INTRODUCTION
The attitude to water problems is changing. A number of products which have
been found suitable in connection with water resources planning for a long
succession of years have exhausted their usefulness, others have come to re-
place them. The hydrological information we can give in future will to a great
extent be based on hydrological models of different types. We will further use
digital map information and satellite images. Modern computer techniques allow
automatic production of maps and diagrams in colour as well as on line display
of such information. Geo-coded data bases will be of great importance.
The most widely used models in hydrology today are lumped models, but they do
not answer sufficiently to the present needs of hydrological information for
water resources planning. The present needs of water information calls for a
new generation of distributed hydrological models. Hydrological and climato-
logical observations are seldom of sufficient density in space to provide the
wished basic information for the distributed models. However new types of
digital data sources are available for supplementary landscape information and
these data sources can be used to refine the models.
The point of departure for all types of hydrological information is a hydro-
logical, climatological and ground water observation network. Some or all of
the watershed characteristics listed in the table below are required for most
hydrological models.
Surface water Meteorology
Stream discharge Rainfall
Lake and reservoir level Temperature
Water temperature Humidity
Sediment concentration Barometric pressure
Chemical and biological Radiation
properties Sunshine duration
Evaporation
Snow depth and water content
Interception
Watershed caracteristics Soil and groundwater
Topography (drainage area Water level
and land slopes) Temperature
Geology Chemical properties
Soil type Storage coefficient
Geomorfology (drainage Permeability
pattern) Moisture content
Vegetation
Land use
One of the main areas of application is in regional analyses in which selected
characteristics are related to different hydrological variables. Selected
characteristics are also used in most lumped conceptual models of the rainfall-
runoff process. Distributed hydrological models are to a still higher degree
dependent on watershed characteristics.Often today the information needed is
not readily available, and the modeller is frequently forced to use a more
simple model.
Normal derivation of watershed caracteristics is laborous, time consuming and
costly. New data sources like Landsat imagery and digital map data opennew
fields for hydrologic model development. The way digital map information can
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