Babak VaheddoostMir Jafar Sadegh SafariMustafa Utku YilmazVaheddoost, BabakYilmaz, Mustafa UtkuSafari, Mir Jafar Sadegh2025-10-06202300334553, 142091360033-45531420-913610.1007/s00024-022-03209-32-s2.0-85145553468https://www.scopus.com/inward/record.uri?eid=2-s2.0-85145553468&doi=10.1007%2Fs00024-022-03209-3&partnerID=40&md5=a0fb033e861f4cb190bb5e84c7b0e29ehttps://gcris.yasar.edu.tr/handle/123456789/8589https://doi.org/10.1007/s00024-022-03209-3For various reasons it is not always possible to obtain adequate and reliable long-term streamflow records in a river basin. It is known that streamflow records are even shorter when the stations located on tributary channels are of the interest. Hence it is necessary to develop dependable streamflow estimation models for the tributary streams that play a key role in the micro-hydrology of the basin. In this study rainfall-runoff models are developed to estimate the daily streamflow in ungauged tributary streams. Precipitation and streamflow in the most similar gauging station on the main channel and lagged values up to three days before on the same tributary station are used as the input variables of the allocated models. To select the most similar gauging station a similarity index criterion is developed and used in the analysis. Then two scenarios based on the streamflow or the corresponding set of direct runoff and base-flow in the same station are used. By applying multivariate adaptive regression spline (MARS) and random forest (RF) methods several rainfall-runoff models are developed and evaluated based on determination coefficient mean absolute percentage error root mean square error relative peak flow scatter plot and time series plot. Alternatively the MARS and RF models are combined with a drainage area ratio (DAR) model to produce the DAR-MARS and DAR-RF models. It is concluded that the direct runoff in the mainstream is more effective on the streamflow of the tributary station while the integration of models with DAR enhanced the capabilities of the models in estimation of extreme values in the streamflow time series. © 2023 Elsevier B.V. All rights reserved.Englishinfo:eu-repo/semantics/closedAccessBase-flow Separation, Coruh River, Drainage Area Ratio, Similarity Index, Turkey, Ungauged Basin, Catchments, Flow Separation, Forestry, Mean Square Error, Rain, Rivers, Runoff, Stream Flow, Area Ratios, Base Flow Separation, Coruh River, Drainage Area, Drainage Area Ratio, Multivariate Adaptive Regression Splines, Similarity Indices, Turkey, Ungaged, Ungaged Basins, Time Series, Baseflow, Drainage, Peak Flow, Rainfall-runoff Modeling, Regression Analysis, Streamflow, Tributary, Coruh RiverCatchments, Flow separation, Forestry, Mean square error, Rain, Rivers, Runoff, Stream flow, Area ratios, Base flow separation, Coruh river, Drainage area, Drainage area ratio, Multivariate adaptive regression splines, Similarity indices, Turkey, Ungaged, Ungaged basins, Time series, baseflow, drainage, peak flow, rainfall-runoff modeling, regression analysis, streamflow, tributary, Coruh RiverCoruh RiverDrainage Area RatioBase-Flow SeparationSimilarity IndexUngauged BasinTurkeyArticle