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1 Spatial Modelling of the Terrestrial Environment - Georeferencial

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5<br />

Flood Inundation <strong>Modelling</strong> Using<br />

LiDAR and SAR Data<br />

Paul D. Bates, M.S. Horritt, D. Cobby and D. Mason<br />

5.1 Introduction<br />

Flood inundation is a major hazard in <strong>the</strong> UK and worldwide. Its prediction and prevention<br />

require considerable investment, even aside from <strong>the</strong> socio-economic consequences <strong>of</strong> severe<br />

flooding episodes. Better flood extent prediction is relevant to a significant percentage<br />

<strong>of</strong> <strong>the</strong> global population, as well as raising fundamental scientific issues and challenges relating<br />

to remote sensing, distributed environmental modelling, risk analysis and uncertainty.<br />

In recent years, remote sensing <strong>of</strong> floodplain environments has increasingly become an<br />

operational tool that may begin to resolve some fundamental problems in flood conveyance<br />

estimation. In a number <strong>of</strong> areas, in particular topography and validation data, we are moving<br />

rapidly from a data-poor to a data-rich and spatially complex modelling environment<br />

with attendant possibilities for model testing and development. The availability <strong>of</strong> rich and<br />

relatively accurate spatial data sources in digital format may lead to significant changes in<br />

scientific and engineering practice in flood conveyance estimation over <strong>the</strong> next 5–10 years<br />

and it is <strong>the</strong> purpose <strong>of</strong> this chapter to identify potential areas in which integration <strong>of</strong><br />

hydraulic models and remotely sensed spatial data may be <strong>of</strong> benefit.<br />

Traditional methods <strong>of</strong> hydraulic investigation for real river reaches have focussed largely<br />

on model validation against bulk flow measurements such as stage and discharge measured<br />

at only a single point in <strong>the</strong> system, typically <strong>the</strong> reach outflow (e.g. Bates et al.,<br />

1998a). The main calibration parameter for <strong>the</strong>se applications is boundary friction, and it<br />

is relatively easy to match <strong>the</strong> available validation data with a spatially lumped parameter<br />

set that has been calibrated to maximize some objective measure <strong>of</strong> fit between <strong>the</strong> observed<br />

and predicted outflow hydrographs. Whilst hydraulic resistance does have a sound<br />

<strong>Spatial</strong> <strong>Modelling</strong> <strong>of</strong> <strong>the</strong> <strong>Terrestrial</strong> <strong>Environment</strong>. Edited by R. Kelly, N. Drake, S. Barr.<br />

C○ 2004 John Wiley & Sons, Ltd. ISBN: 0-470-84348-9.

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