Atmosphere 78% nitrogen, 21% oxygen

Water Vapor up to 4% by volume leaves atmosphere as dew, rain or snow

Density of Air Warm air is less dense than cold air Humid air is less dense than dry air

Air Movement Air near sea level is packed by pressure As air rises - expands and cools As air descends- compresses and warms

Precipitation Warm air can hold more water vapor than cool air As air rises, it cools and water vapor may condense into clouds and eventually precipitation

Fig 7-2a, g

Fig 7-6, g

Pressure

Figure 6.13

Figure 6.7

Uneven Solar Heating

Figure 6.1

Fig. 7-3, g

Atmospheric Circulation Wind = mass movement of air wind patterns caused by variations in solar heating and earth’s rotation

Uneven Solar Heating & Atmospheric Circulation Air is warmed in the tropics and rises Air is cooled near the poles and falls

Fig 7-4b, g

Fig. 7-7, g Earths air Circulation if Uneven Solar heating

Fnft

Remember… …putting all of this together…the hot, humid, air over the tropics is LESS dense (than all other air masses); this means: (a) Less dense air rises (like a hot air balloon); (b) As it rises (vertical) the pressure decreases; (c) As pressure decreases, air EXPANDS; (d) As it expands, it COOLS …then the reverse again…+ horizontal (wind) movement

Fig 7-2, g

Atmos. Circ. Cont… …When you add the horizontal (wind) movement it pushes this (originating hot, dry, tropical air) BOTH up and out (North/South) for distribution throughout the entire atmosphere. How?

Atmos. Circ. Cont… …How? Tropical air rises, meets density around it (more dense than that above it but less dense than that below it) so it can’t “move” vertically …but it must go somewhere! SIDEWAYS! (joins Atmospheric Circ. pattern, moving horizontally, toward POLES) & as it rises poleward it COOLS, gets more dense, and falls back (toward equator) again…and again…

Fig. 6-8, p. 127 Water’s Thermal Properties Affect Climate: Moderate Earth’s Climate

What’s with the WIND? …Influence of the rotation of the earth…

Fig. 7-9, p. 152

Coriolis Deflection “The apparent deflection of objects moving across Earth’s surface to the right of direction of travel in the Northern Hemisphere and to the left in the Southern Hemisphere.” Different because of difference of speed and width of equator vs. poles Increases poleward & as speed increases.

Coriolis Effect The eastward rotation of the earth deflects any moving object away from its initial course the deflection OF THE OBJECT is clockwise in the Northern hemisphere the deflection OF THE OBJECT is counterclockwise in the Southern hemisphere

Figure 6.9

Figure 6.10a

Figure 6.10b

All together now… Wind Coriolis Effect Atmospheric Conditions

Fig 7-12, g

Wind Patterns At bands between cells air is moving vertically winds are weak and erratic doldrums or intertropical convergence zone (ITCZ) at equator –ascending air Subtropical high pressure belt at 30 o –descending air, very dry

Wind Patterns Within cells air moves horizontally from high to low pressure areas produces strong dependable winds –Trade winds or easterlies –westerlies –polar easterlies

Wind Patterns Within circulation cells air moves horizontally from high to low pressure areas (wind belt) produces strong dependable winds –Trade winds (between 0 and 30 o ) –Westerlies (between 30 and 60 o ) –polar easterlies (between 60 and 90 o )

Fnft

Global Wind Circulation

REMEMBER: Movement of air across a pressure gradient parallel to Earth’s surface is called a wind. Winds are designated according to the direction from which they come. In contrast, ocean currents are designated according to the direction towards which they travel.

Table 6.2

Global Wind Circulation

60°N 30°N 30°S 0° 60°W North Pole South Pole 30°E 0°30°W 60°W 0° North Pole South Pole 60°N 30°N 30°S 0° North Pole South Pole Stepped Art Latitude Equator Longitude Prime meridien