

FOLLOWUS
1. Key Laboratory of Submarine Geosciences and Technology of Ministry of Education Ocean University of China
2. Key Laboratory of Marine Hydrocarbon Resources and Environment Geology China Geological Survey Ministry of Land and Resources
3. Qingdao Institute of Marine Geology China Geological Survey
网络首发:2014-07-18,
纸质出版:2014
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Water discharge variability of Changjiang (Yangtze) and Huanghe (Yellow) Rivers and its response to climatic changes[J]. 海洋湖沼学报(英文), 2014,32(6):1392-1405.
Zhang, X., Fan, D., Wang, H. et al. Water discharge variability of Changjiang (Yangtze) and Huanghe (Yellow) Rivers and its response to climatic changes., Chin. J. Ocean. Limnol. 32, 1392–1405 (2014). https://doi.org/10.1007/s00343-015-4034-9
Water discharge variability of Changjiang (Yangtze) and Huanghe (Yellow) Rivers and its response to climatic changes[J]. 海洋湖沼学报(英文), 2014,32(6):1392-1405. DOI: 10.1007/s00343-015-4034-9.
Zhang, X., Fan, D., Wang, H. et al. Water discharge variability of Changjiang (Yangtze) and Huanghe (Yellow) Rivers and its response to climatic changes., Chin. J. Ocean. Limnol. 32, 1392–1405 (2014). https://doi.org/10.1007/s00343-015-4034-9 DOI:
Infl uences of large-scale climatic phenomena
such as the El Niño/La Niña-Southern Oscillation (ENSO) and the Pacific Decadal Oscillation (PDO)
on the temporal variations of the annual water discharge at the Lijin station in the Huanghe (Yellow) River and at the Datong station in the Changjiang (Yangtze) River were examined. Using the empirical mode decomposition-maximum entropy spectral analysis (EMDMESA) method
the 2- to 3-year
8- to 14-year
and 23-year cyclical variations of the annual water discharge at the two stations were discovered. Based on the analysis results
the hydrological time series on the interannual to interdecadal scales were constructed. The results indicate that from 1950 to 2011
a significant downward trend occurred in the natural annual water discharge in Huanghe River. However
the changes in water discharge in Changjiang River basin exhibited a slightly upward trend. It indicated that the changes in the river discharge in the Huanghe basin were driven primarily by precipitation. Other factors
such as the precipitation over the Changjiang River tributaries
ice melt and evaporation contributed much more to the increase in the Changjiang River basin. Especially
the impacts of the inter-annual and inter-decadal climate oscillations such as ENSO and PDO could change the long-term patterns of precipitation over the basins of the two major rivers. Generally
low amounts of basin-wide precipitation on interannual to interdecadal scales over the two rivers corresponded to most of the warm ENSO events and the warm phases of the PDO
and vice versa. The positive phases of the PDO and ENSO could lead to reduced precipitation and consequently affect the long-term scale water discharges at the two rivers.
Chen X Q, Zhang E F, Xu J G. 2002. Large and episodic decrease of water discharge from the Yangtze River to the sea during the dry season. Hydrolog. Sci. J., 47(1): 41–48.
Depetris P J, Kempe S, Latif M, Mook W G. 1996. ENSO controlled flooding in the Parana’s river 1904–1991. Nature, 83(3): 127–129.
Déry S J, Wood E F. 2005. Decreasing river discharge in northern Canada. Geophys. Res. Lett., 32(10): L10401.
Eltahir E A B. 1996. El Niño and the natural variability in the flow of the Nile River. Water Resour. Res., 32(1): 131–137.
Ge Z X, Cao K, Song Y L. 2010. Influence of climatic change in Jianghuai region on runoff of Yangtze River Estuary. Water Resour and Pow., 2: 1–3. (in Chinese with English abstract)
Gordon A L, Giulivi C F. 2004. Pacific decadal oscillation and sea level in the Japan/East Sea. Deep — Sea Res. I: Oceanographic Research Papers, 51(5): 653–663.
Huang N E, Shen Z, Long S R, Wu M C, Shih H H, Zheng Q N, Yen NC, Tung C C, Liu H H. 1998. The empirical mode decomposition and the Hilbert spectrum for nonlinear and non-stationary time series analysis. Proceedings of the Royal Society of London. Series A: Mathematical, Physical and Engineering Sciences, 454(1971): 903–995.
Huang N E, Wu Z. 2008. A review on Hilbert-Huang transform: method and its applications to geophysical studies. Rev. Geophys., 46(2): RG2006.
Huntington T G. 2006. Evidence for intensification of the global water cycle: review and synthesis. J. Hydrol., 319(1–4): 83–95.
Labat D, Ronchail J, Callède J, Guyot J L, Oliveira E D, Guimaràes W. 2004. Wavelet analysis of Amazon hydrological regime variability. Geophys. Res. Lett., 31: L02501.
Labat D. 2006. Oscillations in land surface hydrological cycle. Earth. Planet. Sc. Lett., 242(1–2): 143–154.
Labat D. 2008. Wavelet analysis of the annual discharge records of the world’s largest rivers. Adv. Water Resou., 31: 109–117.
Liu J P, Xu K H, Li A C, Milliman J D, Velozzi D M, Xiao S B, Yang Z S. 2007. Flux and fate of Yangtze River sediment delivered to the East China Sea. Geomorphology, 85(3): 208–224.
Liu Y Q, Ding Y H. 1995. Reappraisal of the influence of ENSO events on seasonal precipitation and temperature in China. Sci. Atmos. Sin., 19(2): 200–208.
