Estimating cell-to-cell land surface drainage paths from digital channel networks, with an application to the Amazon basin

被引:20
作者
Mayorga, E
Logsdon, MG
Ballester, MVR
Richey, JE
机构
[1] Univ Washington, Sch Oceanog, Seattle, WA 98195 USA
[2] Univ Sao Paulo, Ctr Energia Nucl Agr, BR-13416000 Piracicaba, SP, Brazil
基金
美国国家航空航天局;
关键词
river networks; drainage basins; flow direction; watershed extraction; geographic information systems; amazonia;
D O I
10.1016/j.jhydrol.2005.03.023
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
Cell-to-cell surface flow paths are commonly derived from gridded digital elevation models (DEM) by choosing the direction of steepest descent to one of the eight surrounding cells. However, adequate DEMs often are not available. We developed a topography-independent method for creating gridded, land and stream drainage direction maps based on corrected vector river networks. We applied it to the Digital Chart of the World river network in the Amazon basin gridded at 0.005 degrees resolution; in this basin, low relief and poor topographic data have prevented the effective use of DEM-based methods. We geo-registered 224 hydrographic gages against the processed network and compared extracted vs. published drainage areas. Drainage areas ranged from 227 to 4,620,000 km(2). Median relative error was 4.5%, increasing in smaller basins to 94% in basins <= 2000 km(2). The effective limit of reliability may differ from 2000 km2 across the basin. The drainage direction map and derivative datasets represent an improvement over existing datasets for regional research in the Amazon basin. Methods exploiting vector networks complement terrain approaches, and combined they may yield advances in the automated extraction of drainage maps and handling of topologically realistic river systems. (c) 2005 Elsevier B.V. All rights reserved.
引用
收藏
页码:167 / 182
页数:16
相关论文
共 42 条
[1]  
*ANEEL, 1987, INV EST FLUV
[2]  
[Anonymous], [No title captured]
[3]  
CARRASCO N, 1992, SEM PROGR HIDR CLIM, P41
[4]  
Congalton RG, 1997, PHOTOGRAMM ENG REM S, V63, P425
[5]  
COSTA MH, 2002, IN PRESS J GEOPHYS R, V107, DOI DOI 10.1029/2001JD000309
[6]   DIGITAL ELEVATION MODEL NETWORKS (DEMON) - A MODEL OF FLOW OVER HILLSLOPES FOR COMPUTATION OF CONTRIBUTING AND DISPERSAL AREAS [J].
COSTACABRAL, MC ;
BURGES, SJ .
WATER RESOURCES RESEARCH, 1994, 30 (06) :1681-1692
[7]  
DANKO DM, 1992, GEOINFO SYSTEMS, V2, P29
[8]  
Devol A. H., 2001, BIOGEOCHEMISTRY AMAZ, P275, DOI [10.1093/oso/9780195114317.003.0018, DOI 10.1093/OSO/9780195114317.003.0018]
[9]   Validation of a new global 30-min drainage direction map [J].
Döll, P ;
Lehner, B .
JOURNAL OF HYDROLOGY, 2002, 258 (1-4) :214-231
[10]  
Dunne T, 1998, GEOL SOC AM BULL, V110, P450, DOI 10.1130/0016-7606(1998)110<0450:EOSBTF>2.3.CO