Science Curriculum Topic
Study
Air & Atmosphere and
Weather & Climate
I. Identify
Adult Content Knowledge
Science for All Americans
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Planet enveloped by a thin blanket of air
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The earth has a variety of climatic patterns:
temperature, precipitation, humidity, wind, & air pressure
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Energy comes from sun heating land, ocean, and
air
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Transfer of heat energy at interfaces of
atmosphere with land and oceans produces layers at different temperatures in
both air and oceans. The layers rise or sink or mix and give rise to winds and
ocean currents that carry heat energy between warm and cool regions
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EarthÕs rotation curves the flow of winds and
ocean currents
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Water cycle helps to determine climatic
patterns: evaporation, rising, cooling, condensing, precipitation and collection
of water in ground and surface water.
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Climatic changes occur due to factors such as
advance or retreat of glaciers or huge volcanic eruptions or changes in
atmospheric content or ocean temperature
Science Matters
- Three
principal atmospheric cycles (weather, seasons, climate)
- Troposphere
is warm layer of air next to surface of the earth – extends up to 40
feet. It contains most of the cloud systems we see from earth
- Stratosphere
9 to 150,000 feet)
- Mesosphere
(to 260,000 feet)
- Ionosphere
– plays a role in the overall behavior of the ocean of air
- Convection
causes weather in near earth layers
- Lower
atmosphere powered by solar energy – most solar energy is at
equator where warm air expands and rises. The earthÕs 24 hour rotation
creates 3 large east-west convection cells – creating westerlies
and easterlies depending on if it is northern or southern hemisphere
respectively. Stagnant air masses (ÒdoldrumsÓ) are found at the equator
- Weather
terms
- Temperature
– rises and falls on a daily basis and seasonally and with altitude
- Barometric
pressure is the weight of all the air overhead
(14lbs/in2). Large air masses form vast circular currents,
which pile up at margins (high pressure zones) and such air out of their
centers (low pressure zones)
- Humidity
– relative term – reported as a percentage. It is the amount
of water vapor that the air can hold before it produces fog or rain. It
depends on air temperature. Relative humidity is a measure of how much
water the air actually holds, compared to how much water the air can
absorb.
- Wind
speed and direction – depends on topography, the location and
temperature of large bodies or water, and distribution of high and low
pressure air masses.
- Jet
stream – high altitude wind currents that behave like fast moving
rivers (about 8 miles high) Jet stream roughly divides cold northern air
from warmer air in temperate regions. General trend in US is west to
east.
- Airborne
Pollen – pollutants in air reported during weather forecasts. It is
described by arbitrary scale of particles per given volume of air.
- Greenhouse
Effect – Effects of carbon dioxide in atmosphere. In a greenhouse,
sunlight passes through glass and is absorbed by the materials on the
inside. The heated materials give energy back as infrared radiation. The
glass in essence traps the infrared radiation and warms the inside. Like
glass, carbon dioxide transmits visible light energy from the sun. It also
absorbs the infrared radiation that rises from the ground and holds heat
in the atmosphere instead of reflecting it back into space. Global warming
refers to this process of accumulated carbon dioxide (primarily from
burning fossil fuels). Carbon dioxide has always been present in the
atmosphere – more is just being added. Other gases like methane and
water vapor can also add to the greenhouse effect. Carbon dioxide is the
main source of the green house effect. Debate in science occurs on if
global warming has already started and how much warming will eventually
occur.
References:
¤
Hazen, R.M. &
Trefil, J. 1992. Science
Matters: Achieving Scientific Literacy. New York: Anchor Books.
¤
Keeley, P. 2005. Science
Curriculum Topic Study: Bridging the Gap Between Standards and Practice.
Thousand Oaks, CA: Corwin Press.
¤
Rutherford,
F. J. & Ahlgren, A. 1989. Science for
All Americans: A Project 2061 Report. American Association for the
Advancement of Science. New York: Oxford University Press, Inc. Note: This document is also available on the
web at: http://www.project2061.org/publications/sfaa/online/sfaatoc.htm