12.2 Weather Systems – notes...
Transcript of 12.2 Weather Systems – notes...
Name _________________________________________ Date ________________
12.2 Weather Systems – notes sheet What is the Coriolis Effect? Deflection of air to the right in the Northern hemisphere due to the earth’s rotation. The Earth rotates from West to East. The Coriolis Effect combines with the heat imbalance found on Earth to create distinct _____Global wind System ___________ that transport __colder ____ air to warmer areas and ___Warmer_____ air to colder areas. The end result is the ____balancing______________ of heat energy on Earth. Global Wind Systems:
Name Location Description of how wind moves
Towards or Away from the Equator?
Trade Winds
30° N 30° S
from east to west toward
Prevailing Westerlies
30°--60° North and South Latitudes
from west to east away
Polar Easterlies
between 60° and the poles
from east to west toward
Global Pressure Systems: sailors can get stranded due to little or weak winds
Name Location Low or High Pressure? Horse Latitudes
30° N
High
ITCZ (Doldrums)
near equator Low
What causes wind? __differences in temperature and pressure_______________________ Weather systems generally follow the path of what winds? ___narrow bands of fast high altitude westerly winds called jet streams___
Type of Front Map Symbol &
Color Description of air
movement Associated
Weather Cold Front
solid blue line with triangles pointing in the direction of the front’s motion
Cold dense air replaces warm air—by forcing it up. As warm air rises it cools and condenses
Clouds, showers and sometimes thunderstorms
Warm Front
solid red line with semicircles pointing in the direction of the front’s motion
Warm air displaces cold air. Movement is slower and more gradual
extensive clouds and precipitation
Stationary Front
combination of short segements of both warm and cold front symbols
Two air masses meet and neither advances. Boundary stalls
light wind and precipitation
Occluded Front
purple line with alternating semicircles and triangles that point in the direction of motion
cold air mass moves very rapidly and overtakes warm front. Warm air is wedged upward and two cold air masses collide
Strong winds and heavy precipitation on both sides of the front
Use the following list of characteristics to create a Venn diagram that compares/contrasts Low-Pressure Systems with High-Pressure Systems.
• Air moves in circular motion both • Winds move clockwise in northern hemisphere High • Rising air Low • Stormy weather low
• Winds move counter-clockwise in northern hemisphere Low
• Fair weather High • Sinking air High Low-Pressure System High-Pressure System