Week 1
Aquifer: underground layer of permeable rock, from which groundwater can be easily extracted using a well.
Condensation: water changes from a gas to a liquid.
Condensation nuclei: particles of dust, pollen, salt, ice, etc. around which water vapor condenses
Evaporation: water changes to water vapor
Evapotranspiration: evaporation + transpiration
Groundwater: water stored underground, in the pore spaces of rocks and soil
Humidity: measure of the amount of water vapor in the air
Infiltration: water that seeps into the soil and can become groundwater
Precipitation: water falls to Earth as rain, snow, sleet, hail, etc.
Reservoir: place where water is stored
Residence Time: amount of time a water molecule will stay in one reservoir
Runoff: water on the surface of earth that does not infiltrate the ground
Transpiration: liquid water from the leaves of plants changes to water vapor
Water Table: top surface of groundwater
Week 2
Bioaccumulation: pollutants accumulate in the tissues of organisms and become more concentrated as they are passed up the food chain
Central Utah Project (CUP): federal water management project designed to provide water for the state of Utah
Clean Water Act: federal law that protects our nation's waterways from pollution
Dissolved Oxygen: measure of the amount of oxygen available to aquatic organisms; used to measure an increase in organic and/or nutrient pollution
Eutrophication: a type of pollution where there are excessive nutrients in a body of water
Hydrogen Bond: characteristic that makes water molecules attracted to one another; caused by water's polar nature
Nonpoint Source Pollution: pollution that comes from a diffuse area (e.g. stormwater runoff, agricultural fields)
pH: determines the concentration of hydrogen in the water; a measure of the acidity of a water body
Point Source Pollution: pollution that can comes from one particular source (e.g. factory smokestack, industrial pipeline)
Polar Molecule - one end has a slight negative charge and the other a slight positive charge;l water is a polar molecule
Specific Conductivity: a measure of the amount of dissolved solids (salts, minerals) in the water
Specific Heat: refers to the amount of heat required to raise the temperature of 1 gram of a substance by 1 degree Celsius
Turbidity: a measure of the amount of particulates in the water
Universal Solvent: water can dissolve more substances than any other liquid
Week 3
Abyssal Plains: smooth, flat, muddy plains on the sea floor
Beach: the area in which sediment is deposited along the shore
Continental Rise: extends beyond the steep continental slope. It is more gently sloping and is composed of the sediments deposited by turbidity currents at the base of the continental slope
Continental Shelf: extends seaward from the shore and is the shallowest part of the continental margin
Continental Slope: area of the seafloor just beyond the continental shelf, where the slope of the seafloor becomes steeper
Crest: highest point of a wave
Deep Sea Trenches: the deepest areas in the ocean
El Niño: climate phenomenon that influences sea surface temperatures and ocean currents
Estuaries: places where large rivers empty into the ocean
Fetch: distance the wind travels over the ocean surface
Gyres: circular pattern of ocean surface currents
Ions: charged atoms
Longshore Currents: one way sand is deposited on a beach. They are caused by waves striking the beach at an angle
Period: the amount of time that passes between one wave to the next
Polar Easterlies: winds that are closest to the poles and blow from east to west, pushing surface currents westward
Prevailing Westerlies: winds found at mid-latitudes and move from west to east, creating surface currents that also move in that direction
Rip Currents: formed in low areas or breaks in sandbars. They move perpendicularly away from the shore & towards the ocean
Salinity: a measure of the concentration of dissolved salts in a body of water. It is measured as a concentration of grams of salt per kilogram of seawater
Sonar: stands for sound navigation and ranging, works by emitting pulses of sound waves from a ship, which bounce off any objects they hit and return to their source. Allows scientists to map the sea floor
Thermohaline Circulation: network of surface and deep ocean currents that constantly circulates ocean water from one side of the globe to another. Caused by salinity and temperature differences
Trade Winds: winds closest to the equator, blow from east to west; they drive the ocean surface currents from the east to west as well
Trough: lowest point of a wave
Turbidity Currents: fast moving currents of water, mud and sediment
Wave: a disturbance that travels through space and transports energy
Wave Height: distance between the wave's trough and crest
Wavelength: the distance between two consecutive wave crests
Week 4
Abyssal Zone: habitat zone found on the flat, muddy, open plains of the seafloor
Aphotic Zone: light zone found on the ocean floor and receives no sunlight
Bathal Zone: habitat zone found on the continental slope
Benthic: deep waters
Disphotic Zone: light zone located beneath the photic zone; receives some sunlight, but it is very dim at this depth in the ocean
Epifauna: live on top of the seafloor
Euphotic Zone: light zone that receives the most sunlight, and is found at shallow depths in the ocean
Hadal Zone: habitat zone located in the deep ocean trenches
Infauna: benthic organisms that bury themselves in the mud and sediments on the seafloor
Low Intertidal Zone: exposed only during the lowest tides
Mid-Intertidal Zone: generally submerged except during low tide
Nekton: organisms that can propel themselves through the water column
Neritic Zone: habitat zone located in the shallowest waters above the continental shelf
Oceanic Zone: habitat zone found in the open ocean waters
Pelagic: shallow water
Photic Zone: light zone located beneath the euphotic zone; receives abundant sunlight, and therefore supports photosynthetic vegetation
Plankton: float in open waters
Seamounts: underwater, extinct volcanoes that reach a height of greater than 1,000 meters
Spray Zone: can be underwater during very high tides, spring tides, or severe storms
Sub-Tidal Zone: located below the low spring tide line
Tidal Range or Intertidal Zone: difference between the water level at high tide and low tide
Upper Intertidal Zone: flooded during peak tides, but exposed at other times