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- From: hannegan@hyperion.gsfc.nasa.gov (Bryan Hannegan)
- Newsgroups: sci.geo.meteorology
- Subject: Re: Motivation to rain more over forests!
- Message-ID: <1992Nov17.000943.9815@nsisrv.gsfc.nasa.gov>
- Date: 17 Nov 92 00:09:43 GMT
- References: <1992Nov16.164747.1@hamp.hampshire.edu>
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- Organization: Code 916, NASA Goddard Space Flight Center
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-
- In article <1992Nov16.164747.1@hamp.hampshire.edu> ckawecki@hamp.hampshire.edu writes:
- > Preliminary investigation (Brown 72- re strip clearcutting
- >of Minnesota Spruce) suggests that forests for a certain time
- >have lower evapotranspiration rates than that which replaces them,
- >but that groundwater is depleted in the clearcut strips. Reasonable, then,
- >to suggest that a clearcut forest would lose soil moisture content,
- >until the grasses which replaced the forest had too little water
- >to draw from, at which point their evapotranspiration rates would
- >be less than those of forests? This suggests that significant
- >amounts of rainfall were originally not from the ocean, but evaporated.
- >
- > Ideas anyone?
- >
-
- I'm not sure that I completely follow Chris' line of reasoning, but something
- I remembered from a meteorological class I took dealing with the tropics
- took hold.
-
- In the tropics, a primary source of the rainfall over rainforests is not
- so much the transport from the oceans, but rather, the large amount of
- evaporation from the forest canopy itself. In this manner, torrential
- downpours are observed well inland from any external moisture source.
-
- Additionally, the soil under a forest canopy would (if memory serves correctly)
- support a larger field capacity than a grassland in the same situation. The
- capability to hold more mositure would then be available at least in theory.
-
- When clearcutting were to occur, the field capacity would diminsh and the excess
- water which was previously bound to the roots of the forest would be liberated
- to run off from the soon-to-be grassland.
-
- Anyone care to help here? This is cobwebbed knowledge from my undergraduate past
- at Oklahoma, and may be unclear.
-
- Bryan Hannegan
- Dept. of Geosciences, University of CA, Irvine
- hannegan@halo.ps.uci.edu
-