* Astronomy

Members Login
Post Info TOPIC: Arctic superflood


L

Posts: 131433
Date:
RE: Arctic superflood
Permalink  
 


New research indicates that one of the largest fresh-water floods in Earth's history happened about 17,000 years ago and inundated a large area of Alaska that is now occupied in part by the city of Wasilla, widely known because of the 2008 presidential campaign.
The event was one of at least four "megafloods" as Glacial Lake Atna breached ice dams and discharged water. The lake covered more than 3,500 square miles in the Copper River Basin northeast of Anchorage and Wasilla.
The megaflood that covered the Wasilla region released as much as 1,400 cubic kilometres, or 336 cubic miles, of water, enough to cover an area the size of Washington, D.C., to a depth of nearly 5 miles. That water volume drained from the lake in about a week and, at such great velocity, formed dunes higher than 110 feet, with at least a half-mile between crests. The dunes appear on topographical maps but today are covered by roads, buildings and other development.

Read more

__________________


L

Posts: 131433
Date:
RE: Arctic thaw
Permalink  
 


With the coming of spring, the ice on Canada’s Hudson Bay has begun to break up.
Large chunks of ice float near the eastern shore of the bay, while to the west, the centre of the bay remains frozen.


Expand (5386 kb)

In the upper right corner is the Ungava Peninsula, the northern part of the Canadian Territory of Quebec. With its sub-arctic climate, the snow-covered peninsula is home to the Inuit and Cree Nations.
To the south green vegetation slowly blends into the winter-brown landscape, another sign that spring is creeping north.
Ontario borders the Hudson Bay in the southwest, the lower left corner of the image, while Quebec forms the south-eastern border, lower right.

The Moderate Resolution Imaging Spectroradiometer (MODIS) on NASA’s Terra satellite captured this true-colour image on May 21, 2005.

Longer melt seasons in high northern latitudes have attracted the attention of scientists monitoring climate change as Arctic sea ice has reached record lows.
In the Hudson Bay itself, a recent study in the journal Arctic found a significant increase in the ice-free season between 1971 and 2003, consistent with warmer temperatures.

NASA image courtesy Jeff Schmaltz MODIS Rapid Response Team, NASA-GSFC




__________________
Anonymous

Date:
RE: Arctic superflood
Permalink  
 


 


 



REALPLAYER  Station


 


Download the mp3 (8 Mb)



__________________


L

Posts: 131433
Date:
Permalink  
 

A catastrophic 'superflood' following the rupture of a massive glacier-dammed lake in Canada at the end of the Ice Age probably plunged the world into centuries of climatic chaos.

That single event was likely responsible for the most dramatic climate change of the last 10,000 years, according to an old report by a Canadian team led by Professor Garry Clarke, a geophysicist at the University of British Columbia in Vancouver.

The 'superflood' was enough to alter ocean circulation in the Northern Hemisphere: analysis of ice cores taken in Greenland reveal that for the next 200 years or so, the mean temperature dropped by 5°C, snow accumulation decreased sharply and forest fires became more frequent.



Clarke's team found that the water body, known as Lake Agassiz, reached a massive 163,000 cubic km in volume - at least double that of the largest contemporary lake, the Caspian Sea - and that its release was "by far the largest known glacial outburst of the past 100,000 years".

It was formed after the vast Laurentide Ice Sheet, which at its maximum formed a 3-kilometre-thick dome over Hudson Bay, began disintegrating rapidly about 8,500 years ago.

As the ice sheet retreated north, it left behind a large depressed area of land. This sloped towards the former ice dome and gradually filled with meltwater and run-off from precipitation to become Lake Agassiz.

But icebergs and remnants of the ice sheet dammed the lake, which at its maximum elevation had a natural 'spillway' about 230 m above sea level, the researchers said.

"Modern analogues and the known physics of outburst flooding indicate that tunnelling below the ice is the most probable flood release mechanism. Because ice floats on water, thinning ice dams are unstable. Initiation of a flood routed beneath the ice therefore pre-empts the possibility of a flood routed across the ice. Once a subglacial path is established, an ice-walled conduit will tend to grow by melting its walls" - Garry Clarke.



As water tunnelled its way through the ice dam, its rupture became unavoidable. The team said that on the basis of radiocarbon dating, a full torrent was finally unleashed about 8,450 years ago. It took less than a year to discharge.

After the lake water gushed into the Hudson Bay, its freshness altered the strength of ocean circulation, which in turn caused the abrupt climate changes in much of the Northern Hemisphere, the team said.

Geological evidence suggests that this first flood was followed by a smaller one from a lower water level of about 125 m, either because the lake was drained by two successive outbursts or because the first flood drained it to sea level or because the ice-dam reformed and allowed it to partly refill before breaking again.

Either way, once the dam had been permanently breached, the discharge that formerly overflowed to the St Lawrence Valley was routed northward to Hudson Bay.

The researchers argue that understanding the mechanisms underlying past climate change events is increasingly important as people grow more concerned about the magnitude and rate of future climate change.

"Changes in the volume and extent of the ice sheets that once covered much of North America directly influenced the freshwater balance of the North Atlantic and are implicated in many abrupt climate events of the past 100,000 years."
"During the last Ice Age, when a kilometres-thick ice sheet covered most of Canada and parts of the northern United States, armadas of icebergs were episodically launched into the North Atlantic. The melting of this freshwater ice and the associated freshening of ocean surface waters are believed to have changed the strength of the oceanic thermohaline circulation, thereby causing abrupt climate changes".

This has implications on the recent finding on Arctic meltwater.

Related Link:

Update

-- Edited by Blobrana at 19:56, 2006-05-31

__________________
Page 1 of 1  sorted by
Quick Reply

Please log in to post quick replies.



Create your own FREE Forum
Report Abuse
Powered by ActiveBoard