Final New Section Flashcards

1
Q

Cold core system

A

Cold- core anticyclone- actually a dome of continental polar or Arctic air and, depending on the specific type of air mass is labeled either a polar or Arctic high. Products of extreme radiational cooling over the often snow-covered continental interior of North America well north of the polar front.
SHALLOW SYSTEMS- clockwise circulation weakens with altitude and frequently reverses direction aloft.. Hence a cold trough overlies a cold anticyclone.

They exert the highest surface pressures in winter, when is colder and more dense

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

What/where is the ITCZ

A

Intertropical convergence zone

Stimulates thunderstorm activity and its north-south seasonal shifts are responsible for the seasonal variations in precipitation in portions of the tropics

FOLLOWS THE SUN, moving northward in the northern hemisphere spring and southward in the northern hemisphere autumn. The rainy season is summer (high sun) and the dry season is winter (low sun).

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

What is a front?

A

A narrow zone of transition between air masses of contrasting air density, that is different temperature, humidity or both. Fronts are classified as stationary, warm or occluded

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

know meridional/zonal flows and what they mean

A

Zonal flow pattern- the westerlies blow almost directly from west to east nearly parallel to latitude lines, with only w weak meridional component. The north-south exchange of air masses is minimal. Cold air masses stay north and warm air masses remain south.

Meridional flow pattern- the westerlies exhibit considerable amplitude and flow in a pattern of deep troughs and sharp ridges. Masses of cold air surge southward and warm air streams northward. Greater west to east temperature contrasts develop over the United States and southern Canada. Where contrasting air masses collide, warm air overrides cold air, and the stage is set for the development of extra tropical cyclones that are then steered by the westerlies.

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

understand the polar jet and it’s seasonal variations (meridional vs. zonal)

A

Produces strong vertical wind shear that maintains a vigorous updraft and favors great vertical development of thunderstorm cells. The jet contributes to a stratification of air that increases the potential instability of the troposphere.
It causes dry air to subside over a surface layer of maritime tropical air. This produces a layering of air that sets the stage for explosive convection and development of severe thunderstorm cells

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

what is a jet streak/it’s quadrants/ divergence and convergence associated with a jet streak

A

An area of accelerated air flow within a jet stream; the wind may strengthen by as much s an additional 100km per hr. They occur where surface horizontal temperature gradients are particularly steep and play an important role in the generation and maintenance of synoptic-scale Cyclones. The strongest jet streaks develop during winter in the polar front jet stream along the east coasts of North America and Asia.

Play an important role in the generation and maintenance of extra tropical cyclones. Air flowing through a jet streak changes speed and direction.. These changes induce a pattern of horizontal divergence and horizontal converfence.

4 quadrants- left-rear, right- rear, left- front, and right- front,
Horizontal divergence occurs in both the left- front and right-rear quadrants and horizontal convergence takes place in both the right- front and the left-rear,

Provides upper air support for a cyclone by contributing horizontal divergence aloft.

Strongest horizontal divergence occurs in the left-front quadrant- so it’s under this sector of the jet streak that a cyclone typically has the best chance of developing.

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

what is upwelling

A

Ekman transport moves surface waters away from the coast, those waters are replaced by water that wells up from below in a process.

Responsible for the tongue of relatively cool surface waters along the equator in the eastern tropical pacific. Near the equator the northeast trade winds of the northern hemisphere converge with the southeast trade winds of Southern Hemisphere.

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

Maritime- very warm and humid, source regions are tropical and subtropical seas. Keeps properties year round and is responsible for oppressive summer heat and humidity east of the Rocky.

Continental- winter air is cold. Source is ground and is usually snow covered. Short daylight. Solar radiation is weak. Radiational cooling is extreme.

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

know the clouds progression as a warm front approaches

A

Cirrus-cirrostratus- altostratus- nimbostratus- and stratus

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

signs of warm air advection (clouds)/where is typically occurs (which side of a ridge vs trough)

A
  1. High cirrus clouds in the western sky.

Behind (west of a ridge)

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

know how frontal precipitation sets up

-

A

When air cools sufficiently.

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

differential heating of land vs water

-

A

Lake breeze- a relatively cool surface wind directed from a large lake toward land in response to differential heating between land and water daylight

Sea breeze-

Cool wind directed from water onto land

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

what/where is a Chinook wind

-

A

Air that is adiabatically compressed as it is drawn down the leeward side of a mountain range. As a consequence the air is warm and dry causing rapid temperature rises and reduction in snow cover

Strong and gusty

Rocky Mountains

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

Towering cumulus stage.- cumulus clouds form verity calmly and laterally. Surge. Forced convection
UPDRAFT- saturated air streams upward. Keeps water suspended

Mature stage- precipitation reaches the surface.
DOWNDRAFT- the precip pulls the air down.
The downdraft air resembles a cold front and is called a gust front

Dissipating stage- subsiding air replaces the updraft throughout the cloud effectively cutting off the supply of moisture delivered by the updraft. The air warms the humidity decreases precip ends no clouds vaporize

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

higher tops mean

A

more severe thunderstorms

The greater the altitude of the top the more severe the storm.

