The Road to Copenhagen Part 1: Implementing the global framework

greenhouse gases
I have just returned from meetings in Washington DC and Geneva, Switzerland. The IPCC process itself is quite fascinating – with the process of drawing together the collective wisdom into a single consensus seemingly daunting yet achievable through the process. More shortly, but in the meanwhile, Stephen Leahy (an environmental journalist who was also in Geneva) has provided a great writeup on the proposed “Global Framework for Climate Services”:

Imagine being able to know months in advance when and where floods or droughts may occur. That is what over 150 countries participating in the third World Climate Conference, which concluded last Friday in Geneva, pledged to achieve through the creation of a Global Framework for Climate Services.

“Today is a landmark day for making climate services available to all people,” said Michel Jarraud, secretary-general of the World Meteorological Organisation (WMO), convener of the conference, told over 2,000 climate scientists, sectoral experts and decision-makers.

“Climate services” is the long-distance cousin to weather services or weather forecasting. New technology and better climate science has opened the window to very long range forecasting of climate events like droughts weeks and months in advance.

This year, scientists were able to anticipate unprecedented flooding of the Red River Valley in the United States Midwest months in advance, enabling local communities to prepare and avoid the worst consequences, said Jane Lubchenko, a noted ecologist, administrator of the National Oceanographic and Atmospheric Administration (NOAA) and head of the U.S. delegation.  (Read More)

Australia comes last in climate effectiveness

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According to a new report commisioned by the Climate Institute, only two of the G20 countries are currently improving carbon productivity quickly enough to meet carbon reduction targets. What’s more surprising is that Australia ranks 15th in improving carbon productivity, lagged only by South Africa, India, Saudia Arabia and Indonesia. Although a part of this is due to ‘green-house intensive’ exports, the report also blames the use of cars and reliance on coal-based electricity:

(The report)… illustrates that there are a number of countries, including Turkey, Russia, Saudi Arabia, Australia and Canada, that are currently falling well short of the required improvement in carbon productivity and that require significant turnarounds in their performance. The longer these countries take to achieve these turnarounds, the more costly (economically, as well as socially and politically) the eventual transition will be.

(Click here for pdf of full report, or here for The Age newspaper report)

From coal to Copenhagen

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With Australia being a huge exporter of coal, the government seems set on the adoption and use of clean-coal technology. But, is time running out for coal?

“I grew up to a Rolling Stones song that said, “Time is on my side. Yes it is.” For our coal industry, sadly, it is not. In fact, if the US experience is anything to go by, time is fast running out. Projects to build new coal-fired power stations are being abandoned from Florida to Utah. Money is pouring in for renewable energy and legislation is being enacted to support it.

The only long-term hope for coal in the US is clean coal. The same is true for Australia. Australia needs to take a long-term, 20-year view on energy and not just look at the increased demand projections for coal for the next five or 10 years. We need to look at what the energy mix will be in 2030.

The clear and present danger for Australia’s coal industry is, unless there is a powerful push to see clean-coal technology developed and implemented, the traditional markets for its product will start slowly shutting down as green energy becomes more price-competitive and public policy continues to demand greener outcomes”
(“Coal on the outer as US goes green” – The Australian, September 5th 2009)

“There’s an irony in the rushed construction of a new security fence around the Hazelwood power station, in anticipation of a community protest this weekend. The Government, it seems, is more in interested in protecting Hazelwood from protesters, than protecting our climate from Hazelwood.

Victoria has been shamed as the least climate-friendly state, running three of Australia’s four dirtiest power stations. And Hazelwood is one of the dirtiest in the developed world, scheduled to close this year but in 2005 given a lifeline by the State Government to 2031. The timing is significant, because it reflects the climate policy strategy of the major parties: hang on with dirty coal till 2030-35, and hope that by then carbon capture and storage (CCS) technology will work. For now, pour money into CCS research, but stall on serious emission-reduction strategies”
(“Punting on coal is a loser, but try telling the Government” – The Age, September 10th 2009)

Northeast passage opens as the Arctic melts

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There is an interesting, if scary, article in the NYT today about the thawing of Arctic ice sheets which are making it feasible for cargo ships to use the Northeast passage from Europe, over the top of Russia, and into the western Pacific ocean.

