Special Issue "Modeling of Turbulent Processes in the Atmospheric Surface Layer"
Deadline for manuscript submissions: closed (9 October 2020).
Interests: microscale modeling; radiation fog; small-scale turbulence; surface interactions; urban microscale modeling
The lowest part of the atmospheric boundary layer is commonly referred to as the surface layer and has been intensely studied for more than 50 years. The surface layer structure is strongly related to stratification, which can range from unstable, neutral, and weakly stable to strongly stable. During daytime, processes are usually turbulent, while during nighttime strong stability may reduce or even inhibit turbulent and lead to intermittent or laminar flows. Over the last few decades, much progress has been made in understanding the (turbulent) structure of the surface layer and its interaction with surface. Monin-Obukhov Similarity Theory (MOST), for instance, was developed more than 50 years ago, but is the only widely accepted framework to describe the structure of the surface layer and is still used today in most atmospheric models to describe the exchange of energy near the surface. Over the years, microscale modeling and micrometeorological field experiments have revealed, however, that a better understanding of the near-surface boundary layer is needed, particularly in stable conditions and in the presence of surface heterogeneities.
This Special Issue in Atmosphere invites contributions that showcase the most recent progress in surface-layer meteorology in order to improve our basic understanding and to help developing new parameterizations in atmospheric models.
Potential topics include, but are not limited to:
- Turbulence resolving simulations of the surface layer
- Similarity theory (and beyond)
- Shallow stable boundary layers
- Intermittent turbulence and flow laminarization
- New measurement techniques to probe and characterize the surface layer
- Interactions between atmosphere, vegetation, soil, and artificial materials
- Parameterization of surface-layer processes in atmospheric models
- Turbulent exchange in the urban canopy layer
- Effects of surface heterogeneity on near-surface dynamics
Dr. Björn Maronga
Manuscript Submission Information
Manuscripts should be submitted online at www.mdpi.com by registering and logging in to this website. Once you are registered, click here to go to the submission form. Manuscripts can be submitted until the deadline. All papers will be peer-reviewed. Accepted papers will be published continuously in the journal (as soon as accepted) and will be listed together on the special issue website. Research articles, review articles as well as short communications are invited. For planned papers, a title and short abstract (about 100 words) can be sent to the Editorial Office for announcement on this website.
Submitted manuscripts should not have been published previously, nor be under consideration for publication elsewhere (except conference proceedings papers). All manuscripts are thoroughly refereed through a single-blind peer-review process. A guide for authors and other relevant information for submission of manuscripts is available on the Instructions for Authors page. Atmosphere is an international peer-reviewed open access monthly journal published by MDPI.
Please visit the Instructions for Authors page before submitting a manuscript. The Article Processing Charge (APC) for publication in this open access journal is 1500 CHF (Swiss Francs). Submitted papers should be well formatted and use good English. Authors may use MDPI's English editing service prior to publication or during author revisions.
- Small-scale turbulence
- Surface interactions
- Surface-layer dynamics
- Similarity theory
- Microscale modeling
- Surface heterogeneities
- Urban canopy layer