The East Greenland Current(EGC)

The East Greenland Current(EGC)

By Kaycee ColemanBy Kaycee Coleman

Transports very cold, low salinity water as well as Artic icebergs (>90%) southward along the East Coast of Greenland.

There is not much ice formation in the EGC because it is suppressed by the salty water from the Norwegian Atlantic Current. The addition of the saline water to this intense region of cooling destabilizes the water column

Transports very cold, low salinity water as well as Artic icebergs (>90%) southward along the East Coast of Greenland.

There is not much ice formation in the EGC because it is suppressed by the salty water from the Norwegian Atlantic Current. The addition of the saline water to this intense region of cooling destabilizes the water column http://www.geo.uni-bremen.de/Interdynamik/index.php?

option=com_content&task=view&id=35

The East Greenland Current (EGC)

It flows from the Fram Strait at 79ºN to Cape Farewell at 60ºN which is one of “the windiest place in the

world.”

It flows from the Fram Strait at 79ºN to Cape Farewell at 60ºN which is one of “the windiest place in the

world.”

QuickTime™ and aTIFF (Uncompressed) decompressor

are needed to see this picture.

January 2005 http://www.mercator-ocean.fr/html/produits/buoc/buoc_n08/buoc_n08_en.html

Main freshwater sink for the Arctic

It is a source of water for the Labrador Current and the West Greenland Current.

It travels through the Greenland Sea, the Norwegian Sea, and the Denmark Strait

Main freshwater sink for the Arctic

It is a source of water for the Labrador Current and the West Greenland Current.

It travels through the Greenland Sea, the Norwegian Sea, and the Denmark Strait

http://www.answers.com/topic/labrador-current

http://www.whoi.edu/science/PO/people/pwinsor/project_ao02.html

The East Greenland Current (EGC)

The East Greenland Current (EGC)

The EGC remains geostrophically constrained to the continental margin because of its low-density water and the conservation of potential vorticity

Easterly winds can prevent the formation of the eastward extensions to the EGC

The EGC remains geostrophically constrained to the continental margin because of its low-density water and the conservation of potential vorticity

Easterly winds can prevent the formation of the eastward extensions to the EGC

http://oceancurrents.rsmas.miami.edu/atlantic/east-greenland.html

In the upper parts of the EGC at the Jan Mayen Fracture Zone there are some eastern deflections but this is not well understood, it could be because of the interaction between the bathymetry and the barotropic component of the EGC

Water too dense to cross the 620m sill in the Denmark straight goes East, North of Iceland till it reached the 840m sill through the Faeroe-Shetland Channel.

In the upper parts of the EGC at the Jan Mayen Fracture Zone there are some eastern deflections but this is not well understood, it could be because of the interaction between the bathymetry and the barotropic component of the EGC

Water too dense to cross the 620m sill in the Denmark straight goes East, North of Iceland till it reached the 840m sill through the Faeroe-Shetland Channel.

http://www.regjeringen.no/pages/2243615/HFIG/fig3-1.jpg

Three main water masses of the EGC

Three main water masses of the EGC

1. Polar Water (from the Arctic): 0-150 m, temperatures between 0ºC and the freezing point. This layer has a strong halocline, with salinity of 30 psu or less at the surface and 40 psu or more at 150 m.

2. Atlantic Intermediate Water: 150-800 m. Its temperature remains above 0ºC, salinity of 34 psu which increases with depth to between 34.88 and 35 psu ( with a max at 400 m).

3. Deep Water (which circulate cyclonically): below 800 m, temperature is <0ºC, and with a salinity between 34.87 and 34.95 psu.

1. Polar Water (from the Arctic): 0-150 m, temperatures between 0ºC and the freezing point. This layer has a strong halocline, with salinity of 30 psu or less at the surface and 40 psu or more at 150 m.

2. Atlantic Intermediate Water: 150-800 m. Its temperature remains above 0ºC, salinity of 34 psu which increases with depth to between 34.88 and 35 psu ( with a max at 400 m).

3. Deep Water (which circulate cyclonically): below 800 m, temperature is <0ºC, and with a salinity between 34.87 and 34.95 psu.

http://oceancurrents.rsmas.miami.edu/atlantic/east-greenland.html

Current speed of the EGC: measurements range from 4 to 20-30 cm s-1. Transport values for the EGC have vary from 2 Sv to 32 Sv. The computed transport based on the mass and heat budgets obtained an annual mean of 35 Sv. In the North of the EGC the transport in the upper 700 m was calculated to be 3 Sv, half of which was barotropic. Southward, geostrophic transport relative to the bottom is estimated at 4 Sv at 78.4ºN.

Causes of error: preferential sampling, different speeds assumed for the Return Atlantic Intermediate Water, and current varies interannually

Current speed of the EGC: measurements range from 4 to 20-30 cm s-1. Transport values for the EGC have vary from 2 Sv to 32 Sv. The computed transport based on the mass and heat budgets obtained an annual mean of 35 Sv. In the North of the EGC the transport in the upper 700 m was calculated to be 3 Sv, half of which was barotropic. Southward, geostrophic transport relative to the bottom is estimated at 4 Sv at 78.4ºN.

Causes of error: preferential sampling, different speeds assumed for the Return Atlantic Intermediate Water, and current varies interannually

http://oceancurrents.rsmas.miami.edu/atlantic/east-greenland.html

A great deal of ice is transported parallel to the East Greenland coast. In the North the EGC carries about 4-5000 km3 of ice towards the equator annually with an estimated sea ice flux of 1530 km3-3000 km3 a year. There is a great deal of discrepancies with these measurements and predictions.

The ice flux is seasonal with the largest values from October to December and smallest values from January to March.

EGC eddies usually have a cross-stream length of about 10 km. These eddies are abundant but do not play a large role in the heat flux (so local baroclinic instability is probably not a major contributor to the mesoscale eddies). Most of the low observed eddy kinetic energy is generated by wind fluctuations.

A great deal of ice is transported parallel to the East Greenland coast. In the North the EGC carries about 4-5000 km3 of ice towards the equator annually with an estimated sea ice flux of 1530 km3-3000 km3 a year. There is a great deal of discrepancies with these measurements and predictions.

The ice flux is seasonal with the largest values from October to December and smallest values from January to March.

EGC eddies usually have a cross-stream length of about 10 km. These eddies are abundant but do not play a large role in the heat flux (so local baroclinic instability is probably not a major contributor to the mesoscale eddies). Most of the low observed eddy kinetic energy is generated by wind fluctuations.

http://oceancurrents.rsmas.miami.edu/atlantic/east-greenland.html

http://www.expeditiongreenland.com/Portals/0/Headers%20watermarked/Kajak-header.jpg

Questions?Questions?Thank you!Thank you!

References:•http://oceancurrents.rsmas.miami.edu/atlantic/east-greenland.html•http://www.regjeringen.no/pages/2243615/HFIG/fig3-1.jpg•http://www.geo.uni-bremen.de/Interdynamik/index.php?option=com_content&task=view&id=35•http://www.mercator-ocean.fr/html/produits/buoc/buoc_n08/buoc_n08_en.html•http://www.answers.com/topic/labrador-current•http://www.expeditiongreenland.com/Portals/0/Headers%20watermarked/Kajak-header.jpg