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.

Full Bio | Get my RSS |

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.

Yikes! Without Top Predators, CO2 Emissions Skyrocket

| Tue Feb. 19, 2013 1:43 PM PST
The three-spined stickleback is a regulator of carbon dioxide emissions in its ecosystem:

Top predators do more than regulate prey populations (think wolves and deer). They also regulate carbon dioxide emissions. At least they do in freshwater ecosystems—where if you take away the top predators CO2 emissions rise a staggering 93 percent. 

This according to a new paper in the latest Nature Geoscience that holds ramifications for a lot more than marshes. "Predators are disappearing from our ecosystems at alarming rates because of hunting and fishing pressure and because of human induced changes to their habitats," said lead author Trisha Atwood, at the University of British Columbia.

I wrote in an earlier post here on research showing how the loss of biodiversity (itself often a function of the loss of top predators) likely alters CO2 dynamics and other issues of global change as much as greenhouse gases.

The stonefly (Hesperoperla pacifica) whose presence helps keep CO2 emissions in check: Lynette S. / Lynette Schimming via Flickr

Food web theory posits that predators influence the exchange of CO2 between ecosystems and the atmosphere by altering processes like decomposition and primary production (a function of the numbers and diversity of plants).

To test that theory, the researchers experimented on three-tier food chains in experimental ponds, streams, and bromeliads in Canada and Costa Rica by removing or adding predators. Specifically by adding or removing three-spined stickleback fish (Gasterosteus aculeatus) and the invertebrate predators stoneflies (Hesperoperla pacifica) and damselflies (Mecistogaster modesta). When all the predators were removed the ecosystems emitted a whopping 93 percent more carbon dioxide to the atmosphere.

"We knew that predators shaped ecosystems by affecting the abundance of other plants and animals," says Atwood, "but now we know their impact extends all the way down to the biogeochemical     level."

From the paper:

We monitored carbon dioxide fluxes along with prey and primary producer biomass. We found substantially reduced carbon dioxide emissions in the presence of predators in all systems, despite differences in predator type, hydrology, climatic region, ecological zone and level of in situ primary production. We also observed lower amounts of prey biomass and higher amounts of algal and detrital biomass in the presence of predators. We conclude that predators have the potential to markedly influence carbon dioxide dynamics in freshwater systems.

The paper:

  • Trisha B. Atwood, Edd Hammill, Hamish S. Greig, Pavel Kratina, Jonathan B. Shurin, Diane S. Srivastava, John S. Richardson. Predator-induced reduction of freshwater carbon dioxide emissions. Nature Geoscience (2013). DOI:10.1038/ngeo1734

​​

Advertise on MotherJones.com

Polar Bears Need Love…and a Plan

| Mon Feb. 11, 2013 4:02 AM PST

United States Fish and Wildlife Service via Wikimedia Commons

A team of leading polar bear ecologists called for nations to make plans now for dealing with ongoing—and soon to be critical—threats to the survival of polar bears. The biggest problem for this iconic Arctic species is the mindblowingly fast disappearance of sea ice. Their paper appears in Conservation Letters.

For instance, last month (January 2013) the average coverage of sea ice in the Arctic Ocean was 409,000 square miles (1.06 million square kilometers) below the 1979 to 2000 January average. That's the sixth-lowest January extent in the satellite record, says the National Snow & Ice Data Center. Plus 2012 saw the lowest ever summer coverage of sea ice in the Arctic. 

The 19 polar bear populations identified by the IUCN: Andrew E. Derocher, et al, Conservation Letters (2013). DOI: 10.1111/conl.12009

It's not going to be easy to mitigate these challenges, the authors warn. There are 19 populations of polar bears worldwide. Some—like the Western Hudson Bay (WH, in the map above) bears and the Davis Strait (DS) bears—experience complete sea ice melt in summer that forces them onto land where they've got nothing to eat and can only burn through their own fat until the ocean refreezes.

For other populations—the Chukchi Sea (CS), Laptev Sea (LS), and Barents Sea (BS)—many bears remain on drifting pack ice and multiyear ice year round. The problem is that a lot of that pack ice is now retreating far beyond the continental shelf where ocean productivity is higher and polar bear prey more numerous. Meanwhile multiyear ice is disappearing rapidly throughout almost all the Arctic. 

