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Improving flood forecast skill using remote sensing data: annual report 2016-17
Title | Improving flood forecast skill using remote sensing data: annual report 2016-17 |
Publication Type | Report |
Year of Publication | 2017 |
Authors | Pauwels, V, Walker, J, Li, Y, Grimaldi, S, Wright, A |
Document Number | 316 |
Date Published | 09/2017 |
Institution | Bushfire and Natural Hazards CRC |
City | Melbourne |
Report Number | 316 |
Abstract | Floods are among the most damaging natural disasters in Australia. Over the last 40 years, the average annual cost of floods was approximately $377 million per year. The 2010-2011 floods in Brisbane and South-East Queensland alone resulted in 35 confirmed deaths and $2.38 billion damage. The recent floods in 2016 resulted in three casualties with three more people missing. The Insurance Council of Australia stated on June 7 that about 14,500 claims totaling $56 million have already been lodged from across the country. In order to limit the personal and economic damage caused by floods, operational water and emergency managers heavily rely on flood forecasting systems. These systems consist of a hydrologic and a hydraulic model to predict the extent and level of floods, using observed and predicted rainfall. The hydrologic model calculates the amount of water that is flowing through the river network, while the hydraulic model converts this flow volume into river water levels/velocities and floodplain extents. Over recent times, the accuracy and reliability of these flood forecasting systems has significantly improved. However, it remains difficult to provide accurate flood warnings. This is because of errors and/or uncertainties in the model structure, the model parameters, and/or the meteorological forcings (mainly the rainfall). The hypothesis of this project is that remote sensing data can be used to improve modelled flood forecasts. More specifically, in this project we are constraining the hydrologic model using remotely sensed soil moisture values, as this variable determines the partitioning of rainfall into surface runoff and infiltration. Further, we are constraining the hydraulic model using remotely sensed water levels and/or flood extents. Thus every time a remote sensing image becomes available, we correct the model predictions, which should lead to improved model forecasts of flow depth, extent and velocity for a number of days in the future.
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