Exam 2 Flashcards
Coriolis Force
Affects wind direction The apparent deflection of wind and objects relative to the Earth’s surface caused by the rotation of Earth. Deflection right in Northern hemi, left in southern hemi, direction shift increases with latitude.
Three-Cell Model
Geostrophic Flow
Occurs when pressure gradient force = Coriolis force. Air flows parallel to lines of equal pressure. Rare in nature
Gradient flow results from:
a nonuniform pressure gradient
Surface winds are NOT parallel to isobars because:
of friction, reduces wind speed, and therefore reduces Coriolis force
Anticyclones
air diverges from high pressure areas at surface and is deflected by Coriolis force. Clockwise N, counter S. Effect: descending air that warms and creates clear skies.
Cyclones
Air converges toward low pressure center at surface and is deflected by Coriolis force. Counter N, Clockwise S. Effect: ascending air that cools to form clouds.
Unclosed pressure systems are…
elongated areas called troughs and ridges
Single Cell Model
General movement of atmosphere. Heating at equator causes air to expand upward and diverged towards the poles, eventually sinking to the surface and returning to the equator. Easterly surface winds.
Define easterly winds
From east to west
Define westerly winds
From west to east
Three Cell Model
Divide each hemisphere into three cells: Hadley cell, Ferrel cell, Polar cell. With different air circulation patterns. Describes climate patterns.
Hadley Cell
Intense heating at equator creates the equatorial low belt of pressure. Pressure and wind model considered close approx of real world.
ITCZ
Intertropical Convergence Zone, region around equator where trade winds of N and S hemispheres come together
Ferrel Cell
Circulates surface air between subtropical highs and subpolar lows (middle). Deflected by Coriolis, causing westerlies.
Polar cell
circulates surface air between polar highs and subpolar lows. Deflected by Coriolis, causing easterlies.
How accurate are Ferrel and Polar cells?
Does not capture real world well.
Semi-permanent pressure cells
Instead of cohesive pressure belts, there are semi-perm high and low belts that fluctuate seasonally.
Monsoons are caused by:
continental surface heating; seasonal thermal differences between land masses and large bodies of water.
Winter monsoons
Dry air flows southward from the Himalayas. Offshore flow.
Summer monsoons
Moist air is drawn northward from the equatorial oceans. Onshore flow.
Land cools or heats _______ than water
faster
Sea breezes are caused by:
heating and cooling differences between land and ocean
How do sea and land breezes travel?
Land breeze: during day, land is warmer so air expands and rises and moves towards sea.
Sea breeze: during night, water is warmer, so air moves back to land.
Air mass
a volume of air with uniform temp and humidity affecting vast area
continental polar air mass (cP)
source: high-latitude continental interiors.
properties: cold, dry, stable, minimal cloud cover
continental arctic air mass (cA)
source: highest latitudes of Asia, North America, Greenland, Antarctica.
properties: extremely cold and dry and stable. minimal cloud cover.
Maritime polar air mass (mP)
source: high-latitude oceans
properties: cold, damp, cloudy, somewhat unstable
continental tropical air mass
source: low-latitude deserts
properties: hot and dry, very unstable
maritime tropical air mass (mT)
source: subtropical oceans
properties: warm and humid
Walker Circulation
normally trade winds move equatorial surface waters westward, causing higher surface temps and a difference in sea surface height
Warm water creates a surface ______ pressure
low
El Nino
weakening or reversal of Walker circulation
La Nina
strengthening of Walker circulation
El Nino occurs every:
two to seven years
El Nino Southern Oscillation
ENSO, the change in atmospheric pressure caused by the sea surface temperature change during El Nino events
Southern Oscillation Index
SOI, difference in pressure between Tahiti and Australia. Positive/stronger than average during La Nina, Negative/weaker than average during El Nino
Teleconnections
Relationships between weather or climate patterns at two widely separated locations. Because pressure systems affect not just local but also the overall jet stream
North Atlantic Oscillation
Changing difference in pressure between the two semipermanent cells in the atmosphere above the Atlantic Ocean: Bermuda Azores High and the Icelandic Low
Positive phase of NAO Index
pressure gradient greater than normal, intensification and northward shift of polar jet stream, Hanover will have mild wet winter
Negative phase of NAO index
pressure gradient less than normal, weakened polar jet stream, Hanover will have increased cold air outbreaks
Front
Boundaries between different air masses
Mid latitude cyclones occur at:
fronts
Four types of fronts
cold, warm, stationary, occluded
Cold front
mass of cold air displacing warm air upward, associated with heavy precipitation and rapid temp decrease
Warm front
warm air overrunning cold air, associated with shallow clouds and light precipitation
Stationary front
neither air mass is displacing the other
Occluded front
two cold fronts meet, warm air between is displaced up