Julia Whitty

Julia Whitty

Environmental Correspondent

Julia is an award-winning author of fiction and nonfiction (Deep Blue Home, The Fragile Edge, A Tortoise for the Queen of Tonga), and a former documentary filmmaker. She also blogs at Deep Blue Home.

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Julia is a writer and former documentary filmmaker and the author of The Fragile Edge: Diving & Other Adventures in the South Pacific, winner of a PEN USA Literary Award, the John Burroughs Medal, the Kiriyama Prize, the Northern California Books Awards, and finalist for the Dayton Literary Peace Prize, and Deep Blue Home: An Intimate Ecology of Our Wild Ocean. Her short story collection A Tortoise for the Queen of Tonga won an O. Henry and was a finalist for the PEN Hemingway Award. She also blogs at Deep Blue Home.

A Creepy October in the Arctic

| Tue Nov. 6, 2012 4:13 AM PST

View from the 05 Deck on USCG icebreaker Healy on 15 October 2012: Julia WhittyView from the 05 Deck on USCG icebreaker Healy on 15 October 2012: Julia WhittyThis was the view at sunrise from the 05 deck five levels above the main deck of the Coast Guard icebreaker Healy three weeks ago. (For more about this science cruise check out my Arctic Ocean Diaries.) It was a balmy 27°F (-2°C). On the same cruise last year temperatures fell to -20°F (-29°C). Last month the ocean was relatively calm. There wasn't much of anything to indicate we were actually in the Arctic. It looked a lot like South Pacific sunrises I've watched from open boats in a shorty wetsuit. Frankly it was creepy.

Arctic sea ice extent for October 2012 was 2.7 million square miles (7 million square kilometers). Magenta line shows 1979 to 2000 median extent for that month. Black cross indicates geographic North Pole. Yellows shows seas within the Arctic Ocean: National Snow and Ice Data CenterArctic sea ice extent for October 2012 was 2.7 million square miles (7 million square kilometers). Magenta line shows 1979 to 2000 median extent for October. Black cross marks geographic North Pole. Yellow names mark the seas of the Arctic Ocean: National Snow and Ice Data Center

Yesterday the National Snow and Ice Data Center (NSIDC) released their monthly overview of Arctic sea ice for October 2012, which explains a lot of what I saw. The map above shows October 2012 ice in white, compared to the median sea ice extent from 1979 to 2000 (pink line). Here's what the NSIDC report says:

Average ice extent for October was 7.00 million square miles (2.70 million square miles). This is the second lowest in the satellite record, 230,000 square kilometers (88,800 square miles) above the 2007 record for the month. However, it is 2.29 million square kilometers (884,000 square miles) below the 1979 to 2000 average. The East Siberian, Chukchi, and Laptev seas have substantially frozen up. Large areas of the southern Beaufort, Barents, and Kara seas remain ice free.

That's less ice in the Arctic this October than an area of Alaska and Texas combined.

My cruise covered the entire eastern extent of the Chukchi Sea and the entire southern extent of the Beaufort Sea. These are the Alaskan parts (and some Canadian parts) of the Arctic Ocean. The fact that they remain largely ice free even now could bode poorly for ecosystems accustomed to a cap of sea ice most of the year.

a snapshot of how ocean depth in the Arctic influences sea ice extent. Sea ice cover for August 28, 2012 is shown in semi-transparent white; ocean depths are indicated in blues, with deeper blues indicating greater depth: National Snow and Ice Data Center courtesy Jamie Morison/Applied Physics Laboratory, University of WashingtonA snapshot of how ocean depth in the Arctic influences sea ice extent. Sea ice cover for 28 August 2012 is shown in semi-transparent white, ocean depths in blues, deeper blues indicating greater depth: National Snow and Ice Data Center courtesy Jamie Morison/Applied Physics Laboratory, University of Washington

Really interesting in the NSIDC report is an analysis of what forces may affect sea ice formation:

Research by our colleagues Jamie Morison at the University of Washington Seattle and NASA scientist Son Nghiem suggests that bathymetry (sea floor topography) plays an important role in Arctic sea ice formation and extent by controlling the distribution and mixing of warm and cold waters. At its seasonal minimum extent, the ice edge mainly corresponds to the deep-water/shallow-water boundary (approximately 500-meter depth), suggesting that the ocean floor exerts a dominant control on the ice edge position.

They note that in some some cases sea ice survives even in shallower continental shelves because of water circulation patterns. The shelf of the Greenland Sea is nearly always ice covered because of southward-flowing Arctic currents that keep it cold. Meanwhile other shallow areas like the Barents and Chukchi seas lose their ice cover due to warm ocean waters and freshwater runoff from rivers—two forces that are increasing in strength as the land warms too.

