Abstract
Climate change is reshaping vulnerable ecosystems, leading to uncertain effects on ecosystem dynamics, including evapotranspiration (ET) and ecosystem respiration (Reco). However, accurate estimation of ET and Reco still remains challenging at sparsely monitored watersheds, where data and field instrumentation are limited. In this study, we developed a hybrid predictive modeling approach (HPM) that integrates eddy covariance measurements, physically based model simulation results, meteorological forcings, and remote-sensing datasets to estimate ET and Reco in high space-time resolution. HPM relies on a deep learning algorithm and long short-term memory (LSTM) and requires only air temperature, precipitation, radiation, normalized difference vegetation index (NDVI), and soil temperature (when available) as input variables. We tested and validated HPM estimation results in different climate regions and developed four use cases to demonstrate the applicability and variability of HPM at various FLUXNET sites and Rocky Mountain SNOTEL sites in Western North America. To test the limitations and performance of the HPM approach in mountainous watersheds, an expanded use case focused on the East River Watershed, Colorado, USA. The results indicate HPM is capable of identifying complicated interactions among meteorological forcings, ET, and Reco variables, as well as providing reliable estimation of ET and Reco across relevant spatiotemporal scales, even in challenging mountainous systems. The study documents that HPM increases our capability to estimate ET and Reco and enhances process understanding at sparsely monitored watersheds.
Original language | English |
---|---|
Pages (from-to) | 6041-6066 |
Number of pages | 26 |
Journal | Hydrology and Earth System Sciences |
Volume | 25 |
Issue number | 11 |
DOIs | |
State | Published - Nov 25 2021 |
Externally published | Yes |
Funding
Financial support. This research has been supported by the U.S. Acknowledgements. This material is based upon work supported as part of the Watershed Function Scientific Focus Area, funded by the U.S. Department of Energy, Office of Science, Office of Biological and Environmental Research under award no. DE-AC02-05CH11231. We thank Haruko Wainwright and Bhavna Arora for providing comments on East River estimations. We also greatly appreciate all the guidance provided by Yoram Rubin and Dennis Bal-docchi at UC Berkeley to the first author. We also acknowledge the Jane Lewis Fellowship Committee of UC Berkeley for providing fellowship support to the first author.