Record Details

Non-stationary Generation of Weak Turbulence for Very Stable and Weak-Wind Conditions

ScholarsArchive at Oregon State University

Field Value
Title Non-stationary Generation of Weak Turbulence for Very Stable and Weak-Wind Conditions
Names Mahrt, Larry (creator)
Thomas, Christoph (creator)
Richardson, Scott (creator)
Seaman, Nelson (creator)
Stauffer, David (creator)
Zeeman, Matthias (creator)
Date Issued 2013-05 (iso8601)
Note This is the publisher’s final pdf. The published article is copyrighted by Springer and can be found at: http://link.springer.com/journal/10546. The author has paid this publisher's Open Access fee.
Abstract Turbulence measurements for very stable conditions near the surface are contrasted
among three sites: a high altitude basin during winter with grass or snow-covered
grass, a broad valley with complex agricultural land use, and a more narrow valley that is
influenced by a valley cold pool and cold air drainage. In contrast to previous studies, this
investigation emphasizes the very weak turbulence with large bulk Richardson number occurring
during extensive periods between brief mixing events. The relationship of the turbulence
to the non-stationary wind and stratification is examined along with the impact of short-term
flow accelerations, directional shear and downward diffusion of turbulence from higher levels.
The failure of the turbulence for strong stratification to decrease with further increase of
stratification is explored. Additional analyses are applied to weak-wind cases for the entire
range of stratification, including weak stratification associated with cloudy conditions.
Genre Article
Access Condition http://creativecommons.org/licenses/by-nc/3.0/us/
Topic Intermittent turbulence
Identifier Mahrt, L., Thomas, C., Richardson, S., Seaman, N., Stauffer, D., & Zeeman, M. (2013). Non-stationary generation of weak turbulence for very stable and weak-wind conditions. Boundary-Layer Meteorology, 147(2), 179-199. doi:10.1007/s10546-012-9782-x

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