A Case Study of the Weather Research and Forecasting Model Applied to the Joint Urban 2003 Tracer Field Experiment. Part III: Boundary-Layer Parametrizations
Abstract
Numerical weather prediction is often used to supply the mean wind and turbulence fields for atmospheric transport and dispersion plume models as they provide dense geographic coverage in comparison to typically sparse monitoring networks. Here, the Weather Research and Forecasting (WRF) model 4.0 was run over the month-long period of the Joint Urban 2003 field campaign conducted in Oklahoma City. We compare three different simulations in their ability to reproduce the observations, each using a different boundary-layer parametrization. Specifically, we examine the Mellor–Yamada–Janjic (MYJ), Yonsei University (YSU), and Mellor–Yamada–Nakanishi–Niino (MYNN) boundary-layer parametrizations. All three predict the wind speed well during the day but overpredict it at night. The MYNN parametrization is better than MYJ at predicting the daytime turbulence in the surface layer, but both underpredict the nocturnal turbulence. Additionally, the MYJ parametrization is best at predicting the reciprocal Obukhov length, while MYNN and YSU both significantly overpredict thermal stability. Reconstructing the reciprocal Obukhov length from other simulated parameters produces more accurate values for both parametrizations. All three models overpredict the boundary-layer height, particularly under convective conditions. The MYJ parametrization overestimates boundary-layer height the most, while YSU and MYNN have comparable performance with MYNN having an advantage in predicting themore »
- Authors:
-
- Los Alamos National Lab. (LANL), Los Alamos, NM (United States)
- National Center for Atmospheric Research (NCAR), Boulder, CO (United States)
- US Dept. of Homeland Security (DHS), Dugway Proving Ground, Dugway, UT (United States)
- Aeris, LLC, Louisville, CO (United States)
- Publication Date:
- Research Org.:
- Los Alamos National Laboratory (LANL), Los Alamos, NM (United States)
- Sponsoring Org.:
- USDOE
- OSTI Identifier:
- 1862806
- Report Number(s):
- LA-UR-20-27802
Journal ID: ISSN 0006-8314
- Grant/Contract Number:
- 89233218CNA000001
- Resource Type:
- Accepted Manuscript
- Journal Name:
- Boundary-Layer Meteorology
- Additional Journal Information:
- Journal Volume: 183; Journal Issue: 3; Journal ID: ISSN 0006-8314
- Publisher:
- Springer
- Country of Publication:
- United States
- Language:
- English
- Subject:
- 54 ENVIRONMENTAL SCIENCES; Atmospheric surface layer; boundary layer; turbulence; weather research and forecasting
Citation Formats
Nelson, Matthew Aaron, Conry, Patrick Tomas, Brown, Michael John, Costigan, Keeley Rochelle, Meech, Scott, Zajic, Dragan, Bieringer, Paul E., Annunzio, Andrew, and Bieberbach, George. A Case Study of the Weather Research and Forecasting Model Applied to the Joint Urban 2003 Tracer Field Experiment. Part III: Boundary-Layer Parametrizations. United States: N. p., 2022.
Web. doi:10.1007/s10546-022-00696-8.
Nelson, Matthew Aaron, Conry, Patrick Tomas, Brown, Michael John, Costigan, Keeley Rochelle, Meech, Scott, Zajic, Dragan, Bieringer, Paul E., Annunzio, Andrew, & Bieberbach, George. A Case Study of the Weather Research and Forecasting Model Applied to the Joint Urban 2003 Tracer Field Experiment. Part III: Boundary-Layer Parametrizations. United States. https://doi.org/10.1007/s10546-022-00696-8
Nelson, Matthew Aaron, Conry, Patrick Tomas, Brown, Michael John, Costigan, Keeley Rochelle, Meech, Scott, Zajic, Dragan, Bieringer, Paul E., Annunzio, Andrew, and Bieberbach, George. Thu .
"A Case Study of the Weather Research and Forecasting Model Applied to the Joint Urban 2003 Tracer Field Experiment. Part III: Boundary-Layer Parametrizations". United States. https://doi.org/10.1007/s10546-022-00696-8. https://www.osti.gov/servlets/purl/1862806.
@article{osti_1862806,
title = {A Case Study of the Weather Research and Forecasting Model Applied to the Joint Urban 2003 Tracer Field Experiment. Part III: Boundary-Layer Parametrizations},
author = {Nelson, Matthew Aaron and Conry, Patrick Tomas and Brown, Michael John and Costigan, Keeley Rochelle and Meech, Scott and Zajic, Dragan and Bieringer, Paul E. and Annunzio, Andrew and Bieberbach, George},
abstractNote = {Numerical weather prediction is often used to supply the mean wind and turbulence fields for atmospheric transport and dispersion plume models as they provide dense geographic coverage in comparison to typically sparse monitoring networks. Here, the Weather Research and Forecasting (WRF) model 4.0 was run over the month-long period of the Joint Urban 2003 field campaign conducted in Oklahoma City. We compare three different simulations in their ability to reproduce the observations, each using a different boundary-layer parametrization. Specifically, we examine the Mellor–Yamada–Janjic (MYJ), Yonsei University (YSU), and Mellor–Yamada–Nakanishi–Niino (MYNN) boundary-layer parametrizations. All three predict the wind speed well during the day but overpredict it at night. The MYNN parametrization is better than MYJ at predicting the daytime turbulence in the surface layer, but both underpredict the nocturnal turbulence. Additionally, the MYJ parametrization is best at predicting the reciprocal Obukhov length, while MYNN and YSU both significantly overpredict thermal stability. Reconstructing the reciprocal Obukhov length from other simulated parameters produces more accurate values for both parametrizations. All three models overpredict the boundary-layer height, particularly under convective conditions. The MYJ parametrization overestimates boundary-layer height the most, while YSU and MYNN have comparable performance with MYNN having an advantage in predicting the stable boundary-layer height. Several days were found where the WRF simulations predict significant deviations from the prevailing diurnal pattern in wind direction, which are not found in the observations.},
doi = {10.1007/s10546-022-00696-8},
journal = {Boundary-Layer Meteorology},
number = 3,
volume = 183,
place = {United States},
year = {Thu Mar 24 00:00:00 EDT 2022},
month = {Thu Mar 24 00:00:00 EDT 2022}
}
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