Regional climates affect by: average temperature average precipitation altitude and latitude Temperature and precipitation are primarily affect by global air circulation Figure 7-6s which is influenced by: amount of solar energy that drives air circulation - long-term variation in solar orbit, tilted axis of earth -seasonal and latitudinal variation ( Figure 7-3 ) earth axial rotation ( Figure 7-4 Coriolis effect ) affected by physical properties of air and water Recall: special properties of water -e.g. evaporative cooling Figure 7-5 moist warm air rises-expands less dense as it does, it cools and releases moisture as rain or snow thus, heat is releases and may radiate into space then, cool dry airs descends affected by chemical properties of air and water Air chemical composition: carbon dioxide, water vapor, as well as trace amounts of ozone, methane, nitrous oxide, CFC and other gases in the troposphere &quot; greenhouse gases &quot; -heat absorbed by molecules, warming air and some radiates back toward earth&#146;s surface, thus, trapping heat.
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special properties of water - e.g . evaporative cooling Figure 7-5 moist warm air rises - expands less dense cools,List([476, 601))
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by global air circulation Figure
it
by chemical properties of air and water Air chemical composition
by: amount of solar energy that drives air circulation - long-term variation in solar orbit, tilted axis of earth -seasonal and latitudinal variation ( Figure 7-3 ) earth axial rotation ( Figure 7-4 Coriolis effect ) affected by physical properties of air and water Recall: special properties of water -e.g. evaporative cooling Figure 7-5 moist warm air rises-expands less dense as it does, it cools and releases moisture as rain or snow thus, heat is releases and may radiate into space then, cool dry airs descends affected by chemical properties of air and water Air chemical composition: carbon dioxide, water vapor, as well as trace amounts of ozone, methane, nitrous oxide, CFC and other gases in the troposphere &quot greenhouse gases &quot -heat absorbed by molecules, warming air and some radiates back toward earth&#146;s surface
air circulation - long-term variation in solar orbit, tilted axis of earth -seasonal and latitudinal variation
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releases