Wide Angle: Geo-engineering and the Water Cycle
October 09, 2009
When Mt. Pinatubo erupted in the Philippines in 1991, the resulting effect on global climate was staggering. The eruption sent so many millions tons of debris and aerosols into the stratosphere that it, quite literally, blocked the sun. Despite the fact that greenhouse gas emissions continued their steady rise in the year that followed the eruption, the stratospheric debris from Pinatubo caused global temperatures to drop during that time by almost a degree. Scientists hoping to find geo-engineering solutions to cooling the earth took note. Would there be a way to mimic the Pinatubo eruption, without the destruction and sulfur dioxide, and block or reflect enough of the sunlight to stop the heating of the earth? Lots of ideas have been floated, ranging from satellites that deploy giant parasol-like fans, to simply painting roofs a more reflective white. You can read a couple of posts from our friends at Treehugger to find out more: here and here. Here's the thing, though. You can't dramatically tinker with a complex system and not expect the unexpected. In the year after the Pinatubo eruption, scientists noted interesting, and potentially devastating, effects on the water cycle in certain parts of the world. And that's led some scientists to ask just exactly what effects large-scale bio-engineering might have on the earth's water cycle. Ken Caldeira, a climate scientist with the Carnegie Institution's Department of Global Ecology on the Stanford University campus, is running some modeling tests to try the answer those questions about geo-engineering and the water cycle. I caught up with him for this week's podcast, and he started by giving a bit more background on what happened to the Ganges River in India after the Pinatubo eruption:










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