Of course I'd like to know what this storm will do to the ice and coasts, but first and foremost I hope that no one gets hurt.
From CNN via Desdemona Despair:
November 9 (CNN) – A winter storm of hurricane strength was slamming Alaska early Wednesday with winds of up to 100 mph, high seas and blizzard conditions.
The National Weather Service called the storm moving into the state off the Bering Sea "a powerful and extremely dangerous storm of record or near-record magnitude."
Early Wednesday, Twitter reports said wind speeds in Nome in northwestern Alaska had reached 100 mph. That would be the equivalent of a category 2 hurricane if it occurred in the tropics. Twitter postings reported structural damage in Nome, including the roof blown off a building. Landline phones were down, according to a Twitter post.
"These things get named hurricanes down south and get a category. It's that magnitude," said Jeff Osiensky, regional warning coordination meteorologist with the National Weather Service, told the Anchorage Daily News. The storm's scope was also hurricane-like, he said, covering 750 to 1,000 miles in breadth.
Chip Leeper, incident commander with the Nome government, told CNN that people in low-lying areas and on along the town's sea wall had been advised to seek shelter elsewhere.
National Weather Service meteorologist Steven Kearney told CNN that Nome could endure sea levels up to 8 feet above normal as well as 10-foot waves.
Other coastal and island villages were preparing evacuations if surf became too high.
Inland, the storm was expected to produce blizzard or near-blizzard conditions across western Alaska, the weather service said. Snow accumulations of up to 14 inches were possible. A Twitter poster reported winds gusts of 50 mph in the inland village of Aniak early Wednesday.
CNN also has regular updates now that the storm has reached Alaska.
An interesting quote from the Weather Channel:
Offshore, waves have been reported as high as 40 feet, and dangerous heavy freezing spray will affect the Bering and Chukchi Seas. Waves of 15 to 25 feet are expected to crash along portions of the coastline.
The current lack of sea ice in the Bering Sea will allow this storm to maximize its impact. Ice typically acts as a natural barrier that mitigates the effects of destructive wave action and coastal flooding along the shoreline.
This image was on Jeff Masters' blog: Predicted storm surge for today's storm, as forecast by the Ocean Prediction Center's Extratropical Storm Surge Model. Image credit: NOAA Environmental Visualization Lab.:
This sounds serious for villages like Kivalina, which is built on a low gravel bar between Chukchi Sea and a lagoon.
Posted by: L. Hamilton | November 09, 2011 at 19:49
This will be a 100% mortality event for any Polar Bear swimming in the Chukchi Sea. I expect it will also be a high mortality event for young sea mammals, like Walrus pups. I will be instructive to watch the sea ice edge in the Chukchi over the next 2-3 days.
Posted by: Artful Dodger | November 09, 2011 at 20:14
I've updated the post with a storm surge prediction. On Jeff Masters' blog there is a very informative image of Kivalina.
Is Eric May flying around in his chopper to shoot down any nosey scientists? ;-)
Posted by: Neven | November 09, 2011 at 20:26
It would be most interesting if this strong wind were to compress the existing ice and drive extent measurements downward.
Posted by: Bob Wallace | November 09, 2011 at 21:53
This storm has helped seal 2011 moving into dead last on sea ice extent. And will on area as it catches up,
Crazy. This could help November set record lows by months end in monthly sea ice extent.
Posted by: Chris Biscan | November 10, 2011 at 07:59
Hi all, First post for me. It was cool to follow the "ice extent minimum" stories with you.
Check out recent Arctic ice drift maps at http://osisaf.met.no/p/iceproduct_daily.php?&prod=Drift&area=NH
Recent days clearly show a retreat in ice coverage (and breaking-up of Marginal Ice Zone - in grey) as strong winds blow from Chukchi Sea. Might show even stronger effects in the coming days...
Posted by: tom_oslo | November 10, 2011 at 13:56
Great, Tom!
And also the chart from DMI show a DROP in extent, amazing at this point of season, but as so wisely mentioned above: the nilas/new ice is worthy less than the Greek economy these days....
http://ocean.dmi.dk/arctic/icecover.uk.php
Posted by: Christoffer Ladstein | November 10, 2011 at 14:02
I'm Glad I'm not an estate owner in Kivalina, Alaska; in my opinion I can't understand those deciding to settle there in the first place, but again, the times 'a changing!
