scholarly journals DEVELOPMENT OF A STATISTICAL BIAS CORRECTION METHOD FOR DAILY PRECIPITATION DATA OF GCM20

Author(s):  
Hironori INOMATA ◽  
Kuniyoshi TAKEUCHI ◽  
Kazuhiko FUKAMI
Author(s):  
CHOTHANDA NYUNT ◽  
TOSHIO KOIKE ◽  
AKIO YAMAMOTO ◽  
TOSHIHORO NEMOTO ◽  
MASARU KITSUREGAWA

2010 ◽  
Vol 7 (5) ◽  
pp. 7863-7898 ◽  
Author(s):  
J. O. Haerter ◽  
S. Hagemann ◽  
C. Moseley ◽  
C. Piani

Abstract. It is well known that output from climate models cannot be used to force hydrological simulations without some form of preprocessing to remove the existing biases. In principle, statistical bias correction methodologies act on model output so the statistical properties of the corrected data match those of the observations. However the improvements to the statistical properties of the data are limited to the specific time scale of the fluctuations that are considered. For example, a statistical bias correction methodology for mean daily values might be detrimental to monthly statistics. Also, in applying bias corrections derived from present day to scenario simulations, an assumption is made of persistence of the bias over the largest timescales. We examine the effects of mixing fluctuations on different time scales and suggest an improved statistical methodology, referred to here as a cascade bias correction method, that eliminates, or greatly reduces, the negative effects.


2019 ◽  
Vol 694 ◽  
pp. 133680 ◽  
Author(s):  
Bahram Choubin ◽  
Shahram Khalighi-Sigaroodi ◽  
Ashok Mishra ◽  
Massoud Goodarzi ◽  
Shahaboddin Shamshirband ◽  
...  

Atmosphere ◽  
2020 ◽  
Vol 11 (1) ◽  
pp. 109
Author(s):  
Han Liu ◽  
Jie Chen ◽  
Xun-Chang Zhang ◽  
Chong-Yu Xu ◽  
Yu Hui

Bias correction methods are routinely used to correct climate model outputs for hydrological and agricultural impact studies. Even though superior bias correction methods can correct the distribution of daily precipitation amounts, as well as the wet-day frequency, they usually fail to correct the temporal sequence or structure of precipitation occurrence. To solve this problem, we presented a hybrid bias correction method for simulating the temporal sequence of daily precipitation occurrence. We did this by combining a first-order two-state Markov chain with a quantile-mapping (QM) based bias correction method. Specifically, a QM-based method was used to correct the distributional attributes of daily precipitation amounts and the wet-day frequency simulated by climate models. Then, the sequence of precipitation occurrence was simulated using the first-order two-state Markov chain with its parameters adjusted based on linear relationships between QM-corrected mean monthly precipitation and the transition probabilities of precipitation occurrence. The proposed Markov chain-based bias correction (MCBC) method was compared with the QM-based method with respect to reproducing the temporal structure of precipitation occurrence over 10 meteorological stations across China. The results showed that the QM-based method was unable to correct the temporal sequence, with the cumulative frequency of wet- and dry-spell length being considerably underestimated for most stations. The MCBC method can could reproduce the temporal sequence of precipitation occurrence, with the generated cumulative frequency of wet- and dry-spell lengths fitting that of the observation well. The proposed method also performed reasonably well with respect to reproducing the mean, standard deviation, and the longest length of observed wet- and dry-spells. Overall, the MCBC method can simulate the temporal sequence of precipitation occurrence, along with correcting the distributional attributes of precipitation amounts. This method can be used with crop and hydrological models in climate change impact studies at the field and small watershed scales.


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