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52 Cards in this Set

  • Front
  • Back

Tundra

frozen biome in far north latitudes




Soil is permafrost




very short growing season

Taiga / Boreal Forest

coniferous forest - trees with needles




Canada and Siberia




Largest source of wood for timber companies

Temperate Deciduous forest

deciduous trees - lose their leaves in winter




leaf litter makes soil rich

Tropical Rainforest

equitorial forests with lots of rain




nutrient poor soil




most diverse biome

Savanna

African grassland biome




Fire maintains soil fertility




wet and dry seasons

Chapparal

Shrubland near the coast




dry




plant leaves contain flamable oils




depends on fire to burn away competition

Littoral zone

shallow area near the shore




emergent plants grow here




most life is here

Limnetic zone

shallow area far from shore




phytoplankton and zooplankton are base of food chain here

Benthic zone

the bottom of a river / lake / pond




decomposers live here

Wetlands

Very valuable biome, but most have been destroyed




Important ecosystem services


- spawning + nesting habitat for fish/birds


- filter pollution out of water


- source of crops like cranberries


- control stormwater runoff



Mangrove swamp

Trees with roots that can grow in salt water




roots provide important habitat for many fish




prevent coastal erosion

Coral reefs

most diverse marine biome




mutualistic relationship between coral polyp and bacteria inside




corals bleach and die when stressed

Independent variable

the thing which is changed or altered in the experimental group

dependent variable

the variable that is measured in an experiment

experimental group(s)

group or groups in an experiment which are altered in some way

control group

a group in an experiment which is LEFT ALONE, it is not changed as part of the experiment

hypothesis

a testable if ...then statement describing a directional change in the dependent variable in response to the independent variable.

constants

variables in an experiment which are kept the same between the experimental and control groups

positive feedback loops

result in amplified change...




change happens more and more, faster and faster

negative feedback loops

dampen change




return the system to back to its normal state

igneous rocks

form from the cooling and hardening of magma and lava




make up most of the Earth's crust

metamorphic rocks

form from existing rocks that have been altered by intense heat and pressure

sedimentary rocks

form from pieces of other rocks cementing together




make up most of earth's surface rocks

lithosphere

the Earth's crust




outer most layer




broken into plates

asthenosphere

layer beneath the crust




plastic flowing magma




driven by convection currents

stiffer mantle

3rd layer down in the Earth




Mostly superheated rigid magma

outer core

liquid iron and nickle

inner core

solid iron and nickle




most dense layer

evidence for plate tectonics

coastlines of S America and Africa match




earthquakes and volcanoes occur most frequently at plate boundaries




same fossils on distant continents




age and magnetic orientation of rocks at spreading centers



diverging boundary

forms where 2 plates are separating




occurs in middle of oceans




creates a ridge and rift valleys

transform boundary

occur where 2 plates slide along side each other




faults




frequent earthquakes

collision boundary

occurs where 2 continents coverge




forms mountains

subduction boundary

occurs where oceanic plates and continental plates converge




oceanic plate sinks




many earthquakes and volcanoes




tsunamis generated when plate movement displaces water

troposphere

lowest layer of the atmosphere




where we live




where weather occurs




contains most of the air




contains all water va[pr

stratosphere

second layer of the atmosphere




ozone (O3) layer is here



ozone layer

absorbs UV radiation that causes skin cancer




in the stratosphere

atmosphere

thin layer of gasses surrounding Earth




79% Nitrogen (N2)


29% Oxygen (O2)


2% mix of other stuff like CO2 and H2O

weather

condition of the atmosphere at one point, and for one moment of time

climate

average weather conditions for a region over a period of decades

insolation

incoming solar radiation (aka sunlight)


source of all energy on earth




angle that it hits Earth's surface effects temp




low angle at poles = cold always




high angle at equator = hot always

albedo

ability of a surface to REFLECT light




light smooth surfaces = high albedo


dark rough surfaces = low albedo

infrared energy

aka heat




Earth gives off energy as insolation




Absorbed and refelcted back to earth by greenhouse gases

adiabatic cooling

warm air near Earths surface rises




as it rises air pressure decreases allowing it to expand and cool



adiabatic heating

cool air high in the atmosphere sinks




as it sinks pressure increases causing it to contract and warm

latent heat release

as air rises and cools water vapor condenses




this release energy causing air to cool further

Earth's tilt and revolution effect climate

Tilted 23.5 degrees




when N Hemisphere is tilted towards the Sun we have summer




when S Hemisphere is tilted towards Sun we have winter

Earth's rotation effects climate

Coriolis effect causes winds and currents to be deflected




cause by rotation

gyres

looping surface currents on the ocean




driven by differences in temperature




distribute heat from equator to higher latitudes

thermohaline conveyor

global super current that connects all oceans as well as the surface and deep parts of the ocean




driven by differences in salinity




cold high salinity water sinks off the coast of greenland



upwelling

cold nutrient rich water rises to the surface off the WEST COAST of continents




major source of nutrients for fish populations

windward side of mountain

side being hit by wind




always receives more precipitation

El Nino

cyclically occurring reversal of ocean currents in the tropical Pacific




Warm waters reverse, and move towards Central and South America