Fresh Water, Oceans and Coasts Flashcards
How much of the Earth’s water is ocean water/saltwater?
97.5%
How much of the Earth’s water is fresh water?
2.5%
What defines fresh water?
mostly pure with few dissolved salts; largely in glaciers, ice caps and underground aquifers
How much fresh water is actually easily available for use?
1 part in 10,000
Percentage of fresh water that is surface water
1%
Percentage of fresh water locked up in ice caps and glaciers
79%
Percentage of fresh water as groundwater
20%
Percentage of surface water as lakes
52%
Percentage of surface water as soil moisture
38%
Percentage of surface water as atmospheric vapor
8%
Percentage of surface water as water in organisms
1%
Percentage of surface water as rivers
1%
Water cycle
the natural processes that recycle water through interconnected aquatic systems that exchange or involve water itself + pollutants, sediments, organisms and dissolved substances
How can the water cycle be affected by humans?
through the use of dams/levees, by withdrawing water for use and by introducing pollutants
Groundwater
water found beneath the Earth’s surface in pores in soil and rock; flows slowly from high to low pressure; may be underground for thousands of years; held in aquifers
Aquifer
porous rock, sand or gravel formation underground that holds water; has two distinct layers separated by a water table
Zone of aeration
the upper zone of an aquifer where the pore spaces are partly filled with water
Zone of saturation
the lower zone of an aquifer where the pore spaces are completely filled with water
Recharge zone
an area where water infiltrates the Earth’s surface and enters an aquifer (that process = infiltration)
Confined aquifer (AKA artesian aquifer)
trapped between layers of less permeable substrate (often clay), meaning water is under higher pressure; taps into confined aquifers
Unconfined aquifer
has no upper layer confining its water
Ways that groundwater can rise to the surface
wells, springs, wetlands
Well
a human-made method of retrieving groundwater; pulls water out of pore spaces in rock and soil beneath the water table
Runoff
water from rain, springs or melted snow/ice that runs over the Earth’s surface; downhill converges at the lowest spot to form streams, creeks and brooks that can merge into rivers that lead to a lake or the ocean
Tributary
a small river that flows into a larger one
Watershed/drainage basin
the area of land that is drained by a river system; allows a river’s water to be traced back to where it fell as precipitation
River system
includes a river and its tributaries
Length of time for rivers to shape landscapes
thousands to millions of years (through erosion and deposition; can shift position)
Floodplain
the areas near a river’s course that are subject to periodic flooding; very fertile due to the deposition of silt/eroded soil (for agriculture and riparian/riverside ecosystems)
What major factor influences the shape of a river’s course?
flooding - scours new channels, so if dams/levees are constructed meandering decreases dramatically
Inland seas
very large lakes
Zones of lakes and ponds (+ standing water in general)
littoral, benthic, limnetic, profundal
Littoral zone
a shallow, nutrient-rich zone nearest to the edges of a water body where aquatic plants can grow and invertebrates that other animals can eat are abundant
Benthic zone
the zone of a water body running from the shore to the deepest point that is rich in nutrients and low in oxygen; contains many invertebrates that eat detritus or each other
Limnetic zone
the open, shallow part of a water body that is far from the shore but still penetrated by sunlight; photosynthesis supports phytoplankton (algae, protists, cyanobacteria) that support zooplankton (both eaten by other organisms)
Profundal zone
the deepest part of a water body that is also far from the shore; lower in dissolved oxygen and lacks photosynthetic life
How can streams and runoff alter lakes and ponds?
can add sediment and nutrients
Oligotrophic
refers to a water body that is low in nutrients and high in oxygen; considered to have good water quality but to lack biological productivity
Eutrophic
refers to a water body that is high in nutrients and low in oxygen; considered to have poor water quality but to have abundant biological productivity
Aquatic succession/eutrophication
the natural process by which a water body transitions from oligotrophic to eutrophic; may also be induced or accelerated by humans (from nutrient pollution)
Wetland
a system where the soil is saturated with water; features shallow standing water and ample vegetation; rich and productive; includes freshwater marshes, swamps, bogs and vernal pools
Freshwater marsh
tends to have plentiful vegetation like cattails and bulrushes growing above (and thanks to) shallow water
Swamp
vegetation and shallow water within a forest
Bog
a pond covered with thick mats of vegetation; can represent a stage in aquatic succession
Vernal pool
a seasonal wetland that forms in the early spring from rain and snowmelt but dries up as temperatures increase
Benefits of wetlands
serve as valuable habitat, slow runoff, reduce flooding, recharge aquifers, filter pollutants
What actions can damage or destroy wetlands?
