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hydroglogic cycle
describes the movement of water among the different reservoirs
pathways
the connection between reservoirs
transpiration
plants up-taking ground water and using it in their process
reservoirs
where water is stored
evaporation
liquid to gas
evapotranspiration
process of evaporation but with the aid of plants
where is most of Earth’s water?
97% is in the ocean
precipitation
as air mass cools, it starts to condense
condensation occurs
need a neuclei such as dust, salt, ice or water
growth of drop until gravity brings it to the surface
runoff
the collective term to describe the movement of water from point a to point b on the surface
what are the 6 factors that affect runoff?
geology
slope
vegetation covering
time of the year
soil saturation
type of precipitation
factor of runoff: geology
what is it falling on? is it soil? is it unconsolidated? is it fractured? is it porous?
factor of runoff: slope (topography)
a high angle of slope increases runoff
factor of runoff: vegetation covering
the more vegetation the less runoff
factor of run off: time of the year
frozen ground vs non-frozen ground, lower evapotranspiration vs high evapotranspiration
factor of run off: soil saturation
is the soil is saturated there is no room for water to infiltrate
factor of run off: type of precipitation
fast, hard rain increased runoff, while slow, soft rain allows for infiltration, snow vs rain
why does water downcut?
to get to base level
headward erosion
water cutting back
downcutting
repeated precipitation events cause a preferential channel to form
fast water
erodes
slow water
deposits
stream formation
runoff (either sheet flow or channel flow)
headward erosion
downcutting
erosion
transportation
stream transport provides mechanism by which various size particles are separated
alluvium
well sorted material
bars
temporary deposits of sand, gravel, and course components
point bars
bar which occurs on the inside of a bend (streams deposit these)
in a straight stream channel
the highest velocity is in the middle
in a meander
the highest velocity is on the outside of the curve and the inside of the curve is the slowest
meander
curve in a stream