Adaptation

Living with the impacts of climate change.

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Evolving to face climate change

greenkayak73 / flickr

Could this salt marsh be a hotbed of rapid evolution? Saltmarsh killifish and oysters have both demonstrated the ability to rapidly adapt to intense environmental stress.

In the context of climate change, the word ‘adaptation’ often refers to feats of engineering, like beach nourishment or infrastructure improvements. But natural systems must rely on the usually slow and undirected process of evolution – adaptation by natural selection, to be precise. Given the unprecedented and accelerating pace of changes currently gripping the planet – from rising air and water temperatures, to ocean acidification and increasingly extreme weather – many scientists question whether plants and animals can evolve fast enough to survive.

Enter high-speed evolution. Yep. You read that right. High-speed evolution. This from Tara Thean on TIME’s Ecocentric blog:

According to a team of researchers at McGill University in Montreal, adaptation to climate change can happen on the fly, with some organisms able to make key evolutionary changes over the course of surprisingly few generations, keeping themselves and their gene-line thriving in a world that seems to be coming to pieces.

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EPA recommends retreat from rising seas

flickr/hollyladd

Moving homes impacted by erosion - like this one on Smith's Point, Nantucket Island - could be part of a strategy of retreat from rising sea level.

From the Cape Cod Canal and New Bedford’s hurricane barrier, to the levees of the Mississippi River, the Army Corps of Engineers has shaped the very landscape of the United States. But many of the Corps’ greatest feats of engineering are coming to be seen as naive, foolhardy, even misinformed attempts to master nature. When it comes to rising sea level, Darryl Fears (Washington Post) reports that the Army Corps’ way may be the way of the past.

… in the past, municipalities turned to a manual published by the Army Corps of Engineers since 1954 on how to protect shores by holding back the sea.

But earlier this month, the U.S. Environmental Protection Agency published the first manual on how not to hold it back, arguing that costly seawalls and dikes eventually fail because sea-level rise is unstoppable.

So what does the EPA suggest instead?

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Q & A: Can catch shares help fisheries face climate change?

For 35 years, federal fishery regulators have worked to end overfishing in American waters. Federal officials say we’re poised to declare that milestone and enter a new era of recovery and sustainable fishing. But just as the threat of overfishing may be fading, the impacts of climate change are starting to make themselves felt. I recently spoke with Dr. Michael Fogarty, a senior scientist at the Northeast Fisheries Science Center here in Woods Hole, about the expected impacts of climate change on New England’s fisheries and what we can do to prepare.

Dr. Michael Fogarty

So, have we ended overfishing in American waters?
There have been a very dramatic increases in our ability to control fishing and increases in the status of the stocks in a number of places throughout the country. There still are some problem species that we need to continue to work with, but overall the report card is very good for the nationwide goal of ending overfishing.

What about the rest of the world?
There have been a number of recent studies of the progress towards ending overfishing a global basis. Of course, the most detailed information is for the developed world, rather than the developing world where it’s much more difficult to make a clear assessment. But it’s fair to say that the tide has turned in many of the areas in the developed world in terms of sharply reducing overfishing. Just as in the United States, there are still areas of concern and species of concern. But there are hopeful signs on the horizon. The important thing is that we’ve shown that we can do this if we have both the political will and the management tools in place to do it. And so, if we continue on the path that we’re currently on in many parts of the world, the expectation is that overfishing would become much less of a problem.

You and I spoke a few years ago and you predicted that within a matter of 5 to 10 years, overfishing would fade as the biggest threat to ocean ecosystems and climate change would take it’s place. Are we at that point right now?
As fishing becomes less of an overall impact, other aspects of the natural environment will become increasingly important in controlling the changes that we do see in fish stocks. And there are changes underway in terms of the effects of climate change on fish populations in this area. In particular, some species at the southern extent of their ranges will face increasing difficulties.
One of the major impacts is on some species’ patterns of recruitment, or the influx of young animals into the populations. For species recovering from overfishing, the rate of increase in the populations could be slowed or in some cases perhaps halted by other changes in the environment. In other cases, we’re looking at shifts in the distribution patterns where fish may be less available to our fishing fleets.

