Exam 2 Flashcards
radiation (solar radiation)
the fuel that drives the atmosphere. Heats earths atmosphere, but mostly heats the earth
angle of incidence
angle at which solar radiation strikes a particular place at any point in time.
vernal equinox
March 20-21. the perpendicular rays of the sun strike the equator, and the sun is directly overhead. At noon in the N Hemisphere
autumnal equinox
September 22-23. the perpendicular rays of the sun strike the equator, and the sun is directly overhead. At noon in the N Hemisphere
Tropic of Cancer
23.5 deg N latitude. the intensity of solar radiation is reduced to 92% of the level at the equator.
Tropic of Capricorn
23.5 deg S latitude. the intensity of solar radiation is reduced to 92% of the level at the equator.
summer solstice
June 20-21. The sun is directly overhead at noon at 23.5 deg N latitude (Tropic of Cancer)
winter solstice
December 21-22. When the sun is directly overhead at noon in the N Hemisphere at 23.5 deg S latitude.
short waves (insolation)
most insolation is this with wavelengths of .2-5 microns. Sun rays.
long waves (energy)
Most of the energy reradiated by Earth
greenhouse effect
The heating of the atmosphere. The atmosphere limits the loss of heat, causing temp to rise
convection
movement in any liquid, caused when part of the fluid is heated. Heated portion expands and becomes less dense, therefore it rises
advection
Horizontal transfer of air. Heat in ocean currents is an example
condensation
the conversion of water from vapor to a liquid state
relative humidity
the actual water content of the air, expressed as a percentage of how much water the air could hold at a given temp
convectional precipitation
air warmer than its surroundings rises, expands, and cools by this expansion
orographic precipitation
horizontal winds move air against mountain ranges, forcing air to rise as it passes over the mountains. As it rises, it cools
frontal precipitation
forms along a front. air is forced up a boundary between cold and warm air masses
cold front Fig. 2-17a
When cold air mass advances against a warmer one. Wedges under warm air and forces it to rise.
warm front Fig 2-17b
a warm air mass that advances against a cooler air. Less intense precipitation
warm front map symbol
looks like a sun with rounded teeth coming from it
cold front map symbol
looks like a sun with sharp teeth coming from it
average atmospheric pressure (mbs)
at sea level is 1,013.2 millibars
coriolis effect
The deflection of wind (and any other object moving above Earth’s rotating surface)
Fig. 2-22 highs and lows
caused by Earths rotation, deflects wind to the right of its expected path in the Northern Hemisphere. This causes spiraling circulation around high-and-low pressure centers. High (clockwise in N) Low( counter in north)
ITCZ
intertropical convergence zone. a zone between the Tropic of Cancer and Capricorn where surface winds converge
general circulation of atmosphere
patterns vary with seasons. In Jan. the pressure and winds are arranged into broad zones according to latitude. In July, these have moved northward.
hurricanes
tropical cyclones with wind velocities exceeding 119 km/hr (74 mph) in North America
typhoons
tropical cyclones with wind velocities exceeding 119 km/hr (74 mph) in the North Western Pacific
cyclones
tropical cyclones with wind velocities exceeding 119 km/hr (74 mph) in the Indian Ocean and NW Australia