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Weather Basics Temperature Pressure Moisture
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Temperature
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Diurnal Temperature: Why?
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Lag time varies, Phoenix Zoo
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Global Pattern Warm Lower Latitudes Cold Mtns Cold Higher Latitudes Cold Currents
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Classroom Resource Global pattern shows warmer in lower latitudes; colder in higher latitudes
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Why Latitude Temp Differences?
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Seasonal Changes: more with higher latitudes and warmth follows the sun
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Temperature Differences Create Climate Zones
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Why San Diego “even” climate and Phoenix more “extreme”?
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Cold and Warm currents influence temperature THINK San Diego vs Phoenix
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Classroom Resources Can see continentality in these movies (bigger changes in temperature between winter and summer in the middle of North America
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East Coasts: Warm Water
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Pressure
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Classroom Resource: Sea Breeze as example of pressure gradient
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Cold Air Drainage
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Most intense closest to poles because greatest difference in speed of rotation
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Classroom Resources
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Online Resource Atmospheric Pressure and Wind Animations http://serc.carleton.edu/NAGTWorkshops/ visualization/collections/atmospheric_pres sure.html
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Coriolis Effect impacts more than atmosphere and oceans
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Geostrophic Wind
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Combination of all 3
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Effect of Friction: cross the isobars
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Classroom Resource
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Divergence at surface generates uplift and cloud formation
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Opposite in So. Hemisphere
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Global Patterns of Pressure Drive Earth’s Climates: Example of Asian Monsoon Winter High Pressure Siberia. Air flow from Siberia (dry air) outward
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Winter Dry Summer Wet
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Then, in summer, winds reverse
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Monsoon (singular) is a seasonal wind shift
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Indus Floods Before After
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Before
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Arizona (Mexican) Monsoon: Wind shift from westerly winds
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To easterly winds
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Season shift in wind brings trpoical moisture from east and south
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Mexican Monsoon, as reflected by percentage of rain in summer
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Moisture at mid-levels generates weaker storms
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Lower-level moisture often comes from the gulf, giving sudden surge of moisture
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Combination of mid and low level moisture generates stronger storms
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July – mid September (storms not Monsoons)
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Classroom Resource: Movie showing global patterns in water vapor Dark – little water vapor Bright: lots of water vapor
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Example of Condensation by Adding Moisture: Lake Effect Snows
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Example of Condensation by Cooling: Advection Fog
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Advection Fog Common over Cold Currents
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California Cold Current produces fog
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Example of Condensation by Cooling: Air Goes Up & Cools
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Can go up by convergence
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Cloud Types
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Vertical Development: Cumulus
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More horizontal flow: Stratus
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Online Resource
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Need to get large enough to drop out
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Classroom Resource: Precipitation in the U.S. throughout the year Watch Arizona in monsoon months (wetter) Watch Pacific Northwest in winter (wetter)
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Global Pattern of Precipitation More around equator Less in subtropics More around latitude 50 Seasonal shifts (summer monsoon in low laittudes; winter storms in higher latitudes)
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Another way of thinking about moisture: Air Masses
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Classroom Resources Can see outbreaks of Continental Polar air in movie Can see Arizona develop Continental Tropical Air mass in June
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Global Air Masses
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Online Resources Atmosphere Animations http://serc.carleton.edu/NAGTWorkshops/visualization/colle ctions/atmosphere.html Atmospheric Heating Animations http://serc.carleton.edu/NAGTWorkshops/visualization/colle ctions/atmospheric_heating.html Moisture Animations http://serc.carleton.edu/NAGTWorkshops/visualization/colle ctions/moisture.html
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Imagery seen in this presentation is courtesy of Ron Dorn and other ASU colleagues, students and colleagues in other academic departments, individual illustrations in scholarly journals such as Science and Nature, scholarly societies such as the Association of American Geographers, city, state governments, other countries government websites and U.S. government agencies such as NASA, USGS, NRCS, Library of Congress, U.S. Fish and Wildlife Service USAID and NOAA.
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