Keywords
Groundwater; flooding; return period; model; United Kingdom
Start Date
27-6-2018 10:40 AM
End Date
27-6-2018 12:00 PM
Abstract
Groundwater flooding in the UK affects 100,000s of properties and in the winters of 2000/1 and 2013/14 caused widespread disruption. The groundwater flooding during these winters affected transport links for many weeks or months as well as threatening water supply and waste water treatment infrastructure. Groundwater flooding as a phenomena is mainly related to the chalk outcrop in southern England. To predict how groundwater flooding affects properties with respect to increased flood risk a methodology that creates groundwater surfaces with given return periods has been developed. Its basis is a groundwater model of the chalk aquifer for England, stretching from Yorkshire down to Dorset (550 kilometres). Given the model size, the hydraulic conductivity distribution is parametrised using a relationship between distance to river and size of river (mean flow). This model is then calibrated for the period 1962 to 2014 against groundwater hydrographs. Annual maxima are used to create head vs return period relationships at every model node at the chalk outcrop. Groundwater heads for the requisite return period (30, 75, 100, 200, 250, 500, 1000 years) are then used to create groundwater surfaces. These surfaces are then combined with a surface water model to simulate overland flow, for which flooded extent is modelled. The modelling workflow from recharge model driving the groundwater model through to creating the return period defined surfaces is described and results presented. It is believed that this is the first large-scale groundwater model to simulate groundwater flooding and so the challenges overcome during the process are summarised.
Large-scale groundwater modelling of the UK : creation of return period-based groundwater surfaces
Groundwater flooding in the UK affects 100,000s of properties and in the winters of 2000/1 and 2013/14 caused widespread disruption. The groundwater flooding during these winters affected transport links for many weeks or months as well as threatening water supply and waste water treatment infrastructure. Groundwater flooding as a phenomena is mainly related to the chalk outcrop in southern England. To predict how groundwater flooding affects properties with respect to increased flood risk a methodology that creates groundwater surfaces with given return periods has been developed. Its basis is a groundwater model of the chalk aquifer for England, stretching from Yorkshire down to Dorset (550 kilometres). Given the model size, the hydraulic conductivity distribution is parametrised using a relationship between distance to river and size of river (mean flow). This model is then calibrated for the period 1962 to 2014 against groundwater hydrographs. Annual maxima are used to create head vs return period relationships at every model node at the chalk outcrop. Groundwater heads for the requisite return period (30, 75, 100, 200, 250, 500, 1000 years) are then used to create groundwater surfaces. These surfaces are then combined with a surface water model to simulate overland flow, for which flooded extent is modelled. The modelling workflow from recharge model driving the groundwater model through to creating the return period defined surfaces is described and results presented. It is believed that this is the first large-scale groundwater model to simulate groundwater flooding and so the challenges overcome during the process are summarised.
Stream and Session
C11: Integrated Methods and Tools for Flood Risk and Water Supply Management