Chapter 2 Flashcards
A measure of the ability of a solution to behave as an acid, a compound that releases protons (H+) to the water in which it is dissolved.
Acidity
The amount of solar radiation reflected by a surface, usually expressed as a percentage of the incoming solar radiation.
Albedo
A measure of the ability of a solution to behave as a base, a compound that takes up protons (H+) or releases hydroxide ions (OH–).
Alkalinity
The pressure exerted on a surface due to the mass of the atmosphere above it.
Atmospheric Pressure
The long-term description of weather, based on averages and variation measured over decades.
Climate
The transfer of sensible heat through the exchange of kinetic energy between molecules due to a temperature gradient.
Conduction
The climate typical of terrestrial areas in the middle of large continental land masses at high latitudes, characterized by high variation in seasonal temperatures.
Continental Climate
The transfer of sensible heat through the exchange of air and water molecules as they move from one area to another.
Convection
The apparent deflection of air or water currents when viewed from a rotating reference point such as Earth’s surface.
Coriolis Effect
An oscillation of pressure cells and sea surface temperatures in the equatorial Pacific Ocean that causes widespread climatic variation and changes in upwelling currents.
El Niño Southern Oscillation (ENSO)
The warm surface layer of water in a lake, lying above the thermocline, that forms during the summer in some lakes of temperate and polar regions.
Epilimnion
The sum of water loss through evaporation and transpiration.
Evotranspiration
A large-scale, three-dimensional pattern of atmospheric circulation in each hemisphere, located at mid-latitudes between the Hadley and polar cells.
Ferrell Cell
Atmospheric gases that absorb and reradiate the infrared radiation emitted by Earth’s surface, including water vapor (H2O), carbon dioxide (CO2), methane (CH4), and nitrous oxide (N2O).
Greenhouse Gases
A large-scale, three-dimensional pattern of atmospheric circulation in each hemisphere in which air is uplifted at the equator and subsides at about 30° N and S.
Hadley Cell
The amount of energy required to raise the temperature of a substance.
Heat Capacity