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Information Journal Paper

Title

REGIONAL ESTIMATION OF LOW FLOWS FOR MAZANDARAN RIVER BASIN

Pages

  38-38

Abstract

 An approach for regional LOW FLOW frequency ANALYSIS is to use MULTIPLE REGRESSION techniques for obtaining relationships between LOW FLOWs with specific return periods and catchments characteristics. In this paper, this method has been used. After single-site frequency ANALYSIS for 20 stream gauging stations, homogeneity test was performed. Regional relationships between LOW FLOWs with return periods 2 , 5 , 10, and 20 years and catchments characteristics were derived. For this purpose, catchment area, mean elevation, minimum elevation, shape factor, main channel length, length of main channel from catchment centroid to outlet, forest area, mean annual rainfall, and mean catchment slope as model inputs were examined and catchment area, mean elevation, and mean catchment slope entered to the models. Finally, the mean relative error of models for different return period, 2, 5, 10, and 20 years, was computed 41.1, 41.3, 45.0, 47.2 percent, respectively that in comparison with other studies, it displays smaller errors.

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  • Cite

    APA: Copy

    ESLAMIAN, S.S., ZAREI, A., & ABRISHAMCHI, A.. (2004). REGIONAL ESTIMATION OF LOW FLOWS FOR MAZANDARAN RIVER BASIN. WATER AND SOIL SCIENCE (JOURNAL OF SCIENCE AND TECHNOLOGY OF AGRICULTURE AND NATURAL RESOURCES), 8(1), 38-38. SID. https://sid.ir/paper/14610/en

    Vancouver: Copy

    ESLAMIAN S.S., ZAREI A., ABRISHAMCHI A.. REGIONAL ESTIMATION OF LOW FLOWS FOR MAZANDARAN RIVER BASIN. WATER AND SOIL SCIENCE (JOURNAL OF SCIENCE AND TECHNOLOGY OF AGRICULTURE AND NATURAL RESOURCES)[Internet]. 2004;8(1):38-38. Available from: https://sid.ir/paper/14610/en

    IEEE: Copy

    S.S. ESLAMIAN, A. ZAREI, and A. ABRISHAMCHI, “REGIONAL ESTIMATION OF LOW FLOWS FOR MAZANDARAN RIVER BASIN,” WATER AND SOIL SCIENCE (JOURNAL OF SCIENCE AND TECHNOLOGY OF AGRICULTURE AND NATURAL RESOURCES), vol. 8, no. 1, pp. 38–38, 2004, [Online]. Available: https://sid.ir/paper/14610/en

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