Belgium and The Netherlands; Fig. 1a) flooded severely, causing extensive damage and forcing massive evacuations. These events sparked an interest in land-use and climate change as possible causes of the recent, apparent increase in flood frequency. To separate the effects of land-use change and pre
Flood and Megaflood Processes and Deposits || Use of Remote Sensing in Monitoring River Floods and their Effects on the Landscape
โ Scribed by Martini, I. Peter; Baker, Victor R.; Garzn, Guillermina
- Publisher
- Blackwell Publishing Ltd.
- Year
- 2002
- Tongue
- English
- Weight
- 652 KB
- Edition
- 1
- Category
- Article
- ISBN
- 0632064048
No coin nor oath required. For personal study only.
โฆ Synopsis
The objective of this study is to establish a procedure for estimating the effects of river floods in large areas utilizing remote sensing satellite data. Floods usually occur unexpectedly and generally last a short time. Satellite image data can show floods instantaneously over tens of thousands of square kilometres. Radar satellite data can be recorded at scales of 1 : 25 000, 1 : 50 000 and smaller, under any atmospheric situation. They thus can be obtained when needed during various floods stages, the only limiting factor being the satellite orbit position. There are several satellites equipped with radar sensors, such as ERS (Europe)
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In hydrological modelling of runo processes, including water balance, various input data and parameters can be acquired or estimated by the use of remote sensing (RS) techniques.The acquisition and use of synoptic RS areal information rather than traditional point information is an important issue i