Final New Section Flashcards
Cold core system
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
What/where is the ITCZ
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).
What is a front?
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
know meridional/zonal flows and what they mean
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.
understand the polar jet and it’s seasonal variations (meridional vs. zonal)
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
what is a jet streak/it’s quadrants/ divergence and convergence associated with a jet streak
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.
what is upwelling
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.
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.
know the clouds progression as a warm front approaches
Cirrus-cirrostratus- altostratus- nimbostratus- and stratus
signs of warm air advection (clouds)/where is typically occurs (which side of a ridge vs trough)
- High cirrus clouds in the western sky.
Behind (west of a ridge)
know how frontal precipitation sets up
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When air cools sufficiently.
differential heating of land vs water
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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
what/where is a Chinook wind
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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
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
higher tops mean
more severe thunderstorms
The greater the altitude of the top the more severe the storm.
Magnitude of the vertical wind shear