Ansgar Walk via Wikimedia Commons

Here's what we know happens to bears forced ashore for too long in summer, or kept far offshore on multiyear ice:

  • declines in body condition
  • declines in body size
  • declines in reproductive rates
  • declines in survival rates
  • declines in population size
  • declines in sea ice denning habitat
  • altered movements and distribution

How bad will it get? In an earlier paper one author predicted the extinction of polar bears in two thirds of their range by 2050. That's because low ice years will increase as long as greenhouse-gas-induced warming continues—until almost all years will be bad for polar bears. For example:

  • Adult male mortality from starvation is predicted to increase to 28-48 percent in any year when the fasting period is 30 days longer than in recent years.
  • The possible effects on other age and sex classes have not been modeled but are predicted to be more severe.
  • Some years will continue to be better for polar bears and others poorer, even as the frequency of poor years increases until all are poor years.
  • The first occurrences of exceptionally poor years are likely to present a near-term critical challenge to polar bear conservation.

The authors write:

When superimposed over the long-term declining trend, annual variability in sea ice makes it increasingly likely that we will soon see a year where sea ice availability for some polar bear populations is below thresholds for vital-rates. Malnutrition at previously unobserved scales may result in catastrophic population declines and numerous management challenges.

If you have the stomach for it, there's a desperately tragic video of a polar bear mother and her two cubs dying of starvation here. Be forewarned: this is graphic and ghastly. But it's also a sign of what's happening now and what's to come for many many more bears in the future. Knowledge of these kinds of events was one of the reasons this paper was written, lead author, and author of Polar Bears: A Complete Guide to their Biology and Behavior, Andrew Derocher told me.

Orphaned polar bear cubs being sent to a zoo: NOAA via Wikimedia Commons

It's not just about bears either. Starving bears forced ashore are already a threat to local communities and that's only likely to get worse in the near future. The authors write:

The most intensive program for dealing with human-bear interactions, the Polar Bear Alert program in Churchill, Manitoba, Canada, includes extensive hazing, relocation, and temporary housing of bears to mitigate conflict during the ice-free period. That program is expensive and may not be easily applied in small northern communities with limited resources. Nonetheless, we encourage alternatives to killing problem bears, which is a common outcome in northern communities. The Churchill program was established before the effects of climate change were recognized and it is unclear whether it will remain adequate as warming continues. Bears temporarily held in captivity are not currently fed so the cost of temporary holding will increase when the ice-free period extends beyond the fasting capacity of captive bears. Less-expensive options such as reducing attractants and securing storage of food should be included along with plans for increased deterrent capabilities. Training and equipping community polar bear monitors, along with extensive public education and inter-jurisdictional agreements, should be planned to help assure human safety.

Projections of cumulative months per decade where optimal polar bear habitat will be either lost (red) or gained (blue) from 2001–2010 to 2041–2050. Insets show average annual cumulative area of optimal habitat (right y-axis, line plot) for four 10-year periods in the 21st century (x-axis midpoints), and their associated percent. Larger version hereUSGS

Derocher also pointed me towards this successful World Wildlife Fund Canada project to protect villagers from hungry, shore-bound bears in the Hamlet of Arviat, Nunavut.

Among the authors' other concerns:

  • Polar bears are still hunted throughout the Arctic except in Norway and Russia. "Existing harvest management methods are inadequate for declining populations that, by definition, have no sustainable harvest."
  • Feeding some bears might become necessary to keep people safe. "Diversionary feeding could be a viable short-term tool to draw bears away from settlements or industrial facilities." But possible negatives include: "the potential for disease and parasite transmission as well as human-wildlife conflicts may increase as other species such as Arctic fox, wolves, and grizzly bears are drawn into diversionary feeding locations​."
  • Feeding might also be needed to keep bears alive in areas where they might not otherwise survive. [How sad is that?]
  • Some bears might need to be sent to high-quality zoos for captive breeding.
  • Some bears might need to be euthanized if they've starved beyond rehabilitation.

The authors conclude:

Considering the global attention paid to polar bears, managers will be forced to respond to sudden changes in environmental conditions that negatively affect polar bears. We believe that managers and policy makers who have anticipated the effects, consulted with stakeholders, defined conservation objectives, created enabling legislation, and considered possible management actions will be most able to effectively respond to large-scale negative changes.

Andrew Derocher told me: "One thing we try to make clear is that we don't necessarily recommend any of these options but lay them out for consideration and discussion. Further, we don't view these desperate measures as a replacement for dealing with greenhouse gasses.  If we don't deal with climate change we won't have any polar bear habitat left."

