geo exam 2

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139 Terms

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Hydrosphere is in a...
steady-state equilibrium
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Distribution of Earth's water is...
uneven
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Covalent bonding
bonding of atoms through the sharing of electrons (very strong)
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Polarity
electric charge causing the attraction and repulsion of atoms/molecules
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Hydrogen bonding
bonding between water molecules (weaker than covalent, but still strong)
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Phase change requires the...
absorption or release of heat energy
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Latent heat
energy stored in phase change; it is either released or absorbed
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Humidity
amount of water vapor in air
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Relative humidity (RH)
Ratio: actual water vapor in air / max water vapor possible at a specific temperature and expressed in a percentage.
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Dry air has _____ while wet air has _____
low RH; high RH
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Condensation
the addition of more water vapor or a decrease in air temperature
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Dew-Point Temperature
The temperature at which the air will become saturated
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What are the expressions of humidity?
Relative humidity, Vapor Pressure, and Specific Humidity
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Vapor Pressure
air pressure made up of water-vapor molecules
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Saturation Vapor Pressure
Air that contains as much water vapor as possible at a given temperature. Water molecules evaporate and exert pressure.
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Specific Humidity
mass of water vapor per mass of air at any specified temperature Remains constant as temperature & pressure change. Useful in describing moisture content of large air masses that are interacting in a weather system
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Sling psychrometer
measures RH
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Air parcel
body of air (>300 m in diameter) with a specific temperature and humidity
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What happens if the air parcel is LESS dense than surrounding air?
Parcel rises and expands
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What happens if the parcel of air is MORE dense than surrounding air?
Parcel sinks and compresses
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Temperature of the volume of air determines...
density of the air parcel
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Stability
tendency of an air parcel to remain in place or change vertical position; depends on temperature
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Adiabatic
Expansion = Cooling; Compression = Warming
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What are clouds?
Aggregate of tiny moisture droplets & ice crystals. Suspended in air. Large enough in volume & concentration to be seen
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How are clouds formed?
because air is saturated with water; May contain raindrops, but not initially
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Cloud-condensation nuclei
Microscopic particlesDust, soot, ash, aerosols - continentSea salt - ocean Always present
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How do we classify clouds?
Altitude (low, middle, high, vertically developed)Shape (flat, puffy, wispy)
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Stratus
clouds that form in flat layers
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Cummulus
cloud is puffy and formed in heaps
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Cirrus
wispy, feathery thin clouds
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Nimbus
a rain cloud
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Fog
cloud layer on the ground; Air temperature and dew-point temperature are nearly identical at ground level
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What are the different types of fogs?

Radiation fog - moist / wet ground cools at night

Advection Fog - Air in one place migrates to where it can condense. Warm to Cold

Evaporation Fog (sea smoke) - water evaporates from water surface - cold air overlying water surface -condensation

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Weather
Short-term, day-to-day atmospheric conditions
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Climate
Long term weather trends in a region
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Meteorology
The study of the atmosphere (physical characteristics and motions)
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Air Mass
Distinctive body of air, with characteristics of its source region. Has specific conditions of temperature, humidity, and stability (homogenous) and produce weather patterns
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How do you classify moisture in an air mass?
m - maritime [wet], c - continental [dry]
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How do you classify temperature in an air mass?
A - Arctic, P - polar, T - tropical, E - Equatorial, AA - Antarctic
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Air Mass Modification
As air masses move from their source region, their temperature and moisture characteristics change with the regions they come in contact with
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What are the mechanisms for Lift?
Convergent, Convectional, Orographic, Frontal
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Convergent Lifting
Air flows (from different directions) toward an area of low pressure
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Convectional Lifting
Air is stimulated by local surface heating
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Orographic Lifting
Air forced over a topographic barrier
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What is an example of Orographic Lifting?
Sierra Nevada (Rainshadow)
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Frontal Lifting
Lifting caused by the collision of two air masses
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Cold Front
dense air forces lighter warm air aloft (up)
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Warm Front
warm air moves up and over dense cold air
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Ice Storm
Minimum of 6.4 mm (0.25 in) of ice accumulates on exposed surfaces
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Thunderstorms
Fueled by rapid upward movement of warm, moist air (updrafts) eventually cools and condenses. Energy is released due to latent heat from condensation, which heats the air and causes violent updrafts and downdrafts
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What are the characteristics of a thunderstorm?
Turbulence, Wind Sheer, and Lightning
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How are tornadoes formed?
High winds and updrafts collide creating a circulating low pressure. The cloud begins to lower below the cloud base.The low pressure extends to the ground picking up dust and debris forming a tornado.
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What is a mesocyclone?
a spinning, cyclonic, rising column of air, which is typical for a large storm
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Most Thunderstorms do not...
produce tornadoes.
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Funnel Cloud
rotating column of air; is formed extending from thunderstorm base
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waterspout
the tornado is in contact with a body of water
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We can predict _____ days in advance, but for _____, we only have minutes.
storms; tornadoes
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Tropic Cyclones are another name for...
Hurricanes, typhoons, or cyclones
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What are tropic cyclones?
All form destructive storms with high speedsOccur within the tropics
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Water is a...
renewable resource (distribution unequal)
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hydrological cycle (water cycle)
The circulation and transformation of water through the Earth's atmosphere, hydrosphere, lithosphere and biosphere
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The Water-Balance Equation
Effective method to assess portions of the water cycle as they apply to water resources
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How do we measure precipitation?
Rain Gauges (measures depth, weight, or volume)
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Evapotranspiration
The evaporation of water from soil plus the transpiration of water from plants. Measured with a Lysimeter.
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potential evapotranspiration
the amount of evaporation that would occur if a sufficient water source were available. Estimated.
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How are deficits formed?

