ENVS 203- Test 2 Flashcards
(90 cards)
Why is there wind?
- energy imbalances, especially between higher and lower latitudes
- energy surplus at the equator
- Energy deficit at poles
- this leads to differences in atmospheric pressure.
What is the relationship between atmospheric pressure and both altitude and temperature?
- pressure decreases with altitude
- warm air is less dense than cool air
What are the relative nature of high/low pressure zones?
-High and low pressure are relative terms - higher/lower than surrounding area
Pressure gradient…what is it and how does it relate to pressure differences?
- pressure gradient: horizontal rate of pressure change
- larger the pressure difference gradient
What are the three main forces/phenomena that produce our wind patterns?
- pressure gradient
- earths rotation/coriolis effect
- friction
How does pressure gradient relate to wind speed and direction?
- winds generated from high pressure ->low pressure
- larger the pressure difference, larger the pressure gradient
- wind speed is directly proportional to pressure gradient
- winds generated perpendicular to isobars from high -> low
How does the coriolis force affect wind speed and direction?
- once generated the wind is turned by earth’s rotation= coriolis effect
- deflects to the right in northern hemisphere, left in southern
- strongest effect at poles, zero at equator
- effect is proportional to wind speed
- effect influences direction only, not speed
- will turn winds 90 degrees to pressure gradient
How does friction affect wind speed and direction?
- friction with the ground slows speed, thus decreasing coriolis effect
- results in winds crossing isolines at 30 degree angle
- friction extends to a height of about 1600 ft
- increases with roughness of a surface
Draw the net result of these forces on wind direction at the surface or aloft
-Look in slides/chapter about wind (lecture slides 9, page 14)
Cyclonic vs. anticlonic circulation. Relation to pressure and direction of air movement both horizontally and vertically
- anticyclone= high-pressure system. circulation body of air outward. descending air. clockwise circulation in northern hemisphere.
- cyclone= low-pressure system. circulating body of air inward. rising air. counterclockwise in northern hemisphere
What is the idea of a constant isobaric surface? (ridges and troughs)
-an elevated surface in the atmosphere on which all points have the same pressure, usually 500 mb. along this constant pressure surface, isobars mark the paths of upper-air winds
Equatorial low-pressure through? (location, climate, how these shift from jan to jul)
- location:intertropical convergence zone
- thermal
- warm/wet
Subtropical high-pressure? (location, climate, how these shift from jan to jul)
- dynamic
- hot/dry
- produce westerlies
- exist above deserts
Subpolar low-pressure? (location, climate, how these shift from jan to jul)
- dynamic
- cool/wet
- polar front is area of contrast between cold air from higher latitudes battling with warm air from lower latitudes
Polar high-pressure? (location, climate, how these shift from jan to jul)
- thermal
- cold/dry
- polar easterlies
- higher latitudes near antarctica
Trade winds? (model of atmospheric circulation)
-northeast and southeast winds that converge in the equatorial low pressure trough, forming the inter tropical convergence zone
Westerlies? (model of atmospheric circulation)
-the predominant wind flow pattern fro the subtropics to high latitudes in both hemispheres
Polar esterlies? (model of atmospheric circulation)
-a variable weak, cold and dry wind moving away from the polar region; an anticyclonic circulation
Hadley cells, mid-latitude cells, polar cells (model of atmospheric circulation)
-
ITCZ (atmospheric circulation)
-a thermally caused low pressure area that almost girdles earth, with air converging and ascending all along its extent
Polar front (model of atmospheric circulation)
-cold polar air meet warm tropical air
Jet streams (model of atmospheric circulation)
-the most prominent movement in upper level westerly wind flows; irregular, concentrated, sinuous bands of geostrophic wind
Describe the direction of flow of the major ocean gyres?
- indian ocean
- north atlantic
- north pacific
- south atlantic
- south pacific
Explain land/sea breezes, mountain-valley breezes, and monsoons?
- land-sea breezes= daily heating/cooling patterns. onshore/offshore flow
- mtn-valley breezes=daily heating/cooling patterns. up valley/downvalley flow.
- monsoons=seasonal heating/cooling patters. high->low