THE HYDROLOGIC CYCLE OCEAN EVAPORATION WIND PRECIP.

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Presentation transcript:

THE HYDROLOGIC CYCLE OCEAN EVAPORATION WIND PRECIP

TEMPERATURE SCALES PRESSURE PRESSURE Temperature Scales KELVINCELSIUSFAHRENHEIT (freezing=273K)(freezing=0C)(freezing=32F) (boiling=373K)(boiling=100C)(boiling=212F) Pressure(EXAMPLE) STATION A 1000MB STATION B 995MB 990MB995MB 1000MB 1005MB Surface A Surface B In summary we see that at Station A they are Are under the influence of higher pressure then Station B. Pressure=Force/Area

Quick Look Equations Pressure=Force/AreaDensity=Mass/Volume1bar=1000mb=100,000Pa mb=101,325Pa 1mb= in Hg mb=1in Hg

Atmospheric Layers TROPOSPHERE(Weather Layer) 0KM 10KM 50KM STRATOSPHERE Tropopause MESOSPHERE STRATOPAUSE 85KMMESOPAUSE THERMOSPHERE 20C0C-20C-40C-60C