temperature and pressure.
-
polarity of water molecules.
-
is relatively high.
-
sharing of electrons between atoms.
-
high surface tension.
-
surface tension.
-
is a polar molecule.
-
calorie.
-
high heat capacity
-
change states of matter.
-
It remains constant until the ice melts; then it begins to rise.
-
the remaining water is cooled.
-
higher than other liquids.
-
3.5%
-
the relative concentrations of seawater ions do not change.
-
As a whole, the pH of the ocean is slightly acidic.
-
HCO3-.
-
hydrologic cycle.
-
thermocline.
-
pycnocline.
-
buffering capacity. hydrogen ion. pH.
-
a longer wavelength.
-
50%
-
25%
-
23.5oS latitude.
-
to the right of the original direction.
-
Coriolis effect.
-
wet and warm.
-
cold front
-
differences in the heat capacity of ocean and land.
-
be deflected toward the east.
-
intertropical convergence zone.
-
westerly winds.
-
counterclokwise.
-
Saffir-Simpson Scale.
-
redistribute heat from one area to another.
-
higher salinity.
-
SOFAR channel.
-
1000 meters.
-
water vapor.
-
chlorofluorocarbons.
-
chlorofluorocarbons.
-
All of the above are consequences of global warming.
-
respiration
-
30%.
-
Kyoto Protocol.
-
sverdrup.
-
trade winds.
-
wind; the Coriolis effect and land.
-
Langmuir circulation.
-
Two circumpolar currents dominate it, one current that moves water to the east and one current that moves water to the west.
-
North Atlantic Ocean.
-
cold core ring.
-
Labrador Current - Humbolt Current
-
flow from land to sea and are dry.
-
All of the above statements are true of western boundary currents.
-
Brazil Current.
-
Eastern boundary currents are broad and slow.
-
Gulf Stream
-
Gravity
-
All of the above statements are associated with westward intensification.
-
upwelling.
-
where deep ocean water currents are formed.
-
nutrients and oxygen.
-
Drought in the US Gulf coastal states.
-
the relationship between sea surface temperature and high altitude pressure.
-
drought and fires in Australia.
-
wind.
-
to the left of the wind direction.
-
gravity-driven circulation.
-
density differences
-
warmer, and higher in salinity
-
in the Southern Ocean
-
Antarctic Intermediate Water, North Atlantic Deep Water, Antarctic Bottom Water.
-
Gulf of Alaska. Agulhas Current. Peru Current. strong trade winds.
-
westerlies.
-
wave steepness
-
Period.
-
orbital waves.
-
wavelength divided by period.
-
low-pressure systems.
-
wavelength/2
-
wave height.
-
1/2 of wavelength.
-
All of the above are examples of shallow water waves.
-
water depth.
-
wavelength.
-
dominant restoring force.
-
fetch, wind duration, and wind speed.
-
the distance over which wind blows without interruption.
-
at a density boundary within the ocean.
-
increases and wavelength decreases.
-
smaller waves.
-
steepness > 1:7.
-
swell.
-
plunging breakers.
-
spilling breakers.
-
wave refraction.
-
sea, swell, surf.
-
where storm waves move against strong surface currents.
-
wave reflection.
-
tectonic activity on the seafloor.
-
shallow water wave.
-
Spilling. Period. Swell.