The paper:

  • Andrew E. Derocher, Jon Aars, Steven C. Amstrup, Amy Cutting, Nick J. Lunn, Péter K. Molnár, Martyn E. Obbard, Ian Stirling, Gregory W. Thiemann, Dag Vongraven, Øystein Wiig, Geoffrey York. Rapid ecosystem change and polar bear conservation. Conservation Letters (2013). DOI:10.1111/conl.12009

The Ozone Hole: It's Still Up There, Changing Oceans, Maybe Climate

| Wed Feb. 6, 2013 4:21 AM PST

The ozone hole—the thinning of ozone in the lower stratosphere above Antarctica—has changed the way that waters in the Southern Ocean mix. And that has the potential to change how much CO2 the ocean sequesters from the atmosphere. Hence the course of global climate change. This according to a new paper in Science.

"This may sound entirely academic, but believe me, it's not," said lead author Darryn Waugh at Johns Hopkins' Krieger School of Arts and Sciences. "This matters because the southern oceans play an important role in the uptake of heat and carbon dioxide, so any changes in southern ocean circulation have the potential to change the global climate."

Map of local rates of sea level rise due to ocean heating below 4000m (colors and black numbers) for deep ocean basins. Also included is the rate from 1000-4000m warming (magenta) for the Southern Ocean (south of magenta line): via NOAA PMEL

The Southern Ocean has warmed at roughly twice the rate of the global mean ocean over the past few decades (even in its deep waters, map above), with some 40 percent of the anthropogenic carbon in the oceans entering south of 40°S. The authors write:

Southern ocean ventilation is driven primarily by the [prevailing] westerly winds, which have strengthened and shifted poleward over recent decades, primarily as a consequence of Antarctic stratospheric ozone depletion. Modeling studies suggest that this has caused changes in the ocean's overturning circulation and carbon uptake.

Thermohaline circulation (aka the "ocean conveyer") showing overturning circulation (aka deep water formation): Avsa via Wikimedia Commons

The overturning circulation, as I've written before (here and here and here), plays a big part in global climate. The places where the overturning circulation (also known as deep water formation) occur—just a few spots in the high latitudes—are being closely monitored for changes.

For the research reported in this paper, the authors used water samples collected in the Southern Ocean in the early 1990s and resampled again in the the middle and late 2000s. They measured chlorofluorocarbon-12, or CFC-12. That's the ozone-killing stuff that was first produced commercially in the 1930s for use in aerosols, refrigerants, and air conditioners, and which grew rapidly in the atmosphere until the 1990s when it was phased out by the Montreal Protocol. It's been useful to oceanographers ever since as a tracer for measuring water movements over time.

Comparing CFCs in the 1990s versus 2000s samples, the researchers were able to infer changes in how rapidly surface waters have mixed into the depths. They knew that concentrations of CFCs at the ocean surface increased in tandem with those in the atmosphere. So they were able to surmise that the higher the concentration of CFC-12 deeper in the ocean, the more recently those waters were at the surface.

What they found was younger than expected waters in the subtropics and older than expected waters further south. These findings correlate to observed intensification of surface westerly winds driven primarily by the Antarctic ozone hole. Which suggests that dwindling  ozone in the stratosphere is the primary cause of the observed changes in ocean circulation.

As stratospheric ozone recovers, the circulation may recover too. But there are other factors at work here. The authors conclude: 

As stratospheric ozone recovers over the next 40 to 60 years, the recent trend of intensifying summer westerly winds may slow or reverse. However, continued increases in greenhouse gases will likely lead to strengthened westerlies during other seasons. The integrated impact of these trends in Southern Hemisphere westerlies on the ocean's ventilation and uptake of heat and anthropogenic carbon is an open question.

 

We don't hear so much about the ozone hole as we did in the 1990s. But that doesn't mean it's going away anytime soon. The video (above) by the American Museum of Natural History animates projections for a slow recovery.

The ozone layer if CFCs hadn't been banned, progression by decade. Dark blue indicates zero ozone: Goddard Space Flight Center Visualization Studio

And this series of images (above) show projections of what might have become of global stratospheric ozone if we hadn't curbed our emissions through the Montreal Protocol. Dark blue indicates zero ozone.