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Is New Bedford’s hurricane barrier the future of Cape Cod?

southcoasttoday.com

The hurricane barrier that protects New Bedford Harbor has been cleared for federal recertification.

Earlier this week, the New Bedford Standard Times reported that the hurricane barrier that spans the mouth of New Bedford Harbor has passed a federal inspection and is ready for re-certification. Why is that news?

A few fun facts:
  • The wall connects the cities of New Bedford and Fairhaven.
  • At 3.5 miles in length, it is the largest stone structure on the East Coast and the largest hurricane barrier in the world.
  • There is one navigational gate that spans a 150-foot-wide gap. The gate doors weigh 400 tons each and take about 12 minutes to close.
  • The barrier was constructed by the Army Corps of Engineers in 1966 to prevent a repeat of the damage from big hurricanes in 1938, 1944 and 1954.
  • It took four years to build and cost $18 million dollars. The rocks cost the government 5 cents per pound.
  • Maintenance of the barrier costs the city of New Bedford about $50,000 to $60,000
  • It’s not a solid rock wall: there’s a tunnel inside. Take a look:

The barrier protects about 1,400 acres of heavily developed industrial and commercial property – the Whaling City’s working waterfront – and the fishing fleet that consistently makes New Bedford the highest grossing fishing port in the country.

NOAA forecasters are calling for an active hurricane season, so the fact that the barrier is up to snuff is certainly good news. But the re-certification also means that the wall can be included in the Federal Emergency Management Agency’s revisions of flood maps; even as sea level rises, the flood vulnerability of the protected area behind it will remain unchanged.

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The difference between dunes, escarpments, and piles of sand

Heather Goldstone

The real dunes at Menauhant Beach have retreated back and now engulf the Old Menauhant Bridge.

When I wrote about Falmouth’s Menauhant Beach winning a “Best Restored Beach” award, I referred to the “new dunes” created as part of the restoration. Beth Schwarzman, a local geologist and author of The Nature of Cape Cod, emailed this critique:

Heather Goldstone

The photo in question

I am distressed to see your photo labeled new “dunes” at Menauhant Beach.  These dune-shaped objects are clearly built of dredged material, full of Sipper Shells, and high in fines which cement the material together.  Although these piles of material may sit in the location where you would expect to find dunes, and have been planted with Beach Grass, they are not dunes.  A dune is, by definition, “A mound, ridge, or hill of WIND-BLOWN sand”, and therefore made of fine, well-sorted and unconsolidated material.   It was a reasonable choice to create such dune-shaped objects in the process of the beach nourishment, and they may both protect the land and serve as a source of sediment to the beach.  But they are not dunes, any more than that beach is “restored”, no matter what kind of award it got.

This comment reminded me of a conversation I recently had with Bob Hamilton, a coastal engineer with Woods Hole Group, a local engineering consulting firm that specializes in beach restoration and maintenance. He stressed the difference between dunes – which state law protects from most human intervention – and eroding banks, or escarpments.

So, to set the record straight, here are a few definitions:

BEACH: A geological formation consisting of loose rock particles along the shoreline of a body of water. Beaches often occur along coastal areas where wave or current action deposits and reworks sediments.

Heather Goldstone

The escarpment at Coast Guard Beach in the National Seashore.

DUNE: A mound or ridge of sand or other loose sediment formed by the wind, especially on the sea coast or in a desert.

ESCARPMENT: A steep slope or long cliff that results from erosion or faulting and separates two relatively level areas of differing elevations.

UPLAND: An area of high or hilly land, elevated above other land.

Inherent in those definitions are the processes that formed the geography we see. None of them mention bulldozers and dump trucks, let alone the biodegradable fiber mats being used in some restoration projects. With natural erosion processes exacerbated by accelerating sea level rise and a legacy of coastal armoring, more than two-thirds of New England’s beaches are eroding. Those who enjoy said beaches and rely on them for protection from storm damage are increasingly turning to engineering solutions to help preserve them.

So I’m left with a conundrum: what should we call such man-made “beach” structures?

