The University of Southampton
University of Southampton Institutional Repository

Water balance at Ainsdale National Nature Reserve 1975-2100

Water balance at Ainsdale National Nature Reserve 1975-2100
Water balance at Ainsdale National Nature Reserve 1975-2100
Groundwater levels at Ainsdale Sand Dunes National Nature Reserve rise and fall by about 0.5m between winter and summer. There have been several periods where water table levels were considerably lower than average, which caused the dune floors to dry up, with undesirable environmental effects. However these dry periods have been interspersed by occasional wet years where the water table has risen to above average levels. This paper explains a physically based model of the water balance in the dune system and describes how the model was tested against observed water table levels. The model is sensitive to the timing of rainfall events. The effects of expected climate change published by the UK Climate Impact Programme (UKCIP) are simulated in the model. Results suggest that the average water table level in the open dunes will fall by about 1.2m between the years 1990 and 2100
Clarke, D.
9746f367-1df2-4e0e-8d71-5ecfc9ddd000
Sanitwong-Na-Ayutthaya, S.
bfdc32dc-3cd6-43bd-87bd-b72c69ab0595
Clarke, D.
9746f367-1df2-4e0e-8d71-5ecfc9ddd000
Sanitwong-Na-Ayutthaya, S.
bfdc32dc-3cd6-43bd-87bd-b72c69ab0595

Clarke, D. and Sanitwong-Na-Ayutthaya, S. (2006) Water balance at Ainsdale National Nature Reserve 1975-2100. Sefton Coast Partnership Research Meeting 2006, Edge Hill, UK. 14 Jul 2006.

Record type: Conference or Workshop Item (Paper)

Abstract

Groundwater levels at Ainsdale Sand Dunes National Nature Reserve rise and fall by about 0.5m between winter and summer. There have been several periods where water table levels were considerably lower than average, which caused the dune floors to dry up, with undesirable environmental effects. However these dry periods have been interspersed by occasional wet years where the water table has risen to above average levels. This paper explains a physically based model of the water balance in the dune system and describes how the model was tested against observed water table levels. The model is sensitive to the timing of rainfall events. The effects of expected climate change published by the UK Climate Impact Programme (UKCIP) are simulated in the model. Results suggest that the average water table level in the open dunes will fall by about 1.2m between the years 1990 and 2100

This record has no associated files available for download.

More information

Published date: 2006
Venue - Dates: Sefton Coast Partnership Research Meeting 2006, Edge Hill, UK, 2006-07-14 - 2006-07-14

Identifiers

Local EPrints ID: 53147
URI: http://eprints.soton.ac.uk/id/eprint/53147
PURE UUID: c002cb56-4c6b-41b0-832d-a800bdbb78f7
ORCID for D. Clarke: ORCID iD orcid.org/0000-0002-5433-5258

Catalogue record

Date deposited: 23 Jul 2008
Last modified: 23 Jul 2022 01:31

Export record

Contributors

Author: D. Clarke ORCID iD
Author: S. Sanitwong-Na-Ayutthaya

Download statistics

Downloads from ePrints over the past year. Other digital versions may also be available to download e.g. from the publisher's website.

View more statistics

Atom RSS 1.0 RSS 2.0

Contact ePrints Soton: eprints@soton.ac.uk

ePrints Soton supports OAI 2.0 with a base URL of http://eprints.soton.ac.uk/cgi/oai2

This repository has been built using EPrints software, developed at the University of Southampton, but available to everyone to use.

We use cookies to ensure that we give you the best experience on our website. If you continue without changing your settings, we will assume that you are happy to receive cookies on the University of Southampton website.

×