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.

Pygmy Seahorse Discovered on Google Street View

| Wed Sep. 26, 2012 10:43 AM PDT

Denise's pygmy seahorse: O.J.Brett, Norway, via Wikemedia CommonsDenise's pygmy seahorse: O.J.Brett, Norway, via Wikimedia Commons

In the course of mapping the the world's reefs for Google Street View, divers found the teensy weensy Denise's pygmy seahorse (Hippocampus denise) in Australian waters for the first time, reports New Scientist (subscription). The five-eighths-inch long (1.5 cm) seahorse had previously been found living on coral reefs off Vanuatu, Palau, Malaysia, Solomon Islands, New Caledonia, and southern Japan. The mapping team found it off Heron Island on the Great Barrier Reef at 302 feet (92 meters) deep.

"It's very much a critical time for reefs and we want to cover as much as we can in the next two to three years to create a global record," says project founder and director Richard Vevers.

The announcement marks today's launch of Google underwater street view. In the same way you can virtually walk around the topside world you can now virtually dive through the underwater world of a coral reef off Australia. It's stage one of a six-part underwater series. Next up, the deep and shallow coral reefs of Hawaii, the Philippines, and Bermuda.

The mappers are Catlin Seaview Survey—a partnership between the global insurance company Catlin Group Limited and the nonprofit Underwater Earth (check out the insanely beautiful images at their site). One of the two unique cameras used for the project (each capturing ≤50,000 360-degree panoramic images stitched together to create the underwater street views) was named "Sylvia," for legendary marine biologist Sylvia Earle, founder of Mission Blue.

The lucky mappers probably have the coolest job on Earth. And they've given us another unbelievably addicting way to get no work done.

 

 

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"New" CO2 Source Spells Trouble for Marine Life

| Fri Sep. 21, 2012 3:07 AM PDT

CO2 from water pollution interacts with atmospheric CO2 in a warming ocean to intensify changes in acidity, spelling trouble for marine life: Witches: ~Brenda-Starr~; Scallop: walknboston; Anemonefish: lakewentworth; Seahorse: Mr. Mohammed Al Momany | NOAA. Starfish: MikeMurphy. Mashup: Julia Whitty.Witches' brew: CO2 from water pollution interacts with CO2 from atmosphere in a warming ocean to intensify acidification: Witches: ~Brenda-Starr~. Scallop: walknboston. Anemonefish: lakewentworth. Seahorse: Mr. Mohammed Al Momany | NOAA. Starfish: MikeMurphy. Mashup: Julia WhittyA new kind of witchy interaction is underway in the oceans, report the authors of a new paper in Environmental Science & Technology.

William G. Sunda and Wei-Jun Cai created a model to predict how CO2 from water pollution—that is, runoff from chemical fertilizers (farms), human waste (sewage), and animal waste (feedlots, ranches), plus nitrogen oxide from fossil fuel burning—might interact with the better-known source of CO2 that enters the ocean from the atmosphere, much of it a result of fossil fuel burning.

In either case, too much CO2 entering the ocean lowers the pH of seawater, which raises the acidity of the waters, preventing many marine organisms from getting access to the calcium carbonate needed to make their shells or skeletons. The result, called ocean acidification—sometimes called the "other CO2 problem," global warming being the original—is already impacting commercial oyster beds in the Pacific Northwest. This process has been firmly on the scientific radar for the past 10+ years.

But no one has spent a whole lot of time thinking about the excess CO2 created by water pollution running off the land. Here's what happens. Enriched waters wash off farms, feedlots, and cities to fertilize the ocean. Enough fertilized runoff triggers a cascade of catastrophic events:

  • Fertilizing huge algal blooms
  • Which lead to massive die-offs of the huge algal blooms
  • Which settle to the bottom and feed the growth of bacteria
  • Who consume much of the available oxygen in the water and release large amounts of CO2
Clams, oysters, scallops, mussels, and finfish could be the most heavily impacted in affected coastal regions such as the Gulf of Mexico and the Baltic Sea.

The result is a dead zone: where oxygen levels are too low (hypoxic) to support most marine life. A good example is the Gulf of Mexico dead zone that "blooms" every spring and summer when the spring and summer rains wash the excess nutrients from the bread basket of the American heartland downstream into the ocean. I wrote more about that here and here.

But there's the excess CO2 of a dead zone too—which also causes ocean acidification. Basically the other other CO2 problem.

So the authors wondered: what happens when you get ocean acidification from the atmosphere mixing with ocean acidification from water pollution?

Their model predicts that rising acidity from water pollution will interact synergistically—that is, more than just the sum of the two sources—with rising acidity from air pollution at intermediate to higher temperatures. Together, the two processes could substantially increase ocean acidification and impact commercial fisheries in places with dead zone problems, like the northern Gulf of Mexico and the Baltic Sea.

Lead author Bill Sunda says: "The largest acidification effects from decaying algal blooms actually occur in colder waters such as those in coastal waters of Northern Europe or Alaska. However, in warmer ocean waters, where the acidification effects from this source are currently smaller, the rising atmospheric CO2 not only lowers the pH (raises the acidity) of the water, but makes the additional acidification effects from decaying algal blooms much worse; i.e., there's a synergistic effect (the effect of the two processes together are more than additive in lowering pH [or are more than multiplicative in raising acidity])."

