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Ogata, T. et al. Projected future changes of the Asian Monsoon: A Comparison of CMIP3 and CMIP5 model results.
Here we provide an assessment of future changes of the area where precipitation will mainly occur as rain or snow, over the central and eastern U.S. under scenarios of future warming for the late 21st century.
The addition of the discount coefficient that adjusts the future changes of the present money value in the objective function was implemented in two hypothetical cases For comparison, different economic parameters were used to perform a cost evaluation test in terms of present money values.
Future changes of the precipitation regime due to climate change may increase the limitation to time.
Second, sensitivity analysis may help to predict the future changes of the equilibrium as a result of changes in the governing systems.
The future changes of the climate parameters were assessed by calculating the climatic factor of the Wind Erosion Equation WEQ (Klik 2004).
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To assess the future changes of wind erosion hazard the changes of the climate parameters were applied for the two periods (2021 2050 and 2071 2100).
This indicates that the future changes of probability distributions of the snow occurrences are not simply uniform shifts to lower values, but also involve skewness changes towards the lower values.
To assess the future changes of inland excess water hazards, the Humidity Index (HUMI) was applied.
The ultimate effect of the future changes on the glacier and hydrology is unclear and poorly investigated for Central Asia.
Future changes of snow occurrences over the central and eastern U.S. under two emission scenarios were investigated using high spatial resolution downscaled ensemble averages from ten GCMs.
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