I sent my question to a few other geologists and coastal engineers, and will update as responses come in. Continue reading

Fact-Checking Newsweek’s Climate Change Cover Story

flickr/Thomas Bresson

Earlier this week, NewsWeek ran a cover story with the headline “Are you ready for more?” What followed was an in-depth look at climate change impacts and the need for adaptation measures, by science editor Sharon Begley. Sharon argues that the extreme weather of the past year – and the toll it has taken in terms of both dollars and human lives – makes it clear that we aren’t ready for what’s to come.

I certainly won’t quibble with the fact that climate change has begun to – and will increasingly – make life rough for a lot of people, or that we need to put more effort into planning for and adapting to the inevitable impacts of climate change. And I’ve enjoyed Sharon’s work in the past. But in this case, I wondered if the language might feel melodramatic to the average reader. Take this, for example:

It threatens to be a trail of human misery that will make the exodus after Hurricane Katrina look like a weekend getaway.

I questioned a few factual statements, in particular. And I wasn’t alone. Dot Earth blogger Andy Revkin posted a brief retort (nigh on dismissal) on his tumblr account, and several of the comments on the Newsweek website were skeptical.

So I decided to do some fact-checking. I used the Climate Science Rapid Response service to get leading climate scientists’ perspectives. I also drew on direct quotes from scientists found in past media reports. And I sent my critiques to Sharon so she could respond. Here’s the blow-by-blow:

1. Extreme weather

What Sharon wrote:

Even those who deny the existence of global climate change are having trouble dismissing the evidence of the last year. In the U.S. alone, nearly 1,000 tornadoes have ripped across the heartland, killing more than 500 people and inflicting $9 billion in damage. The Midwest suffered the wettest April in 116 years, forcing the Mississippi to flood thousands of square miles, even as drought-plagued Texas suffered the driest month in a century. Worldwide, the litany of weather’s extremes has reached biblical proportions. The 2010 heat wave in Russia killed an estimated 15,000 people. Floods in Australia and Pakistan killed 2,000 and left large swaths of each country under water. A months-long drought in China has devastated millions of acres of farmland.

What the scientists say:

One thing is certain: temperatures are rising, and warmer air holds more energy and more moisture – the ingredients for stronger storms. Climate scientists are virtually unanimous that global warming will lead to more extreme weather.

Climate scientists are virtually unanimous that global warming will lead to more extreme weather. But …
But the question of whether climate change is responsible for the extreme weather of the past year has been a recurring topic virtually anywhere that weather or climate change is mentioned (and that’s a lot of places). Unfortunately, there’s no satisfying answer. There’s not even one single answer. Ask eight different scientists and you’ll get eight different answers; the editorial team at Yale E360 did exactly that, and the result is some highly recommended reading.

I think Katherine Hayhoe, a climate scientist at Texas Tech University, has done a nice job summing up both the human tendency to look for connections and the difficulties of proving those connections scientifically:

Whenever we see a season like we’re having right now, it’s a natural part of being human to say, is there a pattern to it?

And so, of course, that’s what we’re asking right now: Is there a pattern to all of the weird weather that we have been seeing this spring? Unfortunately, at least for those of us who want a pattern immediately, we can’t tie any one event or even one season to climate change.

Climate is the average statistics of weather over at least 30 years. But what we can do is, we can add this season to the books, and we can start looking at whether we see any trends in heavy rainfall events, in droughts and in tornadoes.

When we do that, we do see trends in some things. We see trends in heat wave frequency and severity in many places around the world. We also see increases in heavy rainfall events across the entire U.S., especially in the Midwest and the Northeast.

But when we look at the tornado record, we don’t see any conclusive trends in tornado numbers or severity yet.

Sharon’s response:

That was based on reporting I did for a column last year describing research that’s making progress attributing particular weather events to overall climate change rather than cyclical, non-global-warming events or simply random fluctuations. As you note, the 2010 Russian heat wave has not yet been so attributed (but as you also note, the case is not closed); ditto–to even greater certainty–the recent tornadoes. I included examples of this and other extremes simply to make the point that in a system with more heat energy, we’re going to see more of them. I think it’s interesting that the decades-long mantra–’no single weather event can be blamed of global warming’–might, thanks to the new statistical techniques pioneered at the Met Office, not be true much longer.

