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Hadley Cell Circulation
warm air towards poles
cold air towards equators
ferrel cell circulation
warm air towards equator
cold air towards poles
polar cell circulation
warm air towards poles
cold air towards equator
warm air
air rises
low pressure
cold air
air sinks
high pressure
air circulation around low pressure in NORTHERN
CCW
air circulation around high pressure in NORTHERN
CW
ekman transport in NORTHERN
to the right
subtropical gyre spin direction in NORTHERN
CW & deep thermocline
subtropical gyre spin direction in SOUTHERN
CCW & deep thermocline
subpolar gyre spin direction
CCW & shallow thermocline
NADW
high latitudes in the North Atlantic
salty sea surface water cools and sinks, making dense water (so salty that it doesn’t reach its freezing point before cooling)
SECOND DENSEST
AABW
southern ocean around antarctica
surface water cooling/sinking AND the surface water freezing to form sea ice, leaving behind brine that sinks
DENSEST
AAIW
southern ocean around antarctica
ekman transport (dense surface water gets pushed equator ward, until it gets pushed under a less dense surface water)
MIDDLE DENSEST
NPIW
North Pacific where the subtropical and sub polar gyres meet
cabelling of two surface waters
SECOND FRESHEST
spring tide
full & new moon
lunar bulges LINE UP with solar bulges, making biggest tidal range
neap tide
first & third quarter moons
lunar bulges are PERPENDICULAR to solar bulges, making smallest tidal range
perigee
when the moon is closest to the earth and the lunar tidal range is the largest
apogee
when the moon is furthest from the earth and the lunar tidal range is the smallest
perihelion
when the earth is closest to the sun (in January) and the solar tidal range is the largest
wave frequency
1/wave period (1/T)
shallow water wave
the water base is less than 1/20 of a wavelength
cause of a <5 min wave
wind
cause of a 5min-12hour wave
catastrophes (earthquakes, landslides, etc.)
cause of 12-24hour wave
sun and moon
factors that determine wave energy
wind speed
duration
fetch (the size of the storm from beginning to end, the max distance across which the wind is blowing to generate waves w/out obstruction)
Summer beach profile
low wave energy
wash dominates
sediment is transported onto shore
winter beach profile
high wave energy
backwash dominates
sediment is net transported OFF shore
as wave approaches coast…
deep water wave becomes shallow water wave
wavelength shortens
wave height increases
pelagic zones
defined by depth
epipelagic
mesopelagic
bathypelagic
abyssopelagic
hadal
photic zones
defined by light
euphoric (1/2 of epipelagic)
disphotic (1/2 of epipelagic & mesopelagic)
aphonic (bathypelagic, abyssopelagic, hadal)
macronutrients
OFTEN LIMITING
nitrogen & phosphorus
micronutrients
SOMETIMES LIMITING
sodium chloride, iron, etc.