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scientific investigation of interactions among organisms and between organisms and their physical environment -relatively new branch of biological sciences -coadaptation of organic beings to each other and to their physical conditions of life |
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-provides explanations of the perceptible, palpable world -can often be observed -encompasses the study of the movement of energy and nutrients through ecosystems |
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a science that generates knowledge about interactions in the natural world, as a field of inquiry, not focused on human concerns |
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use of ecological knowledge, along with economics, ethics, and many other considerations, to inform both personal decisions and public policy relating to stewardship of natural resources and ecosystems |
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living components of ecosystems |
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physical and chemical components of ecosystems |
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the networks of interacting organisms in an area and the physical environment they occupy |
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main concern of ecology was understanding the distribution and abundance of organisms |
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new tools have arrived that have change the face of this research -mathematical models -molecular techniques -satellite imaging |
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to provide objective data on the interactions of the different components of the biotic and abiotic environments and, through analysis of the data, to understand these interactions and their various results |
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refer to atmospheric conditions--temp, humidity, precipitation, and wind direction and velocity---but refer to different time scales |
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short term state of atmospheric conditions at a particular place and time |
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refers to the avg atmospheric conditions, and the extent of their variation, at a particular place over a longer time |
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climate is what you expect |
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usually short term for organisms -seeking shelter for sudden rainstorm |
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tend to be evolutionary adaptations that arise within populations over time and affect physiology, morphology, and behavior -can't adapt to, animal won't be found there |
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determines the air's temp. and is the major determinant of climate |
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intensity of solar radiation |
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varies over the course of a year and from place to place due to the shape of the earth, its orbit around the sun, and the tilt of its axis |
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amount of solar energy reaching a given point on Earth's surface |
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depends primarily on the angle of the sun's rays -high latitudes (North and South poles) sunlight strikes Earth's surface at an angle, so solar energy is distributed over a larger area--LESS INTENSE than that of the equator, where sunlight strikes the surface perpendicularly |
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sun's radiation at an angle |
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must pass through more of Earth's atmosphere, so more of its energy is absorbed or reflected before reaching the surface |
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toward the poles (solar energy) |
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sun's rays are absorbed bc they must travel a longer distance through the atmosphere |
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near equator (solar energy) |
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sunlight strikes Earth at a steep angle, delivering more heat and light per unit of area |
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air temp Increase or Decrease with elevation |
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decrease, temp at sea level are warmer than temps on mountaintops at the same latitude |
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what causes seasonal variation in temp and day length |
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Air circulation in Earth's Atmosphere |
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1-(Solar energy drives patterns of atmospheric circulation)-In the tropics, warm, moist air rises, expands and cools, drops its moisture, and flows poleward
2- (those patterns in turn, influence air temps worldwide)-the now cool, dry air warms and retains its moisture as it descends. It reaches Earth's surface at about 30N and 30S |
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result when air is warmed |
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expands, becomes less dense, and rises, and then cools as it rises |
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