Lu X X. 2004. Vulnerability of water discharge of large Chinese rivers to environmental changes: an overview. Reg. Environ. Change., 4(4): 182–191.
Mann M E, Park J, Bradley R S. 1995. Global interdecadal and century-scale climate oscillations during the past five centuries. Nature, 378(6554): 266–270.
Milliman J D, Syvitski J P M. 1992. Geomorphic/tectonic control of sediment discharge to the ocean: the importance of small mountainous rivers. J. Geol., 100: 525–544.
Nilsson C, Reidy C A, Dynesius M, Revenga C. 2005. Fragmentation and flow regulation of the world’s large river systems. Science, 308(5720): 405–408.
Sang Y F, Wang D, Wu J C, Zhu Q P, Wang L. 2009. The relation between periods’ identification and noises in hydrologic series data. J. Hydrol., 368(1): 165–177.
Sang Y F, Wang Z, Liu C. 2012. Period identification in hydrologic time series using empirical mode decomposition and maximum entropy spectral analysis. J. Hydrol., 424: 154–164.
Seager R, Kushnir Y, Naik N H, Cane M A, Miller J. 2001. Wind-driven shifts in the latitude of the Kuroshio-Oyashio extension and generation of SST anomalies on decadal timescales. J. Climate, 14(22): 4 249–4 265.
Sheffield J, Wood E F, Roderick M L. 2012. Little change in global drought over the past 60 years. Nature, 491(7424): 435–438.
Simpson H J, Cane M A, Lin S K, Zebiak S E, Herczeg A L. 1993. Forecasting annual discharge of River Murray, Australia, from a geophysical model of ENSO. J. Climate, 6(2): 386–390.
Vörösmarty C J, Green P, Salisbury J, Lammers R B. 2000. Global water resources: vulnerability from climate change and population growth. Science, 289(5477): 284–288.
Wang H J, Saito Yoshiki, Zhang Y, Bi N S, Sun X X, Yang Z S. 2011. Recent changes of sediment flux to the western Pacific ocean from major rivers in east and southeast Asia. Earth Sci. Rev., 108(1): 80–100.
Wang H J, Yang Z S, Saito Yoshiki, Liu J P, Sun X X, Wang Y. 2007. Stepwise decreases of the Huanghe (Yellow River) sediment load (1950–2005): impacts of climate change and human activities. Global Planet Change, 57(3): 331–354.
Wang H J, Yang Z S, Saito Yoshiki, Liu J P, Sun X X. 2006. Interannual and seasonal variation of the Huanghe (Yellow River) water discharge over the past 50 years: connections to impacts from ENSO events and dams. Global Planet Change, 50(3–4): 212–225.
Wang L, Chen W, Huang R H. 2008. Interdecadal modulation of PDO on the impact of ENSO on the East Asian winter monsoon. J. Geophys. Res., 35(20): L20702.
Wang Y, Ding Y, Ye B, Liu F, Wang J. 2013. Contributions of climate and human activities to changes in runoff of the Yellow and Yangtze rivers from 1950 to 2008. Sci. China — Earth Sci., 56(8): 1 398–1 412.
Wu B, Zhou T, Li T. 2009. Seasonally evolving dominant interannual variability modes of East Asian climate. J. Climate, 22(11): 2 992–3 005.
Wu Z, Huang N E. 2004. A study of the characteristics of white noise using the empirical mode decomposition method. Proceedings of the Royal Society of London. Series A: Mathematical, Physical and Engineering Sciences, 460(2046): 1 597–1 611.
Xu J X. 2005. The water fluxes of the Yellow River to the sea in the past 50 years, in response to climate change and human activities. Environ. Mange., 35(5): 620–631.
Xu K H, Milliman J D, Yang Z S, Xu H. 2007. Climatic and anthropogenic impacts on the water and sediment discharge from the Yangtze River (Changjiang), 1950–2005. Large Rivers: Geomorphology and Management. p.609–626.
Xue F, Liu C. 2008. The influence of moderate ENSO on summer rainfall in eastern China and its comparison with strong ENSO. Chinese Sci. Bull., 53(5): 791–800.
Yang S L, Gao A, Hotz H M, Zhu J, Dai S B, Li M. 2005. Trends in annual discharge from the Yangtze River to the sea (1865–2004). Hydrolog. Sci. J., 50(5): 825–836.
Yang S L, Liu Z, Dai S B, Gao Z X, Zhang J, Wang H J, Luo X X, Wu C S, Zhang Z. 2010. Temporal variations in water resources in the Yangtze river (Changjiang) over the industrial period based on reconstruction of missing monthly discharge. Water Resour. Res., 46(100): W10516.
Yang Z S, Wang H, Saito Y, Milliman J D, Xu K, Qiao S, Shi G. 2006. Dam impacts on the Changjiang (Yangtze) river sediment load to the sea: the past 55 years and after the Three Gorges dam. Water Resour. Res., 42(4): W04407.
Zhang Q, Jiang T, Gemmer M, Becker S. 2005. Precipitation, temperature and runoff analysis from 1950 to 2002 in the Yangtze basin, China. Hydrolog. Sci. J., 50(1).
Zhang Q, Xu C Y, Becker S, Jiang T. 2006. Sediment and runoff changes in the Yangtze River basin during past 50 years. J. Hydrol., 331(3): 511–523.
Zhang Y, Liu S Y, Xu J L, Shangguan D H. 2008. Glacier change and glacier runoff variation in the Tuotuo River basin, the source region of Yangtze River in western China. Environ. Geol., 56(1): 59–68.
Zhang Y, Wallace J M, Battisti D S. 1997. ENSO-like interdecadal variability: 1900–93. J. Climate, 10(5): 1 004–1 020.
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