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A new approach for generating optimal GLDAS hydrological products and uncertainties
Farzam Fatolazadeh1, Mehdi Eshagh2, Kalifa Goïta1
1CARTEL, Département de Géomatique Appliquée, Université de Sherbrooke, Sherbrooke, Québec, Canada.
This study introduces a new method to optimize land surface data from the Global Land Data Assimilation System (GLDAS), improving accuracy for soil moisture and snow water equivalent. The approach reduces uncertainties and enhances the reliability of hydrological modeling. Keywords: GLDAS, land surface models, hydrological products, data assimilation.
Area of Science:
- Hydrology and Earth System Science
- Geophysics and Environmental Monitoring
- Data Assimilation and Modeling
Background:
- Estimating optimal surface state information and uncertainties from multiple land surface models (LSMs) is crucial for accurate hydrological assessments.
- Existing Global Land Data Assimilation System (GLDAS) products require improved methods for uncertainty quantification and optimal value generation.
- Hydrological products like soil moisture, snow water equivalent, and canopy water are key indicators of land surface conditions.
Purpose of the Study:
- To develop and validate a novel approach for generating optimal surface state information and associated uncertainties from GLDAS estimates.
- To assess the performance of the proposed method using key hydrological products (soil moisture, snow water equivalent, canopy water) over the Canadian Prairies.
- To compare the results with established hydrological models and satellite-based observations.
Main Methods:
- Simultaneous application of Förstner and best quadratic unbiased variance component estimators with the least-squares method.
- Focus on soil moisture (SM), snow water equivalent (SWE), and canopy water (CAN) from GLDAS.
- Validation against WaterGAP Global Hydrological Model (WGHM) and Gravity Recovery and Climate Experiment (GRACE) terrestrial water storage anomalies.
Main Results:
- The proposed estimators yielded optimal SM and SWE values with minimal differences from mean values (e.g., 26 mm for SM, 9 mm for SWE).
- Estimated uncertainties for SM, SWE, and CAN varied annually, with total water storage (TWS) uncertainties closely mirroring SM.
- High correlations were achieved between the proposed method's outputs and WGHM (SWE: r=0.97, TWS: r=0.91) and GRACE (TWS: r=0.71, corrected TWS: r=0.81).
Conclusions:
- The novel approach effectively generates optimal surface state information and quantifies uncertainties from GLDAS products.
- The method demonstrates superior performance compared to individual LSMs or their average, with improved RMSE and mean absolute error.
- The results show strong agreement with independent hydrological models and satellite data, highlighting its potential for enhanced land surface monitoring.
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