From the paper:

Thus, while the impact of the two acidification mechanisms by themselves may be moderate in many instances, the combined effect of the two can be much larger. Such large combined acidification effects may cause significant negative impacts on coastal benthic [seafloor] ecosystems that are already stressed by hypoxia and rising water temperatures. Coastal systems support most world finfish production and the overwhelming majority of shellfish production, so the combined negative future impact of these anthropogenic stressors to marine ecosystems and fisheries production could be substantial. However, future impacts will not only be dependent on increasing atmospheric PCO2 [partial pressure of CO2] or the amount of respiratory depletion of O2 [oxygen], but also on temperature and salinity, which will be influenced in the future by a changing climate linked to increasing CO2 in the atmosphere.

 

The bubbling brew of CO2 synergies: Witches: ~Brenda-Starr~. Diagram: Sunda and Cai, ES&T doi: 10.1021/es300626f. Mashup: Julia WhittyThe bubbling brew of CO2 synergies: Witches: ~Brenda-Starr~. Diagram: Sunda and Cai, ES&T doi: 10.1021/es300626f. Mashup: Julia Whitty

The paper:

William G. Sunda and Wei-Jun Cai. Eutrophication Induced CO2-Acidification of Subsurface Coastal Waters: Interactive Effects of Temperature, Salinity, and Atmospheric PCO2. Environmental Science & Technology (2012). DOI:10.1021/es300626f

 

Hottest Ever Water Temperatures Off East Coast All the Way Down to the Bottom of the Ocean

| Tue Sep. 18, 2012 11:49 AM PDT

Cod: Derek Keats. Flame: designshard. Bubbles: Velo Steve. All via Flickr.Cod: Derek Keats. Flame: designshard. Bubbles: Velo Steve. All via Flickr. Mashup: Julia Whitty.

Sea surface temperatures (SSTs) off the East Coast from North Carolina to the Gulf of Maine were the hottest ever recorded for the first six months of 2012, according to NOAA's latest Ecosystem Advisory. Above-average temperatures were found everywhere: from the sea surface to the ocean bottom and out beyond the Gulf Stream.

The area is known as the Northeast Shelf Large Marine Ecosystem. Parts of it were declared a fisheries disaster last week (I posted about that here: Fisheries Declared Disasters on Four Coasts). This was due to the fact that stocks of cod, yellowtail flounder, and other groundfish are not rebuilding even though most fishers have adhered to tough quotas.

The problem lies in the warming waters. The super warm SSTs of 2012 jumpstarted an early and intense spring plankton bloom—which began in some places as early as February—and lasted longer than average. This ricocheted through the marine foodweb from the smallest creatures to the largest marine mammals like whales.

NOAA | NEFSC Ecosystem Assessment ProgramNOAA It forced the ongoing trend whereby Atlantic cod are shifting northeastward from their historic distribution center. That's consistent with a response to ecosystem warming—as you can see that in the two maps above. The top map shows cod distribution between 1968-1972. The bottom map shows cod distribution between 2008-2012. (All other four-year distribution maps for the interim here.)

Kevin Friedland, a scientist in NOAA's Northeast Fisheries Science Center Assessment Program (NEFSC), says the average sea surface temperature exceeded 51°F (10.5°C) during the first half of 2012. Whereas the average SST during this period over the past three decades has typically been below 48°F (9°C). Noteworthy from the Ecosystem Advisory:

  • SST data are based on satellite remote-sensing data and long-term shipboard measurements, plus historical SST conditions based on shipboard measurements dating back to 1854. 
  • Some nearshore locations like Delaware and Chesapeake Bays in the Middle Atlantic Bight region saw SSTs more than 11°F (6°C) above historical average at the surface and more than 9°F (5°C) above average at the bottom.
  • Deeper offshore waters to the north saw bottom water temperatures 2°F (1°C) warmer in the eastern Gulf of Maine and more than 3.6°F (2°C) warmer in the western Gulf of Maine.

 

DIstribution of silver hake, red hake and spotted hake 1968-2008: Janet Nye | NOAA | NEFSCDistribution of silver hake, red hake, and spotted hake 1968-2008: Janet Nye | NOAA | NEFSC NEFSC Ecosystem Assessment Program

Warming ocean temperatures have changed the distribution of other fish stocks besides cod, as reported by the NEFSC in a 2009 study published in Marine Ecology Progress Series. About half the 36 fish stocks studied in the Northwest Atlantic Ocean—many commercially valuable species—have been  shifting northward for the past four decades.

Some, like the three hake species shown in the maps above, have shifted themselves completely out of US waters.

Arctic 1, Shell Oil 0, for 2012 Season

| Mon Sep. 17, 2012 3:15 PM PDT

Noble Discoverer, Shell's Arctic drill rig: US Coast Guard via FlickrNoble Discoverer, Shell's Arctic drill rig: US Coast Guard via Flickr

Shell's comedy-of-errors season of not-drilling in the Arctic drew to a close today as the company announced it was wrapping up ahead of its 24 September deadline.