2. 12,000 years of stability

What Sharon wrote:

From these and other extreme-weather events, one lesson is sinking in with terrifying certainty. The stable climate of the last 12,000 years is gone. Which means you haven’t seen anything yet. And we are not prepared.

What scientists say:
I got feedback from four leading climate scientists on this one. Again, no two answers were identical. Henry Pollack, a professor at the University of Michigan and author of A World Without Ice made the point that stability is a matter of perspective.

The standard answer to that question is ‘yes’, but the important contextual question is, stable compared to what? Over the past 10-12 thousand years the fluctuations in Earth’s average surface temperature have generally been in the range of 1-2 degrees Celsius (or smaller). However, for several tens of thousands of years prior, the fluctuations were an order of magnitude larger, 10-20 degrees Celsius

tim caynes / Flickr

Will airports really have to lengthen their runways to accommodate rising temperatures?

But Ray Bradley from University of Massachusetts, Amherst, pointed out that the climate of the past 10,000 years was not nearly as stable in the tropics as it was in higher latitudes. And Woods Hole Oceanographic Institution’s Lloyd Keigwin emphasized the difference between the rate of change (which he said has been similar for hundreds of thousands years) and the extremes that are reached.

But Robert Wilson, from University of St. Andrews, really got at the heart of the matter:

If we acknowledge that the climate of the last 400,000 years is a result of a natural interchange of factors, … the new factor that we need to worry about is Man’s influence on the atmosphere. If we look at CO2 emission alone for the last 400,000 years, the recent increase in CO2 is unprecedented. It is for this reason why the Newsweek article says that “the stable climate of the last 12,000 years is gone”. We are moving into unexplored territory and temperatures WILL increase. Of course there is uncertainty as to whether this increase is going to be 1 degree, 2 degrees or more, but even a further 1 degree Celsius global change over the next 20-50 years will put the global climate system into a state that the planet has not experienced at least for the last 400,000 years.

Sharon’s response (my emphasis):

Stability is a subjective term, so I used (in my own mind; no room to spell it out in the story) maximum temp variations: the 1-2 degrees of swing over the last 12,000 years is less than over the preceding millennia, and seems to be/may be a regime we are leaving behind. Although global mean temps are up only 1 degree or so, the arctic and even some lower-latitude regions have experienced far more.

3. Longer runways

What Sharon wrote:

Because warmer air provides less lift, airport runways the world over will have to be lengthened in order for planes to take off.

What scientists say:

Here, again, scientists’ responses varied. Some had personal experiences with departures delayed because it was too hot for the plane to take off in the space available. All agreed that, while the theory is sound, the real-world relevance is suspect. This may be an issue in some places, or centuries from now if carbon dioxide emissions go unchecked. But it’s unlikely to be a widespread problem in the near future.

Sharon’s response:

I think the runway example is fascinating, and included it only because it was so different from the other climate-change adaptations we may have to make. ‘Widespread’ issue? Maybe not, but of course I didn’t say so. To my knowledge, no aviation authorities have analyzed how much of a safety margin their airports have – obviously, planes take off from JFK and Logan even when it’s 100 degrees. I was sensitized to this issue when I was stuck in Aspen, after doing a panel at an Aspen Institute health forum a few years ago, because airport authorities wouldn’t let us take off: the heat that day, they said, meant the plane was at risk of not clearing the nearby mountains. It left an impression.

The Verdict

After all that, here’s what I’m left thinking: Sharon and I, and the many scientists whose work we attempt to portray for the public, are on the same page (or at least the same chapter) when it comes to the impacts of climate change. I found no egregious errors in her article. And, as I told Susan in our email exchange, the call for greater attention to adaptation measures is a prudent one.

My discomfort was entirely a matter of nuance. Climate change is complicated; trying to hide or deny that fact does no one any favors. Indeed, exaggeration – even the appearance of exaggeration by omission of details about the complexities and limitations of the science – can backfire, causing readers to discount the whole story. That was apparent in some of the responses to Sharon’s article.