By ANDREW E. KRAMER and ANDREW C. REVKIN

MOSCOW — For hundreds of years, mariners have dreamed of an Arctic shortcut that would allow them to speed trade between Asia and the West. Two German ships are poised to complete that transit for the first time, aided by the retreat of Arctic ice that scientists have linked to global warming. The ships started their voyage in South Korea in late July and will begin the last leg of the trip this week, leaving a Siberian port for Rotterdam in the Netherlands carrying 3,500 tons of construction materials.

Russian ships have long moved goods along the country’s sprawling Arctic coastline. And two tankers, one Finnish and the other Latvian, hauled fuel between Russian ports using the route, which is variously called the Northern Sea Route or the Northeast Passage.

But the Russians hope that the transit of the German ships will inaugurate the passage as a reliable shipping route, and that the combination of the melting ice and the economic benefits of the shortcut — it is thousands of miles shorter than various southerly routes — will eventually make the Arctic passage a summer competitor with the Suez Canal.

“It is global warming that enables us to think about using that route,” Verena Beckhusen, a spokeswoman for the shipping company, the Beluga Group of Bremen, Germany, said in a telephone interview.

Read the full story here and related articles about Arctic melting here

Annual trends in reporting of climate change in the media and scientific literature

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Here’s an interesting graph taken from a recent publication by Russill & Nyssa in the journal Global Environmental Change (“The tipping point trend in climate change communication”, 19:336-344). The entire article is a fascinating read, but if the methods are to be believed, the data implies a HUGE increase in the reporting of the phrase “Climate Change” by the Australian media in the last five years – more than the US and UK media combined at last count (2007). The solid line (ISI Web of Science) represents the use of the phrase “Climate Change” in the scientific literature. Methodological bias or a genuine representation of the climate change ‘feeding-frenzy’ by the Australian press in recent years? Food for thought.

Humpty dumpty and the ghosts

There is a nice, new essay on the NYT.com by Olivia Judson about the complexity of ecological communities.  And about how ecologists strive to understand the impacts of loosing key species from complex ecosystems.  She also discusses the challenges of understanding or untangling how complex systems like coral reefs operate.

I couldn’t help chuckling at myself the other morning as I typed “Humpty Dumpty” into the search box of one of the big science databases. Humpty Dumpty, as anyone who remembers their nursery rhymes will recall, is an egg-shaped fellow who takes a bad fall. At which point, “All the King’s horses / and all the King’s men / Couldn’t put Humpty together again”.

But, as I discovered during my researches, Humpty Dumpty is an important personage. He has, for example, had a gene named after him. In fruit flies, mutations to the Humpty Dumpty gene produce a number of unfortunate effects, including thin egg shells. He has also lent his name to a scale that measures the severity of falls.

But neither of those is what I was looking for. I was looking for papers on the Humpty Dumpty community.

To see what this means, imagine a small pond. Let’s say that it’s home to a flourishing community of species — insects, fishes, algae, weeds, and so on. Now, suppose one of the species disappears — let’s say that humans fish out all members of one of the fish species. You want to undo this little extinction.

The obvious thing to do is to add fish of the missing species back into the pond. Which might work. But it might not. It might be that some other animal has occupied the fish’s niche, preventing the fish from moving in again.

Or it might be that the fish can only become established in the presence of, say, a certain species of insect — but that insect has long-since vanished. If this were the case, you’d have a Humpty Dumpty community: if it disintegrates, you cannot rebuild it from its parts. In other words, the ability to reconstitute the community depends on species that are no longer there.

How common is this phenomenon? It’s not clear. Humpty Dumpty effects often occur in mathematical models of ecosystems. But whether Humpty is important in nature is an open question.

Which isn’t surprising. Ecology is one of the hardest branches of biology, possibly of all science. Real ecological communities are fantastically complex — think of a rainforest, or a coral reef — and hard to dissect and understand. Experiments in the wild are difficult to control, and important variables are often hard to measure. Imagine trying to measure the impact that, say, earthworms have on oak trees: it’s damnably difficult.

