Dust-planetary boundary layer interactions amplified by entrainment and advections

Zhang, Xiaoyan; Xu, Xiyan; Chen, Haishan; Hu, Xiao-Ming; Gao, Lan

doi:10.1016/j.atmosres.2022.106359

Dust-planetary boundary layer interactions amplified by entrainment and advections

Journal Article · Mon Jul 25 00:00:00 EDT 2022 · Atmospheric Research

DOI:https://doi.org/10.1016/j.atmosres.2022.106359· OSTI ID:1882546

Zhang, Xiaoyan ^[1]; Xu, Xiyan ^[2]; Chen, Haishan ^[3]; Hu, Xiao-Ming ^[4]; Gao, Lan ^[5]

Nanjing Univ. of Information Science and Technology (China); Univ. of Oklahoma, Oklahoma City, OK (United States). University of Oklahoma Health Sciences Center
Chinese Academy of Sciences (CAS), Beijing (China). Inst. for Atmospheric Sciences
Nanjing Univ. of Information Science and Technology (China)
Univ. of Oklahoma, Norman, OK (United States). Center for Analysis and Prediction of Storms
Univ. of Oklahoma, Norman, OK (United States)

Mineral dust contributes to more than half of the global aerosol loading. However, the radiative impacts of dust aerosols on planetary boundary layer (PBL) structure have not been explored sufficiently. During a typical dust storm event over Tarim Basin, dust aerosols exhibit a well-mixed distribution during the daytime in spite of a shallow layer of dust particles accumulated at higher altitudes. By contrast, nocturnal dust plumes are located near the surface due to stable stratification. We demonstrate that these differentiated vertical distributions determine the spatial heterogeneity of dust loading, radiative fluxes and PBL height variations. Dust aerosols cause daytime PBL suppression and nighttime PBL promotion through modulating surface and atmospheric radiative budgets. Specifically, dust-induced cooling effect within PBL directly inhibits the daytime PBL development. PBL suppression effect is then amplified by entrainment processes resulting in excessively low PBL height, especially for dust particles below but near the PBL top. Dust plumes weaken updrafts from PBL and downdrafts of the free atmosphere, which further reduce the entrainment mixing through attenuating horizontal and vertical advection, and eventually amplify PBL suppression. At night, near-surface dust aerosols stimulate a warm and unstable lower atmosphere, generate warm advection heating and promote the PBL development. Our study highlights the importance of specifying entrainment parameters and nighttime advection activities in quantifying the dust-PBL interactions.

View Accepted Manuscript (DOE)

Research Organization:: ARM Data Center, Oak Ridge National Laboratory (ORNL), Oak Ridge, TN (United States)

Sponsoring Organization:: National Natural Science Foundation of China (NSFC); USDOE Office of Science (SC), Biological and Environmental Research (BER)

Contributing Organization:: PNNL, BNL, ANL, ORNL

Grant/Contract Number:: SC0021159

OSTI ID:: 1882546

Journal Information:: Atmospheric Research, Journal Name: Atmospheric Research Vol. 278; ISSN 0169-8095

Publisher:: ElsevierCopyright Statement

Country of Publication:: United States

Language:: English

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Quantifying the range of the dust direct radiative effect due to source mineralogy uncertainty Li, Longlei; Mahowald, Natalie M.; Miller, Ron L. Atmospheric Chemistry and Physics, Vol. 21, Issue 5 https://doi.org/10.5194/acp-21-3973-2021	journal	January 2021
Modeled and observed properties related to the direct aerosol radiative effect of biomass burning aerosol over the southeastern Atlantic Doherty, Sarah J.; Saide, Pablo E.; Zuidema, Paquita Atmospheric Chemistry and Physics, Vol. 22, Issue 1 https://doi.org/10.5194/acp-22-1-2022	journal	January 2022
Evidence of mineral dust altering cloud microphysics and precipitation Min, Q. -L.; Li, R.; Lin, B. Atmospheric Chemistry and Physics, Vol. 9, Issue 9 https://doi.org/10.5194/acp-9-3223-2009	journal	January 2009
Particulate absorption of solar radiation: anthropogenic aerosols vs. dust Wang, C.; Jeong, G. R.; Mahowald, N. Atmospheric Chemistry and Physics, Vol. 9, Issue 12 https://doi.org/10.5194/acp-9-3935-2009	journal	January 2009
Taklimakan dust aerosol radiative heating derived from CALIPSO observations using the Fu-Liou radiation model with CERES constraints Huang, J.; Fu, Q.; Su, J. Atmospheric Chemistry and Physics, Vol. 9, Issue 12 https://doi.org/10.5194/acp-9-4011-2009	journal	January 2009
An elevated large-scale dust veil from the Taklimakan Desert: Intercontinental transport and three-dimensional structure as captured by CALIPSO and regional and global models Yumimoto, K.; Eguchi, K.; Uno, I. Atmospheric Chemistry and Physics, Vol. 9, Issue 21 https://doi.org/10.5194/acp-9-8545-2009	journal	January 2009
Characteristics and performance of wind profiles as observed by the radar wind profiler network of China Liu, Boming; Guo, Jianping; Gong, Wei Atmospheric Measurement Techniques, Vol. 13, Issue 8 https://doi.org/10.5194/amt-13-4589-2020	journal	August 2020

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