The runoff formation process is believed to be highly non-linear, time varying, spatially distributed, and not easily described by simple models. Considerable time and effort has been spent to model this process, and many hydrologic models have been built specifically for this purpose. These models are generally known as a rainfall — runoff (R-R) models.
Weitere Kapitel dieses Buchs durch Wischen aufrufen
- An Approach for Runoff Computation Using Three Data Mining Techniques
- Springer Netherlands