Title: Land use impact on the Uruguay River discharge
Authors: Ramiro I. Saurral and Vicente R. Barros: Center for Atmospheric and Oceanic Research, National Scientific and Technical Research Council, University of Buenos Aires, Buenos Aires, Argentina; also at Department of Atmospheric and Ocean Sciences, University of Buenos Aires, Buenos Aires, Argentina;
Dennis P. Lettenmaier: Department of Civil and Environmental Engineering, University of Washington, Seattle, Washington, U.S.A.
Source: Geophysical Research Letters (GRL) paper 10.1029/2008GL033707, 2008; http://dx.doi.org/10.1029/2008GL033707
6. Reexamining stratosphere effects on lower-atmosphere warming
It is well established that the troposphere, the atmospheric layer closest to the Earth's surface, significantly influences the circulation of the stratosphere, the layer above the troposphere. The alternate possibility, that the stratosphere can have significant downward influence on tropospheric circulation, is less well established. Sigmond et al. investigate the potential for such downward influence to alter current predictions of global warming. Comparing the predicted warming response in two general circulation modelsone with a well-resolved stratosphere (high-top version) and one without a well-resolved stratosphere (low-top version)they find significant differences. While similar results in the past have been taken as evidence that a well-resolved stratosphere is essential for modeling future climate projections, the authors que
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