Abstract
Increasing levels of atmospheric CO2 will not only modify climate, they will also likely increase the water-use efficiency of plants by decreasing stomatal openings. The effect of the imposition of "doubled stomatal resistance' on climate is investigated in off-line simulations with the Biosphere-Atmosphere Transfer Scheme (BATS) and in two sets of global climate model simulations: for present-day and doubled atmospheric CO2 concentrations. The anticipated evapotranspiration decrease is seen most clearly in the boreal forests in the summer although, for the present-day climate (but not at 2 × CO2), there are also noticeable responses in the tropical forests in South America. -from Authors
Original language | English |
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Pages (from-to) | 1738-1756 |
Number of pages | 19 |
Journal | Journal of Climate |
Volume | 8 |
Issue number | 7 |
DOIs | |
Publication status | Published - 1995 |