Horizontal Vorticity and Convection Flashcards

(80 cards)

1
Q

What are the three terms of the vertical vorticity equation?

A

1) advection
2) tilting
3) stretching

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2
Q

____ horizontal vorticity is generated at the leading edge of the cold pool, causing the cold pool to ___ along the surface

A

negative | causing cold pool to move (or spread) along the sfc

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3
Q

There is ___ pressure underneath cold air, which causes the cold air to accelerate _____

A

higher pressure | accelerate outward

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4
Q

The ambient air flows ___ the cold pool from the east, and is lifted at the ___ edge of the cold pool

A

flows toward the cold pool | lifted at the leading edge

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5
Q

In the absence of any other sources of horizontal vorticity, the lifted air is then guided ___ by the cold pool general circulation

A

guided rearward

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6
Q

In the absence of any generated ____ buoyancy produced by lifting (i.e. if the ambient air does not reach its LFC), the ambient air will not travel any farther above the cold air

A

positive buoyancy

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7
Q

When a cold pool has vertical wind shear, a positive environmental vorticity couples with negative vorticity at the edge of the gust front to develop an ____ ____

A

updraft jet

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8
Q

When the vertical wind shear vector points to the east, it signifies ____ horizontal vorticity

A

positive horizontal vorticity

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9
Q

If the magnitude of the positive horizontal vorticity associated with the ambient shear is the same as the magnitude of the negative horiz vorticity produced along the leading edge of cold air, then the air approaching the cold pool will tend to rise as a ____ ____ ___

A

vertically-oriented jet (updraft jet)

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10
Q

This produces ____ lifting at the leading edge of the cold air than from the case of no ambient vertical wind shear

A

deeper lifting

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11
Q

When the cold pool interacts with vertical wind shear, the ambient air has a much greater chance of being lifted to its ____

A

LFC

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12
Q

Evenly matched, but opposite horiz vorticity in the vorticity dipoles maintains ___ ____

A

deep updraft

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13
Q

The triggering of convective cells is favored along the ____ portion of a spreading cold pool

A

downshear

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14
Q

The strongest, most-lived convective systems will be produced when there is a strong ___ ___ ___ to balance the cold pool generated circulation

A

LL vertical wind shear

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15
Q

____ shear is important in how a storm’s updraft may evolve

A

environmental shear

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16
Q

How can you evaluate environmental wind shear?

A

plotting a hodograph

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17
Q

hodographs depict the _____ ____ of the horiz wind

A

vertical distribution

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18
Q

with hodographs, points are plotted as a function of ___ ____ and ____

A

wind direction and speed

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19
Q

with hodographs, each point represents the ____ wind at a specified elevation

A

horizontal wind

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20
Q

with a hodograph, wind vectors for each level are produced by connecting the hodograph’s ____ origin point with the ____ point

A

central origin with the plotted point

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21
Q

with hodographs, ____ shear vectors are produced by connecting two sequential points

A

layer shear vectors

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22
Q

The ___ ___ is the leading edge of the rain-cooled air in the planetary boundary layer

A

gust front

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23
Q

The gust front forms along ___ ___ of mesoscale domes of rain-cooled air that result from the amalgamation of ____-____ downdrafts from individual thunderstorm cells

A

leading edges | evaporatively-cooled

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24
Q

thunderstorm cold pools are associated with ___-___ and may actually be crudely analyzed on a synoptic surface chart

A

meso-highs (i.e. bubble highs)

