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Retrospections Culture Wet and Dry
 
Wet and Dry
Source: The Hot Zone
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Climate
Posted:   03/28/11

Summary: From extreme precipitation events to catastrophic droughts, the effects of climate change may be heralding in a new era of extreme weather. Scientists are trying to determine what the repercussions for the Earth's biosphere could be.

Extreme precipitation events pinpointed to global warming

These Landsat 7 scenes show a comparison of the region surrounding Exeter, England, before and after the floods. Credit: Robert Simmon and Brian Montgomery, NASA GSFC. Data provided by Ron Beck, USGS EROS Data Center
Extreme precipitation events seem to be becoming more common in the Northern Hemisphere. But it’s been very hard for scientists to pinpoint a major weather event to global warming. Still, when a 100-year flood comes and then returns in a matter of a few years, it’s hard not to consider it a sign of a warming world.

Several papers published in the journal Nature demonstrate that such extreme precipitation events in specific localities is the result of climate change and not an overactive imagination. The scientists studied the actual, observable precipitation patterns in the 20th century and then compared them to climate model simulations and a splash of probability to discover a close, predictive match up.

They claim that their results provide “first formal identification of a human contribution to the observed intensification of extreme precipitation.” The scientists, led by Seung-Ki Min at the Climate Research Division from Environment Canada in Toronto, say that the global climate models may, in fact, be underestimating the amount of extreme weather events, “which implies that extreme precipitation events may strengthen more quickly in the future than projected and that they may have more severe impacts than estimated.”

In another study, this one led by Pardeep Pall at the University of Oxford, looked at a specific weather event: the 2000 floods in England and Wales, which occurred during the wettest autumn since 1766. About 10,000 properties were flooded over, causing evacuations, disruptions in rail service and power supplies, and an economic dent of about a £ 1 billion.

Oxford scientists used a climate model and simulated different scenarios of rainfall patterns based on greenhouse gas levels in the atmosphere. The results were fed into a model that simulated severe river runoff and found that in nine out of 10 cases, the model forecast an increased risk of floods when 20th century levels greenhouse gases were included. Specifically, the increase in risk for floods in the autumn of 2000 in England and Wales was more 20 percent, and in two out of three cases more than 90 percent.

The scientists conclude that human-caused greenhouse gas emissions contributed to the flood risk in England and Wales in 2000. With such techniques, scientists are coming closer to determining which weather events are nothing more than the result of statistical flukes, and which may seem like aberrant behavior but are really right in line with what we might expect from a warming world.

Climate change could signal prolonged droughts in American Southwest

Think the 1930s “Dust Bowl” was bad in the American West? Scientists have found evidence of “mega-drought” events that lasted centuries to millennia in the same region during warm, interglacial periods in the Pleistocene era (370,000-550,000 years ago). The evidence heightens concern over how the region will react to the modern day global temperature spikes.

A dust storm in Oklahoma, 1936. Photo: Arthur Rothstein
The American Southwest is already predicted to get pretty dry during climate change, due to a drop in winter precipitation that would increase evaporation rates and lead to smaller snow packs that normally provide water during the warmer months.

Led by University of New Mexico earth scientist Peter Fawcett, the paper published in this week’s journal Nature discusses the discovery of extreme arid conditions in the Valles Caldera region of New Mexico during the warmest phases of interglacials, when the mean annual temperature was comparable or higher to that of modern day temperatures.

In one interglacial period they studied, temperatures rose almost 10 degrees Fahrenheit, leading at first to an abundance of vegetation such as oak and juniper that like warm conditions. However, as temperatures persisted the record shows a collapse in drought-resistant species and the Valles Caldera lake dried out, indicating a drought that scientists estimate lasted several thousand years. They write:

Our results strongly indicate that interglacial climates in the southwestern US can experience prolonged periods of aridity, lasting centuries to millennia, with profound effects on water availability and ecosystem composition. The risk of prolonged aridity is likely to be heightened by anthropogenic forcing.



The droughts they’ve studied make the 10-year Dust Bowl look like a blink in time.

 


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