a t m o s f e r a
- wind develops from spatial difference in atmosphere pressure
- result from uneven absorption of solar radiation
- isolines indicate pressure
- newton's second law of motion
- force = ( mass x acceleration )
- acceleration = force/mass
- wind acceleration is measured by density, pressure, and newtons
- intense area of temperature difference results in frontal zone / front
- frontal zones not moving against each other are stationary fronts
- warm front happens when warm subtropical moist air mass replaces cold dry polar air mass
- occluded fronts are cold fronts catching up and overtaking warm front
- cold type occluded: air behind front is colder than air ahead
- warm type occluded: air behind front is warmer than air ahead
- in the tropics weather is dominated by storms that form in intertropical convergence zone, subtropical high pressure zone, oceanic disturbances in trade winds
- intertropical convergence zone has wide band of cumulus & cumulonimbus clouds
- hurricanes are powered by latent heat energy released from condensation
v o c a b u l a r i o
- wind: air in motion
- anemometer: measures wind speed
- wind vane: measures wind direction
- air mass: large body of air of relatively similar temperature and humidity ( continental or maritime )
- source region: area of formation of air mass ( equatorial, tropical, polar, arctic )
- thunderstorms: form when moistunstable air is lifted vertically into atmosphere, releases latent heat
- mesocyclone: severe thunderstorms that develop strong vertical updraft
- tornado: vortex of rapidly moving air
- tropical depression: storm whose wind speed increases between 37 to 63 kmph
e s t r u c t u r a
- troposphere about 80% of atmospheric mass
- tropopause is top of this area, thicker over equator and thinner at poles
- thermosphere slowly merges into space
- mesosphere coldest layer
- stratosphere warming with height
h i s t o r i a
- most tornadoes happen in united states in april, may, june, july
- 40k tornadoes have happened overlast 50 years
- 689 died in missouri / illinous / indiana in 1925
- oklahoma 1999 por 6 horas 70 tornados spawned
o c e a n o s
- contain 97% of earth's water
- atlantic ocean makes up 21% of earth's surface area, receives freshwater from terrestrial runoff
- arctic ocean is smallest at 3% surface area
- indian ocean covers 14% has deepest point at java trench of 7258 meters
- pacific ocean largest region covering 30%
- southern ocean occupies 4% has deepest point at south sandwich trench
a g u a g l o b a l
- humidity is measured by three factors
- mixing ratio: mass of specific gas component relative to mass of remaining gas components
- saturation mixing ratio: mass of water vapor that can be held in kilogram of dry air at saturation
- relative humidity: amount of water in air relative to saturation amount air can hold at given temp. x100
- clouds formed by condensation or deposition
- orographic uplift air forced to rise because of phycisal presence of elevated land
- convectional lifting surface heating of air at ground surface
- convergence / frontal lifting two masses of air come together
- radiative cooling sun is no longer supplying ground and overlying air with energy
- clouds with temp. below freezing develop large ice crystals because of vapor pressure difference between ice crystals and supercooled water droplets
- types of fog
- radiation/ground near surface cooling of atmosphere due to longwave radiation, shallow
- upslope air flows over higher topography, hills or mountains
- advaction air flows over suface with different temp.