The water demands exceeds the moisture from precipitation, irrigation, and soil moisture.

(Potential Evapotranspiration - Evapotranspiration)

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What do deficits result?
Droughts
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Surplus
Additional water beyond Potential Evapotranspiration demands
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Storage is defined by...
the balance between: recharge (surplus) and soil moisture loss (deficit)
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Saturation
occurs when pore spaces are filled with water, unable for plant roots to do gas exchange.
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field capacity
ability of a soil to hold water against the downward pull of gravity
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wilting point
the water potential at which most plants can no longer retrieve water from the soil.
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Where are surface water resources found?
Snow and Ice, Rivers and Lakes, and Wetlands
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Snow and Ice
Largest amount of surface freshwater; Snow melts provide streamflow.
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Rivers
Vast arterial network of surface runoff (Snow Melts and Ground waters)
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Lakes
bodies of water fed by precipitation, streamflow, and groundwater
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Wetlands
An area that is permanently or seasonally saturated with water and characterized by vegetation adapted to saturated soils (hydric soils) May develop anaerobic conditions.
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Wetlands could contain...
either fresh water or salt water
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drainage basin
land area that drains into a specific trunk stream
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drainage divide
separates adjacent drainage basins. A raindrop flows to one basin or the other, depending on which side of the divide it falls.
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Colorado River Compact
an agreement signed in 1926 that allocated to Wyoming, Colorado, Utah, Nevada, New Mexico, Arizona, California, and Mexico different portions of the Colorado River's normal and stored river flow.
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Groundwater Resources
Water below the surface, beyond the soil-moisture zone and the reach of most plant roots
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Porosity
spaces or voids between particles in a material such as soil or rock
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Permeability
the ability of water to flow through soil or rock
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Aquifer
A subsurface body of permeable rock or sediments through which water can flow in amounts adequate for wells and springs
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unsaturated zone (zone of aeration)
Pore spaces only partially full of water, lies between the water table and the surface, only partially full of air.
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zone of saturation
The lower zone where water accumilates between small rock particles (sand, gravel, and rock)
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unconfined aquifer
has a permeable layer on top and an impermeable one beneath
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water table
The upper level of the saturated zone of groundwater
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confined aquifer
is bounded above and below by impermeable layers
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artesian wells
groundwater comes to surface without having to pump
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Drawdown
A lowering of the water table
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groundwater mining
when rate of water pumping is higher than rate of recharge beyond its capacity.
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Land subsidence
sudden sinking or gradual downward settling of the Earth's surface
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Earth Fissures
a crack, break or fracture in the rocks associated with land subsidence
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Saltwater encroachment
the intrusion of saltwater into the ground with the removal of fresh groundwater
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What are the components that reveal general climate types?

temperature, precipitation (Generally its these two),

Insolation, energy availability, air pressure, and air mass

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Genetic classification
based on causative factors (e.g., interaction of air masses); based on why a certain mix of climatic ingredients in certain locations occurs
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Empirical classification
based on statistical weather data (e.g., precipitation, temperature, potential evapotranspiration)
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Empirical Approach
A study conducted via careful observations and scientifically based research.