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uneven warming pattern
variation in angle sun’s ray hits earth
variation in surface area sun’s ray is distributed
albedo
equator
receives sunlight at 90 degree angle
albedo
percentage of incoming sunlight reflected off surface
perpendicular
region near equator (tropics) sun’s ray hits earth at a _____ angle
travels a shorter distance to equator than other latitudes
more solar energy than mid-latitudes and polar regions
oblique
at higher and lower latitudes, sun’s ray hit at an ____ angle
smaller surface
when sun’s ray hits equator, solar energy is distributed over ____ ____ than near poles
more solar energy/square meter
white surface
__ ___ has higher albedo (reflects more solar energy) than black surface, stays cooler
ex. dense forest = low albedo
snow covered polar regions = high albedo
axis of rotation
__ __ __ is tilted at 23.5 degrees, so amount of solar energy reaching various latitudes shifts over course of year
earth’s tilt
an orbit around the sun causes seasonal changes in temperature and precipitation
more pronounced when northern hemisphere is toward sun and southern hemisphere is away, and vice versa
december solstice
northern hemisphere is tilted AWAY from sun, shortest day of year
at tropic of capricorn at 23.5 degrees south latitude
NH = winter
SH = summer
march equinox
sun is directly over equator, entire earth gets 12 hours day/night
NH = spring
SH = fall
june solstice
northern hemisphere is tilted TOWARD sun, longest day of year
over tropic of cancer at 23.5 north latitude
NH = summer
SH = winter
september equinox
sun is overhead equator, everywhere has 12 hours day/night
NH = fall
SH = spring
axis of rotation’s tilt
causes seasons
solstice
longest/shortest day of year
earth’s axis tilted away/toward sun
equinox
day and night are EQUAL in length
adiabatic cooling
cooling effect of reduced pressure on air as it rises higher in atmosphere and expands
saturation point
maximum amount of water vapor in air at given temperature
latent heat release
release of energy when water vapor in atmosphere condenses in liquid water
adiabatic heating
heating effect of increased pressure on air as it sinks toward surface of earth and decreases in volume
atmospheric convection current
global patterns of air movement initated by unequal heating of earth
atmospheric convention current
major contributor to different climates and move air and moisture around globe
cycle of air
warming at earth’s surface causes air to rise → lower pressure, adiabatic cooling, latent heat release
cool air at top of atmosphere is displaced horizontally then sinks
experiences adiabatic heating + moves horizontally
intertropical convergence zone
ITCZ
latitude that receives MOST intense sunlight, causes ascending branches of 2 hadley cells to converge
hadley cell
convection current in atmosphere that cycles between equator and 30 deg N and 30 deg S
trade wind
caused by hadley cells
hadley cell
atmospheric convention current between 30 deg N and 30 deg S
solar energy warms humid air in tropics → rises → cools below saturation point
air sinks to 30 deg N and 30 deg S → warmed by adiabatic heating
water vapor condenses into clouds and precipitation
CAUSES DESERT ENVIRONMENTS TO DEVELOP
polar cell
convection current in atmosphere formed by air
rises at 60 deg N and 60 deg S
sinks at 90 deg N and 90 deg S
ferrell cell
convection current in atmosphere between hadley cells and polar cells
air currents
driven by nearby hadley cells and ferrell cells
warm air from hadley cells move towards poles
cool air from ferrell cells move towards equator
westerlies winds
caused by ferrell cells
atmospheric convection current
responsible for locations of rainforest, deserts, grasslands bc determine patterns of temperature and precipitation
north to south
atmospheric convection currents cause air to move ___ to ___
but is DEFLECTED because earth is rotating
faster
as earth rotates, surface moves ___ at equator than mid-latitude/polar regions
faster rotation speeds at equator cause objects moving north or south to deflect
coriolis effect
deflection of object’s path due to rotation of earth
prevailing winds
produced by combination of atmospheric convection currents and coriolis effect
rain shadow effect
humid winds blowing inland from ocean meets MOUNTAIN RANGE
windward (wind facing) side of mountains: air rises and cool (adiabatic cooling), large amounts of water vapor condense to form clouds and precipitation
leeward side of mountains: dry air falls and warms (adiabatic warming), causes much drier conditions = rain shadow
ocean currents
driven by combination of temperature, gravity, prevailing winds, salinity, coriolis effect, continent location
warm water
expands and rises
raises surface of water in tropics to be 3 inches higher than mid-latitudes
slight slope + gravity causes water to flow AWAY from equator
gyre
large scale pattern of water circulation moving clockwise in NH and counterclockwise in SH
gyre
redistribute heat in ocean causing cold water from polar regions to move along west coast of continents
cool air above water brings cooler temperatures to these continents
gyre
driven by trade winds in tropics and westerlies in mid-latitudes
california current
causes coastal areas of california to have cooler temperatures than areas of similar latitudes along easy coast of us
upwelling
upward movement of ocean water toward surface because of diverging currents
west coast
upwelling occurs along __ __ of most continents
when surface currents diverge, deeper waters rise to replace water that has moved away
upwelling
brings nutrients from ocean bottom that supports producers → support large populations of fish
HIGHLY PRODUCTIVE ECOSYSTEMS
thermohaline circulation
oceanic circulation pattern that drives mixing of surface water and deep water
takes hundreds of years to complete
thermohaline circulation
crucial for moving heat and nutrients around globe
thermohaline circulation
driven by surface waters that contain unusually large amounts of SALT
mixes water of ALL oceans
gulf stream
originates in gulf of mexico but flows toward western europe + brings warmer water/temperature to cold places
englands average winter temperature is 20 deg celsius warmer than newfoundland canada (at a similar latitude)
el nino southern oscillation
ENSO
reversal of wind and water currents in south pacific between south america and australia/southeast asia
caused by shift in ocean currents
coast of south america
shifts regularly from el nino (warmer, rainier) to la nina (cooler, drier) conditions along ___ of __ ___
normal year
trade winds push warm surface waters from coast of SA towards australia and SE asia
promotes upwelling of water near SA
drier conditions in SA
wetter, warmer conditions on australia and SE asia
el nino southern oscillation
trade winds near SA weaken → warm equatorial water from western pacific (australia/SE asia) move toward west coast of SA
warm water/air suppresses upwelling off peru coast + decreases productivity there, reduces fish populations near coast
ENSO consequences
reduces upwelling off coast of SA → decreases nutrients, productivity, fish populations, income
ENSO consequences
causes warmer and wetter conditions in americas → increases flooding
ENSO consequences
causes cooler, drier conditions in australia and SE asia → drought
poor crop yields → death in developing countries
ENSO consequences
decreased hurricane activity in atlantic
ENSO consequences
weakened monsoon activity in india + SE asia
la nina
stronger than normal trade winds
east to west, warmer/rainier in australia/SE asia
increased upwelling off coast of SAS → cooler conditions, extra fisheries