Climate change analysis on historical watershed-scale precipitation by means of long-term dynamical downscaling

2016 ◽  
Vol 31 (1) ◽  
pp. 35-50 ◽  
Author(s):  
K. Ishida ◽  
M. L. Kavvas
2005 ◽  
Vol 42 ◽  
pp. 331-336 ◽  
Author(s):  
Fuyuki Saito ◽  
Ayako Abe-Ouchi

AbstractThe response of the Greenland ice sheet to global warming is simulated by two different numerical approaches, in order to evaluate the sensitivity of the analysis to the numerical structure employed. It is found that the thickness near the margin differs appreciably in these two simulations under identical conditions of modest warming, primarily due to a significant increase in the warming effect by an elevation–ablation feedback mechanism in one of the simulations. The change in ice-sheet volume differs by as much as a factor of two under strong climate-change forcing, demonstrating the need for care in interpreting the results of such climate-change analysis.


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