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If the prevailing synoptic weather situation results in weak pressure gradients and low wind speeds, the very small turbulent heat flux cannot balance the surface energy loss, resulting in cooling of the surface and the development of a surface-based inversion and stable boundary layer.
“If the prevailing synoptic weather situation results in weak pressure gradients and hence low wind speeds, the very small turbulent heat flux cannot balance the surface energy loss, resulting in a cooling of the surface and the development of a surface-based inversion (SBI) and SBL (Bourne et al., 2010;Mahrt, 1999;Serreze et al., 1992;Stull, 1988).”
From In situ vertical observations of the layered structure of air pollution in a continental high-latitude urban boundary layer during winter (2025) · cites this paper as Mahrt, 1999
Conventional stable boundary layer descriptions from the literature may not be fully appropriate to explain the vertical distribution of pollution layers in the high-latitude winter stable boundary layer.
“This means that conventional SBL descriptions from the literature (Mahrt, 1999;Mahrt and Vickers, 2002;Stull, 1988) may not be fully appropriate to explain the vertical distribution of pollution layers in the high-latitude winter SBL.”
From In situ vertical observations of the layered structure of air pollution in a continental high-latitude urban boundary layer during winter (2025) · cites this paper as Mahrt, 1999
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- Authors
- Mahrt, L.
- Affiliations
- Oregon State University (US)
- Corresponding author
- Mahrt, L.
- ORCID
- Mahrt, L.
- Venue
- Boundary-Layer Meteorology
- Published
- 1999-03
- Volume
- 90
- Issue
- 3
- Pages
- 375-396
- ISSN
- 0006-8314 (ISSN-L)
- 1573-1472
- OpenAlex
- W1656281027
- Cited by
- 652
- References
- 78
- Citations by year
- 2026: 30 · 2025: 24 · 2024: 26 · 2023: 25 · 2022: 36 · 2021: 33 · 2020: 28 · 2019: 22 · 2018: 15 · 2017: 24 · 2016: 32 · 2015: 28 · 2014: 29 · 2013: 24 · 2012: 30
- FWCI
- 10.94
- Type
- journal article
- Language
- en
- Open access
- closed
- Licence
- Locations
- Boundary-Layer Meteorology (publishedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Meteorological Phenomena and Simulations
- Physical Sciences › Engineering › Computational Mechanics › Fluid Dynamics and Turbulent Flows
- Physical Sciences › Environmental Science › Environmental Engineering › Wind and Air Flow Studies
- Keywords
- stable boundary layer, stratified boundary layer, roughness sublayer, surface layer, local similarity, low-level jet, gravity waves, boundary layer breakdown, turbulent flux measurement
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