremely important

A

Initial location, motion

33
Q

TC forecasters ________ and _________ these wobbles in order to mitigate large track forecasts errors

A

Must anticipate, smooth through

34
Q

Initial motion estimates should ____ reflect ______ track wobbles that will not persist

A

Not, short-term

35
Q

NHC philosophy is that it is better to ___ events a little bit than to be going ________ with analyses of forecasts

A

Lag, back and forth

36
Q

Intensity Output initial conditions: tropopause:

A

-70 deg C

37
Q

Minimum attainable surface pressure (mb) as a function of surface air temp (Ts) and weighted mean outflow temperature (Tout) assuming ambient surface pressure of 1015 mb, ambient surface RH of 80% 20 deg latitude, outer radius of 500 km and __________

A

No vertical wind shear

38
Q

The _____ the ______ temperature and the ____ the surface _______ temperature the _________ a hurricane can become

A

Colder, outflow, warmer, inflow, more intense

39
Q

We can only sample a _____ of the TC each observation has strengths and weaknesses we want a value that is __________ of the TC’s mean circulation

A

Part, representative

40
Q

Always weigh the more accurate _______ data over remotely sensed data

A

In situ

41
Q

Sea Surface Temperatures: _______(cool) SSTs generally produce _______(weaker) hurricanes

A

Warm, stronger

42
Q

Ocean Heat Content: the greater the depth, more available heat can be potentially converted to energy and also_________

A

Prevent cold upwelling

43
Q

_______ in the low-levels results in a ________ and ________

A

Drier Air, Higher LCL, Higher LFC

44
Q

If lifting mechanism is weak, then low-level air parcels may not reach the LFC and release the conditional instability resulting in ___________

A

No deep convection

45
Q

Tropical cyclone intensity change can be caused by inner-core processes such as

A

Eyewall replacement cycles (ERC) or concentric eyewalls

46
Q

In major hurricanes, we often see an _________ eye wall occur at larger distances from the center than the radius of the original eye wall

A

Outer concentric

47
Q

The occurrence of ERC’s appears to be at least partly related to the _______ and _______(RMW)

A

Hurricane’s intensity, radius of maximum winds

48
Q

The more intense hurricane and smaller the RMW, the more likely that an ERC will occur; this is due to ________ winds in the ________ flowing ______

A

Supergradient, inner eye wall, outward

49
Q

When this outer eye wall becomes ________, weakening ________ occurs

A

Dominant, invariably

50
Q

Winds weaken over land due to lack of………

A

Latent heat and increased friction

51
Q

Terrain and Higher Elevations: These wind speeds are not considered to be

A

Representative of a TC’s actual tangential winds

52
Q

SHIPS forecasts are _______ to interpret

A

Easier

53
Q

Experimental tests using GOES lightning in the _________ in RII show improved skill

A

Inner-core region

54
Q

Lightning is a _____ for ____ strength owing to lightning generation mechanisms

A

Proxy, updrafts

55
Q

Problems with representation of shear; regional models such as HWRF, HMON, HAFS-A/-B models are

A

To shear resistant

56
Q

Dynamic models are more _______ for basin-wide ______ forecasts

A

Skillful, intensity

57
Q

Statistical methods more _______ skillful for identifying ________

A

Generally, RI cases

58
Q

Extreme events are almost

A

Never forecasted