Shell was hoping that its $4.5 billion investment and multiple years of preparation would allow it to pierce the virgin seafloor of Alaska's Chukchi Sea and squeeze out some of the 22 percent of Earth's undiscovered fossil fuels believed to be underlying the Arctic and recoverable by current technology, according to the USGS.

Here's a list of some of what went awry with Shell's opening season:

  1. Their drill ship Noble Discoverer—seriously, that's its name—sailed late from New Zealand. Remember Xena the Princess Warrior, aka Lucy Lawless, occupied the ship briefly in protest in February?
  2. The late start ate into a season already shortened by the US Bureau of Ocean Management.
  3. En route to the Chukchi Sea, Noble Discoverer ignobly dragged anchor in the port of Dutch Harbor in the Aleutian Islands under only 35mph of wind... a morning breeze in the Arctic.
  4. Drilling was delayed again because Shell's primary safety vessel, the oil spill containment barge Arctic Challenger, wasn't still being built in the shipyards in Bellingham, WA.
  5. Shell failed to meet some limits on air pollution emissions for its operations set by the EPA.
  6. Test drilling (nowhere near a real oil field, because Arctic Challenger wasn't there) finally began on 9 September, nearly two months later than scheduled. "This is an exciting time for Alaska and for Shell," said Royal Dutch Shell on its website. "We look forward to continued drilling progress throughout the next several weeks and to adding another chapter to Alaska's esteemed oil and gas history."
  7. Noble Discoverer got in 300+ feet of a thin pilot hole—the first drilling offshore in the Alaska Arctic in two decades—before it was halted the next day when a massive iceberg 30 miles long by 12 miles wide came within 105 miles of the drill rig.
  8. Also, damagingly, documents obtained by PEER (Public Employees for Environmental Responsibility) under a Freedom of Information Act request showed that original field-testing of the "capping stack"—a containment dome designed to contain a Deepwater Horizon type blowout—deployed on Arctic Challenger took place over a mere two hours on 25 and 26 June and was not verified by anyone other than two officials from the Bureau of Safety and Environmental Enforcement. "The first test merely showed that Shell could dangle its cap in 200ft of water without dropping it," said Kathryn Douglass, a Peer staff lawyer, via The Guardian. "The second test showed the capping system could hold up under laboratory conditions for up to 15 minutes without crumbling.
  9. Finally that same "capping stack" was damaged during final testing off Bellingham, Washington, benching it for the remainder of the season... and ending Shell's miserable Noble Discoverer season.

Peter Slaiby, a VP of Shell Alaska, claimed: "The [Arctic] sea conditions in terms of the wind, waves and currents are not even as extreme as the North Sea, although, clearly, there is no ice in the North Sea." Sounds like the prelude to dangerous hubris.

Fisheries Declared Disasters on 4 Coasts

| Thu Sep. 13, 2012 2:37 PM PDT

jekrub via Flickrjekrub via FlickrToday the US Commerce Department declared disasters not of fishermen's making in three key fisheries on four US coasts: the North Atlantic, the Gulf of Mexico, the Bering Sea, and the Gulf of Alaska in the Pacific Ocean. The declaration opens the door for Congress—if they choose to accept the mission—to appropriate funds to help struggling fishers. The disasters are:

  1. The Northeast, where even though most fishers have adhered to tough quotas on several key groundfish—including cod in the Gulf of Maine and yellowtail flounder in the Georges Bank—stocks are not rebuilding.

  2. Alaska, where low returns of chinook salmon have resulted in commercial fishery disasters in the the Yukon River fishery (ongoing since 2010), the Kuskokwim River (ongoing since 2011), and Cook Inlet fishery (beginning in 2012).

  3. Mississippi, where historically high flooding of the lower Mississippi River in spring 2011 wiped out the oyster fishery and the blue crab fishery from massive freshwater flows. (This disaster might have included the inshore shrimp fishery too, since flooding drove landings down by 41 percent in 2011. But Commerce didn't deem it a commercial failure since revenue losses were "only 19 percent less than the 2006-2009 average.")

The causes run the gamut of natural and anthropogenic. In other words, something of everything, including plenty of unknowns. The disaster declaration for Alaska states:

Exact causes for recent poor Chinook salmon returns are unknown, but may involve a variety of factors outside the control of fishery managers to mitigate, including unfavorable ocean conditions, freshwater environmental factors, disease, or other factors.

The causes in New England are deemed unknown, and severe fishing quotas are pending for 2013, reports Boston.com:

The final numbers aren't in, but officials said preliminary information indicates that catch limits could go down by 72 percent for the cod population in the Gulf of Maine and 70 percent for cod on the Georges Bank fishing grounds east of Cape Cod.

The New England disaster declaration is "a huge win" for fishers, says Democratic Massachusetts Senator John Kerry, via the AP. "Our fishermen are the farmers of the sea and today our fishermen are facing exactly what farmers in the Midwest are facing—a drought. They need our help to get through it."

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