Investigating Terrestrial Water Storage Response to Meteorological Drought in the Canadian Prairies

Abstract

The Canadian Prairies region is considered a climate change hot spot due to the extreme drought events and their impacts on water resources. The overall goal of this research is to understand the linkage between meteorological droughts and Total Water Storage (TWS) variations in the Canadian Prairies. To achieve this goal, a diversified database is collected and analyzed by geostatistical tools and cross-wavelet transform approach. It concerns a multitude of climatic data (four CMIP6 multi-model datasets) and satellite observations (GRACE data). The results indicate that: (1) the models overestimate the precipitation rate over the Canadian Prairies, and the Norwegian Earth System Model version 2 (NorESM2–LM) is the most suitable model for the context of the Canadian Prairies; (2) Sen’s slope estimator of annual rainfall can reach −2.5 mm/year/year, with a decreasing magnitude of trends in the NE to SW direction; (3) the Standardized Precipitation Index (SPI) and the Modified China-Z Index (MCZI) demonstrate that, in the past, most of the climatological years were near normal with some extremely dry years (1952, 2000, 2003, and 2015) and one extremely wet year (1960); (4) the projections in the far future indicate an increase in the number of extremely dry years (2037, 2047, 2080, 2089, and 2095); (5) the combined analysis of GRACE-derived TWS and drought indices show the direct impact of the meteorological drought periods on the water resources. The TWS values decreased from 23 cm in 2002 to −54 cm in 2020, indicating a significant water reserve decline in the region. The results of this study are expected to provide a valuable perspective to understand the dynamic of hydrosystems in a climate change context in the Canadian Prairies.

Possible Future Climate Change Impacts on the Meteorological and Hydrological Drought Characteristics in the Jinghe River Basin, China

“…Furthermore, different GCM models have different simulations for precipitation and temperature in different regions [47,48]. Although the GFDL-CM3 model is better used on the JRB, more GCM models should be considered in the other regions.…”

Analysis of Groundwater Depletion in the Saskatchewan River Basin in Canada from Coupled SWAT-MODFLOW and Satellite Gravimetry

“…The exploitation of groundwater in this area remains an important issue as many communities and industries depend on groundwater for their water needs. In fact, groundwater in this area is an essential In reality, aquifer recharge can decrease despite increased liquid precipitation in the SRB [42] for several reasons. Possible explanations include: (i) evapotranspiration can reduce the amount of water that seeps into the soil to reach aquifers; and (ii) the amount of water stored in the aquifer decreases, resulting from excessive extraction when water is pumped from an aquifer faster than it can be replaced by natural recharge.…”