- evaporation/steam/sea smoke type of advaction fog where cold air advances on warm air
- frontal on warm fronts when rain descends on colder air
v o c a b u l a r i o
- humidity: water vapor in atmosphere
- saturation: addition of water vapor to mass of air leads to condensation
- precipitation: liquid or solid deposit that forms in saturated atmosphere
- dew point: temp. at which water vapor saturates from air mass into liquid
- if below freezing it's called frost point
- change of states of water
- condensation: vapor → liquid
- freezing: liquid → solid
- deposition: vapor → solid
- rain: liquid deposit that falls from atmosphere diameter 0.5-5 millimeters
- freezing rain: falling water droplets meet surface below 0°C
- temperature inversion: warm air found on top of cold air
- ice pellets / sleet: translucent spheres of frozen water
- snow pellets / graupel: spherical bits of ice diameter less than 5 millimeters
- hail: frozen precipitation more than 5 millimeters diameter
- fog: cloud of minute water droplets at ground level
l i t o s f e r a
- earth is ~ 4.6 billion yrs
- big bang creates earth from molten mass from solar nebula
- giant impact from body ~ 4.5b creates tilt & moons
- water brought by comets & asteroids
- life emerges in cambrian ~ 580m
- measures of time
- eons, eras, periods & epochs
- hadean eon = no life
- archaen = simple life
- proterozoic = multicellular
- anthropocene is modern life
- humans permanently affect geographical force
- mid-20th century with industrialization & globalization
- plate boundaries & tectonics
- 3 main types
- divergent (constructive) moving apart, creates new crust
- convergent (destructive) move together, subduction and collision
- transform (conservative) slide/grind alongside
- caused by mantle convection
- move from divergent to convergent zones
- plate tectonics split in pangea ~260ma
r o c k c y c l e
- minerals combine to make rock
- igneous formed by solidification of molten magma
- metamorphic forms from recrystallization of other rocks through pressure increase, temperature rise, chemical alteration
- sedimentary formed by the deposition/alteration/compression or lithification of weathered rock debris, chemical precipitates, organic sediments
- geological provinces: shield, platform, orogen, basin, lip, extended crust
m a s s w a s t i n g & f l o o d i n g
- downslope movement of earth materials
- shear stress - downslope by gravity acting on mass (t)
- shear strength - retaining forces by particle arrangement, friction, moisture (s)
- factor of safety: (resisting force) / (driving force) or s/t
- fs > 1 stable
- fs < 1 unstable
- process-response system
- hillslopes receive solar radiation, precipitation, weathering
- output evapotranspiration
- controlling factors are strength of slope materials, oversteepening, water content
- F = W sin Ø
- f gravitational force
- w weight of material
- Ø angle of slope
- heavy rainfall causes instability
- soil saturation increases weight
- reduces cohesive bonds between individual soil particles
- bedding plane on hillslopes makes other plane slide across lubricated surface
- clays & slit slopes have unique mass wasting, rotational slip and mudflow
- floods are most common natural hazard, occur when flow height > channel capacity
- 4 types of floods
- regional, high ppt snowmelt
- flash, high ppt in mountains
- ice jam, ice damming
- dam failure, breech of levees or dams
- predited by recurrence interval aka flood probability
- riverflow sources are runoff, interflow
- water movement in soil controlled by gravity, capillary action, and soil porosity
- stream discharge equation Q = W x D x V
- q stream discharge
- w channel width
- d channel depth
- v velocity of water
v o c a b u l a r i o
- deposition: change in state of matter from gas to solid that occurs with cooling
- subducting plate: plate being pushed down by convergence
- evatranspiration: loss of water to atmosphere via evaporation and transpiration
- rainsplash: microscale process of soil erosion from impact of raindrops
- rill: small steep sided channel carrying water
- soil creep: movement of sediments in cyclical steps, caused by temp fluctuations, moisture, gravity
- solifluction: slow movement of soil caused by freeze-thaw action
- interception: capture of precipitation by plant canopy and evaporation or sublimation
- streamflow: water flowing in the organized channels of a stream or river
- stemflow: process that directs precipitation down plant branches and stems
- canopy drip: directs rainfall or snowfall along the edge of the plant canopy
- throughfall: process of precipitation passing through the plant canopy
- infiltration: movement of water into soil layer
- hygroscopic water: held within 0.0002 millimeters of soil surface, non-mobile, only removed via heating
- matric force: soil water from 0.0002 to 0.06 millimeters from surface
- capillary water: moves horizontally and vertically in soils by the process of capillary action
- gravitatonal water: moves through soil due to gravitational forces
- wilting point: point at which the rate of water leaving a plant's leaves > water uptake by the roots
- throughflow: sporadic horizontal flow of water within soil layer
[http://www.physicalgeography.net/fundamentals/images/ground_hydro.jpg]