期刊
JOURNAL OF HYDROLOGY
卷 394, 期 3-4, 页码 447-457出版社
ELSEVIER
DOI: 10.1016/j.jhydrol.2010.09.018
关键词
Rainfall-runoff modelling; Climate non stationary; Climate chang; Model calibration; Runoff estimation
资金
- eWater CRC Catchment Water Yield Estimation Tool (CWYET)
- South Eastern Australian Climate Initiative (SEACI)
This paper presents results from a modelling study carried out to investigate whether the calibrated parameter values for rainfall-runoff models based on historical observed data can be used to reliably predict runoff responses to changes in future climate inputs The modelling experiments are carried out for four rainfall-runoff models using long records of historical daily climate and streamflow data from 61 catchments in southeast Australia The results indicate that the models when calibrated using more than 20 years of data can generally be used for climate Impact studies where the future mean annual rainfall is not more than 15% drier or 20% wetter than the mean annual rainfall in the model calibration period It is generally more difficult for a model calibrated over a wet period to predict runoff over a dry period compared to a model calibrated over a dry period to predict runoff over a wet period For southeast Australia there is a good reason to use the recent records to calibrate rainfall-runoff models to represent the current prolonged drought over the region and for climate change impact studies where the large majority of climate models predict a drier future across this region (C) 2010 Elsevier B V All rights reserved
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