Lesson 2: The Physical Environment 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
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
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.
evapotranspiration
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
The densest, coldest water layer in a lake, lying below the thermocline.
hypolimnion
Of or relating to a condition of oxygen depletion, usually below a level that can sustain most animals.
hypoxic
The zone of maximum solar radiation, atmospheric uplift, and precipitation within the tropical zone.
Intertropical Convergence Zone (ITCZ)
The amount of solar radiation reflected by a surface, usually expressed as a percentage of the incoming solar radiation.
albedo
The rate at which atmospheric temperature decreases with increasing distance from the ground.
lapse rate
Heat transfer associated with the phase change of water, such as evaporation, sublimation, or condensation.
latent heat loss
The climate typical of coastal terrestrial regions that are influenced by an adjacent ocean, characterized by low daily and seasonal variation in temperature.
maritime climate
Cycles of regular change over thousands of years in the shape of Earth’s orbit, in the angle of tilt of its axis, and in its orientation toward other celestial bodies that change the intensity of solar radiation received by Earth.
Milankovitch cycles