BIL 160 Lecture Notes - Lecture 22: Irradiance, Subtropics, Natural Selection

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14 May 2018
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BIL 160 Lecture 22
Ecology
the study of interactions of organisms with each other and with their environment.
Consists of biotic components (the living organisms) and abiotic components (nonliving like
light)
Natural selection is driven by ecological interactions
species - similar organisms able to interbreed under natural conditions to produce fertile, viable
offspring
population - all members of a single species living in a defined location
community - all populations living in a defined location
ecosystem - the community and the abiotic components of its world
landscape - interactions between adjacent ecosystems
biosphere - all the earth's ecosystems, considered collectively
Solar Energy
Solar Irradiance
Terrestrial irradiance is the solar radiation striking earth's surface
Shorter and longer wavelengths are absorbed or reflected by atmospheric molecules such as
ozone and water vapor.
Less than half of the solar radiation striking the earth's atmosphere successfully penetrates the
atmosphere to reach earth.
Sunlight Quality and Quantity
Irradiance intensity and spectral distribution depend on
o environmental conditions
o sunlight angle of incidence
The tropics lie between the
o Tropic of Cancer and the Tropic of Capicorn
o receive the highest annual input of solar energy
o are the only place on earth where the sun ever shines directly overhead
o This occurs on the equinoxes, March 21 and September 21.
Subtropic lie
o Tropic of Cancer and 30oN in the northern hemisphere
o Tropic of Capricorn and 30oS in the southern hemisphere
Seasonal Changes in Sunlight
The tilt of earth axis results in seasons
Global Air Temperature
Solar warming creates movement of air and water vapor in the oceans and atmosphere.
This generates characteristic climate patterns across the globe.
o Tropics: warm, high levels of precipitation
o Subtropics: relatively warm, arid
o Temperate: relatively warm, arid
o High Latitude Temperate: cool, high levels of precipitation
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