| dc.identifier.citation | [1] K. Paik, D. Jung and J. H. Kim, Flow Variability and Channel Geometry of The Seomjin River, in Kusuda T. (Eds) Preprints of The Fifth APHW Conference“Hydrological Regime and Water Resources in the Context of Climate Change”, Vietnam,November 8 – November 10, pp. 79-95. 2010. [2] J. D. Allan, Stream Ecology: Structure and function of running waters. Chapman & Hall, New York, USA. 1995. [3] Google Earth software, 2010. [4] A. Crosato. Analysis and modelling of river meandering. IOS Press, Netherland, 2008. [5] Rosgen Stream Classification (2004), www.RosgenStreamClassification.pdf [6] Leopold, et al, Fluvial processes in geomorphology. W. H. Freeman & Company, San Francisco, USA, 1964. [7] USDA. Stream Corridor Restoration: Principles, Processes, and Practices. 2001. | in_ID |
| dc.description.abstract | It must be recognized that rivers differ among themselves, and through time,one river can vary significantly in itsdownstream direction. Most of the riversclassification was published by US or European researchers. In fact, these classifications of the river cannot be applied thoroughly to other regions such Asian Countries due to its differentcharacteristics and situations. Therefore, the general purpose of thisresearch is to establish a simple and easy-to-use practice in interpreting the morphological aspect of river by using planimetric characteristics. We selected four major rivers to develop the conceptual model for classification of meandering rivers in Borneo (Kalimantan) Island. Further, we divided the meandering rivers in Borneo Island by three zones to get the informed data in detail. Based on the results, the variability variesin all planimetric characteristics except the slope, which is considered as conformity. | in_ID |