Experiments in the laboratory are problematic too. Microcosm experiments — where you set up miniature worlds inhabited by just a few species of single-celled beings — quickly become massive. For instance, suppose you’re interested in the question of whether individuals of different species can live together. (This is an important question, for it bears on how ecosystems form.) To keep things simple, you decide to investigate a mere six species. You want to be thorough, so you’re going to consider all combinations, from each species living alone, to all six together.

But that’s already 63 combinations. Worse, in order to be more confident about the results, you can’t just do each one once, you need to replicate them. So you set up each combination six times. That’s 378 microcosms. Worse still, ecosystems — even small and simple ones — don’t stabilize in an afternoon. You have to wait for several months before you can be sure the system has settled into a “final” form. See what I mean? (Incidentally, I didn’t invent this experiment: it has actually been done. Those 60-plus combinations produced only eight different communities that were stable and persistent. Most of these were simple, containing only one or two species.)

Of course, Out There in Nature, there’s no such thing as a “final” form. New immigrants regularly arrive, whether we’re talking about a mangrove swamp in Florida, or the most remote islands in the Pacific. Sometimes these new arrivals fail to thrive. Sometimes they become established, perhaps driving other species extinct as they do so.

Or perhaps they have a more subtle effect: they fail to thrive and yet they drive other species extinct. Such species have been called “ghosts,”, the idea being that they have a definite, but unseen, impact on the stability of the community.

Again, ghosts have been detected in mathematical models more often than they’ve been sighted in nature. In fact, it’s not clear that they exist. The best evidence that they might be important comes from those microcosms I was mentioning. Earlier, I described only the first half of the experiment. The second half took the persistent, “final” form communities and subjected them to various invasions. In several cases, the invaders could not become established, yet the composition of the community shifted, with one of the original species going extinct.

Humpty Dumpty and the ghosts — the names are light-hearted, the theory is esoteric, but the problems they touch on are urgent. How do ecosystems form? How much impact do invaders have? What are our chances of restoring damage done by fishing or farming? We are pushing our ecosystems to the brink. If we don’t understand how they work, we can’t hope to limit the damage. And we need to try: after all, this is our home.

Link

PS-for you climate shifts junkies following the horse race, I just tied Jez in our race to 100 posts and the grand prize sponsored by OHG.

PSS-for UQ people, I am in Chapel Hill in a seminar sitting next to Ann Mooney!

Feeling the heat in Hawaii – climate change and the pacific decadal oscillation

A new paper published in Geophysical Research Letters sheds some interesting light on the impacts of climate change and regional shifts in temperature. Whilst it’s generally accepted that the instrumental temperature record shows an upward trend (see here for a graph), the regional patterns of climate change are less well known. Through analysis of an 85 year dataset of 21 base stations across the Hawaiian Islands, Giambelluca and his team from the University of Hawai’i show a dramatic increase in temperature trends over the past 30 years, with a stronger trend in the high altitude regions. According to their data, most of this warming is attributed to increases in minimum temperatures rather than the maxima, resulting in a decrease in the diurnal range of temperatures:

Hawaii_-Temperature-gradient

At a glance, it’s easy to ‘eyeball’ this graph and consider it a skeptical field day. After all, according to the data the temperature was warmer in the 1940’s than throughout the last two decades, right? Even more alarming: for the majority of the dataset, the temperature cycles have followed the pacific decadal oscillation (PDO, a natural pattern of climate variability in the pacific on a 20-30 year cycle). The long-term trends of the PDO look like follow a trend as follows:

800px-Reconstructed_PDO_since_1660

The recent Hawaii data set suggests that although the PDO is currently in a ‘cool’ phase, climate change has effectively ‘derailed’ the PDO cycle, as evident in the increase in linear trends of temperatures from 1975 onwards. Such changes on a regional scale are a huge cause for concern, particularly in the high altitude areas of Hawaii such as Mauna Kea (the worlds tallest mountain when measured from the base of the Pacific Ocean), which has a high rate of endangered endemic flora and fauna.

