ARTICLES
ZHANG Jinping, CHENG Weiming, WANG Ruibo, LONG En, ZHANG Yang
.
2005, 7(2):
36-41.
In the vast domain of China, topographic and geomorphic conditions are quite varied. Geomorphology is one of the most main factors of physical geographical environment, and its maps have been widely used in the scientific research, economic construction, eco-environmental protection, education and military affairs etc. Modern geomorphology and its mapping started in 1950's. In the last 50 years, Chinese scholars made great progress in regional geomorphology, geomorphologic mapping and other branches of geomorphology, formed comparative integrated scientific system, finished and published lots of geomorphologic maps with the different scales and regions. However, only 15 sheets of geomorphologic maps (total 77 sheets, including land and ocean) with a scale of 1:1 000 000 were finished and compiled in 1980's, and field geomorphologic surveying was the main traditional mapping methodologies, some geomorphologic borderlines were not exact, which cannot satisfy the objective demands. With the development and application of technology and methodology based on Remote Sensing and GIS, lots of work can be finished in indoors. So, based on Landsat TM, DEM with a scale of 1:250 000 and lots of historic geomorphologic maps, this topic will try to research geomorphologic mapping method and technology with a scale of 1:1 000 000 using GIS and RS. Some parameters, such as slope, aspect, hillshade and watershed units are calculated from DEM, which can help distinguish from different landform and topographic units in the Landsat TM imageries. Some key problems, such as the relationship between land-cover and geomorphologic types, landform and countor lines, are discussed. The research is foundation for updating the geomorphologic borderline and finish all geomorphologic maps in with a scale of 1:1 000 000 by means of GIS and RS in the future.