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Construction of precipitation index based on ensemble forecast and heavy precipitation forecast in the Hanjiang River Basin, China

dc.contributor.authorJin, Haoyu
dc.contributor.authorChen, Xiaohong
dc.contributor.authorZhong, Ruida
dc.contributor.authorLiu, Moyang
dc.contributor.authorYe, Changxin
dc.date.accessioned2024-08-21T05:59:49Z
dc.date.available2024-08-21T05:59:49Z
dc.date.issued2023
dc.date.updated2024-05-12T08:15:34Z
dc.descriptionThis research is financially supported by National Key Research and Development Program of China (2021YFC3001000), National Natural Science Foundation of China (Grant No. U1911204, 51861125203).
dc.description.abstractUncertainty about the occurrence of extreme precipitation events has increased significantly under global climate change. The Hanjiang River Basin (HRB) is located at the junction of the north and the south of China, and extreme precipitation events occur frequently due to the impact of climate change. Extreme precipitation is the leading factor causing flood disasters in the HRB, and effective forecasting of extreme precipitation is of great significance for preventing flood disasters. In this study, we take full advantage of the uncertainty information in THORPEX Interactive Grand Global Ensemble (TIGGE) ensemble forecasts datasets and perform statistical postprocessing through the Bayesian model averaging (BMA) method. Then, the extreme precipitation index (EPI) is constructed using the cumulative distribution functions (CDFs) of historical model precipitation and the forecast precipitation. The research results show that the constructed EPI index can well reflect the occurrence intensity of precipitation in the HRB. According to the Spearman correlation coefficient, the CMA model has the best effect, followed by the control forecast (CF) model, and the JMA model has the worst effect. As indicated by the area under curve (AUC) indicator at the 25 mm precipitation threshold, the forecast effect of CMA model is still the best, followed by the CF model, and the third is the control forecast and perturbed forecast (CFPF) model. The comprehensive effect of the JMA model is significantly worse than other models. Under the precipitation threshold of 50 mm, the prediction effect of the NCEP model is the best, followed by the ECMWF model, and the third is the CF model. The least effective is also the JMA model, followed by the UKMO model. Under the precipitation threshold of 25 mm, the prediction effect of all models is better than that of the precipitation threshold of 50 mm. The prediction stability of NCEP and ECMWF models is the strongest, and the effects of CF and CFPF models integrating multiple models are in the middle. This study provides an important reference for the theory and application of extreme precipitation forecasting in the HRB.
dc.format.mimetypeapplication/pdfen_AU
dc.identifier.issn0169-8095
dc.identifier.urihttps://hdl.handle.net/1885/733715067
dc.language.isoen_AUen_AU
dc.publisherElsevier BV
dc.rights© 2023 Elsevier B.V.
dc.sourceAtmospheric Research
dc.subjectExtreme precipitation
dc.subjectPrecipitation forecasting
dc.subjectTIGGE
dc.subjectBMA
dc.subjectThe Hanjiang River Basin
dc.titleConstruction of precipitation index based on ensemble forecast and heavy precipitation forecast in the Hanjiang River Basin, China
dc.typeJournal article
local.bibliographicCitation.lastpage14
local.bibliographicCitation.startpage1
local.contributor.affiliationJin, Haoyu, School of Civil Engineering, Sun Yat-sen University
local.contributor.affiliationChen, Xiaohong, School of Civil Engineering, Sun Yat-sen University
local.contributor.affiliationZhong, Ruida, School of Civil Engineering, Sun Yat-sen University
local.contributor.affiliationLiu, Moyang, College of Science, ANU
local.contributor.affiliationYe, Changxin, School of Civil Engineering, Sun Yat-Sen University
local.contributor.authoruidLiu, Moyang, u7093228
local.description.embargo2099-12-31
local.description.notesImported from ARIES
local.identifier.absfor370202 - Climatology
local.identifier.absfor370704 - Surface water hydrology
local.identifier.absfor370903 - Natural hazards
local.identifier.absseo180103 - Atmospheric processes and dynamics
local.identifier.absseo180104 - Weather
local.identifier.absseo190400 - Natural hazards
local.identifier.ariespublicationa383154xPUB40672
local.identifier.citationvolume287
local.identifier.doi10.1016/j.atmosres.2023.106701
local.identifier.scopusID2-s2.0-85150028624
local.publisher.urlhttps://www.sciencedirect.com/
local.type.statusPublished Version
publicationvolume.volumeNumber287

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