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Two distinct forms of water resources
Surface water and groundwater
Cultural hearth
A source area from which new ideas radiate
Qanat
Underwater channel tapping groundwater supplies which wells could be drilled into; common in middle east and still used today
Aquaduct
Gravity fed delivery system to bring water to urban centers; invented in Rome
Cistern
Underground reservoirs lined with clay or dug into limestone
Hydrologic cycle
Movement of water between the land, oceans, and atmosphere; most found in oceans, very little accessible as fresh drinking water
Precipitation
The process of water in the atmosphere returning to the earth’s surface in liquid or solid form (rain, sleet, snow, virga)
Rain gauge
Instrument used to measure rainfall amounts; not to be placed near buildings or trees
Arithmetic mean
Measures average rainfall for an area (total rainfall/number of gauges)
Thiessen Method
Alternative method to measure average rainfall in area; weighted to be more accurate; plot gauges on map and connect with lines. Using perpendicular bisectors, gauge area is determined
Isohyetal method
Method for weighting rainfall using contours of equal precipitation
Doppler Radar
More accurate method of precipitation measurement in terms of coverage; uses energy bursts to determine strength and distance from storm, and how fast storms are moving
Snow tube
Used to observe snow cores to determine snow depth and characteristics, as well as water equivalent
Snow Pillow
Device that measures snow depth and water equivalents using a pressure plate
Runoff
The amount of water that flows of the land’s surface after a storm event or melting snow; climate, terrain, and precipitation volume/intensity effect runoff values
Lake vs reservoir
Reservoir manmade, lake natural
Wetland
remnant of meandering river
Aral sea
Big lake in arid region (needs river runoff to maintain water levels); severe shrinkage after river water was diverted to farming and irrigation
Evaporation
The process whereby water changes state from a liquid to a gas due to solar radiation and wind action
US class A evaporation pan
Standard instrument used to measure evaporation; pan coefficient used to correct error caused by excess heat from the walls of the pan; must be leveled for accurate calculations and water must be held 50 mm below rim; cup anemometer is often placed next to pan to measure wind
Sublimation
The process in which water changes from a solid to gas state without entering the liquid phase
Transpiration
The process of a plant releasing water vapor through its living tissue
Evapotranspiration
Includes all evaporation from water and land and all transpiration
Potential evapotranspiration
Maximum amount of evapotranspiration that would occur if soil moisture was unlimited
Penman equation
Equation used to determine evaporation rate from an open water surface
Blaney-Criddle method
Equation used to determine evapotranspiration rates
Lysimeters
Field device containing soil and vegetation used to measure evapotranspiration
Consumptive use
The total amount of water used by the plant in transpiration and evaporation in any specific time; may vary among crop species, as well as within species over time or location
Climate
Sum of all statistical weather information that helps describe a region and can be generally predicted for centuries into the future
Weather
The state of the atmosphere at any given time or place; only predictable in the short term
Conevection
When warm, light air at the earth’s surface rises and cold, dense air from the troposphere sinks
Troposphere
The lower levels of the atmosphere extending from the earth’s surface up to the tropopause
Wind
Occurs when air moves from high to low pressure areas (caused by unequal heating of earth’s surface), small scale: lake effect, larger scale, sea breeze, global scale, wind belts
Intertropical convergence zone
Low-pressure zone at the equator where northwest and southwest trade winds flow together; strong upward air movement and heavy rainfall
Coriolis effect
Deflection force of the earth’s rotation on all free-moving objects, including the earth’s atmosphere and oceans; deflects to the right in the northern hemisphere and to the left in the southern; strongest at poles, weakest at equator
Dendrochronology
The study of tree rings to study the historic climate data
Ice cores
Oxygen isotopes can reveal changes in climates over thousands of years
Ocean corals
Another way to observe historic climate data
Sediment cores
Climate, environmental, and geological information as far back as 5 million years
Five factors of weather
Air pressure, humidity, temperature, heating, and wind speed/direction
Radiation
The only form of weather that can be propagated without a transfer medium; greatest input to atmosphere; shorter wavelengths=higher energy
Dew point/frost point
Rate of total saturation in the atmosphere; when dew point is reached condensation occurs
Adiabatic Process
When an air mass rises and expands without exchanging heat with its surroundings
Adiabatic lapse
Unsaturated rising and expanding air will drop in temperature at a constant rate of 1 C/100 m; the same parcel will gain temperature as it rises at the same rate
Clouds
Dense concentration of suspended water droplets or tiny crystals in the atmosphere; classified based on shape, appearance, and height
Cumulus clouds
Puffy, round, individual cloud masses, often have a flat base, formed when hot humid air rises due to convection
Stratus clouds
Low sheet (blanket appearance) or layers of clouds covering much of the sky
Cirrus clouds
Highest clouds in the sky; composed of thin and delicate ice crystals; looks like filaments or feathers
Warm fronts
Frontal lifting caused by warm, moist air moving over cool air; leads to cloud buildup and precipitation
Cold front
Frontal lifting caused by cool air moving under warmer air ; leads to cloud building and precipitation
Stationary front
Weather fronts with little to know movement
Orographic lifting
Occur when moisture-laden air meets a mountain and the air is forced to ascend; leads to high amounts of precipitation
Convergence lifting
Occurs when two air masses collide and both are forced upwards
Convergence
The process where two air streams come together into a smaller central area, pushing the air molecule in the center to form an upward current (high pressure); divergence is when are moves away from a central area (low pressure)
High pressure vs low pressure northern hemisphere
Low pressure counterclockwise, high pressure clockwise (opposite in southern hemisphere)
Occluded front
Occurs when a cold front takes over the warm front, forcing it aloft
El nino
A natural phenomena that occurs when a warm surface ocean current forms in the eastern pacific ocean off of the coast of Ecuador and Peru; associated with the southern oscillation
La nina
A natural phenomena caused by cooler water in the equatorial Pacific
Southern oscillation
Changing pattern of atmospheric pressure along the equator in the Pacific ocean
Isobars
Lines on a map that connect locations of equal air pressure (barometers)
Jet stream
Very strong winds at high latitudes created by differences in air Pr gradient
Air Pr gradient
Determined by the distance between isobars
Cloud seeding
Introduction of dry ice or silver iodide into clouds to enhance precipitation or retard hail development
Causes of floods
Summer thunderstorms
melting snow
Ice jams in swollen
seasonal monsoons
Drought
Period of extended dry weather that is abnormal for a region
Aridity
Permanent, dry climatic conditions in a region where annual precipitation is less than 10 inches
Meteorological drought
Departure from normal precipitation
Hydrological drought
Below surface and groundwater supplies
Agricultural drought
Inadequate water supplies to grow a particular crop
Socioeconomic drought
Inadequate water supplies to serve local community
Drought indices
Numerical method to assess the severity of below average precipitation in a region
Palmer index
Index used to determine when to provide emergency drought assistance