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25
The gust front is a ____ discontinuity
density
26
___, ___ surface air flows outward from the meso-high
cooler, denser
27
High theta-e air is uplifted ___ the outward-flowing cold pool
above
28
New convection may form in association with this uplift if the lifted parcels can reach their ____
LFC (level of free convection)
29
____ ____ ___ can play a major role in determining how high a parcel may be lifted prior to reaching its LFC
environmental wind shear
30
gust front passage is characterized by what 5 things?
1) wind shift and abrupt increase in wind speed 2) abrupt temperature drop (most of the time) 3) sharp pressure rise 4) arc cloud (if BL is moist) 5) strong VWS
31
A gust front is a ____ feature
mesoscale
32
The ___ ___ ___ represents the gust front
low cloud line
33
air lifted upward by the gust front produces a ___ ___
shelf cloud
34
What three physical mechanisms control storm structure?
1) buoyancy processes 2) gust front processes 3) dynamic proceses
35
What are two examples of buoyancy processes?
1) lapse rate (CAPE) | 2) moisture stratification
36
Environmental VWS affects the ability of the gust front to trigger new ___ ____
convective elements
37
environmental VWS affects the ability of the updraft to interact with this environmental shear to produce enhanced, ___-___ storm structure
quasi-steady
38
for the storm, shear is relative to the ____ of the storm
motion
39
a storm travelling at the speed of the mean vector wind (MVW) automatically develops an enhanced ____ _____ into its updraft
inflow of BL air
40
the LL air has a strong component of ___ ___ toward the approaching storm
low-level
41
the magnitude of the inflow can be properly matched to the magnitude of the ____ updraft
buoyant updraft
42
in the absence of suitable shear, the inflow will be _____ to sustain the vigorous updraft that might result from large thermal instability
insufficient
43
what are 2 examples of gust front processes?
1) strength of cold pool | 2) strength of LL VWS
44
What are 2 examples of dynamic processes?
1) strength of 4-6 km AGL VWS 2) development of rotational (helical) updrafts and associated favorable vertical pressure gradients on the updraft flank
45
With an ordinary cell, ____ more important in maintaining updraft than ___ processes
buoyancy | dynamic
46
with supercells, ____ processes are more important than ____ in maintaining updraft
dynamic | buoyancy
47
vertical wind shear produces ____ ___ ___
horizontal vorticity tubes
48
horizontal vorticity tubes are incorporated into a ____ ____ and tilt ____
thunderstorm updraft | tilt vertically
49
the updraft begins to rotate in the same sense as the ____ ____ (cyclonic or anticyclonic)
vertical vorticity
50
updraft intensity is _____ within rotating cores
maximized
51
precipitation loading in updraft weakness between rotating cores produces a ____
downdraft
52
a downdraft separates the ____ updraft from the ___ updraft
cyclonic | anticyclonic
53
____ ____ occurs as each updraft sustains a separate storm cell
storm splitting
54
what is the first stage of storm splitting?
cyclonic and anticyclonic updrafts
55
what is the second stage of storm splitting?
the initial storm now splits into two
56
a rotating updraft can cause the storms motion to significantly deviate from the ___ ___ ___
mean vector wind (MVW)
57
with a cyclonically-rotating updraft, the Bernoulli effects produce ___ pressure on the ___ side of the cyclonic updraft in the mid-troposphere
low (high) | right (left)
58
with a cyclonically-rotating updraft, cyclonic storms move to the ____ of the MVW
right
59
with a cyclonically-rotating updraft, ___ supercells are favored within veering vertical wind profiles
SR supercells
60
cyclonically-rotating storms develop a ____ motion (right-mover) relative to MVW
rightward motion
61
with a anti-cyclonically-rotating updraft, the Bernoulli effects produce ____ pressure on the ____ side of the anticyclonic updraft in the mid-troposphere
low (high) | left (right)
62
with a anti-cyclonically-rotating updraft, anticyclonic storm moves to the ___ of the MVW (SL supercell)
left
63
with a no-shear ordinary cell, the gust front rapidly ____ the storm
outruns
64
with a no-shear ordinary cell, the storm is left totally _____ over BL cold pool
entrenched
65
with a moderate-shear multicell, the storm will move downshear at roughly the same speed as the _____ between the sfc and 6 km altitude AGL
MVW
66
with a moderate-shear multicell, new cell growth is enhanced along the ____ portion of the gust front
downshear
67
new cell growth along the downshear portion of the gust front ____ relative flow into the newly-developed cells
increases
68
new cell growth along the downshear portion of the GF ____ the length of time cells stay in the vicinity of strong LL convergence zone and associated lifting near GF
increases
69
for strong-shear supercells, rotation develops on the ___ ___ ___ ____ due to vertical tilting of pre-existing horizontal vorticity within the sheared flow
flank of the updraft
70
for strong-shear supercells, if the VWS extends through the middle-levels of the storm, the rotation dynamically induces a ____ pressure anomaly in the middle troposphere
negative (low) pressure
71
What does NPA stand for?
Negative pressure anomaly
72
the NPA produces a strong _______ pressure gradient which accelerates BL air violently upward
non-hydrostatic
73
rotating updrafts associated with mid-level NPA's are _____ and remain ____ after the storm moves into a more stable environment
long-lived | remain vigorous
74
rotation also causes storm motion to deviate from the ____
MVW
75
_____ shear favors storm splitting as NPA
unidirectional shear
76
____ shear forms at mid-levels within rotating updrafts on both right (cyclonic) and left (anticyclonic) side of original storm
unidirectional shear
77
____ shear has split cells that are nearly identical rotate in opposite directions
unidirectional shear
78
____ shear has a climatologically favored veering shear pattern
curved shear
79
___ shear has strongly veering winds that favor strongly right-moving cells with cyclonic rotation.
curved shear
80
With curved shear, left moving anticyclonic cells are ____ _____
not favored