Articles | Volume 15, issue 13
https://doi.org/10.5194/acp-15-7269-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/acp-15-7269-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Impact of planetary boundary layer turbulence on model climate and tracer transport
E. L. McGrath-Spangler
CORRESPONDING AUTHOR
Universities Space Research Association, Columbia, MD, USA
Global Modeling and Assimilation Office, NASA Goddard Space Flight Center, Greenbelt, MD, USA
Global Modeling and Assimilation Office, NASA Goddard Space Flight Center, Greenbelt, MD, USA
Earth System Sciences Interdisciplinary Center, University of Maryland, College Park, MD, USA
L. E. Ott
Global Modeling and Assimilation Office, NASA Goddard Space Flight Center, Greenbelt, MD, USA
S. Pawson
Global Modeling and Assimilation Office, NASA Goddard Space Flight Center, Greenbelt, MD, USA
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Cited
13 citations as recorded by crossref.
- Wavelike Structures in the Turbulent Layer During the Morning Development of Convection at Dome C, Antarctica I. Petenko et al. 10.1007/s10546-016-0173-6
- Thoughts on Earth System Modeling: From global to regional scale E. Canepa & P. Builtjes 10.1016/j.earscirev.2017.06.017
- Air quality and radiative impacts of downward-propagating sudden stratospheric warmings (SSWs) R. Williams et al. 10.5194/acp-24-1389-2024
- Using statistical models to explore ensemble uncertainty in climate impact studies: the example of air pollution in Europe V. Lemaire et al. 10.5194/acp-16-2559-2016
- The determination of highly time-resolved and source-separated black carbon emission rates using radon as a tracer of atmospheric dynamics A. Gregorič et al. 10.5194/acp-20-14139-2020
- The turbulent future brings a breath of fresh air C. Stjern et al. 10.1038/s41467-023-39298-4
- Evaluation of the Antarctic Boundary Layer Thermodynamic Structure in MERRA2 Using Dropsonde Observations from the Concordiasi Campaign M. Ganeshan & Y. Yang 10.1029/2019EA000890
- Diurnal asymmetry of desert amplification and its possible connections to planetary boundary layer height: a case study for the Arabian Peninsula L. Zhou 10.1007/s00382-021-05634-x
- Statistical-mechanical approach to study the hydrodynamic stability of the stably stratified atmospheric boundary layer G. Nevo et al. 10.1103/PhysRevFluids.2.084603
- Dust-planetary boundary layer interactions amplified by entrainment and advections X. Zhang et al. 10.1016/j.atmosres.2022.106359
- Frequency and impact of summertime stratospheric intrusions over Maryland during DISCOVER‐AQ (2011): New evidence from NASA's GEOS‐5 simulations L. Ott et al. 10.1002/2015JD024052
- Integrating continuous atmospheric boundary layer and tower-based flux measurements to advance understanding of land-atmosphere interactions M. Helbig et al. 10.1016/j.agrformet.2021.108509
- The KPP Boundary Layer Scheme for the Ocean: Revisiting Its Formulation and Benchmarking One‐Dimensional Simulations Relative to LES L. Van Roekel et al. 10.1029/2018MS001336
13 citations as recorded by crossref.
- Wavelike Structures in the Turbulent Layer During the Morning Development of Convection at Dome C, Antarctica I. Petenko et al. 10.1007/s10546-016-0173-6
- Thoughts on Earth System Modeling: From global to regional scale E. Canepa & P. Builtjes 10.1016/j.earscirev.2017.06.017
- Air quality and radiative impacts of downward-propagating sudden stratospheric warmings (SSWs) R. Williams et al. 10.5194/acp-24-1389-2024
- Using statistical models to explore ensemble uncertainty in climate impact studies: the example of air pollution in Europe V. Lemaire et al. 10.5194/acp-16-2559-2016
- The determination of highly time-resolved and source-separated black carbon emission rates using radon as a tracer of atmospheric dynamics A. Gregorič et al. 10.5194/acp-20-14139-2020
- The turbulent future brings a breath of fresh air C. Stjern et al. 10.1038/s41467-023-39298-4
- Evaluation of the Antarctic Boundary Layer Thermodynamic Structure in MERRA2 Using Dropsonde Observations from the Concordiasi Campaign M. Ganeshan & Y. Yang 10.1029/2019EA000890
- Diurnal asymmetry of desert amplification and its possible connections to planetary boundary layer height: a case study for the Arabian Peninsula L. Zhou 10.1007/s00382-021-05634-x
- Statistical-mechanical approach to study the hydrodynamic stability of the stably stratified atmospheric boundary layer G. Nevo et al. 10.1103/PhysRevFluids.2.084603
- Dust-planetary boundary layer interactions amplified by entrainment and advections X. Zhang et al. 10.1016/j.atmosres.2022.106359
- Frequency and impact of summertime stratospheric intrusions over Maryland during DISCOVER‐AQ (2011): New evidence from NASA's GEOS‐5 simulations L. Ott et al. 10.1002/2015JD024052
- Integrating continuous atmospheric boundary layer and tower-based flux measurements to advance understanding of land-atmosphere interactions M. Helbig et al. 10.1016/j.agrformet.2021.108509
- The KPP Boundary Layer Scheme for the Ocean: Revisiting Its Formulation and Benchmarking One‐Dimensional Simulations Relative to LES L. Van Roekel et al. 10.1029/2018MS001336
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Short summary
PBL processes are important for weather, climate, and tracer transport and concentration. In the GEOS-5 AGCM, the PBL depth is used in the calculation of turbulent mixing. This study analyzes the impact of using different PBL depth definitions in this calculation. Near surface wind speed differences modify Saharan dust on the order of 1e-4kg m-2. CO surface concentrations are modified by up to 20 ppb over biomass burning regions. Instantaneous CO2 differences are on the order of 10 ppm.
PBL processes are important for weather, climate, and tracer transport and concentration. In the...
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