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DEVELOPMENT OF A BASIN GEOMORPHIC INFORMATION SYSTEM USING A TIN‐DEM DATA STRUCTURE 1
Author(s) -
Tachikawa Y,
Shiiba M.,
Takasao T
Publication year - 1994
Publication title -
jawra journal of the american water resources association
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.957
H-Index - 105
eISSN - 1752-1688
pISSN - 1093-474X
DOI - 10.1111/j.1752-1688.1994.tb03268.x
Subject(s) - triangulated irregular network , geology , digital elevation model , watershed , tin , grid , surface runoff , channel (broadcasting) , hydrology (agriculture) , geographic information system , structural basin , computer science , remote sensing , geomorphology , geotechnical engineering , geodesy , ecology , computer network , materials science , machine learning , metallurgy , biology
To make a distributed rainfall‐runoff model, it is very important to build a model of topographic surface of a basin which takes account of the direction of water flow. In this paper, a geographic information system in hydrologic modeling, the BGIS (Basin Geomorphic Information Systems) are presented for modeling a river basin using a TIN‐DEM (Triangulated Irregular Network ‐ Digital Elevation Model) data structure. The BGIS have two core systems, which are the TIN‐DEM generating system and the topographic analysis system. In the TIN‐DEM generating system, landscapes are modeled as a set of contiguous non‐overlapping terangular facets whose vertices are made up of points on a regular grid DEM and on river segments. These triangular facets are subdivided, if needed, so that each of them has only one side through which water flows out. The TIN‐DEM generating system is made up of four modules, (1) a module for generating triangles from a grid DEM, (2) a module for getting rid of pits, (3) a module for joining discontinuous valley segments to a channel network, (4) a module for subdividing triangular facets. In the topographic analysis system, using datasets processed with the TIN‐DEM generating system, a watershed source area for any segments in a stream network are delineated automatically, and topographic attributes of slopes, aspects, flow path lengths and upslope contributing areas are computed.