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Just curious, Pugwash. What is the significance of "pugwash"? I have pugs, and the idea of washing them is not my favorite thing to contemplate, hence my curiousity.

To the person wishing that we could all tool around in golf carts.....think about how that electricity is produced to power said cart.....burning fossil fuels thus adding to the carbon output.

too bad they dont make golf carts powered by coal. that'd be fun stinkin' up the whole town and of course all the golf courses then one could dump the ashes in the ocean - proper disposal of course!
oops gotta go havent outputted enough carbon yet today!

Your methane output seems fairly healthy today.

One should get so close to be aware!

I think Belize has gone Hydro with the electricity. Lots from Mexico but The new Hydro project started up now with hopes of less purchesed from Mexico.

HEY BOBBER,
CAPTAIN PUGWASH WAS A CARTOON PIRATE IN AN OLD ENGLISH KIDS PROGRAM IN THE 60'S. HE WAS THE FEARLESS LEADER OF MASTER MATE, TOM THE CABIN BOY, WILLY AND BARNABUS AS THEY BATTLED CUT-THROAT JAKE FOR MASTERY OF THE SEAS. MY WIFE ANOUNCED THAT STANDING AT THE HELM OF MY BOAT AS IT SAT ON A TRAILER BEHIND MY HOUSE IN UTAH "YOU LOOK LIKE CAPTAIN PUGWASH" AND SHE WHISTLES THE THEME TUNE WHENEVER I GO OUT TO DO ANY WORK ON IT (THE BOAT)
http://en.wikipedia.org/wiki/Captain_Pugwash

Arctic sea ice begins to re-freeze
This summer's dramatic loss of Arctic sea ice peaked on September 15, and the polar ice cap is finally beginning to re-freeze, according to a press release http://nsidc.org/news/press/2007_seaiceminimum/20071001_pressrelease.html
issued by the National Snow and Ice Data Center on October 1. Extent of the September polar sea ice fell 39%, compared to the 1979-2000 average. To put this loss in perspective, in one year we lost as much ice as we lost during the previous 28 years. Summertime Arctic sea ice is now at 50% of what it was in the 1950s (Figure 1). One may look at at graph and wonder, but what about sea ice loss in other seasons? It hasn't been nearly so severe. True, but it is the summer ice we care most about, since summer is when the thick, multi-year ice melts, which can then precondition the Arctic for much greater ice loss in future years. As sea ice melts in response to rising temperatures, more of the dark ocean is exposed, allowing it to absorb more of the sun's energy. This further increases air temperatures, ocean temperatures, and ice melt in a process know as the "ice-albedo feedback" (albedo means how much sunlight a surface reflects). There is an excellent chance that the summer of 2007 will be remembered as the "tipping point" for Arctic sea ice, when an irreversible ice-albedo feedback process firmly established itself.



Figure 1. Arctic sea ice extent since 1900, as estimated from satellite and ship reports compiled by Walsh and Chapman (2001). Image credit: University of Illinois cryosphere group. http://arctic.atmos.uiuc.edu/cryosphere/IMAGES/seasonal.extent.updated.jpg

Northwest Passage opens for the first time in recorded history
Long before the Panama and Suez Canals made commercial trading between the Atlantic and Pacific Oceans economically feasible, ships made the long and perilous trip around the African and South America continents. Explorers, traders, and world leaders looking for faster and less dangerous shipping routes to far-away areas of the world have long eyed two routes through the ice-choked Arctic Ocean--the fabled Northwest Passage, through the cold Arctic waters north of Canada, and the Northeast Passage, extending along the northern coast of Russia. The first recorded attempt to find and sail the Northwest Passage was in 1497, and ended in failure. The thick ice choking the waterways thwarted all attempts at passage for the next four centuries. Finally, in 1905, Roald Amundsen completed the first successful navigation of the Northwest Passage. It took his ship two-and-a-half years to navigate through narrow passages of open water, and his ship spent two cold, dark winters locked in the ice during the feat. More recently, icebreakers and ice-strengthened ships have on occasion battered their way through the ice-blocked route.



Figure 2. The Northwest Passage shipping route (red line) and Northeast Passage (green line) superimposed on an ice coverage map from August 22, 2007. The Northwest Passage was ice-free and navigable for 36 days between August 14 and September 18, 2007. The Northeast Passage was blocked by a narrow strip of ice most of the summer. Image credit: National Snow and Ice Data Center. http://nsidc.org/news/press/2007_seaiceminimum/20070810_index.html

Times are changing. In 2001, the Bering Strait, a key portion of both the Northwest and Northeast Passages, was completely ice free. This was followed in 2005 by record-breaking sea-ice melt in the Arctic, leading to the first ever recorded opening of the Northeast Passage. The fabled Northwest Passage remained closed in 2005. Arctic ice recovered a bit in 2006, and both passages remained closed. But the unprecedented melting during the summer of 2007 saw the Northwest Passage become ice-free and navigable along its entire length without the need for an icebreaker as of August 14, 2007. Remarkably, the Northwest Passage remained ice-free for 36 days, finally refreezing over a small section on September 19. The Northeast Passage was blocked by a narrow strip of ice all summer. However, this strip of ice thinned to just 30% coverage on September 25 and 26, making the Northeast Passage passable for ordinary ships on those days.

When is the last time the Northwest Passage was open?
We can be sure the Northwest Passage was never open from 1900 on, as we have detailed ice edge records from ships. It is very unlikely the Passage was open between 1497 and 1900, since this was a cold period in the northern latitudes known as "The Little Ice Age". Ships periodically attempted the Passage and were foiled during this period, and the native Inuit people have no historical tales of the Passage being navigable at any time in the past.

A good candidate for the last previous opening of the Northwest Passage was the period 5,000-7,000 years ago, when the Earth's orbital variations brought more sunlight to the Arctic in summer than at present. Prior to that, the Passage was probably open during the last inter-glacial period, 120,000 years ago. Temperatures then were 2-3 degrees Centigrade higher than present-day temperatures, and sea levels were 4-6 meters higher.

Final thoughts
If we have reached the tipping point for Arctic ice, what are the implications? I'll discuss this more in a future blog. Sea ice is very complicated, and it is not a sure thing that we have reached the tipping point. For more on the complexities of sea ice, read wunderblogger Dr. Ricky Rood's latest blog. http://www.wunderground.com/blog/RickyRood/comment.html?entrynum=45&tstamp=200710

NASA http://earthobservatory.nasa.gov/NaturalHazards/natural_hazards_v2.php3?img_id=14572 has posted a beautiful satellite image of the Arctic ice cap at the September 15 2007 minimum, showing the open water of the Northwest Passage.

I thank Edalin Michael of the University of Michigan's School of Natural Resources and Robert Grumbine of NOAA's Sea Ice Group for their contributions to this blog.

References
Walsh, J.E and W.L.Chapman, 2001, "Twentieth-century sea ice variations from observational data" http://www.ingentaconnect.com/content/igsoc/agl/2001/00000033/00000001/art00071 , Annals of Glaciology, 33, Number 1, January 2001 , pp. 444-448

Jeff Masters