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2. Ocean Currents
Currents flow in complex patterns affected by wind, the water's salinity and heat content, bottom topography, and the earth's rotation.
Ocean waters are constantly on the move. How they move influences climate and living conditions for plants and animals, even on land.
Types of Ocean Currents• Surface currents
– Anti-cyclonic current gyres are driven by the westward flow of equatorial surface wind.
– Gravity driven roll-back from the resulting rise of western sea surface runs equatorial counter current.
– Circum-Antarctic circulation, or “West Wind Drift” is driven by Earth’s rotation.
• Deep-water current– This is thermohaline circulation or the
“Global Conveyor Belt”.
The North Atlantic Gyre System
The factors that govern the oceanic gyres
Gulf
stream
N. Equatorial Current
Canary
Current
Atlantic Ocean meridional section at 25°W(a) Potential Temperatures (°C)
http://sam.ucsd.edu/sio210/lect_6/
Atlantic Ocean meridional section at 25°W(b) Salinity (‰)
Atlantic Ocean meridional section at 25°W(c) Density at 0 dbar (0F)
Atlantic Ocean meridional section at 25°W(d) Density at 4 dbar (4F)
Atlantic Ocean meridional section at 25°W(e) Dissolved Oxygen (DO2 in ml/l)
South Atlantic meridional section at 25°W(e) Silicate content (umol/Kg)
Su
rface curren
ts in th
e Paficific
1. shoe spill, May 27, 19902. 250 recovered, March 26, 19913. 200 recovered, May 18, 19914. 100 recovered, January-February 19915. 200 recovered, November-December 19906. 200 recovered, February-March 19917. 150 recovered, April 4, 19918. 200 recovered, May 9-10, 19919. several recovered, January-March 1993
Nike shoes and the Pacific gyreThe North Pacific gyre has been dropping off shoes around the Pacific since 1990. The shoes washed ashore one at a time but were wearable after a scrub-down to remove barnacles, algae, and tar. Beachcombers held swap meets to find matched pairs
Pacific ocean meridional section at 150°W(a) Potential Temperatures (°C)
Pacific Ocean meridional section at 150°W(b) Salinity (‰)
Pacific Ocean meridional section at 150°W(c) Density at 0 dbar (0F)
Pacific Ocean meridional section at 150°W(c) Density at 4 dbar (4F)
Surface currents in the Indian
Ocean
Circu
m-A
ntarctic C
irculatio
n
Pacific at normal times
Du
ring
the E
l Niñ
o T
imes
Equatorial surface wind
High air pressure
Wes
tE
astCold deep waters
Equatorial counter current
The normal or La Niña conditions
Warm surface waters
Low air pressure
http://www.nodc.noaa.gov/dsdt/sst_ani.htm
Animation of Monthly-averaged Sea Surface Temperatures
El Niño Continues to Grow: Pacific Ocean Shows Higher Than Normal Sea Surface Heights December 02, 2002 The latest image from NASA's Jason oceanography satellite, taken during a 10-day collection cycle ending December 2, 2002, shows the Pacific dominated by two significant areas of higher-than-normal sea level (warmer ocean temperatures). In the central equatorial Pacific, the large area of higher than normal sea surface heights (warmer than normal sea surface temperatures) associated with growing El Niño conditions has recently migrated eastward toward the coast of South America. Meanwhile, the
influence of the 20- to 30-year larger than El Niño/La Niña pattern called the Pacific Decadal Oscillation continues to create warm, higher-than-normal sea-surface heights in the north Pacific that are connected in a warm horseshoe pattern with the western and southern Pacific. http://topex-www.jpl.nasa.gov/elnino/20021202.html
Geostrophic Currents
Upwelling and downwelling
The Ekman Spiral
The Ekman Spiral
Mapping the Gulf Stream
The Gulf Stream wobbles, much like the streams on land, so creating rings and eddies.
The Oceanic Conveyor Belt