Sokolov, A.P., Stone, P.H., Forest, C.E., Prinn, R.G., Sarofim, M.C., Webster, M., Paltsev, S., Schlosser, C.A., Kicklighter, D., Dutkiewicz, S., Reilly, J., Wang, C., Felzer, B., Melillo, J. and Jacoby, H.D. (2009) Probabilistic Forecast for 21st Century Climate Based on Uncertainties in Emissions (without Policy) and climate Parameters. Journal of Climate, 22, 5175-5204.
http://dx.doi.org/10.1175/2009JCLI2863.1

has been cited by the following article:

• TITLE: Hydrological Impact Assessment of Climate Change on Lake Tana’s Water Balance, Ethiopia

  AUTHORS: Zemede Mulushewa Nigatu, Tom Rientjes, Alemseged Tamiru Haile

  KEYWORDS: Climate Change, Water Balance, SDSM, Statistical Downscaling, Lake Tana

  JOURNAL NAME: American Journal of Climate Change, Vol.5 No.1, March 15, 2016

  ABSTRACT: The aim of this study is to evaluate the hydrological impacts of climate change on the water balance of Lake Tana in Ethiopia. Impact assessments are by downscaled General Circulation Model (GCM) output and hydrological modeling. For A2 and B2 emission scenarios, precipitation, maximum and minimum temperature estimates from the HadCM3 GCM were used. GCM output was downscaled using the Statistical DownScaling Model (SDSM 4.2). Impact analyses were applied for three future time periods: early, mid and late 21st century. Over-lake evaporation is estimated by Hardgrave’s method, and over-lake precipitation is estimated by inverse distance weighing interpolation, whereas inflows from gauged and ungauged catchments are simulated by the HBV hydrological model. Findings indicate increases in maximum and minimum temperature on annual base for both emission scenarios. The projection of mean annual over lake precipitation for both A2 and B2 emission scenarios shows increasing pattern for 21st century in comparison to the baseline period. The increase of mean annual precipitation for A2 emission scenario is 9% (112 mm/year), 10% (125 mm/year) and 11% (137 mm/year) for the three future periods respectively. B2 emission scenario mean annual precipitation shows increase by 9% (111 mm/year), 10% (122 mm/year) and 10% (130 mm/year) respectively for the three future periods. Findings indicate consistent increases of lake storage for all three future periods for both A2 and B2 emission scenarios.