Unit 3 Flashcards
Thermosphere
Not many gases
Where satellites orbit ans the aurora’s are found
Mesosphere
Coldest layer
Where most meteorites burn
1st layer to have atmospheric gasses
Stratosphere
Where ozone is that protects us from uv radiation
No weather
Exosphere
Space
Troposphere
1st 10 km
Where airplanes fly and weather occurs
Weather
Short term changes of an area
Occurs in troposphere
Climate
Long term average weather of an area
Atmosphere
78% nitrogen ans 21% oxygen
Air has more weight and density closer to ground
Higher you go = lower temp and lower pressure
Factors that contribute to climate ans weather
Earths tilt and orbits
Unequal heating kf earth
Atmospheric convention current
Earths rotation
Oceans
Microclimayes
Earths tult and orbits
Axis of 23.3 degrees
365.25 days to orbit
Part of earth tilted toward sun will experience summer because of direct rays
Part of earth tilted away from sun will experience winter bc of less direct rays
Seasons caused by angle of which rays hit earth
Unequal heating of earth
Equator receives most direct and constant sun = stable and warm climates
Closee to poles = increasing angle = temp decrease
Atmospheric convection currents
Adiabatic hearing ans cooling
Are is wadmes by sun radiation = less dense and less pressure = rises
High altitudes = air cools and continues to rise being bushed by hot air
Cold air precipitated
Cool air falls to ground and rewards
Large scale currents called cells
Earths rotation
Earth spins counter clockwise in n hemisphere and clockwise in s hemisphere
Coriolis effect: wind ans water deflected right in n hemisphere and left in s hemisphere
Effect is largest and poles ans smallest at equator
Global winds
6 convection cells
2 polar cells at poles
Ferrell cells from 60 to 30 degrees
2Hadley cells from 30 to equator
60 degrees latitude
Westerlies
30 latitude
Cool air falls
High pressure deserts
Equator
Warm air rises
Low pressure rainforest
Oceans
Driven by winds
Sea breeze
Land heats up faster than ocean
Breeze will blow from sea (high prssure) to land (low pressure)
Ocean gyres
5 massive circular current systems caused by the coriolis effect
Upwellings
Winds push water away from coast and js replaced with nutrients dense deep ocean water
Plankton use these nutrients to produce energy, supporting their food we’ve
Takes past along w coast kf some continents
El nino
Some yrs tropical trade winds slow down or reverse direction
Push warm waters toward the coast = mo unwilling
Collapsed food web
Economic loss from fishing
Rainy and floody in s America
Droughts ans wild fires in Australia
la nina
an enhancement of natural tropic trade winds/ opposite of el nin
more upwelling = more biodiverse food web and fishing $
cold and dry in S america and wet in australia
microclimates
climate of a local area is i=different from the general climate around it
caused by humidity, elevation, and urban islands
humidiity
WATER HAS a high heat capacity = temp change resistant
more humid a place is = less temp fluctuation b/w day and night
warm air holds onto moisture more
caused by: air temp, proximity to water, and evapotranspiration
elevation
elevateed terrain lifts air until it cools and percipitates
rainshadow effectr
rainshadow effect
LEEWARD SIDE OF A MT HAVING ARID CONDITIONS DUE TO THE COOLING/PRECIPITATION THAT OCCURON THE WINDWARD SIDE
urban island heat
man-made microclimate
metro area temp is hootter in city than outside
caused by buildings bloking colder air, industry heat, little vegetation, dark surfaces
albedo
percetange of incoming sunlight that is reflected from a surface
a white surface has a higher albedo than a blakc surface
solutions ot urban island heat
strategic building so that wind passes through city
place factories on outskirs
light colored buildings
increase green spaces
use less energy
most important climatic factors
temperature and percipitation
glbal rainfall
depends on global winds driven by the sun
rays hiting the equaot causies air to rise and then percipitate
tropical rainforest
highest percipitation
most stable temperature
high humidiity
large tropic trees
highet biodiversity
epiphytes
nutrient poor soils
hot deserts
low rainfall
occur at latittures of 30 north and s of equator
plants and animals need special adaptations
savanna/tropical grassland
open grassland w/ scacre shrubs and trees
b/w rainforests and deserts
warm temp yr round
periodic fires
wet and dry seasons
large herbivores and predators dominate
temperate grasslands
cooler temps than tropical grasslands
wet and dry seasosns are much more dramatic
praries
seasonal precipitation
lower biodiversity than tropical grasslands
richest soils
ex” great plains
temperate rainforests
yr round rainfall
large, old growh trees
seen at higher latitudes than tropical rainforests
moderate temps
temperate decidupus forest
dominated by decidous trees like oak, hickory, elm, maple and ash which lose leaves in winter
moderate rainfall
dramatic appearance of all 4 seasosn
coniferous forest/taiga.boreal forest
largest biome
higher latittude than deciduous
coniferous trees that dont lose their leaves in winter: pine
shorter growing season
ong cold winters, mild summers
high humidity
moderate percipitation
ex” redwoods
chaparral
coastal biome
hot, dry summers and mild, rainy windters
spiny evergreen shrubs
maintaed by fire
tundra
cold desert
bitter cold, high winds
short growing season
permafrost
arctic
low perciptation
primary productivity
a measure of producers in an ecosystem
NPP = GPP - R
helps perdict biomass/biodiversiy in other trophic levels
rainforest = highest
desert = lowest
tundra = 2nd lowest
deforestation
tropical rainforests using land for soul, cattle, and palm oil
loss of biodiversity
more co2
timber operations more regulated in US
soil erosion
tilling
overgrazing
compaction
salination
soultion: leve it alone
climate change
heating of the planet is causing weateher patterns and biomes to shift
extended growing seasons
changes in migration
droughts = fires
melting permafrost = release of carbon = positive feedback loop
lithosphere
crust
asthenosphere
upper liquid mantle