Weather notes 4 Flashcards
The Southern Oscillation was not recognized until ___
the early 80s
Colder than avg. equatorial Pacific Ocean water temp (W of S Africa)
Created offshore wind which leads to upwelling
Subtropical jet has no excess warm air to move Northward
L<H
La Nina
Warmer than avg. equatorial Pacific Ocean water temp
H>L
warmer water expands toward east
El Nino
El Nino Event: 1982-1983
Strong event-$8 bil damage
El Nino Event: 1986-1987
Weaker event; ended in drought in SE USA
El Nino Event 1991-1992
Strong event; severe Texas flooding, 5 year drought ended in California
Sea Breeze
Day time
Land Breeze
Night time
Valley Breeze
day time
Mountain Breeze
night time
Monsoon - what and where?
a seasonal wind shift, India/SE Asia
Baby monsoon
SW US summer thermal low
Winter Monsoon
High Pressure over land/offshore wind
Summer Monsoon
Low pressure over land/onshore wind
A low pressure circulation created by changes in air temp (strong daytime heating over SW USA during summer months)
result in Summer Monsoon
Thermal Lows
Months of thermal low pressure in S California and Arizona
June 15-early September
cold, downsloping, destructive wind
Greenland, Antarctica
aka Mistral
Katabatic Wind
Warm, downslope wind
Eastern slopes of Rockies in US/Canada
Chinook Wind
warm, dry downslope wind in California
Most common in October
Strong surface pressure over the great sale lake region
Santa Ana Wind
North Africa/India
Saharan Dust Storm/Dust Devils/Haboob
Desert Wind
a current of water or air running contrary to the main current; especially : a circular current : whirlpool
Eddy
rapid change in wind speed and/or direction in a small area and/or a short period of time
Wind Shear—>Thunderstorms
A or cA
Continental Arctic - very cold, Arctic circle
cP
Continental Polar - source: Central, N Canada
produce lake effect snows on the Great Lakes
mP
Maritime Polar - over water, chilly, Seattle
mT
Maritime Tropical, warm and humid, Gulf of Mexico
moves moisture necessary for thunderstorms
cT
Continental Tropical - hot and dry
surface convergence and upper air divergence causing rising motion of air
Low Pressure system
boundary between two air masses
front
when a front develops
frontogenesis
when a front dies
fronolysis
a less dense(warm) air mass overruns a more dense(cold) air mass
overrunning
when warm air actively advances into a region where warm air used to be Steep slope (1:50); most dynamic
Cold front
warmer air occupies an area formerly occupied by colder air
warm eats away top down=real overrunning
more gentle slope (1:150); less dynamic
Warm front
little forward movement of either air mass, upper level winds PARALLEL to the surface frontal boundary, difficult to predict weather
Stationary front
wind is blowing at least somewhat perpendicular when?
when a front is moving
What has been correlated with flash flood/heavy rain events?
Stationary fronts and hurricanes
when a cold front overruns/overtakes a warm front in the vicinity of a surface low
more common in the northern US
occluded front
Boundary between cT(heavier) and mT air masses, most commonly found over US plains states (TX northward)
DRY LINE
not a front, no big pressure difference, thunderstorms can occur