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Riding the Storm: Messenger on a Bike From the Entrails of Hurricane Sandy

| Fri Nov. 2, 2012 11:30 AM PDT

 

 Hurricane Sandy on Bikes in NYC from Casey Neistat on Vimeo.

"No city authorized filming will take place," announced New York Mayor Bloomberg as Hurricane Sandy approached. But that didn't stop filmmaker Casey Neistat from getting out on his bike and shooting this crazy awesome scary footage during the storm.

Not a Polar Bear in Sight: Arctic Ocean Diaries No. 11

| Wed Oct. 31, 2012 2:19 PM PDT

Polar bear diorama at Anchorage airport: Julia WhittyPolar bear diorama at Anchorage airport: Julia WhittyI'm home from my cruise aboard the US Coast Guard icebreaker Healy and its science mission to study the effects of a changing climate on the Arctic Ocean. When I set out a month ago I never imagined that we'd never encounter any sea ice (I wrote more on that here). And that the only polar bears I'd see were these stuffed specimens on display at the Anchorage airport. Naturally I'm disappointed.

But for the bears who couldn't find any sea ice within 500 miles of Alaska, and for the seals who need sea ice to haul out onto for pupping, and for the Arctic foxes who make a living following polar bears across the ice, and for the ivory gulls who do the same, and for the people of the Western Arctic who rely on subsistence hunting, the situation may well have been desperate this year.

As Jeremy Mathis, chemical oceanographer at University of Alaska Fairbanks and one of the principle investigators aboard my Healy cruise, told me: "We fell off a cliff in 2007 when Arctic sea ice extent hit a record low. And we fell of another this year."

2012 Arctic sea ice minimum (top). 1984 Arctic sea ice minimum (bottom): NASA Earth ObservatoryThe 2012 Arctic sea ice minimum (top) compared to the 1984 Arctic sea ice minimum (bottom): NASA Earth ObservatoryThings are changing so rapidly in the Arctic. Yet we have few baseline data with which to understand these changes. Aboard Healy I watched every scientist working as hard as humanly possible just to try and catch up with events racing away from us.

It reminds me of another monumental story I covered: disastrous change, few data, poor understanding, and the need to learn faster than we've ever learned before. That was BP's Deepwater Horizon oil debacle in the Gulf of Mexico.

Deploying a mooring buoy from UCGC icebreaker Healy, Arctic Ocean, October 2012: Julia WhittyScience and Coast Guard crew work to deploy a mooring buoy from USCG icebreaker Healy in the Arctic Ocean, October 2012: Julia WhittyWhat I found most hopeful aboard USCGC Healy was the impressive cooperation between US military personnel—the hardworking Coast Guard crew—and scientists from around the world. They worked different aspects of this science mission. But it was clear they were working the same mission and shared many of the same concerns.

I'll be writing more about this cruise in the coming months, what the data are revealing, and what that might mean for our collective future as Earth's climate continues to warm.

Jeremy Mathis' research aboard Healy is supported by the National Science Foundation, Office of Polar Programs. My personal thanks go out to Jeremy Mathis, to Bob Pickart at WHOI, Principle Investigator aboard, to Captain Beverly Havlik, Commanding Officer of Healy, and to all the science and Coast Guard crew who worked the Healy 1203 mission.

The Little Glider That Could: Arctic Ocean Diaries No. 10

| Thu Oct. 25, 2012 3:13 AM PDT
Donglai Gong with the Slocum glider on the flight deck of USCG icebreaker Healy.

Editor's note: Julia Whitty is on a three-week-long journey aboard the the US Coast Guard icebreaker Healy, following a team of scientists who are investigating how a changing climate might be affecting the chemistry of ocean and atmosphere in the Arctic.

One of the more engaging stories on the ship has been that of Donglai Gong, an assistant professor at the Virginia Institute of Marine Science, and his Slocum glider, named after the legendary 19th-century sailor Joshua Slocum, the first man to sail single-handedly around the world.

This Slocum is an unmanned robot that can fly underwater for 20 to 30 kilometers a day for weeks to months collecting high-resolution data on temperature, salinity, pressure, and other water qualities.

Plan A was to deploy the glider in the region of Barrow Canyon, a dynamic pathway of Pacific Ocean water into the Arctic Ocean. But due to the bowhead whaling season underway, Plan B in the Chukchi Sea was launched.

Donglai Gong watches the glider launch from the Healy Bridge.  Julia Whitty.]Donglai Gong watches the glider launch from the Healy Bridge. Julia Whitty.

