Definitions Flashcards
Atmosphere
thin blue region on edge of Earth
Hydrosphere
liquid realm
Lithosphere
rock and geologic material
Biosphere
where life exists
Enviro Lapse Rate (ELR)
temp decreases with altitude
-does not involve movement of air parcel
Air Pollutant
gas, aerosol, particulate added to atmosphere that have harmful effects/affects climate
Primary Pollutants
direct product of combustion/evaporation
-have natural sources-volcanic eruptions, dust storms
Secondary Pollutants
products of interactions with primary pollutants
ex: nitric acid
Point Source
one controllable sight
ex: smoke stacks
Fugitive Sources
open areas exposed to wind action
ex: land clearing
Area Sources
well defined areas within which several sources of air pollutants
ex:small urban communities
Mobile Sources
move place to place while emitting pollutants
ex: car
Rayleigh Scattering
short wavelengths likely to scatter
Transmission
solar radiation passing thru air un-interupted
Insolation
incoming solar radiation (related to solar angle)
Albedo
percent of shortwave radiation returning from given surface compared to amount of radiation striking surface
Conduction
transfer of heat from molecule to molecule
Convection
transfer of heat occurs as a mass movement of fluid
Industrial Smog
fog/humid air and sulphur dioxide/particulates from burning coal
Photochemical Smog
sunlight and nitrogen oxides/volatile organic compounds
Humidity
amount of water vapour in air
-warm air can hold more liquid than cold
Absolute humidity
mass of water vapour per volume of air
- increase in V=decrease in abs. humidity
- decrease in V=increase in abs. humidity
Specific humidity
given mass of water vapour in given mass of air
- actual quantity of water vapour in air
- volume does not affect
Unsaturated Air
- water escapes into overlying air due to evaporation
- some vapour collides and bond thru condensation
Saturated Air
equilibrium between evaporation and condensation
Dew Point
temp at which saturation occurs in air
-dependant on amount of water vapour present
Relative Humidity
amount of water vapour in air relative to max that can exist at given temp/saturation point
Dry Adiabatic Lapse Rate (DALR)
temp decrease with increase elevation
- unsaturated
- cooling/warming constant
Moist Adiabatic Lapse Rate (MALR)
lesser rate than DALR
- saturated
- not constant, varies w temp
Atmospheric Stability
comparing temp of rising parcel to surroundings
Absolutely Stable Air
air cooler/heavier (denser) than surrounding
-occurs when ELR less than SALR
Absolutely Unstable Air
warm, less dense than surrounding air
-DALR less than ELR
Orographic Uplift
occurs when mass of air deflected over/around terrain
-upward movement of air=adiabatic cooling=cloud formation/precipitation
Convergence
horizontal movement of air into region
Fog
surface cloud formed when air cools to dew pt. as moisture added/when cooler air mixed w moist air
Radiation fog
form on clear/calm nights when cool moist air is overlay by dry air and rapid radiation cooling occurs
Advection fog
when warm, moist air moves horizontal over cold surface and moist air cools to dew pt.
Upslope fog
as moist air rise and cools and condenses over elevated terrain/orographic barrier
Evaporation fog
cool air in contact w warmer water structure is warmed by water and became saturated by evaporation
Precipitation
any form of water that falls from cloud and reaches ground
Accretion
where falling ice crystals may freeze cool waterdrops on contact forming ice particles
Aggregation
process of ice crystals colliding and sticking together =snowflake
Cryosphere
where natural material (water/soil) occurs in frozen form
Permafrost
ground which temp
Acidification
increase of conc. in H+ in water/soil
-occurs thru wet deposition, precipitation of acids, dry deposition (acid in dust/smoke)
Buffers
non-basic compounds neutralize acids
Residence time
amount of time water spends in given compartment of Earth’s system
Capillary water
returns to atmosphere by evaporation and transpiration
Gravitational water
becomes groundwater
Hygroscopic water
water tightly bound to soil molecules
Impermeable surfaces
roads, parking lots, etc.
-result in stream exceeding max cap. =flooding
Gaining river
located above groundwater, increase discharge
-found in wet climate
Losing river
discharge water by percolation
River discharge
amount of water carried by river at one time
Watershed
total land area that drains water to common pt.
Water balance
represents hydrologic cycle at local scale