Surface Currents Flashcards
Types of ocean circulation
Surface ocean:
- currents driven by winds
- water above pycnocline, upper 1000 meters
Deep ocean:
- currents driven by density differences (from changes in T & s)
- water at or below pycnocline
Coriolis force
- to the right in norhtern hemisphere
- to the left in southern hemisphere
Understanding wind-driven gyres
- gyre = a large system of circular ocean currents
- driven by global winds (westerlies & trade winds) + earth’s rotation
Voyage of the Fram (1893 - 1896)
Led by Norwegian Fridtjof Nansen, intending to reach North Pole
Ekman Explained Nansen’s Observations
Showed mathematically why:
- ocean velocity spirals with depth
- surface current & icebergs move 45 degrees to the right of the wind
- net surface transport is 90 degrees to the right of the wind
Global scale of westerlies and trade winds
What direction is ocean transport in response to those winds? southeast
Ekman transport
- convergence, pile up water in gyre, creating a bulge in the sea surface
- water wants to flow “downhill”, but it’s deflected by Coriolis
- Coriolis deflects the downhill flow so water flows perpendicular to the slope (pressure gradient)
- causes accumulation of plastic debris in the ocean
geostrophic flow
balance between pressure gradient force and coriolis force
Ocean gyre ciruclarion
- driven by winds
- deflected by coriolis
- occurs in all major ocean basins
Western intensification of currents in a gyre
at high lats:
- coriolis is stronger
- turns flow towards the equator sooner, leading to currents on the eastern side of the gyre that are spread out and weak
at low lats:
- coriolis force is weaker
- water doesn’t turn rowards the poles until it hits the continent, leading to a very strong current on the western side of the gyre
speed of current proportional to slope of hill
Boundary currents
Western boundary currents
- in both northern and southern hemisphere
- warm water + flow toward the poles = poleward heat-transport mechanism
global sea surface temp
temp of current reflects region of origin
Effects of currents on regional climate
Western coundary curretns
- warm currents from equator -> warm, humid air -> humid climate on land
Eastern boundary currents:
- cold currents from poles -> cool, dry air -> dry climate on land
Case study: north atlantic gyre