Downscaling methods are utilized to assess the effects of large scale atmospheric circulation on local hydrological variables such as precipitation and runoff. In this paper, a methodology of statistical downscaling using a support vector machine (SVM) approach is presented to simulate and predict the precipitation using general circulation model (GCM) data. Due to the complexity and issues related to finding a relationship between the large scale climatic parameters and local precipitation, the climate variables (predictors) affecting monthly precipitation variations over Wales are identified using a combination of the methods including the principal component analysis (PCA), fuzzy clustering, backward selection, forward selection, and Gamma test (GT). The effectiveness of those tools is illustrated through their implementations in the case study. It has been found that although the GT itself fails to identify the best input variable combination, it provides useful and narrowed-down options for further exploration. The best input variable combination is achieved by the GT and forward selection method. This approach can be a useful way for assessing the impacts of climate variables on precipitation forecasting.
Skip Nav Destination
Article navigation
Research Article|
December 13 2012
Identification of dominant sources of sea level pressure for precipitation forecasting over Wales
Azadeh Ahmadi;
1Department of Civil Engineering, Isfahan University of Technology, Isfahan, Iran
E-mail: [email protected]
Search for other works by this author on:
Dawei Han
Dawei Han
2Water and Environmental Management Research Centre, Department of Civil Engineering, University of Bristol, Bristol, UK
Search for other works by this author on:
Journal of Hydroinformatics (2013) 15 (3): 1002–1021.
Article history
Received:
June 19 2012
Accepted:
October 26 2012
Citation
Azadeh Ahmadi, Dawei Han; Identification of dominant sources of sea level pressure for precipitation forecasting over Wales. Journal of Hydroinformatics 1 July 2013; 15 (3): 1002–1021. doi: https://doi.org/10.2166/hydro.2012.110
Download citation file: