[go: up one dir, main page]

Skip to main content
Log in

The relationship between ENSO cycle and high and low-flow in the upper Yellow River

  • Natural Resources and Environmental Change
  • Published:
Journal of Geographical Sciences Aims and scope Submit manuscript

Abstract

Firstly, the hydrological and meteorological features of the upper reaches of the Yellow River above Tangnag are analyzed based on observation data, and effects of EI Nino and La Nina events on the high and low flow in the upper Yellow River are discussed. The results show El Nino and La Nina events possess consanguineous relationship with runoff in the upper Yellow River. As a whole, the probability of low flow occurrence in the upper Yellow River is relatively great along with the occurrence of El Nino event. Moreover, the flood in the upper Yellow River occurs frequently with the occurrence of La Nina event. Besides, the results also show dissimilarity of El Nino event occurring time exerts greater impact on high flow and low flow in the upper Yellow River, that is, the probability of drought will be greater in the same year if El Nino event occurs in spring, the high-flow may happen in this year if El Nino occurs in summer or autumn; the longer the continuous period of El Nino is, the lower the runoff in the upper Yellow River is.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Subscribe and save

Springer+ Basic
$34.99 /Month
  • Get 10 units per month
  • Download Article/Chapter or eBook
  • 1 Unit = 1 Article or 1 Chapter
  • Cancel anytime
Subscribe now

Buy Now

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Similar content being viewed by others

References

  • Dong Jie, Liu Limin, 2000. The relationship of temperature and precipitation in China and the ocean temperature in the Equatorial East Pacific.Journal of Climate, 26(2): 25–28.

    Google Scholar 

  • Glantz M H, Katz R W, Nicholls N, 1991. Teleconnections Linking Worldwide Climate Anomalies: Scientific Basis and Social Impact. Cambridge, UK: Cambridge University.

    Google Scholar 

  • Jones P D, 1988. The influence of ENSO on global temperatures.Climate Monitor, 17(3): 80–89.

    Google Scholar 

  • Kiem A S, Franks S W, 2001. On the identification of ENSO-induced rainfall and runoff variability: a comparison of methods and indices.Hydrological Sciences-Journal, 46(5): 715–727.

    Article  Google Scholar 

  • Kiladis G N, Diaz H, 1989. Global climatic anomalies associated with extremes in the Southern Oscillation.Journal of Climate, 1069–1090.

  • Lan Yongchao, 2002. relationship between ENSO cycle and abundant or low runoff in the upper Yellow River.Journal of Desert Research, 22(3): 262–266. (in Chinese)

    Google Scholar 

  • Lan Yongchao, 1998. Runoff of upper Yellow River above Tangnag: characteristics evolution and changing trend.Advance in Earth Science, 13(Suppl.): 112–120. (in Chinese)

    Google Scholar 

  • Li Dongliang, Zhao Qingyun, 2000. A study on spring rainfall anomaly in Northwest China and Pacific SSTA features in autumn and their correlations.Plateau Meteorology, 19(1): 100–110. (in Chinese)

    Google Scholar 

  • Li Dongliang, Yao Hui, 1991. The relationship between El Nino phenomena (1470–1979) and dryness and wetness of China.Arid Land Geography, 14(2): 48–52. (in Chinese)

    Google Scholar 

  • Luo Gaoyuan, 2000. A general survey of the studies on El Nino and La Nina in China.Scientia Geographica Sinica, 20(3): 264–270. (in Chinese)

    Google Scholar 

  • Ma Quanjie, Ma Jianhua, 2000. Responses of runoff in the Yellow River above Lanzhou to El Nino Phenomenon.Yellow Riwer, 22(5): 18–20. (in Chinese)

    Google Scholar 

  • Ropelewski, Halpert M S, 1987. Global and regional scale precipitation-patterns associated with the El Nino/Southern Oscillation.Mon. Weather. Rev., 15: 1606–1626.

    Article  Google Scholar 

  • Ropelewski, Halpert M S, 1989. Precipitation patterns associated with the high index phase of the Southern Oscillation.Journal of Climate, 2: 268–284.

    Article  Google Scholar 

  • Ropelewski, Halpert M S, 1996. Quantifying Southern Oscillation-precipitation relationships.Journal of Climate, 2(5): 1043–1059.

    Article  Google Scholar 

  • Wang Shaowu, Gong Daoyi, 1999. ENSO events and their intensity since about 100 years.Acta Meteorologica Sinica, 25(1): 9–13. (in Chinese)

    Google Scholar 

  • Zhang Zhibing, 1999. El Nino event and prediction of large-scale, extra long-range biology disasters.Sciences Journal, 46(2): 34–36. (in Chinese)

    Google Scholar 

  • Zhu Qiangen, Teng Ying, Xu Guoqiang, 2000. The possible mechanism of the effects of SSTA in North Pacific on East China summer rainfall.Journal of Nanjing Institute of Meteorology, 23 (1): 1–8. (in Chinese)

    Google Scholar 

  • Zhu Binyuan, Li Dongliang, 1989. The relation between ENSO phenomena and summery precipitation of Gansu province.Plateau Meteorology, 8(1): 64–69. (in Chinese)

    Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Lan Yongchao.

Additional information

Foundation item: Knowledge Innovation Project of Cold and Arid Regions Environmental and Engineering Research Institute of CAS, No.210100, No.210016; Knowledge Innovation Project of CAS, No.KZCX1-10-03; National Natural Science Foundation of China, No.49731030

Author: Lan Yongchao (1957–), Associate Professor, specialized in water resources and hydrology in Northwest China.

Rights and permissions

Reprints and permissions

About this article

Cite this article

Lan, Y., Ding, Y., Kang, E. et al. The relationship between ENSO cycle and high and low-flow in the upper Yellow River. J. Geogr. Sci. 13, 105–111 (2003). https://doi.org/10.1007/BF02873153

Download citation

  • Received:

  • Accepted:

  • Issue Date:

  • DOI: https://doi.org/10.1007/BF02873153

Key words

CLC number

Navigation