The paper:

  • Darryn W. Waugh, Francois Primeau, Tim DeVries, Mark Holzer. Recent Changes in the Ventilation of the Southern Oceans. Science (2013). DOI:10.1126/science.1225411

 

Butterflies Booking It North as Climate Warms

| Thu Jan. 31, 2013 4:21 AM PST
Giant swallowtail, normally a butterfly of the southern US, now increasingly appearing in the northeast: Thomas Bresson via Wikimedia Commons
 

Butterflies from the southern US that used to be rare in the northeast are now appearing there on a regular basis. The trend correlates to a warming climate report the authors of a paper in Nature Climate Change.

Subtropical and warm-climate butterflies—including the giant swallowtail (photo above) and the zabulon skipper (photo below)—showed the sharpest population shift to the north. As recently as the late 1980s these species were rare or absent in Massachusetts.

At the same time southern butterflies are moving north, more than 75 percent of northern species—with a range centered north of Boston—are rapidly declining in Massachusetts now. Disappearing fastest are the species that overwinter as eggs or larvae. Which suggests that changes in the winter climate (like more drought or less snow cover) may be harming nonadult butterflies.

Southern species like the zabulon skipper are replacing northern species in Massachusetts: Kenneth Dwain Harrelson via Wikimedia Commons

"For most butterfly species, climate change seems to be a stronger change-agent than habitat loss," lead author Greg Breed tells the Harvard Gazette. "Protecting habitat remains a key management strategy, and that may help some butterfly species. However for many others habitat protection will not mitigate the impacts of warming."

Breed points to the frosted elfin (photo above), a species that receives formal habitat protection from Massachusetts, and has increased 1,000 percent there since 1992. Meanwhile common summer butterflies that have no protection in Massachusetts (atlantis and aphrodite fritillaries) have declined by nearly 90 percent. From the paper:

Conservation agencies should not use our results to infer that all southern species are safe nor that all northern species are doomed to extinction. However, understanding mechanisms of population decline could improve management practices and limit potentially costly efforts that will have little influence on species conservation.

 

The frosted elfin is one of the most rapidly increasing butterfly species in Massachusetts with an estimated 1,000 percent increase since 1992: Geoff Gallice via Wikimedia Commons

What's extra cool about this research is that the data come from citizen scientists at the Massachusetts Butterfly Club. Over the last 19 years members have logged butterfly species and numbers on some 20,000 expeditions through Massachusetts. Their records fill a crucial gap in the scientific record.

Butterflies are turning out to be the canaries in the coal mine of climate warming:

  • This study in Biology Letters found that Australia's common brown butterfly emerged from their pupae on average 1.6 days earlier each decade between 1941 and 2005, when average air temperature increased by 0.14°C per decade.
  • Butterflies and other species living in the mountains suffer from the "escalator effect"... i.e., when there's no higher "latitude" for them to shift to beyond the summit.
  • MoJo's Kiera Butler wrote here about the Karner blue butterfly and the problem of what to do when conditions force them northward but they can't make it past urban roadblocks.
  • I reported here about populations of Apollo butterflies in the Rocky Mountains so fragmented by the escalator effect that they could be wiped out by one particularly bad weather event.
  • Check out this Google Scholar search page for just how many papers are being published on butterflies feeling the heat.

The Nature Climate Change paper:

  • Greg A. Breed, Sharon Stichter & Elizabeth E. Crone. Climate-driven changes in northeastern US butterfly communities. Nature Climate Change (2013). DOI:10.1038/nclimate1663

With Warming, Soil Releases More CO2... Though Less Over Time as Microbes Adapt

| Sun Jan. 20, 2013 11:06 AM PST
Study plots at the Harvard Forest Long-Term Ecological Research site in Massachusetts where researchers have been warming two areas with underground cables to simulate a warmer climate. The photo shows a January thaw on a 50°F day. The heated plots melted before the unheated ones: Alix Contosa, postdoctoral researcher at University of New Hampshire

Warmer temperatures from a warming climate force the release of carbon dioxide from soils into the atmosphere, driving even more climate warming. That's the bad news. The good news is that the effect diminishes over time—over 18 years, and counting. This according to a new paper just published in Nature Climate Change.

We know that microorganisms in the soil release 10 times the CO2 that humans release on a yearly basis. These soil processes are normally kept in check by plants, which uptake C02 from the atmosphere. But a warming climate is driving changes in the carbon cycle.  

