Determination of Trends and Dominant Modes in 7-Day Annual Minimum Flows: Additive Wavelet Transform-Based Approach

被引:9
作者
Tosunoglu, Fatih [1 ]
Kaplan, Nur Huseyin [2 ]
机构
[1] Erzurum Tech Univ, Dept Civil Engn, TR-25200 Erzurum, Turkey
[2] Erzurum Tech Univ, Dept Elect & Elect Engn, TR-25200 Erzurum, Turkey
关键词
7-day annual minimum flows; Mann-Kendall trend test; Sequential Mann-Kendall trend test; Additive wavelet transform; Euphrates and Coruh Basins; MANN-KENDALL; RIVER-BASIN; CORUH BASIN; FREQUENCY-ANALYSIS; STREAMFLOW TRENDS; CASPIAN PATTERN; DETECT TREND; IMAGE FUSION; CHANGE-POINT; NORTH-SEA;
D O I
10.1061/(ASCE)HE.1943-5584.0001710
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
The main purpose of this study is to define the most effective periodic components (modes) that produce the trends in 7-day annual minimum flows (AM7) in two important river basins in Turkey, namely, Euphrates and Coruh. To achieve this aim, additive wavelet transform (AWT) in conjunction with the Mann-Kendall (MK) and the sequential MK tests is applied for the first time. According to the MK test, significant decreasing trends were detected for the AM7 series of the stations located in the middle and lower parts of the Euphrates Basin and in the upper part of the Coruh Basin. Moreover, the MK test showed significant increasing trends for the AM7 series at the stations located in upper part of the Euphrates Basin. No significant trend was detected for the AM7 series of the stations in the lower and middle parts of the Coruh Basin. Moreover, the sequential MK test applied to the AM7 series showed that the detected decreasing trends become significant after 1988, whereas the increasing trends become significant after 2007, and these significant trends continue during the present time. Then, by using AWT, the original AM7 series at each station were decomposed into their approximation and wavelet subbands, representing 2, 4, 8, and 16 yearly time series. Furthermore, by using AWT coupled with the MK and sequential MK tests, it was found that the 2- and 4-year periodic components are the most dominant modes that produce trends in the original data series of the Euphrates and Coruh Basins, respectively. The results demonstrated that the AWT-based trend approach can be successively applied for defining the dominant modes in the AM7 series and effectively used in any hydroclimatic time series cases. (C) 2018 American Society of Civil Engineers.
引用
收藏
页数:13
相关论文
共 66 条
[1]   Development of a new method of wavelet aided trend detection and estimation [J].
Adamowski, Kaz ;
Prokoph, Andreas ;
Adamowski, Jan .
HYDROLOGICAL PROCESSES, 2009, 23 (18) :2686-2696
[2]  
AHN KH, 2016, J HYDROL ENG, V21, DOI DOI 10.1061/(ASCE)HE.1943-5584.0001286
[3]  
[Anonymous], 1975, J. Econ
[4]   Using wavelet transforms to estimate surface temperature trends and dominant periodicities in Iran based on gridded reanalysis data [J].
Araghi, A. ;
Baygi, M. Mousavi ;
Adamowski, J. ;
Malard, J. ;
Nalley, D. ;
Hasheminia, S. M. .
ATMOSPHERIC RESEARCH, 2015, 155 :52-72
[5]   LONG-TERM TRENDS IN STREAMFLOW AND PRECIPITATION IN NORTHWEST CALIFORNIA AND SOUTHWEST OREGON, 1953-2012 [J].
Asarian, J. Eli ;
Walker, Jeffrey D. .
JOURNAL OF THE AMERICAN WATER RESOURCES ASSOCIATION, 2016, 52 (01) :241-261
[6]   Regional flood frequency analysis for Coruh Basin of Turkey with L-moments approach [J].
Aydogan, D. ;
Kankal, M. ;
Onsoy, H. .
JOURNAL OF FLOOD RISK MANAGEMENT, 2016, 9 (01) :69-86
[7]   Probabilities and return periods of multisite droughts [J].
Bayazit, M ;
Önöz, B .
HYDROLOGICAL SCIENCES JOURNAL-JOURNAL DES SCIENCES HYDROLOGIQUES, 2005, 50 (04) :605-615
[8]   Seasonal trends in Romanian streamflow [J].
Birsan, Marius-Victor ;
Zaharia, Liliana ;
Chendes, Viorel ;
Branescu, Emilia .
HYDROLOGICAL PROCESSES, 2014, 28 (15) :4496-4505
[9]   Detection of hydrologic trends and variability [J].
Burn, DH ;
Elnur, MAH .
JOURNAL OF HYDROLOGY, 2002, 255 (1-4) :107-122
[10]   Estimating T-year flood confidence intervals of rivers in Coruh basin, Turkey [J].
Can, I. ;
Tosunoglu, F. .
JOURNAL OF FLOOD RISK MANAGEMENT, 2013, 6 (03) :186-196