But before Plan B could get started, Donglai needed to perform a buoyancy test on the glider. That was conducted 70 kilometers away from the Plan B launch site. Unfortunately, the glider never surfaced from this test and when the crew on the small boat pulled in the buoy attached to the glider to see what was up, the glider was gone.

Donglai was watching from the Healy Bridge. His excitement—I thought he looked like an expectant father—gave way to shock at the realization that the glider might be lost and his experiment abruptly ended. Worse, the glider wasn't even his own, but on loan to him from the Woods Hole Oceanographic Institute (WHOI). Ooops.

Donglai with email from the glider. Julia WhittyDonglai with email from the glider. Julia Whitty

But the story wasn't over. An hour and half later Donglai got an email on his iPhone. It was a message from the glider, which had kicked into emergency mode and surfaced to uplink its location to a satellite.

By then night had fallen and recovery wouldn't be possible until the following morning.  Donglai made the risky but scientifically rewarding decision to leave the glider where it was and to ask it to its start its mission right there, 70 km away from the Plan B starting point.

Map of the glider's flight from 12 to 20 October 2012 in the Arctic Ocean. Steve Roberts / National Center for Atmospheric Research.]Map of the glider's flight from 12 to 20 October 2012 in the Arctic Ocean. Steve Roberts / National Center for Atmospheric Research.]

So the little glider that could jumped the starting pistol and took off towards the Beaufort Sea on Amended Plan B.

In the map above you can see the eventual flight path of the glider, here named we04. For eight days it flew roughly 200 nautical miles along the outer edge of the Beaufort shelf where shallower water drops off to deeper water. A current flowing in the same direction helped the glider on its way. Each green point on the map marks where the glider surfaced every ~2.5 hours to upload its data collected roughly every 1 kilometer of distance travelled.

From unintended launch to successful retrieval, Donglai, with assistance from colleagues at WHOI and Rutgers University, kept the glider on its track, flying towards its eventual rendezvous location with Healy last Saturday.

Last night Donglai let me listen in on some of the recordings the glider had captured from its travels across the Beaufort Sea, including calls that sounded to me like bearded seals. Part 2 of his project will be to test using acoustics as a way to communicate with a glider or gliders deployed under the Arctic ice pack. Maybe next year.

Donglai's glider research was conceived on last year's Healy cruise with his (then) postdoc mentor Bob Pickart at WHOI, Principle Investigator on that cruise and on this one too.

Where's the Ice?: Arctic Ocean Diaries No. 9

| Mon Oct. 22, 2012 12:18 PM PDT

Editor's note: Julia Whitty is on a three-week-long journey aboard the the US Coast Guard icebreaker Healy, following a team of scientists who are investigating how a changing climate might be affecting the chemistry of ocean and atmosphere in the Arctic.

Sea ice in the Western Arctic on 03 October 2012.  Steve Roberts / National Center for Atmospheric Research (NCAR) Sea ice in the Western Arctic on 03 October 2012. Steve Roberts / National Center for Atmospheric Research (NCAR)

The big story of this cruise is sea ice. As in, there isn't any. At least not in our part of the Arctic Ocean. This year set a new record for lowest Arctic sea ice extant. So our odds of seeing any at this time of year weren't good to begin with.

Still, almost everyone who set foot on the icebreaker Healy was hoping to encounter some. Sadly we haven't seen any ice aside from what's frozen on the decks and windows of the ship.

But the sea ice is growing fast now. The top map shows sea ice extent in this part of the Arctic on 03 October, the day I arrived in Dutch Harbor, Alaska. This analysis comes from the National Ice Center (NIC). Pink areas suggest ice cover of 80 percent or greater. Yellow marks marginal ice formation.

If you measure from due north of Point Barrow, Alaska, the ice front was roughly 440 nautical miles (506 miles / 815 kilometers) from land on 03 October.

Sea ice extent in the western Arctic as of 20 October 2012. Steve Roberts / National Center for Atmospheric Research (NCAR)Sea ice extent in the western Arctic as of 20 October 2012. Steve Roberts / National Center for Atmospheric Research (NCAR)

This next map shows the sea ice extent as of yesterday, 20 Oct 2012. On that day, according to the NIC analysis, the ice front reached to within ~133 nautical miles (153 miles / 246 kilometers) of Point Barrow.

Averaged out, that out a growth rate of 18 nautical miles (20 miles / 33 kilometers) a day. Though in reality the sea ice advanced more slowly in the early part of the month and is galloping faster now.

The red track line marks Healy's meandering for the past two-plus weeks as we visit mooring stations and CTD lines across the Beaufort and Chukchi Seas.

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