Use LEFT and RIGHT arrow keys to navigate between flashcards;
Use UP and DOWN arrow keys to flip the card;
H to show hint;
A reads text to speech;
33 Cards in this Set
- Front
- Back
how much of the earth is covered by water?
|
~3/4
|
|
ocean currents
|
gyres
|
|
surface currents
|
fast
|
|
deep currents
|
slow
|
|
concentration of dissolved solids
|
salinity
|
|
average salinity of the ocean
|
35 ppt
|
|
as the temperature of the water decreases, the salinity...
|
decreases and sinks
|
|
as depth increases, temperature...
|
decreases
|
|
as depth increases, salinity...
|
decreases
|
|
as depth increases, oxygen...
|
decreases
|
|
as depth increases, carbon dioxide...
|
increases
|
|
4 factors why the sea levels change constantly
|
tides, waves, currents, weather
|
|
calculated from average tidal levels obtained from a large number of gauges
|
mean sea level
|
|
2 reasons why the sea level has been rising
|
melting of ice and thermal expansion
|
|
the change in sea level due to a larger volume of water
|
eustatic rise
|
|
what we can actually observe, the relative rise/drop compared to the coast
|
relative sea level
|
|
the upward/downward movement of the crust based on weight; like a cork bobbing on water; controls relative sea level
|
isostacy
|
|
the median value of the sea level
|
.48 m
|
|
what 2 things control tides?
|
moon and sun
|
|
moon and sun additive effects
|
large tides
|
|
moon and sun subtractive effects
|
small tides
|
|
2 high, 2 low per day; atlantic coast
|
semi-diurnal tides
|
|
1 high, 1 low per day; gulf coast
|
diurnal tides
|
|
random high and low tides; pacific coast
|
mixed tides
|
|
water goes inland
|
flood tide
|
|
water goes out
|
ebb tide
|
|
difference in elevation between high and low tides
|
tidal range
|
|
where does friction begin?
|
wavelength/2
|
|
swash zone
|
surf
|
|
wave approaches shore at an angle; closest part hits shallow water first then slows down; wave approaches shore at lower angle
|
wave refraction
|
|
beach type; short and steep
|
reflective
|
|
beach type; long, flatter, bars
|
dissipative
|
|
generally results from position on tectonic plates; gulf and atlantic coasts
|
depositional coast
|