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Weather. Miscellaneous. El Niño and Amigos. Global Warmth and Warming. Global Winds. 1 pt. 1 pt. 1 pt. 1 pt. 1 pt. 2 pt. 2 pt. 2 pt. 2 pt. 2 pt. 3 pt. 3 pt. 3 pt. 3 pt. 3 pt. 4 pt. 4 pt. 4 pt. 4 pt. 4 pt. 5 pt. 5 pt. 5 pt. 5 pt. 5 pt.
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Weather Miscellaneous El Niño and Amigos Global Warmth and Warming Global Winds 1 pt 1 pt 1 pt 1 pt 1 pt 2 pt 2 pt 2 pt 2 pt 2 pt 3 pt 3 pt 3 pt 3 pt 3 pt 4 pt 4 pt 4 pt 4 pt 4 pt 5 pt 5 pt 5 pt 5 pt 5 pt
Air that is warmer than the surrounding air leads to this type of pressure
Air flows counterclockwise around this type of pressure center in the Northern Hemisphere
Low precipitation on the far side of mountains resulting from prevailing winds blowing up and over the mts.
A mid-latitude storm over an estuary would be most likely to have this effect on the estuary’s salinity
Antarctic Spring (September) The returning sunlight triggers the release of Cl atoms from the CFC’s
Summarize the process of stratospheric ozone depletion. FOUR MAIN STEPS!
PSC’s form in the circular winds above Antarctica in dark winter. • Chlorine-containing compounds (CFC’s) stick to cloud surface. • Returning sunlight triggers release of Cl atoms. • One Cl catalyzes breakdown of thousands of ozone molecules.
El Niño has this effect on fish populations off the coast of Peru
These specific winds cause "normal" conditions in the equatorial Pacific
Easterly Trade Winds
Normally, sea surface height is highest in this portion of the equatorial pacific
This northern latitude is the farthest north you would find a solar angle of 90o
~23.5 degrees North (Tropic of Cancer)
Besides Water Vapor: Carbon Dioxide, Methane and Nitrous Oxide
THREE impacts on warming that result from changing forests to farmland
-Fewer trees to absorb CO2, • -Fewer trees increases surface temp. and thus evaporation, • - Surface becomes more reflective
Infrared (longwave)
This is the farthest poleward of the tropospheric circulation cells
This is the name for the large scale circulation cell that takes air from the equator and deposits it at 30º N and S of the equator
The winds at the point located on the map would be called this.
Winds pushing water off the coast of a continent cause this portion of thermohaline circulation to occur.