Web Toolbar by Wibiya

Best Places to Live in the US:
How the States Rank in the Face of Climate Change

Plus: The 10 Greenest Cities
Download
| Maps and analysis for you and your family.


When the media says There's "No Valid Arguments Against ___"

Try these:

Hydrofracking
Nuclear / Indian Point
Gardasil
Vaccination
Genetically-Modified Food
AIDS | HIV

The articles and reports the mainstream media tries to silence.

Health

LISTEN LIVE!

Tell Governor Cuomo:
Don't Frack New York
SIgn up for the bus today!



PLAY IN POPUP!

Trouble? Choose from our alternate ways to listen:

   

You can also call in to hear our live stream at (832) 280-0066!

CONTACT US AT: 888-874-4888

Subscribe to Our Full Podcast Feed!

Fill out your e-mail address
to receive our weekly newsletter,
with exclusive updates,
giveaways, and event invitations!
E-mail address:
 
(We will never, ever share your info with 3rd parties.)

 NEW: Find us on Google+ !

« Academy of Sciences defends climate-change research, conclusions | Main | Slick Operator: The BP I've known too well »
Thursday
May202010

Scientists say Arctic sea ice melting toward record

The latest satellite data show ice coverage is equal to what it was in 2007, the lowest year on record, and is declining faster than it did that year.

"Could we break another record this year? I think it's quite possible," said Mark Serreze of the National Snow and Ice Data Center in Boulder, Colo.

"We are going to lose the summer sea-ice cover. We can't go back."

In April, the centre published data showing that sea ice had almost recovered to the 20-year average. That ignited a flurry of interest on climate change skeptic blogs.

But much of that ice was thin and new. The warmest April on record in the Arctic made short work of it.

Ice cover has already fallen back to where it was in 2007 at this time of year and is disappearing at a faster pace than it did then. Serreze said winds, cloud cover or other weather conditions could slow the melt, but he points out that the decline is likely to speed up even more in June and July.

"Will (thawing) this year be particularly fast?" asked Serreze. "We don't know. We really don't know."

One of Canada's top sea-ice experts suggests things might even be worse than Serreze thinks. His data could be underestimating the collapse of summer ice cover, said David Barber of the University of Manitoba. Researchers can't learn anything from satellite data about the state or thickness of the ice.

"What we think is thick multi-year ice late in the summer is in fact not," he said. "It's heavily decayed first-year ice. When that stuff starts to reform in the fall, we think it's multi-year ice, but it's not."

Arctic explorers and scientific expeditions are finding more open water and untrustworthy ice ever, said Barber.

He pointed out the Arctic continued to lose multi-year ice even in 2008 and 2009, when total ice coverage rebounded somewhat.

True multi-year ice — the thick, hard stuff that stops ships — now comprises about 18 per cent of the Arctic ice pack. In 1981, when Barber first went north, that figure was 90 per cent.

"This is all just part of a trajectory moving toward a seasonally ice-free Arctic," he said. "That's happening more quickly than we thought it would happen."

Once northern waters are clear in the summer, there will be little difference between navigating the Northwest Passage and the Gulf of St. Lawrence, Barber suggested.

He recounts sailing through degraded ice in an icebreaker. The ship's top speed in open water was 13.7 knots. Its speed through the decayed ice was 13 knots.

"It was almost like it didn't exist."



PrintView Printer Friendly Version

EmailEmail Article to Friend

Reader Comments

There are no comments for this journal entry. To create a new comment, use the form below.

PostPost a New Comment

Enter your information below to add a new comment.

My response is on my own website »
Author Email (optional):
Author URL (optional):
Post:
 
Some HTML allowed: <a href="" title=""> <abbr title=""> <acronym title=""> <b> <blockquote cite=""> <code> <em> <i> <strike> <strong>