Japan aims for 25% reduction in CO2 emissions by 2020

Japan vows big climate change cut” (BBC News, 7th September 2009)

Japan’s next leader has promised a big cut in greenhouse gas emissions, saying he will aim for a 25% reduction by 2020 compared with 1990 levels.

Democratic Party leader Yukio Hatoyama is due to take over as prime minister on 16 September, after a resounding election victory in August.

His predecessor, Taro Aso, had pledged cuts of only 8%.

Mr Hatoyama said the plan was dependent on other nations agreeing targets at December’s climate talks in Copenhagen. (Read More)

Armed forces may be the agents of climate change” (The Age, 5th September 2009)

THE oceans are getting warmer, coral reefs are increasingly under threat, Arctic ice is dropping into the sea. July was the warmest month in 130 years of testing ocean temperatures. Who are we going to call?

The admirals and the generals. It appears that the US military is as concerned about the fate of the Earth as the man and woman on Civvy Street. And, as history has shown, what troubles the US generals troubles the rest of the world. (Read More)

One minute to midnight for Maldives’ corals” (Minivan News, 6th September 2009)

If the experts are right, however, the Maldives’ coral reefs are in terminal decline. A UN report entitled The Economics of Ecosystems and Biodiversity released last week in Berlin, stated the world’s coral infrastructure and accompanying biodiversity would be the first ecosystem to go due to climbing greenhouse gases.

The message is critical; the reality is grim. “Corals are the foundation of the whole ecosystem, the building blocks of the reef itself,” said Guy Stevens, a British marine biologist at Four Seasons resort. “If the reef went, the Maldives would cease to exist, the islands themselves would be eroded and washed away. Without them, there’s nothing.” (Read More)

Global warming warps marine food webs

Dina Leech and Virginia Schutte collect zooplankton from Bogue Sound using a plankton tow net. Plankton from the net were rinsed into a sieve and then added to the experimental microcosms. Photo: M. O'Connor

Dina Leech and Virginia Schutte collect zooplankton from Bogue Sound using a plankton tow net. Plankton from the net were rinsed into a sieve and then added to the experimental microcosms. Photo: M. O'Connor

Humans rely on marine ecosystems for economic and nutritional sustenance—including about 16% of animal protein consumed by humans—making it especially important for natural scientists, economists, conservationists and long-term policy planners to understand how climate change is likely to affect oceanic food webs. Yet the general effects of warming on food web productivity are completely unknown. The productivity of consumers (such as zooplankton), in food webs is determined in large part by their metabolic rates and the availability and productivity of their limiting metabolic resources. A general theory relating food web dynamics to temperature suggests that fundamental differences between consumers and primary producers (such as phytoplankton) may lead to predictable shifts in their relative abundance and productivity with warming. A team of UNC scientists led by my former PhD student Mary O’Connor experimentally tested the effects of warming on food web structure and productivity under two resource supply scenarios. Our results show that warming alone can strengthen the role of consumers in the food web, increasing consumer biomass relative to producer biomass, and reducing the total biomass of the food web despite increases in primary productivity. In contrast, when resources were less available, food web production was constrained at all temperatures. These results demonstrate that small changes in water temperature could drive dramatic shifts in marine food web structure and productivity, and potentially provide a general, species-independent mechanism of ecological response to climate change.

Mary O’Connor checks temperatures in the food web experiment. Eight water tables each contain five microcosms, which are shielded from UV and full sunlight by plexiglass and window screen. The water bath maintains the temperature, and air tubes going into each microcosm deliver oxygen. Photo: A. Anton

Mary O’Connor checks temperatures in the food web experiment. Eight water tables each contain five microcosms, which are shielded from UV and full sunlight by plexiglass and window screen. The water bath maintains the temperature, and air tubes going into each microcosm deliver oxygen. Photo: A. Anton

From an article about the paper in Science Now:

By Erik Stokstad, 26 August 2009

Teasing apart the complex ways in which global warming will affect ocean life has been tough. But new research suggests that a simple ecological theory may explain at least one piece of the puzzle: the effect on marine food webs. And the news may not be all bad.

