Comparison of the SCS-CN and Hydrograph Separation Method for Runoff Estimation in an Ungauged Basin: The Izmit Basin, Turkey

Meral Erdoğan Topçuoğlu, Remzi Karagüzel, Ahmet Doğan3=
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Abstract

The separation of surface runoff and base flow is a very specific problem in water balance calculations, particularly if there is not enough measured flow data. In this study, the SCS-CN method is used to estimate the surface runoff in the ungauged Izmit Basin. The CNs are estimated using the Hydrologic Soil Groups map, based on soil data of the General Directorate of Rural Services of Turkey and land use obtained from the CORINE-2006 database for different AMCs. The surface runoff was computed using the SCS-CN method for the ungauged Izmit Basin that corresponds to 17% and 21% of the rainfall, i.e. 134 mm (for Kocaeli Meteorological Station; rainfall=804 mm) and 171 mm (for Sakarya Meteorological Station; rainfall=820 mm). According to SCS-CN method estimates, approximately 41-42% of the annual rainfall in the Izmit Basin directly contributes to the total streamflow, and 21-25% of it contributes to base flow and unmeasured infiltration. To compare the results of the SCS-CN method along with hydrograph separation method, the gauged Yuvacık Dam Sub-Basin, which is hydro-meteorologically similar to the Izmit Basin, was selected. The results showed that 16% of the rainfall in the Yuvacık Dam Sub-Basin became surface runoff. Also, it was found that about 42% of the annual rainfall in the Yuvacık Dam Sub-Basin directly contributes to the total streamflow and 23% of it contributes to the base flow and unmeasured infiltration. These results confirm that the ratio of surface runoff obtained by the hydrograph separation method in the Yuvacık Dam Sub-Basin matches with the ratio of surface runoff calculated using the SCS-CN method for the entire Izmit Basin.
未测量流域径流估算的SCS-CN与水文分离方法的比较:土耳其伊兹米特盆地
地表径流和基流的分离是水平衡计算中的一个非常具体的问题,特别是在没有足够的实测流量数据的情况下。在本研究中,采用SCS-CN方法估算了未测量的伊兹米特盆地的地表径流。CNs是根据土耳其农村服务总局的土壤数据和从CORINE-2006数据库获得的不同AMCs的土地利用情况,利用水文土壤组图估算的。使用SCS-CN方法计算了未测量的Izmit盆地的地表径流,对应于降雨量的17%和21%,即134 mm(对于Kocaeli气象站;雨量=804毫米)和171毫米(Sakarya气象站);降雨= 820毫米)。根据SCS-CN方法估算,伊兹米特流域年降雨量中约41-42%直接贡献了总流量,21-25%贡献了基流和未测入渗。为了比较SCS-CN方法和水文线分离方法的结果,选择了与伊兹米特盆地水文气象相似的Yuvacık坝子流域。结果表明:Yuvacık坝子流域16%的降水转化为地表径流;此外,Yuvacık坝次流域年降雨量中约42%直接贡献了总流量,23%贡献了基流和未测入渗。这些结果证实了Yuvacık坝子流域用水文线分离法得到的地表径流量比值与用SCS-CN方法计算的整个Izmit流域的地表径流量比值吻合。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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