## Abstract In this study, large‐scale atmospheric variables are downscaled to meteorological variables at local scale for the daily time step to assess hydrological impacts by climate changes. Large‐scale atmospheric modelling was by the HadCM3 General Circulation Model (GCM) while downscaling and
Modelling climate change impacts in the Peace and Athabasca catchment and delta: III—integrated model assessment
✍ Scribed by Alain Pietroniro; Robert Leconte; Brenda Toth; Daniel L. Peters; Nicholas Kouwen; F. Malcolm Conly; Terry Prowse
- Publisher
- John Wiley and Sons
- Year
- 2006
- Tongue
- English
- Weight
- 459 KB
- Volume
- 20
- Category
- Article
- ISSN
- 0885-6087
- DOI
- 10.1002/hyp.6428
No coin nor oath required. For personal study only.
✦ Synopsis
Abstract
This study utilized the hydrodynamic model, ONE‐D, coupled to the distributed hydrological model WATFLOOD, to evaluate the potential effects of a shift in climate on the hydrological regimes of three large lakes (Athabasca, Claire, and Mamawi), and two important sources of inflow (the Peace and Athabasca rivers) in the Peace‐Athabasca Delta (PAD). The coupled WATFLOOD/ONE‐D system was forced by current climatology and downscaled climate change scenarios from five selected general circulation models (GCMs).
Under the selected climate change scenarios, water levels in Lakes Athabasca, Claire, and Mamawi peaked, on average, 40–50 days earlier than at present. Some GCM scenarios predicted an increase in peak lake levels while others predicted suppressed lake levels. Inter‐annual water level variability was also sensitive to predicted changes in precipitation and temperature, increasing in winter and decreasing in summer.
Water level fluctuations in the major input rivers of the PAD were found to be more variable under the climate change simulations. Moreover, spring freshet peaks were estimated to occur earlier (20–30 days) and to be considerably reduced (up to 1·0 m reductions).
Although the simulations converged towards the same general results in seasonality shift, flow level amplitude was GCM‐dependent. Simple downscaling methods may well be too coarse to adequately address the important spatial variations that can occur in the long‐term climate signal. It is therefore important to understand the sensitivity of this regime to local climatic influences to produce more reliable, quantitative results. An ensemble of approaches that provide meaningfully downscaled results should be considered to confirm the results presented. Copyright © 2006 Crown in the right of Canada, and John Wiley & Sons, Ltd.
📜 SIMILAR VOLUMES
## Abstract Hydrological models are recognized as valid scientific tools to study water quantity and quality and provide support for the integrated management and planning of water resources at different scales. In common with many catchments in the Mediterranean, the study catchment has many probl
## Abstract This special issue has highlighted recent and innovative methods and results that integrate observations and modelling analyses of regional to global aspect of biophysical and biogeochemical interactions of land‐cover change with the climate system. Both the Earth System and the Integra
## Abstract The impacts of climate change on water resources were analysed for the Hii River basin and downstream Lake Shinji. The variation between saline and fresh water within these systems means that they encompass diverse ecosystems. Changes in evapotranspiration (ET), snow water equivalent, d