2023
DOI: 10.1029/2023ms003750
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The Benefits and Challenges of Downscaling a Global Reanalysis With Doubly‐Periodic Large‐Eddy Simulations

B. J. H. van Stratum,
C. C. van Heerwaarden,
J. Vilà‐Guerau de Arellano

Abstract: Global reanalyzes like ERA5 accurately capture atmospheric processes at spatial scales of  km or larger. By downscaling ERA5 with large‐eddy simulation (LES), LES can provide details about processes at spatio‐temporal scales down to meters and seconds. Here, we present an open‐source Python package named the “Large‐eddy simulation and Single‐column model—Large‐Scale Dynamics,” or (LS)2D in short, designed to simplify the downscaling of ERA5 with doubly‐periodic LES. A validation with observations, for several … Show more

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Cited by 4 publications
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“…Large-scale tendencies are dynamically integrated in high-resolution simulations, thus overcoming several idealizations in canonical LES that relies on steady-state forcing [30]. Realistic inhomogeneous terrain can also be incorporated, which overcomes limitations of downscaling attempts with doubly-periodic boundary conditions that integrate unsteady large-scale tendencies [31,32]. The full online coupling approach is particularly important to study transient phenomena (e.g., frontal passages [33], thunderstorm outflows, baroclinic systems, low-level jets) and changes in atmospheric stability associated with the diurnal-nocturnal cycle [34], topography-induced flow [35], and to link site-specific wind conditions to the long-term climatology of the area [34].…”
Section: Introductionmentioning
confidence: 99%
“…Large-scale tendencies are dynamically integrated in high-resolution simulations, thus overcoming several idealizations in canonical LES that relies on steady-state forcing [30]. Realistic inhomogeneous terrain can also be incorporated, which overcomes limitations of downscaling attempts with doubly-periodic boundary conditions that integrate unsteady large-scale tendencies [31,32]. The full online coupling approach is particularly important to study transient phenomena (e.g., frontal passages [33], thunderstorm outflows, baroclinic systems, low-level jets) and changes in atmospheric stability associated with the diurnal-nocturnal cycle [34], topography-induced flow [35], and to link site-specific wind conditions to the long-term climatology of the area [34].…”
Section: Introductionmentioning
confidence: 99%