Java Games: Flashcards, matching, concentration, and word search.

APES Ch 4 Vocab Review

Global Climates and Biomes

AB
layers of atmospheretroposphere (temp decreases), stratospere (temp increases due to ozone layer absorbing UV), mesophere (temp decreases), thermosphere (temp increases)
albedoreflectivity of a surface. ice, snow, clouds, and water have high albedo. land, pavement have low.
hadley cella convection current in atmosphere between the equator and 30 degress N/S. Warm air rises @ equator creating a low pressure, wet weather system. Air sinks at 30 degrees creating dry, desert conditions.
ferrell cellatmospheric convection cell between 30 and 60 degrees
polar cellatmospheric convection cell between 60 and 90 degrees. Cold air sinks at poles creating high pressure system with dry weather.
ITCZintertropical convergence zone. An area of earth that receives the most intense sunlight; where the ascending branches of the two Hadley Cells converge.
Coriolis Effectthe deflection of an objects path due to the rotation of Earth. Bends ocean and wind currents clockwise in norhtern hemisphere, counterclockwise in southern hemisphere.
gyresa large scale pattern of wate circulation that moves clockwise in northern hemisphere and counterclockwise in the southern hemisphere, due to Coriolis effect. See map of ocean currents!
Thermohaline circulationThermo=temperature/Haline=salt. This is an oceanic circulation pattern where salty cold water sinks in northere oceans and circulates until it is warmer and less dense, rising in southern oceans. Thermohaline circulation drives the mixing of surface and deep ocean water.
ENSO (El nino southern oscillation)The periodic slow down in trade winds over equatorial Pacific Ocean, which normally blow from west to east. (See Map!!) This causes a large mass of warmer ocean water. The changes prevent upwelling along coast of South America (bad!), wet weather in South America, dry weather in Australia and Indonesia (See Map!). Global weather changes include wetter conditions in SE U.S. and dry weather in S Africa, S.E. Asia.
Rain shadowA region with dry conditions found on the leeward side of a mountian range as a result of humid winds from the ocean causing precipitation on the windward side of a mountain
Latent heat releasethe release of energy when water vapor in the atmosphere condenses
terrestrial biomestundra, taiga (boreal), temperate rain forest, temperate deciduous forest, grassland, chapparel, desert, savanna, tropical rainforest
fire adapted biomesgrassland, chapparel
lake zoneslittoral, limnetic, profundal, benthic (be able to label or describe)
ocean zonesintertidal, photic, aphotic, benthic
chemosynthesisa process used by some bacteria in the ocean to generate energy using chemicals instead of light, such as methane and hydrogen sulfide
types of wetlandsswamps, marshes, bogs, estuaries, mangroves. (know characteristics of each!)
wetland identificationsoil saturated with water all or part of year, special hydric soil, special plants adapted to wet conditions
wetland servicesspongy soil absorbs water preventing flooding, water filtered and cleaned by soil and bacteria, has high biodiversity and several endangered species, carbon sequestation due to high primary productivity
coral reefthe most diverse marine biome on earth, found in warm, shallow waters beyond the shoreline
coral bleachinga phenomenon in which algae inside corals die, causing corals to turn white
upwellingthe upward movement of ocean water toward the surface as a result of diverging currents. Brings up nutrient rich water that food chains depend on.
specific heata measure of the ability of a substance to change temperature. Water has a high specific heat compared to land because it takes greater energy to change temp. Causes land and sea breezes.


Biology & AP Environmental Science Teacher
Burnt Hills-Ballston Lake High School
NY

This activity was created by a Quia Web subscriber.
Learn more about Quia
Create your own activities