✦ LIBER ✦

Mean scalar concentration profile in a sheared and thermally stratified atmospheric surface layer

✍ Scribed by Katul, Gabriel G.; Li, Dan; Chamecki, Marcelo; Bou-Zeid, Elie

Book ID: 118750684
Publisher: The American Physical Society
Year: 2013
Tongue: English
Weight: 630 KB
Volume: 87
Category: Article
ISSN: 1063-651X
DOI: 10.1103/PhysRevE.87.023004

No coin nor oath required. For personal study only.

📜 SIMILAR VOLUMES

Mean concentration and flux profiles for

Mean concentration and flux profiles for chemically reactive species in the atmospheric surface layer

✍ David R. Fitzjarrald; Donald H. Lenschow 📂 Article 📅 1983 🏛 Elsevier Science 🌐 English ⚖ 863 KB

Concentration profiles of particles sett

Concentration profiles of particles settling in the neutral and stratified atmospheric boundary layer

✍ Marcelo Chamecki; René van Hout; Charles Meneveau; Marc B. Parlange 📂 Article 📅 2007 🏛 Springer 🌐 English ⚖ 399 KB

Fluxes and Concentrations of Non-Conserv

Fluxes and Concentrations of Non-Conserved Scalars in the Atmospheric Surface Layer

✍ Leif Kristensen; Peter Kirkegaard 📂 Article 📅 2006 🏛 Springer Netherlands 🌐 English ⚖ 254 KB

An ensemble of dynamically identical the

An ensemble of dynamically identical thermals and vertical profiles of turbulent moments in the convective surface layer of atmosphere

✍ A. N. Vulfson; O. O. Borodin 📂 Article 📅 2009 🏛 Allerton Press, Inc. 🌐 English ⚖ 217 KB

Profiles of polar conductivities and of

Profiles of polar conductivities and of radon-222 concentration in the atmosphere by stable and labile stratification of surface layer

✍ A.I. Petrov; G.G. Petrova; I.N. Panchishkina 📂 Article 📅 2009 🏛 Elsevier Science 🌐 English ⚖ 724 KB

Relations between surface fluxes and mea

Relations between surface fluxes and mean profiles of velocity, temperature and concentration, downwind of a change in surface roughness

✍ P. J. Mulhearn 📂 Article 📅 1977 🏛 John Wiley and Sons 🌐 English ⚖ 790 KB

## Abstract Changes in surface fluxes (of momentum, heat, and mass) downwind of a surface roughness change, are related to changes in mean profiles (of velocity, temperature, and concentration). the theory assumes that changes in mean quantities are self‐preserving. At fetches sufficiently large fo