Posted by: Christoffer Ladstein | November 10, 2011 at 14:20
Hi guys,
CapitalClimate presents a lot of detail on this mega-storm as well :
http://capitalclimate.blogspot.com/2011_11_06_archive.html
Posted by: Rob Dekker | November 10, 2011 at 18:58
http://gifshack.com/203
Unreal. Has to be the largest loss on the data set in NOvember.
Posted by: Chris Biscan | November 11, 2011 at 12:10
Very impressive. Thanks for that, Chris.
Probably a lot of ridging, meaning thicker ice come next melting season.
Posted by: Neven | November 11, 2011 at 13:50
Christoffer, you're right that Kivalina is in a precarious location, even before the modern era of climate change. The Inupiat people who settled there (and whose descendents today comprise most of the population) almost certainly knew that, but they weren't consulted when the U.S. decided to establish the town.
A local view of Kivalina's history can be found here:
http://www.kivalinacity.com/history.html
Good aerial view here, you can see the problem:
http://en.wikipedia.org/wiki/File:Kivalina_Alaska_aerial_view.jpg
Although the Army Corps of Engineers has constructed a $16 million barrier (as they do) to protect Kivalina, the people are facing tough choices on the "front line" of Arctic change. I wish them well.
Posted by: L. Hamilton | November 11, 2011 at 14:29
Just FYI, for anyone interested in the slightly longer term effects of this storm on Arctic sea ice, here is the latest profile from ITP55 :
http://www.whoi.edu/itp/images/itp55dat3.jpg
ITP55 was located about 100 km from the ice margin at the time of the storm (Nov 11) and the profile shows the temperature and salinity under the ice. At the time of the storm, the upper layer of water was fresh (salinity less than 25 psu). After the storm, the the salinity gradient was disrupted in the upper 50 meters, with more saltier water reaching the surface.
It then took a week or two for heat (at 50-75m) to convect upward, and overall, after 4 weeks, the upper 75 meter of the water under the ice was disrupted, with significant amounts of heat "bubbling" upward.
It is difficult (without a thorough heat content investigation through the upper layers) to determine exactly how much heat made it to the surface, but a back-of-the-envelope calculation reveals that enough heat to (bottom) melt some 10cm of ice should have convected upward due to the stratification disruption that this storm caused.
These are very rough numbers, and only at one spot under the ice, about 100km from the ice margin, so the overall effect of the storm (especially closer to the ice margin) may have been larger (or smaller) than that.
Posted by: Rob Dekker | December 02, 2011 at 07:35
How stormy is it by Svalbard now?
Posted by: crandles | December 03, 2011 at 12:56
Paint.net is free:
http://paint.net/
and can be used to cut images
down to 420 pixels wide so
they fit better.
Posted by: Andrew Xnn | December 03, 2011 at 21:12
Crandles,
This graph shows 50 knot winds near St. Nord in East Greenland but the wind near Svalbard is only 10 knots. The red flags show one line for each ten knots of wind and a triangle for 50 knots (for less than 30 knots the flags are not red). There was a big windstorm in the North Sea yesterday.
Posted by: michael sweet | December 04, 2011 at 01:55
Not to redirect attention away from the developments in the Northern Atlantic, but in the Beaufort, ITP55 continues to amaze :
IPT55 already showed that the Arctic hurricane from Nov 11 caused disruption of Arctic stratification down to 75 meters under the ice, a hundred km away from the ice margin, releasing significant heat from below that was accumulated during the summer melt season.
Now this same thethered profiler shows a massive amount of heat being released from the depths of the Arctic. Difficult to assess exactly how much heat is bubbling up, and it is unlikely that this is all caused by the Nov 11 hurricane, but significant amounts of warm salty water are making it to the surface, disrupting the stratification layer down to 700 meters depth or more.
Did anyone see such deep ocean salinity disruptions before ? What causes it, and how much heat is released to the surface ?
Posted by: Rob Dekker | December 06, 2011 at 10:46
Here is the profile from ITP55 again :
http://www.whoi.edu/itp/images/itp55dat3.jpg
The hurricane occurred aroound day 316.
Posted by: Rob Dekker | December 06, 2011 at 10:48
Hi folks,
Further to the big storm of Nov 2011, here are two other resources:
Kivalina: A Climate Change Story
By Christine Shearer
ISBN: 9781608461288
Published: July, 2011
A new article by Christine was featured on Climate Progress yesterday:
http://thinkprogress.org/romm/2011/12/13/387253/fossil-fuel-companies-face-liability-for-climate-change-disinformation/
Posted by: Artful Dodger | December 14, 2011 at 10:30