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Mon. Sep 8. Today Earth’s Atmosphere ( chp 1 cont’d) Geography 101 Warming the Atmosphere ( chp 2) Wednesday (9/10) Air Temperatures ( chp 3). Weather Review. Weather Review. Weather Review. Monsoon Haboob. Weather Review. 5?/7?. 79. 59/79. 57/76. 58/76.
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Mon. Sep 8 • Today • Earth’s Atmosphere (chp 1 cont’d) • Geography 101 • Warming the Atmosphere (chp 2) • Wednesday (9/10) • Air Temperatures (chp 3)
Weather Review Monsoon Haboob
Weather Review 5?/7? 79 59/79 57/76 58/76 Was this a good forecast?
OZONE (O3) • Two types • “Good” ozone - Stratosphere (40-50K ft.) • Absorbs ultraviolet (UV) radiation • “Bad” ozone – Near the earth’s surface • Main ingredient of photochemical smog. • 3rd most potent greenhouse gas
Ozone Formation • Surface Ozone
Ozone Destruction • Stratospheric Ozone • UV radiation has enough energy to naturally break up the molecule. • Accelerated by CFCs’ • Hairspray, freon etc. • Catalyst • Accelerate Breakdown
Ozone Hole 1978
Ozone Hole 1988
Ozone Destruction 1989MontrealProtocol
Ozone Hole 1998
Ozone Hole 2008
Ozone Hole 2012
Meteorology Conventions Meteorological Directions(Cardinal Directions) N = 0 W = 270 E = 90 S = 180 Example: 225 degrees = Southwest
Meteorology Conventions • Plotted Data • Altitude is represented on charts as increasing upward (y-axis) • Temperature increases to the right (x-axis) Altitude Temperature
Meteorology Conventions • Greenwich Mean Time • GMT • UTC (Coordinate Universal Time) • Zulu (Z) • PST = UTC – 8 hours • PDT = UTC – 7 hours • 0000 UTC = 1700 PDT = 5 PM PDT • 1200 UTC = 0500 PDT = 5 AM PDT
71 % covered by water • N. Hemi = 61% • S. Hemi = 81% 3 5 4 Map Classwork 1 6 2 9 7 1. Gulf of Mexico 2. Caribbean Sea 3. Bering Sea 4. Mediterranean 5. North Sea 6. Arabian Sea 7. Bay of Bengal 8. Tasman Sea 9. S. China Sea 8
Cascades NewEngland GreatLakes Map Classwork SierraNevada Rocky Mountains GreatBasin Midwest AtlanticSeaboard Great Plains MississippiValley PACIFICOCEAN ATLANTICOCEAN Gulf Coast Gulf of Mexico
ENERGY AND HEAT TRANSFER • What is Energy? It’s the capacity to do work on some form of matter • Potential energy: The total amount of stored energy • Kinetic energy: Energy of motion
Cold Air vs. Warm Air Slower and closer together | Faster and farther apart
ENERGY AND HEAT TRANSFER • Atoms and molecules have kinetic energy due to their motion (heat energy) • Sun’s radiant energy most important • Air temperature is a measure of the average kinetic energy of its molecules
ENERGY AND HEAT TRANSFER • Heat = energy transferred because of a temperature difference • After heat is transferred, it is stored as internal energy • Heat is transferred in the atmosphere by • Conduction • Convection • Radiation
ENERGY AND HEAT TRANSFER • Latent heat: energy required to change a substance, such as water, from one state to another • Evaporation = cooling process, absorption of latent heat from the environment • Condensation = warming process, release of latent heat to the environment
ENERGY AND HEAT TRANSFER • Conduction: the transfer of heat from molecule to molecule • Always flows from warmer to colder • Air is an extremely poor conductor of heat
ENERGY AND HEAT TRANSFER • Convection = heat transfer by the mass movement of a fluid (water or air) • Example • Pan of boiling water • Rising air currents • Convection circulation • Warm air expands • Rises • Cools and sinks
ENERGY AND HEAT TRANSFER • Radiation = Energy transfer via electromagnetic waves • Radiative Properties • Hotter objects • Emit shorter wavelengths • Emit radiation at a greater rate or intensity
Electromagnetic Radiation Fig. 2.7, p. 41