ocean gyres - combine knowledge of global winds and ekman flow - surface transport can be determined...
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Ocean Gyres
- combine knowledge of global winds and Ekman flow
- surface transport can be determined from wind direction/velocity
- surface transport alters ocean surface dynamic height
- dynamic height differences => geostrophic flow in ocean
Geography 104 - “Physical Geography of the World’s Oceans”
Ekman transport is 90° to right (NH) of the wind
global atmospheric circulation
tropical
Global Atmospheric Pressure and Winds
July
January
cyclonic & anti-cyclonic wind effects
L H
cyclonic & anti-cyclonic wind effects
Ekman transport
convergence, downwelling
Ekman transport
divergence, upwelling
generally cooler water from upwelling
generally warmer surface waters
cyclonic & anti-cyclonic wind effects
Ekman transport
convergence, downwelling
Ekman transport
divergence, upwelling
Global Winds and Atmospheric Pressure
July
January
TradeWinds
Westerlies
Westerlies
= High Pressure
Geostrophic Currents
Ekman transport alters sea level (dynamic topography)
Sloped sea surface => pressure gradient
Geostrophic Flow in Ocean – Pressure and Coriolis force balance
Subtropical Gyre Circulation from Figure in Text
Subtropical Gyre Circulation from Figure in Text
Southern Hemisphere Subtropical Gyre going
wrong direction!!!!
geostrophic subtropical gyres
major ocean gyres and currents
global chlorophyll & primary productivity - Aug. 2004
lowest chlorophyll concentration in center of sub-tropical gyres
measuring dynamic height by satellite
deviation due to ocean currents
geoid
global dynamic height – satellite measurements
global dynamic height
Global Surface Currents from Altimetry
http://argo.colorado.edu/~realtime/gifs_tmp/global_ssh/gmt.13083.gif
dynamic height in the Gulf of Mexico
Mapped SSH in California Current
geostrophic flow direction is along lines of constant SSH
CTD deployment for dynamic height measurement
global dynamic height – shipboard measurements units: meters
5.3
4.1
5.6
5.0
6.35.6
4.4
5.5
Differences in dynamic height are important, not absolute values
Ocean Currents Associated with Dynamic Height Contours
major ocean gyres and currents
trash in the North Pacific subtropical gyre
Curtis C. Ebbesmeyer
~ 6 years to orbit N Pacific subtropical gyre
Summary
- cyclonic winds => surface divergence, upwelling
- anticyclonic winds => surface convergence, downwelling
- direct wind driven Ekman transport sets up sea level variations
- sea level variations (dynamic height) => geostrophic circulation
- for geostrophic flow currents are along lines of constant sea level (dynamic height)
- subtropical gyres are primary characteristic of ocean circulation
Readings (Surface and Deep Circulation):Text Chapter 9 (pgs 170 – 172)Reader pgs. 131 - 132