Abstract
Uncrewed aircraft system (UAS) observations collected during the 2018 Lower Atmospheric Process Studies at Elevation-a Remotely Piloted Aircraft Team Experiment (LAPSE-RATE) field campaign were assimilated into a high-resolution configuration of the Weather Research and Forecasting Model using an ensemble Kalman filter. The benefit of UAS observations was assessed for a terrain-driven (drainage and upvalley) flow event that occurred within Colorado's San Luis Valley (SLV) using independent observations. The analysis and prediction of the strength, depth, and horizontal extent of drainage flow from the Saguache Canyon and the subsequent transition to upvalley and up-canyon flow were improved relative to that obtained both without data assimilation (benchmark) and when only surface observations were assimilated. Assimilation of UAS observations greatly improved the analyses of vertical variations in temperature, relative humidity, and winds at multiple locations in the northern portion of the SLV, with reductions in both bias and the root-mean-square error of roughly 40% for each variable relative to the benchmark run. Despite these noted improvements, some biases remain that were tied to measurement error and/or the impact of the boundary layer parameterization on vertically spreading the observations, both of which require further exploration. The results presented here highlight how observations obtained with a fleet of profiling UAS improve limited-area, high-resolution analyses and short-term forecasts in complex terrain.
| Original language | English |
|---|---|
| Pages (from-to) | 1459-1480 |
| Number of pages | 22 |
| Journal | Monthly Weather Review |
| Volume | 149 |
| Issue number | 5 |
| DOIs | |
| State | Published - May 2021 |
Bibliographical note
Publisher Copyright:© 2021 American Meteorological Society.
Funding
Acknowledgments. We thank Pedro Jiménez for help in setting up the initial configuration of the Weather Research and Forecast Model used in this study. The surface meteorological data were obtained from the Iowa Environmental Mesonet at Iowa State University and Colorado State University CoAgMET mesonet data archive. The authors are also appreciative of the National Center for Atmospheric Research Computational and Information Systems Laboratory (CISL)’s support of the Cheyenne and Casper supercomputers used to produce the simulations. The National Center for Atmospheric Research is sponsored by the National Science Foundation. This work was specifically supported in part by NSF Award AGS-1755088. Julie Lundquist’s contribution to this paper was funded, in part, by the National Renewable Energy Laboratory, operated by Alliance for Sustainable Energy, LLC, for the U.S. Department of Energy (DOE) under Contract DE-AC36-08GO28308 via the Office of Energy Efficiency and Renewable Energy Wind Energy Technologies. The views expressed in the article do not necessarily represent the views of the DOE or the U.S. government. The publisher, by accepting the article for publication, acknowledges that the U.S. government retains a nonexclusive, paid-up, irrevocable, worldwide license to publish or reproduce the published form of this work, or allow others to do so, for U.S. government purposes. Gijs de Boer was supported by the NOAA/Physical Sciences Laboratory. Support for the LAPSE-RATE campaign was provided by the International Society for Atmospheric Research using Remotely Piloted Aircraft (ISARRA), with the U.S. National Science Foundation (NSF AGS 1807199) and the U.S. DOE (DE-SC0018985) supporting the participation of early career scientists. This work was also supported, in part, by the NASA University Leadership Initiative (ULI) under Award 80NSSC20M0162.
| Funders | Funder number |
|---|---|
| National Renewable Energy Laboratory | |
| National Oceanic and Atmospheric Administration | |
| NASA University Leadership Initiative | |
| Office of Energy Efficiency and Renewable Energy Wind Energy Technologies | |
| International Society for Atmospheric Research | |
| NOAA Physical Sciences Laboratory | |
| Anambra State University of Science & Technology, Uli | 80NSSC20M0162 |
| U.S. Department of Energy | DE-AC36-08GO28308, DE-SC0018985 |
| National Science Foundation Arctic Social Science Program | AGS 1807199, AGS-1755088 |
Keywords
- Complex terrain
- Data assimilation
- Drainage flow
- Ensembles
- Mesoscale models
- Short-range prediction
ASJC Scopus subject areas
- Atmospheric Science
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