I’m not saying every minute detail needs to be trotted out; I certainly left out more than a few from the email exchanges that went into this piece. But I wanted to point out that this is difficult, that these questions are nuanced, and the complexities of the science might not respect our space limitations. If we state our perceptions too boldly, we run the risk of crying wolf. But if we don’t talk about climate science at all, we risk an even greater peril.

On the transience of sand

Heather Goldstone

The view from the parking lot at Menauhant Beach in Falmouth, MA. The boulders, dunes, and dune grasses were part of a beach restoration project completed about six months before this photo was taken.

You know it’s bad when you win a “Best Restored Beach” award. It’s like Nip-and-Tuck meets Miss America.

Seriously, though, Falmouth’s Menauhant Beach is one of five recipients of the American Shore and Beach Preservation Association’s 2010 Best Restored Beach Awards. The others are Isle of Palms, South Carolina; Miami Beach, Florida; Moonlight Beach, California; and Presque Isle, Pennsylvania.

Menauhant is an outstanding example of what erosion can do. A few decades ago, this bridge (and the road it was part of) spanned the cut-through to the back bay behind the beach. As wind and waves have taken their toll, the beach has retreated. Old Menauhant Bridge now sits firmly in the middle of the dunes and was replaced with a new road years ago.

Heather Goldstone

Old Menauhant Bridge was engulfed in sand as the beach retreated from the forces of wind and waves.

Several years ago, Menauhant was in pretty rough shape – a narrow strip of rocky beach. Then came the restoration. More than 20,000 cubic yards of sand dredged from a navigation channel in Woods Hole was transported to Menauhant and used to re-create almost 2,000 feet of beach and build or bulk up dunes at the back of the beach. Wooden fences and beach grasses planted on the dunes help hold the whole thing together.

Heather Goldstone

In this photo from the spring of 2009, a sign reading "These dunes aren't meant for walking" warns visitors to keep off the restored dunes and newly planted dune grass.

It just so happens Menauhant Beach is “my” beach; I live a mere two miles up the road. We moved in a year before the project was completed in fall of 2008. Before, it wasn’t a place where we spent much time. Now, it’s one of my family’s three favorite beaches in Falmouth. In addition to hours of sandcastle fun, it’s where we watch Fourth of July fireworks and where we went to watch Hurricane Earl rolling by last September.

Heather Goldstone

The parking attendant's booth at Menauhant Beach turned on its side in preparation for Hurricane Earl.

I know it’s horribly nerdy of me, but every time we pass Old Menauhant Bridge and pull into the parking lot behind those beautiful dunes, I can’t help but wonder how long it will all be there. Knowing what wind and waves did in the past several decades, and knowing that those same forces will be getting a helping hand from rising sea level and intensifying storms in coming decades … well, let’s just say the only thing that’s certain is that Menauhant Beach will look very different when my kids are grown.

But beach restoration and nourishment is one of the very few options we have for coping with rising sea level. And if you’re gonna do it, you might as well do it well. So congratulations to Menauhant Beach and those who rebuilt it.

Borrowing sand to build beaches

Jetties and seawalls can be instrumental in protecting vulnerable property or infrastructure, but they have a dark side: they rob nearby areas of the sand and silt that sustain beaches and marshlands. Town Neck Beach in Sandwich is a prime example. Jetties constructed in the 50′s to help keep shipping lanes in the Cape Cod Canal open have resulted in dramatic erosion of nearby Town Neck Beach and the marsh behind it.

Sandwich town officials have been working for years to address the problem. Cape Cod Times’ George Brennan reports that they may be getting closer:

At a meeting earlier this week, officials from across the Cape met with Cape Cod Commission staff to discuss the possibility of mining sand offshore to renourish sand-starved beaches.

Sand mining is allowed under the state’s Ocean Management Plan, but not for commercial purposes, commission Executive Director Paul Niedzwiecki said. The commission is in the process of mapping areas where sand mining would be prohibited under the marine district of critical planning concern.

The Cape Cod Commission has released a preliminary map of areas that could be used for sand mining; critical habitat for endangered right whales would be off-limits. But there are other areas that could be considered, and the Commission expressed willingness to include sand mining areas in their ocean use planning.

The commission is open to the idea of pre-permitting so-called “borrow pits” to help Cape communities deal with ongoing erosion problems, Niedzwiecki said. It’s something that New Jersey already does and by providing these predetermined sites here, it would cut down on the expense of permitting, he said.