draining and filling them for agricultural purposes, withdrawing water, diverting water, channelizing rivers and building dams
Proportion of wetlands in the U.S. and Canada lost
> 50% (since European colonization)
Inland seas, not the oceans, receive the greatest input of water, sediment, organisms and pollutants.
false
Proportion of Earth’s surface that the oceans take up
71%
Contents of the ocean
96.5% water, rest = ions from salts (final destination for runoff with salt)
Ocean salinity
33,000 - 37,000 ppm
Fresh water salinity
< 500 ppm
What makes the ocean’s temperature decrease with depth?
amount of sunlight that can penetrate decreases with depth
Currents (horizontal)
vast riverlike flows of water in the upper 400 m of ocean water that move horizontally over great distances; long-lasting, predictable, interact with the climate, used for navigation; driven by the density of seawater, heating/cooling, wind and the Coriolis effect; increase with cooler or saltier water
Vertical currents
generated by surface winds and heating; involve upwelling and downwelling
Upwelling
the rise of deep, cold, dense water to the surface of the ocean; increases primary productivity since deeper water is richer in nutrients, which means fishing is more successful
Downwelling
the sinking of warm, oxygen-rich surface water to the bottom of the ocean; provides an influx of oxygen to organisms living there and “buries” carbon dioxide in sediment
Bathymetry
the depth of water in the ocean
Complexity of the ocean floor (about)
has underwater volcanoes/mountain ranges; underlain by continental sediment; vast areas of flat abyssal plains; seafloor spreading at ridges + crust subduction at trenches; continental shelves slope gently until the shelf-slope break (division between the continental shelf and slope)
Thermohaline circulation
the global current system wherein warm and low-salt water moves along the ocean’s surface while cold and high-salt water moves deep below it; vertical and horizontal water movements affect climate everywhere; warm water eventually evaporates (leaves behind salt) and cools (sinks) but can travel long distances first; hypothesis that interrupting the system causes rapid climate change (ice melt = influx of fresh water = surface water less dense, so downwelling ceases + rapid cooling occurs + areas closer to the poles don’t receive warm traveling water)
El Niño-Southern Oscillation (ENSO)
a systematic shift in atmospheric pressure, sea surface temperature, and ocean circulation in the tropical Pacific; normally winds travel east to west (high to low pressure) along the equator so warm surface water “piles up” in the west (50 cm higher and 8 degrees C warmer in Indonesia vs. South America, higher risk of flooding, upwelling in South America) – but every 2-8 years the winds weaken and warm water flows backward to South America (due to decreased air pressure in the east and increased in the west)
Effects of El Niño
lack of upwelling around South America means a lack of nutrients for surface sea life and fisheries; creates rainstorms/floods where typically dry and drought/fire where typically moist
La Niña
a systematic shift where cold ocean water rises and moves west in the equatorial Pacific with strengthened winds; has the opposite climatic effects as El Niño
What is the effect of global warming on the ENSO cycle?
increases the frequency and strength (due to warmer air and sea temperatures)
Intertidal (littoral) ecosystem
the collection of biotic and abiotic factors located where the ocean meets land between the uppermost part of high tide and the lowest limit of low tide; organisms within are lashed with waves, exposed to air/sun and submerged at different parts of the day
Tides
the periodic rising and falling of the ocean’s height at a given location caused by the gravitational pull of the Moon and Sun
Supratidal/splash zone and subtidal zone
zones beyond the edges of the intertidal zone; former is splashed by waves but not fully submerged, latter is always submerged
Tide pools
shallow pools of water created at low tide when seawater is trapped in rocky crevices; serve as shelter for some organisms
What makes the intertidal ecosystem so biologically diverse?
temperature, salinity, moisture and other conditions change a lot from the highest to lowest reaches