Please note: You are viewing the unstyled version of this website. Either your browser does not support CSS (cascading style sheets) or it has been disabled. Skip navigation.

About the Expedition

Dallas Murphy

  Email    Print  PDF  Change text to small (default) Change text to medium Change text to large

Enlarge Image


Enlarge Image

The Knorr at sea off the coast of Iceland. (Rachel Fletcher)


Enlarge Image

Iceberg and black-legged kittiwakes near the east coast of Greenland. (Rachel Fletcher)


Enlarge Image

The mountainous, unpopulated east coast of Greenland. (Rachel Fletcher)


"The narrow Denmark Strait is the main portal for southbound water."

There is this obscure body of water separating Iceland from Greenland called the Denmark Strait.  It’s not very wide, only some 600 miles, but it’s one of the most important stretches of water in the entire world-ocean circulation.  Here’s why:  Every second of every day millions of cubic meters of warm water flow north along the British Isles and up the coast of Norway aboard an arm of the Gulf Stream System, treating Western Europe to a far more moderate climate than their latitude deserves.  However, if all that warm water flows north, an equal quantity of cold water must flow south to maintain the circulation—the stability of our climate depends on it.  The narrow Denmark Strait is the main portal for southbound water.  Therefore, it’s vital we understand the upstream system that delivers water to the strait.

The accepted theory has held that a current flowing down the East Greenland coast delivered most of the water to the strait.  It sounded reasonable.  Besides, this region was so under-measured no one had enough data to offer another hypothesis.  But then in 2004 two Icelandic oceanographers, Drs. Jonsson and Valdimarsson, found intriguing evidence of an unknown current.  That doesn’t happen very often these days; in fact, it’s almost unprecedented.  The current seemed to pass over the north slope of Iceland and then flow into the Denmark Strait.  The Icelanders were certain enough of its existence to give it a name—the North Icelandic Jet.  Then during a follow-on expedition in 2008, WHOI oceanographer Bob Pickart verified its existence with more extensive measurements.  Not only is this a new current, not only does it flow into this important Denmark Strait—it supplies fully half the water that exits the strait to form the return-flow current.  At least that’s the hypothesis.  It remains to be proven.  That’s what this cruise is all about.

"For the first time ever, we will lay a string of instruments across the entire Denmark Strait."

For the first time ever, we will lay a string of instruments across the entire Denmark Strait.  These will remain in the water for a full year gathering new data to answer long-delayed questions.  That done, we’ll spend the rest of the month-long cruise aboard the WHOI research vessel Knorr searching for the origin of the North Icelandic Jet.  This truly international team of ocean scientists, including the original discoverers, postulates that the origin of the current lies somewhere north of Iceland, but they don’t know for certain.  No one does.  So in this sense, ours is a voyage of exploration different only in objective from those of the legendary Arctic explorers.  They sailed in search of new lands and sea routes; we go in search of new waters.

We hope you’ll use this website, its text, photos, and videos, to follow along.  It’s liable to be cold out there and stormy.  But then heavy wind and wild, icy seas have always been major characters in the grand story of Arctic exploration.

(The Principal Investigators:  Steingrimur Jonsson, Robert Pickart, Laura de Steur, Kjetil Våge, and Hedinn Valdimarsson.)

 



Last updated: September 3, 2011
 


whoi logo

Copyright ©2007 Woods Hole Oceanographic Institution, All Rights Reserved, Privacy Policy.
Problems or questions about the site, please contact webdev@whoi.edu