“We understand that this is a pressing need for many local communities,” Niedzwiecki said. The commission should have standards in place by the end of the summer, he said.

Of course, sand mining and beach nourishment aren’t cheap, and there’s the question of who would pay. The jetties were built by the Army Corps of Engineers.

If the Corps were to agree that its jetties are the source of the problem, it would be obligated to pay for the solution, [state Rep. Randy] Hunt said.

Even if Sandwich officials find the sand and the funding, they may face challenges to beach nourishment plans.

Not only will sand mining trigger Cape Cod Commission oversight, but it will also require Massachusetts Environmental Policy Act (MEPA) review. Sandwich has opposition from the state’s Natural Heritage in the past because its main stretch of beach is the habitat for the endangered piping plover.

So, really, the situation at Town Neck Beach shines a light on the dark sides of both coastal armoring and beach nourishment.
But here’s my question: Why are they called “borrow pits”? Nobody’s planning to put the sand back.

Climate research to meet the needs of decision-makers

We continue our exploration of the National Academies’ America’s Climate Choices series with …

Volume 3: What can be done to better understand climate change and its impacts?

The Big Picture: There is ample scientific evidence that climate change is happening, that it is largely caused by human activities, and that it poses serious risks for humans and natural systems. But there are many areas of uncertainty that impede effective responses to climate change. Scientific research can, of course, fill gaps in our understanding of how and why climate change is happening. In addition, the scientific community can play an important role in evaluating options and developing technologies for responding to climate change. What science cannot do is tell policy-makers the best or right thing to do, as that decision involves value judgements beyond the technical merits of a given action.

The Recommendations:

  1. In order for climate science research in the U.S. to reach its full potential, the panel recommends that “a single federal entity or program be given the authority and resources to coordinate a national, multidisciplinary research effort.” They note that the U.S. Global Change Research Program, which has coordinated research at thirteen federal departments or agencies since 1990, could fill the bill with some improvements and modifications.
  2. There are also crucial infrastructure needs – a comprehensive climate observing system (satellite, buoys, and other high-tech gadgetry), better computer models to channel the vast quantities of information into meaningful predictions, and well-trained individuals to do the research and – importantly – bridge the gap between scientists and policy-makers.

Of course, this all requires resources, and money for climate science has been in short supply in Washington, D.C. lately.

Want more? Download a brief summary or read the full report online.

And, just in case you missed it:
Volume 1: What can be done to limit the magnitude of future climate change?
Volume 2: What can be done to adapt to the impacts of climate change?

How do we adapt to climate change?

On Thursday, the National Academies of Science will release the fifth and final volume in its series on climate change, America’s Climate Choices. Each volume in the series addresses a specific question and provides several recommendations for policy makers. The first volume addressed policy options for reducing future climate change. The second focuses on living with the current and future impacts of climate change.

Volume 2:What can be done to adapt to the impacts of climate change?

The Big Picture:

The impacts of climate change are already visible in some places, and many more impacts are inevitable, even if immediate and aggressive action is taken to curtail greenhouse gas emissions. While there is a lot of uncertainty about when and where we’ll see changes, and how severe they’ll be, waiting for certainty could be disastrous. To date, adaptation efforts have been piecemeal, enacted at the local, state, or regional level with little or no coordination between them. Additionally, planners face a serious lack of information about which strategies work best and are most cost-effective.

The Recommendation:

Because climate change impacts vary from place to place (sea level rise is only an issue on the coast, while heat waves may be more problematic inland), specific adaptation strategies need to be tailored locally or regionally. But the panel recommends developing a national adaptation strategy that encourages, supports, and coordinates local and regional efforts to adapt to climate change by:

  • providing information, technical resources, and incentives for adaptation planning and action;
  • helping to avoid unintended consequences and inconsistent or inefficient investments and outcomes;
  • continually evaluating needs for additional risk management at a national level;
  • and serving as a role model by considering adaptation in federal programs.

Want more? Download a brief summary of the report or read the full report online.

Tomorrow, Volume 3: Advancing the Science of Climate Change.