A new statistical precipitation downscaling method with Bayesian model averaging: a case study in China
| LEADER | caa a22 4500 | ||
|---|---|---|---|
| 001 | 605472874 | ||
| 003 | CHVBK | ||
| 005 | 20210128100340.0 | ||
| 007 | cr unu---uuuuu | ||
| 008 | 210128e20151101xx s 000 0 eng | ||
| 024 | 7 | 0 | |a 10.1007/s00382-015-2491-7 |2 doi |
| 035 | |a (NATIONALLICENCE)springer-10.1007/s00382-015-2491-7 | ||
| 245 | 0 | 2 | |a A new statistical precipitation downscaling method with Bayesian model averaging: a case study in China |h [Elektronische Daten] |c [Xianliang Zhang, Xiaodong Yan] |
| 520 | 3 | |a A new statistical downscaling method was developed and applied to downscale monthly total precipitation from 583 stations in China. Generally, there are two steps involved in statistical downscaling: first, the predictors are selected (large-scale variables) and transformed; and second, a model between the predictors and the predictand (in this case, precipitation) is established. In the first step, a selection process of the predictor domain, called the optimum correlation method (OCM), was developed to transform the predictors. The transformed series obtained by the OCM showed much better correlation with the predictand than those obtained by the traditional transform method for the same predictor. Moreover, the method combining OCM and linear regression obtained better downscaling results than the traditional linear regression method, suggesting that the OCM could be used to improve the results of statistical downscaling. In the second step, Bayesian model averaging (BMA) was adopted as an alternative to linear regression. The method combining the OCM and BMA showed much better performance than the method combining the OCM and linear regression. Thus, BMA could be used as an alternative to linear regression in the second step of statistical downscaling. In conclusion, the downscaling method combining OCM and BMA produces more accurate results than the multiple linear regression method when used to statistically downscale large-scale variables. | |
| 540 | |a Springer-Verlag Berlin Heidelberg, 2015 | ||
| 690 | 7 | |a Statistical downscaling |2 nationallicence | |
| 690 | 7 | |a Bayesian model averaging |2 nationallicence | |
| 690 | 7 | |a Monthly precipitation |2 nationallicence | |
| 690 | 7 | |a Multiple linear regression method |2 nationallicence | |
| 700 | 1 | |a Zhang |D Xianliang |u College of Forestry, Shenyang Agriculture University, 110866, Shenyang, China |4 aut | |
| 700 | 1 | |a Yan |D Xiaodong |u State Key Laboratory of Earth Surface Processes and Resource Ecology, Beijing Normal University, 100087, Beijing, China |4 aut | |
| 773 | 0 | |t Climate Dynamics |d Springer Berlin Heidelberg |g 45/9-10(2015-11-01), 2541-2555 |x 0930-7575 |q 45:9-10<2541 |1 2015 |2 45 |o 382 | |
| 856 | 4 | 0 | |u https://doi.org/10.1007/s00382-015-2491-7 |q text/html |z Onlinezugriff via DOI |
| 898 | |a BK010053 |b XK010053 |c XK010000 | ||
| 900 | 7 | |a Metadata rights reserved |b Springer special CC-BY-NC licence |2 nationallicence | |
| 908 | |D 1 |a research-article |2 jats | ||
| 949 | |B NATIONALLICENCE |F NATIONALLICENCE |b NL-springer | ||
| 950 | |B NATIONALLICENCE |P 856 |E 40 |u https://doi.org/10.1007/s00382-015-2491-7 |q text/html |z Onlinezugriff via DOI | ||
| 950 | |B NATIONALLICENCE |P 700 |E 1- |a Zhang |D Xianliang |u College of Forestry, Shenyang Agriculture University, 110866, Shenyang, China |4 aut | ||
| 950 | |B NATIONALLICENCE |P 700 |E 1- |a Yan |D Xiaodong |u State Key Laboratory of Earth Surface Processes and Resource Ecology, Beijing Normal University, 100087, Beijing, China |4 aut | ||
| 950 | |B NATIONALLICENCE |P 773 |E 0- |t Climate Dynamics |d Springer Berlin Heidelberg |g 45/9-10(2015-11-01), 2541-2555 |x 0930-7575 |q 45:9-10<2541 |1 2015 |2 45 |o 382 | ||