Persistence of Water within Perched Basins of the Peace-Athabasca Delta, Northern Canada

The Peace-Athabasca Delta (PAD) is one of the world’s largest freshwater deltas. Many of its shallow (<1.5 m) lakes and wetlands are perched above surrounding waterways. The delta has experienced a number of wetting and drying intervals. The latest drying trend ended in 1996 when high waters, generated under ice-jam and open-water conditions, recharged a number of the perched basins. The objective of this study was to determine the relative importance of hydroclimatic components on the persistence of water. A water-balance model was developed to simulate water-level responses following a flood event. Basin response was tested against a range of historical hydroclimatic conditions that have occurred in the delta during the 20th century. Ponded water duration in a 0.8 m deep perched basin was 5 years for the cool-dry period of the 1920s, slightly longer for the post-1974 flood era, and up to 9 years for the wet conditions of the 1940s and 1950s. Water drawdown occurred in almost every year and was almost exclusively due to evaporation exceeding precipitation. Net groundwater flux was minimal. Given the overlying importance of the floodwater component in the water balance of perched basins, the next step is to investigate the causes, spatial sources and frequency of flooding. This water balance model presented in this paper offers a useful tool for the management of the duration of water in perched wetlands of the PAD, which can help preserve essential habitat for wildlife.