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Earth Systems Exam 2

TermDefinition
air masses large bodies of air with similar temperature and moisture
cP (continental polar) cold and dry
mP (maritime polar) cold and moist
mT (maritime tropical) warm and moist
cT (continental tropical) hot and dry
A (arctic) extremely cold
fronts boundaries between air masses
cold front cold air pushes under warm air --> storms, heavy rain
warm front warm air slides over cold air --> gentle rain, clouds
stationary front air masses dont move --> cloudy, wet weather
occluded front cold front catches warm front --> complex storms
midlatitude cyclones large- low pressure systems
cyclogenesis first, storm begins forming
mature stage second, storm is strongest
occlusion/decay third, storm weakens
movement of midlatitude cyclones usually moves west --> east across North America
anticyclones high-pressure systems --> calm, clear, fair weather
Saffir- Simpson scale rates hurricanes 1-5 by wind speed and damage
features of tropical cyclones/hurricanes spiral rain bands around a calm eye
equator factor hurricanes cannot form at the equator because of the Coriolis effect is too weak to make air spin
convective storms caused by rising warm air
mature stage of thunderstorms most intense stage --> heavy rain, lighting, strong winds
climographs show average monthly temp (line) and precipitation (bars) for a location, used to describe climate patterns
Af tropical rainforest --> hot, wet all year
Aw tropical savanna --> wet and dry seasons
Am tropical monsoons --> heavy seasonal rain
Csb mediterranean --> mild summer, dry summer
Bs steppe --> semiarid, some rain
Bw desert --> very dry
ET tundra --> cold, little vegetation
EF ice cap --> very cold, permanent ice
mediterranean climate dry summers, subtropical high pressure systems block rain
paleoclimatology study of ancient climates
climate proxies solution to direct measurements (thermostats) dont go far back enough
tree rings rainfall and temp
ice cores trapped gasses for past CO2 and temp
sediments ocean/lake history
pollen past vegetation
corals past sea temps
GCMs (global climate models) simulate climate systems
RCPs and SSPs scenarios predicting future climates based on emissions
hydrosphere all the water on earth (solid, liquid, gas) - includes oceans, lakes, rivers, groundwater, ice and water vapor
cryosphere all FROZEN water on earth- glaciers icecaps, icebergs, sea ice
icebergs made of freshwater, less dense than seawater --> they float, about 90% is below the surface
ice shelves floating edges of glaciers/ice sheets attached to land and extend out over the ocean
porosity how much space is in soil/rock, how much water it can hold (storage)
permeability how easily water can flow through it and how fast it can move
water table the top of groundwater, boundary between dry and fully saturated ground
zone of saturation area below the water table, all spaces filled with water
aquiclude a layer that blocks water flow (like clay)
cone of depression a dip in the water table caused by pumping water from a well, water levels drop around the well forming a cone shape
biodiversity variety of all life in an area
genetic diversity differences within a species, helps populations adapt to change, low genetic diversity = higher extinction
species diversity number of species
ecosystem diversity different habitats
species richness the number of different different species in one area
biome a large region like a desert
ecosystem smaller more specific within a biome
light needed photosynthesis
moisture water availability
temperature affects survival ad growth
wind can dry out or damage plants
edaphic conditions soil factors (nutrients, texture, drainage)
photoperiodism organisms and responding to day length (like flowers and the seasons)
succession how ecosystems change over time, gradual replacement of one plant community by another
primary succession starts from bare ground (no life)
pioneer community first organisms to grow there (hardy like moss)
climax vegetation final, stable plant community
Whittaker biome diagram show biomes based on temps (x-axis) and precipitation (y-axis), helps identify what biomes exists in certain climate conditions
how to read biome diagram 1. find temp (left cold, right hot) 2. find precipitation (bottom dry, top wet) 3. locate where they meet, thats the biome
predict changes if precipitation decreases but temperature stays the same: biome becomes drier (ex. forest ---> grassland)
crust outermost, thinnest layer
mantle thickest layer, semi-solid, where magma forms
core innermost layer, very hot (outer core liquid, inner core solid)
magma molten rock below earths surface, when reaches surface it is called lava
Alfred Wegener proposed contents were once joined
Pangea ancient super continent
seafloor spreading new crust forms at mid ocean ridges
paleomagnetic patterns magnetic strips in ocean rust show movement, ocean floor rocks are older the further form the ridge
divergent plates move apart, new crust forms
convergent plates collide, forms mountains
transform plates slide past each other, causes earthquakes
sedimentary rocks formed from weathered material
erosion rocks broken down and moved
deposition material is dropped
compaction pressure squeezes it
cementation minerals glue it together
Created by: user-2034746
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