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o The relationship between patterns on the landscape and in the natural world and the processes that create them |
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Fundamental Process of Biogeography: movement of organisms from one place to another |
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Fundamental Process of Biogeography: diversification and adaptation |
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non-living portion of landscapes |
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living portion of environment |
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change between a trait or observation between poles and equator |
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body mass changes at different latitudes |
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Why do animals weigh more at higher latitudes? |
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The more massive you are, the more insulation and heat you can keep. (Note: big mass not bigger surface area) |
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appendages change in size of similar animal. Bigger appendages provide the dispersal of heat and keep you cooler |
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drives the latitudinal gradient |
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rays from the sun that go directly through the Earth's atmosphere |
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rays that have to go through more atmosphere and therefore are less intense due to the angle in which they are coming from |
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a point on the surface of the Earth and where direct rays fall |
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Located 23.5 degrees above the equator |
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Located 23.5 degrees below the equator |
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gradual shifting of climate |
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Subsolar point is at the Tropics of Capricorn. Takes place on December 21/22 |
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subsolar point is at the Tropics of Cancer. June 20/21 |
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subsolar point is at the equator. September 22/23 |
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subsolar point is at the equator. March 21/22 |
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Earth's axis is fixed (about 23.5 degrees) |
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Located 66.5 degrees S of the equator |
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Smaller Scale Features that Affect Climate Locally |
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1. Latitude 2. Elevation 3. Continentiality 4. Cloud Cover 5. Ocean Currents |
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Latitude as a Scale Feature Affecting climate |
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Temperatures decrease as you go towards the poles |
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Elevation as a Scale Feature Affecting climate |
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Temperatures increase as elevation increases due to the decrease in air particles in these elevations. With fewer air particles you have fewer collisions and reduced heat |
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Continentiality as a Scale Feature Affecting climate |
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Land is easier to heat and cool so if a location is land-locked it will have a wider range of temperature than if the location were near a body of water |
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Prevent radiation from coming in during the day as well as prevent radiation from leaking out at night. Controls daily temperature range |
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The temperature of the ocean currents can affect the temperature of the air |
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The greater the earth's tilt the more seasonality |
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Location in which Earth is furthest from the sun |
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Location in which Earth is closest to the sun |
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General Circulation of Earth's Air |
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set up by the sun's energy due to unequal heating of Earth's surface |
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cools and loses its ability to hold water vapor |
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warms and gains ability to hold water vapor |
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measure of water vapor content relative compared with what it can hold given its temperature |
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pressure exerted by water vapor |
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Saturation Vapor Pressure |
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maximum amount of water vapor air can hold at a given pressure and temperature |
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Relative Humidity Equation |
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Relative Humidity= vapor pressure/saturation vapor pressure |
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temperature that you need to cool air to in order to condense water vapor |
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If relative humidity is not at 100%, air will cool at 10 degrees C/1000m |
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does not change as air ascends |
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Evaporation is a _____ process |
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Condensation is a ______ process |
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Sun heats ground, the air heats up and rises. Seen at the equator |
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air pushes from all directions |
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cold wedge and warm wedge hit --> warm air goes up and cold air goes down (Polar Vortex) |
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rain shadow effect. Air moves up a mountain and rains and then becomes dry on as it moves down the other side |
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How much energy is absorbed by the Earth? |
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convert energy from the sun to produce complex organic compounds |
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may exchange energy, but never matter, self-contained |
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exchange both energy and matter with component parts and the surrounding environment |
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living and dead, abiotic and biotic systems of life |
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how energy and matter move around/interaction between components that alters patterns within an ecosystem as time passes |
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important check, counteract changes |
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reinforce or perpetuate a change |
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What is the chemical base for all life? |
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Carbon dioxide+water -> oxygen+water+sugar |
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Sugar+oxygen->carbon dioxide+water |
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Climate=f(T,P, day-length) |
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2 Control Influences of Climate |
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The amount (biomass) Form (physiognomy) |
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mass of living biological organisms in a given area or ecosystem at a given time |
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Global Net Primary Productivity |
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The warmer it is the more plants that will grow in that location |
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Allocation of the Sun's Energy to Primary Producers |
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20% absorbed 14.5% respiration maintaining systems 5.6% net primary productivity 2.8% consumption 2.8% Biomass remaining (making plants bigger) |
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