A non-parametric, statistical downscaling algorithm applied to the Rohini River Basin, Nepal

Climate change scenarios generated by general circulation models have too coarse a spatial resolution to be useful in planning disaster risk reduction and climate change adaptation strategies at regional to river basin scales. This study presents a new non-parametric statistical K-nearest neighbor algorithm for downscaling climate change scenarios for the Rohini River Basin in Nepal. The study is an introduction to the methodology and discusses its strengths and limitations within the context of hindcasting basin precipitation for the period of 1976–2006. The actual downscaled climate change projections are not presented here. In general, we find that this method is quite robust and well suited to the data-poor situations common in developing countries. The method is able to replicate historical rainfall values in most months, except for January, September, and October. As with any downscaling technique, whether numerical or statistical, data limitations significantly constrain model ability. The method was able to confirm that the dataset available for the Rohini Basin does not capture long-term climatology. Yet, we do find that the hindcasts generated with this methodology do have enough skill to warrant pursuit of downscaling climate change scenarios for this particularly poor and vulnerable region of the world.

[1]  Huan Wu,et al.  Principal Modes of Rainfall–SST Variability of the Asian Summer Monsoon: A Reassessment of the Monsoon–ENSO Relationship , 2001 .

[2]  Balaji Rajagopalan,et al.  A stochastic nonparametric approach for streamflow generation combining observational and paleoreconstructed data , 2008, Water Resources Research.

[3]  Upmanu Lall,et al.  A k‐nearest‐neighbor simulator for daily precipitation and other weather variables , 1999 .

[4]  H. Storch,et al.  Statistical Analysis in Climate Research , 2000 .

[5]  P. Jones,et al.  Evaluation of the North Atlantic Oscillation as simulated by a coupled climate model , 1999 .

[6]  Jean Palutikof,et al.  Precipitation Scenarios over Iberia: A Comparison between Direct GCM Output and Different Downscaling Techniques , 2001 .

[7]  Upmanu Lall,et al.  A Nearest Neighbor Bootstrap For Resampling Hydrologic Time Series , 1996 .

[8]  R. Kripalani,et al.  Association between extreme monsoons and the dipole mode over the Indian subcontinent , 2007 .

[9]  P. Whetton,et al.  Guidelines for Use of Climate Scenarios Developed from Statistical Downscaling Methods , 2004 .

[10]  Arun Kumar,et al.  Long‐range experimental hydrologic forecasting for the eastern United States , 2002 .

[11]  P. Webster,et al.  Monsoons: Processes, predictability, and the prospects for prediction , 1998 .

[12]  Kenneth J. Berry,et al.  A Single-Sample Estimate of Shrinkage in Meteorological Forecasting , 1997 .

[13]  Jai-Ho Oh,et al.  South Asian summer monsoon precipitation variability: Coupled climate model simulations and projections under IPCC AR4 , 2007 .

[14]  P. Vinayachandran,et al.  Droughts of the Indian summer monsoon: Role of clouds over the Indian Ocean , 2003 .

[15]  K. Wolter,et al.  Measuring the strength of ENSO events: How does 1997/98 rank? , 1998 .

[16]  S. Manabe,et al.  The Role of Mountains in the South Asian Monsoon Circulation , 1975 .

[17]  Arun Kumar,et al.  Seasonal Predictions, Probabilistic Verifications, and Ensemble Size , 2001 .

[18]  P. Webster,et al.  A Hydrological Definition of Indian Monsoon Onset and Withdrawal , 2003 .

[19]  Janette Lindesay,et al.  ENSO and climatic signals across the Indian Ocean Basin in the global context: part I, interannual composite patterns , 2000 .

[20]  M. Hoerling,et al.  The Perfect Ocean for Drought , 2003, Science.

[21]  G. Meehl,et al.  The Tropospheric Biennial Oscillation and Asian–Australian Monsoon Rainfall , 2002 .

[22]  P. Coulibaly,et al.  Hydrologic impact of climate change in the Saguenay watershed: comparison of downscaling methods and hydrologic models , 2005 .

[23]  S. Gangopadhyay,et al.  Generating streamflow forecasts for the Yakima River Basin using large-scale climate predictors , 2007 .

[24]  Walter Collischonn,et al.  Predicting daily streamflow using rainfall forecasts, a simple loss module and unit hydrographs: Two Brazilian catchments , 2007, Environ. Model. Softw..

[25]  Allan H. Murphy Scalar and Vector Partitions of the Ranked Probability Score1 , 1972 .

[26]  V. Ramanathan,et al.  Weakening of North Indian SST Gradients and the Monsoon Rainfall in India and the Sahel , 2006 .

[27]  Francisco J. Doblas-Reyes,et al.  A Debiased Ranked Probability Skill Score to Evaluate Probabilistic Ensemble Forecasts with Small Ensemble Sizes , 2005 .

[28]  W. Briggs Statistical Methods in the Atmospheric Sciences , 2007 .

[29]  Corinne Le Quéré,et al.  Climate Change 2013: The Physical Science Basis , 2013 .

[30]  H. Douville Impact of Regional SST Anomalies on the Indian Monsoon Response to Global Warming in the CNRM Climate Model , 2006 .

[31]  A. Fedorov,et al.  Is El Nino changing? , 2000, Science.

[32]  Hayley J. Fowler,et al.  Linking climate change modelling to impacts studies: recent advances in downscaling techniques for hydrological modelling , 2007 .

[33]  M. Hoerling,et al.  Unraveling the Mystery of Indian Monsoon Failure During El Niño , 2006, Science.

[34]  Ravi S. Nanjundiah,et al.  Downscaling precipitation to river basin in India for IPCC SRES scenarios using support vector machine , 2008 .

[35]  R. Miller,et al.  Modeling daily river flows with precipitation input , 1981 .

[36]  Chris Kilsby,et al.  Precipitation and the North Atlantic Oscillation: a study of climatic variability in northern England , 2002 .

[37]  S. Solomon The Physical Science Basis : Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change , 2007 .

[38]  M. Cane,et al.  Indian summer monsoon rainfall and its link with ENSO and Indian Ocean climate indices , 2007 .

[39]  Kenneth Strzepek,et al.  A technique for generating regional climate scenarios using a nearest‐neighbor algorithm , 2003 .

[40]  James P. Hughes,et al.  Statistical downscaling of daily precipitation from observed and modelled atmospheric fields , 2004 .

[41]  Balaji Rajagopalan,et al.  Statistical downscaling using K‐nearest neighbors , 2005 .

[42]  R. Reynolds,et al.  The NCEP/NCAR 40-Year Reanalysis Project , 1996, Renewable Energy.

[43]  K. Tolika,et al.  An evaluation of a general circulation model (GCM) and the NCEP–NCAR reanalysis data for winter precipitation in Greece , 2006 .

[44]  P. Webster,et al.  Interdecadal changes in the ENSO-monsoon system , 1999 .

[45]  Trevor D. Davies,et al.  Atmospheric circulation and surface temperature in Europe from the 18th century to 1995 , 2001 .

[46]  K. Miyakoda,et al.  Recent Change in the Connection from the Asian Monsoon to ENSO , 2002 .

[47]  Roger Jones,et al.  Regional climate projections , 2007 .

[48]  William N. Venables,et al.  Modern Applied Statistics with S , 2010 .