Abstract
Bias correction is a necessary post-processing procedure in order to use Regional Climate Model (RCM) simulated local climate variables as the input data for hydrological models due to systematic errors of RCMs. Most of present bias correction methods adjust statistic properties between observed and simulated data based on calendar periods, e.g., month or season. However, this matching statistic is only a necessary condition, not a sufficient condition, since temporal distribution of the precipitation between observed and simulated data is ignored. This study suggests an improved bias correction scheme which considers not only statistical properties but also the temporal distribution between the time series of observed and modelled data. The ratio of the observed precipitation to simulated precipitation is used to compare the behaviour between the observed and modelled precipitation data and three criteria are proposed when dividing bias correction periods: 1) over/under estimation of precipitation, 2) stability of precipitation ratio and 3) oscillation of precipitation ratio. The results show that the output of the proposed bias correction method follows the trend of the observed precipitation better than that of the conventional bias correction method. This study indicates that temporal distribution should not be ignored when choosing a comparison period for bias correction. However, the study is only a preliminary attempt to address this important issue and we hope it will stimulate more research activities to improve the methodology. Future efforts on several unsolved problems have been suggested such as how to find out the optimal group number to avoid the overfitting and underfitting conditions.
Original language | English |
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Pages (from-to) | 2258-2266 |
Number of pages | 9 |
Journal | Hydrological Processes |
Volume | 29 |
Early online date | 17 Oct 2014 |
DOIs | |
Publication status | Published - 14 Apr 2015 |
Research Groups and Themes
- Water and Environmental Engineering
Keywords
- bias correction
- rainfall characteristic
- temporal distribution
- quantile mapping