New experiments confirm that phytoplankton, which form a bottom rung of oceanic food chains, will become less productive in warmer, nutrient-rich water. However, the results also show that zooplankton should boom in these warmer areas, which could benefit certain fisheries.

The food-web theory hinges on the assumption that temperature affects the metabolism of organisms that rely on other creatures for food, like zooplankton, while not having much of an impact on photosynthetic organisms like phytoplankton. That suggests that in warmer waters, zooplankton should generally grow faster and start reproducing sooner than they do in cooler waters. As zooplankton become more abundant and eat more phytoplankton, the population of phytoplankton should shrink.

Mary O’Connor, now a postdoc at the National Center for Ecological Analysis and Synthesis in Santa Barbara, California, and her colleagues set up an experiment to test the theory. They put zooplankton and phytoplankton into 4-liter tubs and let them sit for 8 days. Some were kept at the ambient temperature; others were heated by 2°, 4°, or 6°C. Recognizing that nutrient levels vary in the ocean, they added extra nitrogen and phosphorous to half the tubs in each group.

As temperatures rose, the productivity of the communities without extra nutrients hardly changed. Nor did the food web. This suggests to O’Connor and her colleagues that nutrient-poor food webs may be relatively resilient to global warming. The tubs that got additional nutrients were another story: The zooplankton in warmer water became more abundant while the numbers of phytoplankton fell. In fact, the ratio of zooplankton to phytoplankton rose 10-fold, the team reports in a paper posted online on 25 August in PloS Biology. “It matched our predictions really well,” O’Connor says. She adds that even though overall biological productivity declined as temperature rose, the increase in zooplankton could benefit fish that eat them in nutrient-rich waters.

TFW5 plankton color

Concentrated phytoplankton at the end of the experiment. Phytoplankton from 50 mls (1/60) of each microcosm are filtered onto a white filter before the concentration of chlorophyll is measured. Higher density of phytoplankton results in deeper green color.

There is a great synopsis of the article in PLoS which starts out with a pretty politically charged perspective:

While politicians like United States Representative Michele Bachmann (RMinn.) rail against efforts to curb human contributions to global warming—she thinks carbon dioxide, a ‘‘natural byproduct of nature,’’ could not possibly be harmful—scientists are documenting the damage. Numerous studies describe how climate change is threatening the persistence of a broad range of plant and animal species across diverse taxa, geographic regions, and trophic levels, from the polar bear at the top of the food chain to the shrimp-like krill at the bottom. As they catalog the ecological casualties.

Mary also published the study-related haiku in the New Yorker, which originally appeared at the website Dissertation Haiku.


Hungry herbivores,

It’s warm; feel your tummies growl?

Graze down hot seaweed.

See the related story in Scientific American here

Reference

O’Connor MI, Piehler MF, Leech DM, Anton A, Bruno JF (2009) Warming and Resource Availability Shift Food Web Structure and Metabolism. PLoS Biol 7(8): e1000178. doi:10.1371/journal.pbio.1000178

Download the PDF: http://biology.plosjournals.org/perlserv/?request=get-document&doi=10.1371/journal.pbio.1000178

Download the PLoS Synopsis: http://www.plos.org/press/plbi-07-08-OConnorSynopsis.pdf


Where would you want to live under sea level rise? Interactive floods maps

Ever wondered where the wise investment in the property market is going to be under the IPCC projected scenarios? Check out the Sea Level Rise Explorer over at Global Warming Art:

During the twentieth century, sea level rose 20 cm. It is predicted that sea level rise will accelerate during the twenty-first century, but many model predictions still foresee a sea level rise of less than 1 additional meter by 2100.

Regardless of the time scale involved, an analogy to the previous interglacial suggests that a few degrees Celsius of sustained warming can cause enough melting to raise sea level 4-6 m before the ice sheets reach equilibrium. This level of warming is likely to be achieved or even exceeded by 2100 in the absence of intervention to combat climate change, though as above, it would take far longer to realize the full sea level change.