Theoretical Studies of Hydro-Geomorphologic Basin Response

对极端水文事件的分析通常需要大量的径流数据。这种情况很少发生，记录仅限于不存在。这项工作将通过在贝叶斯意义上用物理理解代替数据来加深对控制盆地动力学的机制的理解。流域尺度的地貌单位线将与山坡径流的物理特征和表示一起使用，如几何、地形、气候等。其目的是建立一个统一和一致的流域枯水期和丰水期径流生产理论，并为流域行为建立一个自洽的水文地貌模型。

The analysis of extreme hydrologic events generally requires considerable amounts of streamflow data. This is seldom the case and records are limited on non-existent. This work will further the understandings of the mechanisms controlling basin dynamics by substituting, in a Bayesian sense, physical understanding for data. Basin scale geomorphological unit hydrographs will be used together with physical characteristics and representation of hillslope run-off, e.g., geometry, topography, climate, etc. The objectives are to develop a unified and consistent theory of run-off production in a basin for dry and wet periods and to formulate a self-consistent hydro-geomorphologic model for catchment behavior.