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the increase in average global temperatures |
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those gases capable of absorbing and re-emitting infrared radiation (See page(s) 102) |
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process by which atmospheric gases trap and return a major portion of the heat (infrared radiation) radiated by the Earth (See page(s) 103) |
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enhanced greenhouse effect" |
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process in which atmospheric gases trap and return more than 80% of the heat energy radiated by the Earth (See page(s) 105) |
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four-cornered figure with four equal triangular sides (See page(s) 111) |
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numbers often expressed in units of cm-1 and used on the x-axis of an infrared spectrum; inversely proportional to wavelength (See page(s) 116) |
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noncontinuous energy distribution that consists of many individual steps (See page(s) 71, 118) |
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natural reservoir that removes CO2 from the atmosphere (See page(s) 121) |
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average mass of an atom of an element compared with an atomic mass of exactly 12 amu for carbon-12 121; mass (in grams) of the same number of atoms found in exactly 12 g of carbon-12 (See page(s) 122) |
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number of atoms in exactly 12 g of carbon-12 (See page(s) 122) |
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an Avogadro's number of objects (See page(s) 123) |
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mass of one Avogadro's number, or "mole," of whatever particles are specified (See page(s) 124) |
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global atmospheric lifetime |
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time required for a gas added to the atmosphere to be removed. Also referred to as the "turnover time." (See page(s) 126) |
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bacteria that can function without the use of molecular oxygen (See page(s) 127) |
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ratio of electromagnetic radiation reflected relative to the amount of radiation incident on a surface (See page(s) 131) |
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factors that affect the annual global mean surface temperature (See page(s) 131) |
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process of keeping some things apart. Chemically this is accomplished by forming stable bonds between the sequestering agent and the substance "trapped." (See page(s) 136) |
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