Meteorology I

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Created by:

mjcarp97  on December 1, 2011

Classes:

MPHS Class of 2015

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Meteorology I

glaze
supercooled water that freezes when it touches a solid
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glaze supercooled water that freezes when it touches a solid
sleet tiny clear translucent ice particles
ozone made up of 3 oxygen atoms that are bonded together
troposphere layer of atmosphere that contains weather
thinnest layer of the atmosphere thermosphere
most abundant gas in the atmosphere nitrogen
most abundant - least abundant nitrogen, oxygen, argon, CO2, other
tropopause seperates the troposphere from the stratosphere
hot seatbelt against skin conduction
earth receives energy fron the sun radiation
higher elevations lower temperatures
isotherms lines that connect points of equal temperature
rain, snow, sleet, and hail precipitation
solid-gas sublimation
gas-solid deposition
air that has reached its water vapor capacity saturated
can hold more water warm air
dew point temperature that air must reach in order to reach saturation
examples of condensation nuclei salt, ash, dust, crystals, soil
cumulus clouds cotton-like and puffy
nimbostratus clouds low and produce rain
prefix alto middle height clouds
fog vs. clouds fog is at ground level, clouds can produce rain
supercooled water water is liquid below its freezing point
isobars lines that connect points of equal air pressure
weather in high pressure system clear
closely spaced isobars indicate steep pressure gradient and high winds
winds of a high pressure system blow clockwise
wind influence differences in pressure,temperature, and the Coriolis Effect
coriolis Effect direction of wind
cyclones low pressure,counterclockwise, clouds
anticyclones high pressure, clockwise, clear skies

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