Model soil bacteria: pmecologic via Flickr

To examine how that might be unfolding on at least one patch of our planet—the Harvard Forest Long-Term Ecological Research site in Massachusetts—the researchers warmed two plots with underground cables, one plot for two years, the other for 18. They then measured the efficiency of soil organisms in utilizing food sources that come from plants. Here's some of what they found:

"When the soil was heated to simulate climate warming, we saw a change in the [soil] community to be more efficient in the longer term," says Frey.
  • In the two-year scenario, warming temperatures drastically reduced the efficiency of soils to utilize complex food sources (specifically phenol) from decomposing wood and leaves by 60 percent.
  • In the long-term scenario, where soils were warmed to 9°F (5°C) above ambient temperatures for 18 years, the soil microorganisms regained some efficiency—suggesting that warmed soils might eventually release less CO2 than otherwise predicted.

Why the change? The authors hypothesize that long-term warming may change the community of soil microorganisms to become more efficient. Perhaps the composition of the species changes, or the original species adapt, or the availability of various nutrients changes, or some or all of the above.

"While they're low on the charisma scale soil," says lead author Serita Frey, at the University of New Hampshire, "[soil] microorganisms are so critically important to the carbon balance of the atmosphere."

(Thanks microorganisms!)

These findings could lead to critical changes in the way the carbon cycle is predicted, since common ecosystem models don't factor in the temperature response of the microbial community. "There is clearly a need for new models that incorporate an efficiency parameter that is allowed to fluctuate in response to temperature and other environmental variables," says co-author Johan Six, at the University of California, Davis.

In the video, author Serita Frey describes her long-term work with soil.

The paper:

  • Serita D. Frey, Juhwan Lee, Jerry M. Melillo, and Johan Six. The temperature response of soil microbial efficiency and its feedback to climate. Nature Climate Change. DOI: 10.1038/NCLIMATE1796
Mon Mar. 26, 2012 12:51 PM PDT
Fri Mar. 23, 2012 12:12 PM PDT
Wed Mar. 21, 2012 11:03 AM PDT
Tue Mar. 20, 2012 11:34 AM PDT
Mon Mar. 19, 2012 11:18 AM PDT
Wed Mar. 14, 2012 11:29 AM PDT
Tue Mar. 13, 2012 10:44 AM PDT
Fri Mar. 9, 2012 2:35 PM PST
Thu Mar. 8, 2012 1:20 PM PST
Tue Mar. 6, 2012 3:29 PM PST
Mon Mar. 5, 2012 2:52 PM PST
Fri Mar. 2, 2012 1:20 PM PST
Tue Feb. 28, 2012 3:46 PM PST
Fri Feb. 24, 2012 1:06 PM PST
Thu Feb. 23, 2012 1:17 PM PST
Wed Feb. 22, 2012 3:37 PM PST
Fri Feb. 17, 2012 1:07 PM PST
Wed Feb. 15, 2012 2:52 PM PST
Mon Feb. 13, 2012 1:00 PM PST
Fri Feb. 10, 2012 1:41 PM PST
Thu Feb. 9, 2012 11:36 AM PST
Mon Feb. 6, 2012 1:29 PM PST
Mon Jan. 30, 2012 1:58 PM PST
Fri Jan. 27, 2012 3:07 PM PST
Thu Jan. 26, 2012 3:53 PM PST
Tue Jan. 24, 2012 2:20 PM PST
Fri Jan. 20, 2012 11:50 AM PST
Wed Jan. 18, 2012 1:26 PM PST
Tue Jan. 17, 2012 1:48 PM PST
Fri Jan. 13, 2012 1:48 PM PST
Thu Jan. 12, 2012 3:23 PM PST
Tue Jan. 10, 2012 1:31 PM PST
Mon Jan. 9, 2012 1:19 PM PST
Fri Jan. 6, 2012 4:04 AM PST
Thu Jan. 5, 2012 12:13 PM PST
Tue Jan. 3, 2012 1:49 PM PST
Wed Dec. 28, 2011 1:59 PM PST
Thu Dec. 22, 2011 12:20 PM PST
Tue Dec. 20, 2011 2:20 PM PST
Mon Dec. 19, 2011 3:23 PM PST
Fri Dec. 16, 2011 11:09 AM PST
Wed Dec. 14, 2011 5:03 PM PST
Wed Dec. 14, 2011 1:26 PM PST
Fri Dec. 9, 2011 1:52 PM PST
Fri Dec. 9, 2011 12:54 PM PST
Thu Dec. 8, 2011 2:35 PM PST