Magnitude of the vertical wind shear

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

what is a squall line … where it forms

A

An elongated cluster of thunderstorm cells that is accompanied by a continuous gust front at the lines leading edge. It is most likely to develop in the warm southeast sector of a mature extra tropical cyclone ahead of and parallel to the cold front.

Their cells are usually more intense.

As it surges forward warm humid air is lifted and forced into the updraft located at the leading edge of the squall line.

Dry line

17
Q

what is a mesoscale convective complex

-

A

Is nearly circular cluster of many interacting thunderstorm cells covering an area that may be a thousand times larger than that of a single isolated thunderstorm cell. It can cover an area equal to that of the state of Iowa.

Warm season- march through September.

Not front associated.

Upper level ridge of high pressure.

18
Q

what type of weather can a severe thunderstorm produce

A

Flash floods or tornados.

Strong winds and hailstones

19
Q

Where in the U.S. are thunderstorms most common

-

A

Central Florida

North to South increase

Great Plains

20
Q

what makes thunder

A

Is a sharp clap or rumbling sound after lightening.

Lightening heats the narrow conducting path to high temps. The rapid rise in temps is accompanied by a tremendous increase in air pressure locally that generates a shock wave. The shock wave propagates outward producing sound waves that are heard as thunder. The first thunder clap we bear is generated by the nearest part of the lightening flash. Subsequent sound waves reach us from portions of the flash that are progressively further away. Hence the rumble

21
Q

how do tornadoes rotate

A

Move in circles and even to describe as figure 8s.

Northern hemisphere tornados rotate counterclockwise direction. Only 5% rotate clockwise. Counterclockwise comes from the parent thunderstorm.

The changing direction of the inward directed pressure gradient force produces the centripetal force that maintains the rotation of the air column.
They track from southwest to northeast but any direction is possible.

22
Q

what is a funnel cloud

A

Localized lowering of a cloud base into tapering rotating column composed of tiny water droplets. If it remains aloft it is a funnel cloud if it touches ground it is a tornado.

23
Q

how to protect yourself from a tornado

A

Get to the lowest surface

24
Q

where is tornado alley

A

A north- south corridor stretching from eastern test and the Texas panhandle northward through Oklahoma, Kansas, Nebraska, and into South Dakota.

Kansas and Oklahoma have the highest annual incidence of tornados per unit, whereas local tornado frequency maxima occur from central Iowa eastward into central Indiana and along the gulf coast.

25
Q

what is a dry line

A

A boundary between continental tropical air and maritime tropical air in the southeast sector of a mature extra tropical cyclone likely site for the squall line and severe thunderstorm development

Advanced eastward during the day and retreats westward at night.

Brings uplift similar to cold front

26
Q

peak months for tornadoes

A

May and June when atmospheric conditions are optimal for deep convection and the severe thunderstorms that spawn tornados

27
Q

What is most destructive about a hurricane

A

Heavy rains and inland flooding, strong winds, tornadoes and storm surge.

FLOODING

28
Q

where are the strongest winds in a hurricane

A

Eye wall

29
Q

general characteristics about a hurricane

A

Intense cyclone

Summer or early fall when sea- surface temps are highest.

Maximum sustained wind speed of at least 119 km per hr (74 mph).

Develops on a uniformly warm and humid air mass. No associated fronts or frontal weather.

EYE- area of cloudless skies subsiding air and light winds. Shrinks in diameter as the Hurricanes strengthen.

Eye wall- the ring of the thunderstorm. STRONGEST

30
Q

it is usual for tornadoes to accompany a hurricane

A

It can happen.. But not typical. It happens after the hurricane enters the westerly steering current and curves toward the north northeast

31
Q

understand latitudinal winds .. ie.. trade winds, horse latitudes

A

horse latitudes- areas of high persistent light winds or calm air between about 30-35 degrees N and S under subtropical anticyclones. Region of calm air.

Trade winds- surface winds blown from the northeast out of southern flanks of the anticyclones. The most persistent winds on the planet in some regions blowing from the same direction 80% of the time.

32
Q

Warm core cyclone

A

Forms south of the polar front and consists of extensive areas of subsiding warm, dry air. Strengthen with altitude. Massive systems with a circulation extending from Earth’s surface up to the tropical troposphere.
Subtropical May stretch across North America other warm core anticyclones may develop over the interior of North America. In summer.

Vertical structure and the density contrast between warm and cold core.

The total mass of air over the center of a warm-core anticyclone related to a higher tropopause, compared to the surrounded atmosphere is responsible for the warm anticyclones high surface pressure.

33
Q

that a cold front moves

A

faster than a warm front