local flux-profile relationships of wind speed and temperature in a canopy layer in atmospheric stable conditions
Clicks: 7
ID: 128630
2010
Article Quality & Performance Metrics
Overall Quality
Not rated
Combines reader engagement with the AI quality analysis. This
article has not been analysed, so there is no overall score —
reader engagement is measured and shown alongside.
Reader Engagement
Popular Article
1.8
/100
7 views
3 readers
AI Quality Assessment
Not analyzed
Readership in this journal
PopularRanked #344 of 345 articles by views in tetrahedron letters
Most read
Least read
Bar heights use a square-root scale. Only the 120 most-read articles are drawn; the journal has 345 in total.
Mint this article as an NFT
Not yet mintedCreate a permanent, verifiable on-chain record of this article on the Scimatic Network. The NFT is held in your Journament account, and you can withdraw it to your own wallet at any time.
5
SUSD
one-off · no wallet required
Abstract
The particularities of the physics of the canopy layer pose challenges to the determination and use of traditional universal functions so helpful in the atmospheric surface layer. Progress toward "universal-like functions" such as those provided by Monin-Obukhov similarity theory for the canopy layer has been modest. One of the challenges lies in that the assumptions underlying Monin-Obukhov similarity theory do not hold within a canopy layer. This paper thus examines the local flux-profile relations for wind (<i>Φ</i><sub><i>m</i></sub>) and for temperature (<i>Φ</i><sub><i>h</i></sub>). It uses three different stability parameters, i.e., <i>h/L(h)</i> at tree top, local <i>z/L(z)</i>, and the local bulk Richardson number (<i>Ri</i>), within a tall forest canopy in nighttime stable (indicated by <i>h/L(h)</i> > 0) conditions. Results suggest that the in-canopy <i>Φ</i><sub><i>m</i></sub> can be described using the local Richardson number <i>Ri</i>. Furthermore, <i>Φ</i><sub><i>m</i></sub> is found to increase linearly with <i>Ri</i> in the upper canopy layer for |<i>Ri</i>| < 1. When local |<i>Ri</i>| > 1, |Φ<sub><i>m</i></sub>| decreases with |<i>Ri</i>| in a power function, a result consistent for all levels of measurements within the canopy. When both local <i>Φ</i><sub><i>h</i></sub> and local <i>Ri</i> are positive, i.e., the local downward turbulent heat flux is consistent with the local temperature gradient, the local <i>Φ</i><sub><i>h</i></sub> increases with the local <i>Ri</i> when <i>Ri</i> < 1. However, <i>Φ</i><sub><i>h</i></sub> does not change with <i>Ri</i> (or much more scattered) when <i>Ri</i> > 1. The relationship between local <i>Φ</i><sub><i>h</i></sub> and <i>Ri</i> disappears when counter-gradient heat transfer occurs in strongly stable conditions. A self-correlation analysis is used to examine the influence of self-correlation and the physical meaning of these relationships.
| Reference Key |
zhang2010biogeoscienceslocal
Use this key to autocite in the manuscript while using
SciMatic Manuscript Manager or Thesis Manager
|
|---|---|
| Authors | ;G. Zhang;M. Y. Leclerc;A. Karipot |
| Journal | tetrahedron letters |
| Year | 2010 |
| DOI |
10.5194/bg-7-3625-2010
|
| URL | |
| Keywords | Keywords not found |
Citations
No citations found. To add a citation, contact the admin at info@scimatic.org
Comments
No comments yet. Be the first to comment on this article.