The Heat Is Online

Greenland Winds Tied to Ocean Circulation Changes

Greenland winds linked to global climate

Researchers say so-called 'tip jets' drive ocean circulation

 

LiveScience.com, March 26, 2007

 

Greenland is not known for hurricanes, but the frigid land mass does host some of the strongestand most mysteriouswinds on the planet. Now scientists say the bizarre winds could be linked to weather and climate phenomena far from the icy realm.

 

After two weeks of flying head-on into hurricane-force winds that whipped recently around the southern tip of Greenland, a group of scientists has a better idea of just how these winds relate to broader weather patterns, global ocean circulation and climate.

 

Weather experts have only really known about these so-called tip jets for less than a decade, and most of what they knew was from satellite data. The team of scientists, as part of the International Polar Year effort, recently sought  to go airborne for a close-up look at the roaring winds.

 

Distorted flow

 

Tip jets form at Greenland when cyclones, large rotating weather systems, meet with the island's hulking mass on their northward journey across the Atlantic Ocean, causing air flow to be distorted and winds to speed up.

 

The air is forced to move around the obstacle, [which] causes these accelerations of the wind, said study team member Kent Moore of the University of Toronto.

 

These accelerations are created in the same way as a plane gains lift. The planes wing diverts the air into two directions: air traveling over the top of the wing flows over a flat surface, while air flowing under the bottom travels over a curved surface; because the curved surface creates a longer path for the air to travel, the air must speed up to meet up with the wind flowing over the top.

 

The air parcels that are forced to go around Greenland have a longer path than [parcels] that go over it, for instance. And because they have to all meet up at the end, the ones that go around have to accelerate, Moore explained.

 

Depending on the cyclones position relative to Greenland, either a reverse tip jet, which blows from east to west, or a forward tip jet, which blows from west to east, forms. When the low pressure system is south of Greenland, a reverse tip jet forms, and when it is northeast of Greenland a forward tip jet forms.

 

This dual wind behavior is highly unusual: in the United States, for example, large-scale winds blow primarily from the west, while winds from the east are rare except on local scales where mountains or other landforms control the flow.

 

Cape Farewell is this really odd place where you get really strong winds of both directions, and thats very rare. Theres very few places in the world where the winds blow very strong from two different directions, Moore said.

 

Adding turbulence

 

What makes these narrow jets of sometimes 100 mph winds so important? They could be one of the drivers of the oceans main circulation.

 

On the global conveyor belts path, warm water from the tropics flows northward to the pole, where it becomes denser and sinks to the ocean floor, and then returns to the tropics. The waters density increases as it becomes colder and saltierwinds blowing over the water can transfer heat and moisture away from the surface waters, which is what Moore suspected the tip jets were doing.

 

This experiment was to test the hypothesis that we could actually get enough heat and moisture transfer between the ocean and the atmosphere in these tip jet events to actually trigger convection in the ocean, Moore said.

 

Turbulence in the air near the oceans surface are the mechanism for the heat transfer, just as bubbles transfer heat in a pot of boiling water.

 

Theres all these little eddies, or little turbulent activity, and thats actually the thing that is transferring the heat from the ocean into the atmosphere, Moore said.

 

Though Moores results are not yet final, it appears as if enough heat is transferred to cause the ocean water to overturn, he said.

 

Catch-22

 

As the tip jets form when a cyclone travels by Greenland, the cyclone itself is affected by the frozen mass: If Greenland wasnt there, the cyclones would have a very different track, Moore said.

But because Greenland is in the way, the cyclones diverge into different directions.

 

Greenlands ice cap relies on precipitation from the cyclones to sustain itself, but when cyclones are diverted, less precipitation falls, and the ice cap shrinks, which in turn diverts the cyclones less.

These cyclones are being distorted byits kind of a Catch-22but theyre sort of being affected by the presence of the ice mass modifying how they deliver precipitation to the ice cap.

 

Moore hopes that by clarifying the role the tip jets play in driving ocean circulation and how the cyclones that create them affect Greenlands climate, a better picture of just how climate change is affecting the island will come into focus.

 

© 2007 LiveScience.com. All rights reserved.