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What is the water
cycle?
Continuous movement of
water from the atmosphere
to the earth’s surface and
back to the atmosphere
again.
Transpiration -
plants giving off
water vapor into the
atmosphere.
Evaporation – liquid
water changing into
water vapor
Condensation: water vapor (gas) changes into
liquid water.
Precipitation: water falls from clouds to the
ground.
The underground water that
fills almost all the pores in
rock and sediment.
Makes up 90% of the
earth’s unfrozen freshwater
supply.
Aquifer: a body of rock in which large
amounts of water can flow and be
stored.
Porosity: percentage of open spaces in rock.
◦ Determined by :
◦ Sorting: well-sorted- equal sized = more
porous
◦ Poorly sorted-unequal sized = less porous
Permeability: how easily water flows through
open spaces. (can water pass through or
not?)
Zone of Saturation: the layer of ground where all the pores are filled with water.◦ The upper surface of the
zone of saturation is called the water table.
Russia
Beginning of a river
Usually found in the mountains.
Runoff from mountains flows to lowest point.
Smaller rivers that feed into a big river.
More often found in mountains than on flat land.
Where the river flows into a larger body of water
Ex. a lake, ocean, another river.
Watershed – area that drains into a body of water (stream, river etc.)
River Basin - A region of land that drains into a river system (contains many different watersheds).
Separates one river basin from the next.
The course of the water in a river or stream.
The volume of water flowing past a certain point in a given unit of time.
Usually measured in cubic meters per second (m3/s).
Young river: v-shaped channel; steep sides
Mature river: u-shaped channel; more sloping sides; some meanders (bends)
Old river: flatter u-shaped channel; sloping sides; lots of meanders
Sediment is deposited in a stream when
there is a decrease in the speed of the
water.
Decreased slope (steeper--> faster)
Bed widening (more friction)
Obstruction (slows down when it goes
around rock, tree, bridge)
Can create landforms or change the river
valley in the following ways:
Sloping fan-shaped deposit of sediments
Occurs where a stream descending a steep
slope flat land.
Part of the valley floor covered with water
during a flood.
Sediment is deposited making flood plains
fertile.
Raised river banks caused by flooding.
Curves in a river caused by an obstruction.
Erosion occurs on the outside of a bend.
Deposition occurs on the inside of a bend.
Crescent shaped body of water resulting
when a part of a meander is cut off and
abandoned by the river.
Buildup of sediments at the mouth of a river.
Occurs because the water slows down as it
empties into another body of water.
Oceans and Ocean Circulation
70%!
96% PURE
WATER
4% dissolved elements:
Cl, Na, Mg S, Ca, K
A measure of dissolved solids in sea water
Number of grams of dissolved salts in 1 kilogram of water
Measured in parts per thousand (ppt)
Evaporation and freezing increases salinity
Density is the mass of a substance per unit volume (D=m/v)
Affected by two things:◦Salinity: dissolved solids make water more dense
◦Temperature: Cold water is more dense
Factors affecting Seawater density
Salinity–increase in salinityincreases density
Temperture
–decrease in tempincrease density
*Tempereature has a greater influence
*Occurs at low latitudes. Thermocline is absent at high latitudes.
http://marinebio.org/oceans/temperature/
Nitrogen (N2), Carbon dioxide (CO2), and oxygen (O2) are the most abundant
CO2 dissolves most easily
Cold water holds more dissolved gases than warm water
Divided into 3 major oceans: the Atlantic, the Pacific, and the Indian Oceans
Has the longest distance North to South
Covers 30% of surface of the Earth
Mostly in the Southern Hemisphere
The Arctic and the Southern Oceans
The term “sea” refers to smaller areas of the ocean that are partially surrounded by land.
Ex: Mediterranean and Caribbean.
Ocean water moves in giant streams called currents that flow like rivers at the surface or far below.
There are 2 types of currents:◦ Surface
◦ Density
Move on the surface of the ocean
Driven by wind
Only affect the upper surface of the water.
1.Warm:
Flow away from the equator on the west sides of ocean basins
Because areas near the equator are warm
Example: Gulf Stream
2. Cold Flow toward the
equator on the east sides of ocean basins
Originate at the poles where the water is cold
Example: California current
Red are Warm Currents and
Black are cold currents
Surface Currents
Wind is the driving force behind the formation of surface currents.
2 sets of wind patterns involved in forming most surface currents.◦ Trade Winds – Blow toward the equator
◦ Westerlies – Blow away from the equator
Trade winds and Westerlies
Five Major Ocean Gyres
1. North Pacific Gyre
2. South Pacific Gyre
3. North Atlantic Gyre
4. South Atlantic Gyre
5. Indian Ocean Gyre
Western side of ocean has warm currents traveling from equator
Eastern side of ocean has cool currents moving toward equator
Move beneath the surface of the ocean
Caused by differences in the density of water due to its different temperatures and salinities
a.k.a.Thermohaline Circulation
Zone of rapid temperature changeWarmer water on top of layer
Colder, denser on bottom of layer
Begins at the poles where cold dense water sinks.
Warmer water moves in to take its place creating a current.
This drives the “global conveyer belt”
Process moves very slowly
One section on the “global conveyer belt”make take 1,000 years to fully cycle through the ocean!!
Crucial to the base of the world's food chain.
Adds CO2 and nutrients to surface waters by carrying them deeper in the ocean where those elements are abundant.
◦ This enables the growth of algae and seaweed that ultimately support all forms of life.
Helps to regulate temperatures