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- From: ckawecki@hamp.hampshire.edu
- Subject: Motivation to rain more over forests!
- Message-ID: <1992Nov16.164747.1@hamp.hampshire.edu>
- Lines: 33
- Sender: usenet@nic.umass.edu (USENET News System)
- Organization: Hampshire College
- Date: Mon, 16 Nov 1992 20:47:46 GMT
-
- Researching rainfall as it relates to vegetation and albido, I have come
- across many a perplexing theory. I seek any ideas and alalyses which
- may have better dealt with this problem. Thus far, I am disappointed:
-
- One proposed mechanism is that air confronts a thermal mountain
- (Malkus and Stearn, 1953), rises, cools, and hence precipitation
- (Johnathan Sands, 1981). This is based on very sketchy evidence
- that forests are significantly hotter (6 deg C is suggested) Yet
- the data is based on albido as a function of net radiation and
- radiated longwave energy to suggest that trees use less of their
- net radiation on evapotranspiration. It seems, however, that in this case
- albido ought to have been defined in terms of shortwave incoming
- radiation, not net radiation! (for, the question would be: under
- similair soil moisture contents, and light, would trees or
- grasslands have greater evapotranspiration levels?) (remember
- to consider that radiated energy can be once again reflected by
- cloud
-
- 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?
-
- chris kawecki
- hampshire college
- ckawecki@hamp.hampshire.edu
-