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This item was posted on January 31, 2010, and it was categorized as Climate Change, Global Warming, drought.
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The climate bats last…

cave-study2

As an international media storm continues to rage over allegations of fraud by the Intergovernmental Panel on Climate Change and its director, Rahendra K. Pachauri, new research suggests that a warming world will bring drier conditions to the already drought-stricken American Southwest.

As part of the research, published last week in Nature Geosciences (sub req), scientists gleaned a new climate record from stalactites and stalagmites in a New Mexico cave. The record suggests that warming will “lead to increasingly arid conditions in southwestern North America in the future.”

Credit goes to my colleague John Fleck of the Albuquerque Tribune, one of the nation’s top science writers, for highlighting this new research in a story (sub req) and in a posting at Inkstain, his personal blog.

As Fleck tells the story, 45,000 years of water dripping slowly within New Mexico’s Fort Stanton Cave have deposited stalactites and stalagmites. By analyzing chemical fingerprints in the calcite of these cave formations, Yemane Asmerom of the University of New Mexico and his colleagues were able to reconstruct a record of aridity during the last glacial period and deglaciation.

The researchers say warming temperatures tended to nudge the jet stream over North America to the north, as is depicted in the map above. (The map also depicts shifts in the Intertropical Convergence Zone, where trade winds originating in the Southern and Northern Hemispheres converge.)

It’s the jet stream that typically steers winter precipitation into the American Southwest. So with a northward shift, winter snows bypassed the American Southwest, resulting in dryer conditions.

Scientists have already documented a northward shift of the jet  stream in response to current global warming. And computer simulations of a warming climate have predicted that northward shifts of the world’s jet streams would occur. Now, the research by Asmerom and his colleagues documents that this has actually occurred in the past.

The findings are “particularly ominous for drought-sensitive regions, such as the western United States,” Asmerom and his colleagues write. And if future warming unfolds as it did at the end of the last interglacial period — suddenly and rapidly — the Southwestern United States could be pushed “into an even more arid phase, unseen since the early Holocene, or even go beyond this, into conditions not represented since 125,000 [years] ago.”

Meanwhile, the Southwestern United States remains in the grip of a drought that began in October of 1999. According to the U.S. Bureau of Reclamation, Lake Mead in the lower Colorado River Basin stands at just 44 percent of capacity. And there’s very little hope of recovery in the short run. The flow of the Colorado River  from April through July is forecast at 6.0 million acre-feet, or just 76 percent of average.

Once again, nature is trying to tell us something. Are we simply too distracted by politics, ideology and good, old-fashioned scandal, to listen?

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This thing has 3 Comments

  1. Posted February 1, 2010 at 8:28 am | Permalink

    “Are we simply too distracted by politics, ideology and good, old-fashioned scandal, to listen?”

    No, people are distracted by their own problems–finding (and keeping) a job, raising a family, etc., to pay attention.

    Tom, ask yourself this: how well do people plan for drought out there in the SW? And that’s natural to the climate, something that is historically well documented. Yet everytime a nasty, multi-year drought hits, panic sets in. Why is that? Why does this always replay itself?

    And you expect people to respond better to global warming?

  2. Steve Bloom
    Posted February 4, 2010 at 1:45 pm | Permalink

    Ironically Tom’s very next post provides further evidence that we are indeed too distracted by those things.

  3. Steve Bloom
    Posted February 4, 2010 at 3:02 pm | Permalink

    These slightly earlier results with similar methods and conclusions received almost no attention, although in combination with the AZ and NM papers JF mentions they give a very good representation of the whole region.

    More importantly, I have yet to see a single story discussing the larger picture relating to this research. Recent PRISM results show that as climate warms beyond the Pleistocene range (which will happen in the coming century) the PSW will get not just much more arid but very hot indeed (see the graphic on page 7 of this paper; note also the strong teleconnection to the Atlantic sector of the Arctic Ocean, which confirms model results reported a few years ago). The only question is how fast it will happen given the lags built into the climate system. (You’d think that the fact that in the coming Pliocene-style climate the tropics remain equable while the heat rushes generally poleward — precisely where we don;t want it — would also be worth a mention in some article somewhere, but I haven’t seen that one either.)

    BTW, JF’s story mentions that Cristina Archer’s recent work didn’t attribute the cause of the shift in the jet (fair enough since she was studying high-altitude wind resources), but this paper from a year ago did. I’ll give you one guess as to the identified cause.

    So yeah, some journalist or another ought to cover this, but even if they do it’ll still be stuffed into the same tiny fraction of the (largely non-front-page) news hole that implies to readers that they can safely ignore it.

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