Probabilistic Analysis of Extreme Discharges and Precipitations with a Nonparametric Copula Model
Affiliation
Univ Arizona, Dept Hydrol & Water ResourcesIssue Date
2018-07Keywords
nonparametric Copulaconditional probability
extreme precipitation
extreme discharge
Urumqi River
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MDPICitation
Liu Y, Liu Y, Hao Y, Wang T, Yeh T-CJ, Fan Y, Zhang Q. Probabilistic Analysis of Extreme Discharges and Precipitations with a Nonparametric Copula Model. Water. 2018; 10(7):823.Journal
WATERRights
© 2018 by the authors. Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license.Collection Information
This item from the UA Faculty Publications collection is made available by the University of Arizona with support from the University of Arizona Libraries. If you have questions, please contact us at repository@u.library.arizona.edu.Abstract
Urumqi River is an important river in the Xinjiang autonomous region, China, where floods or droughts are the major concerns of the local communities. This river's discharge is mainly influenced by the natural factors such as precipitation and climates, rather than human activities. This paper quantifies the interdependent structure between Urumqi River's discharge and precipitation using a nonparametric Copula method. It then analyzes the relationship between the extreme discharges of this river and extreme precipitation of the region. Comparison between simulation result and real data is conducted to verify the rationality of the model. Furthermore, the conditional probabilities of maximum and minimum discharge at different precipitation levels are also investigated using the Copula distribution functions. The results show a strong relationship between large discharge and heavy precipitation in this region. The upper dependence coefficient is nearly 0.6 and the probability of large discharge reaches 0.64 when the rainfall is greater than 159.56 mm. The relationship between small discharge and rainfall is insignificant. The lower dependence coefficient is zero, suggesting that the base flow and snowmelt from Tianshan likely contribute to Urumqi River's discharge during the dry season.Note
Open access journal.ISSN
2073-4441Version
Final published versionSponsors
National Natural Science Foundation of China [41471001, 41402210, 41272245, 11601244]; Scientific Research Foundation for Qingjiang Scholars of Jiangxi University of Science and Technology [JXUSTQJBJ2017002]; innovation team training plan of the Tianjin Education Committee [TD12-5037]; US National Science Foundation-Division of Earth Sciences [1014594]; Outstanding Oversea Professorship award through Jilin University from Department of Education, China; Global Expert award through Tianjin Normal University from the Thousand Talents Plan of Tianjin CityAdditional Links
http://www.mdpi.com/2073-4441/10/7/823ae974a485f413a2113503eed53cd6c53
10.3390/w10070823
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Except where otherwise noted, this item's license is described as © 2018 by the authors. Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license.

