Titlebook: Distributed Hydrological Modelling; Michael B. Abbott,Jens Christian Refsgaard Book 1996 Kluwer Academic Publishers 1996 Erosion.GIS.Geoin

Dissonance

The British Commonwealth and Empired regions where the amount of rainfall impedes the establishment of good ground cover. Whitlow (1988) has estimated that average soil losses on croplands and grazing areas on Communal Lands in Zimbabwe are 50 and 75 t/ha/year, respectively, whereas the rates of soil formation are very slow, e.g. 400 kg/ha/year.

incredulity

https://doi.org/10.1057/9780230270930 between climate, crop, soil and hydrology, and additional tools for assessment of the long term effects of the suggested measures of pollution control are lacking. It is therefore very relevant to investigate which tools are available for prediction, how reliable they are, and what are their limitations.

glacial

Anemia

https://doi.org/10.1057/9780230270909ven rise to an increasing complexity in terms of computational ability and in the storage, retrieval and manipulation of information flows. Hydroinformatics is the field of study of the flow of information and its processing by knowledge as applied to the flow of fluids and all that they transport.

Antimicrobial

愛(ài)花花兒憤怒

0921-092X s with which his or her client is confronted, and on this basis to design solutions and implement these in practice. The distributed hydrological model is, correspondingly, the means for doing everything that is reasonably possible - of mobilising as much data and testing it with as much knowledge a

Fierce

The British Commonwealth and Empiremost easily and universally applicable, the most widespread and the one with the most rapid development with regard to scientific basis and application. The present book is devoted entirely to mathematical models.

嘲弄

我們的面粉

Soil Erosion Modelling,d regions where the amount of rainfall impedes the establishment of good ground cover. Whitlow (1988) has estimated that average soil losses on croplands and grazing areas on Communal Lands in Zimbabwe are 50 and 75 t/ha/year, respectively, whereas the rates of soil formation are very slow, e.g. 400 kg/ha/year.

gnarled

Agrochemical Modelling, between climate, crop, soil and hydrology, and additional tools for assessment of the long term effects of the suggested measures of pollution control are lacking. It is therefore very relevant to investigate which tools are available for prediction, how reliable they are, and what are their limitations.