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contributor authorYi, Chuixiang
date accessioned2017-06-09T16:18:15Z
date available2017-06-09T16:18:15Z
date copyright2008/01/01
date issued2008
identifier issn1558-8424
identifier otherams-65371.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4206588
description abstractTo understand the basic characteristics of the observed S-shaped wind profile and the exponential flux profile within forest canopies, three hypotheses are postulated. The relationship between these fundamental profiles is well established by combining the postulated hypotheses with momentum equations. Robust agreements between theoretical predictions and observations indicate that the nature of momentum transfer within canopies can be well understood by combining the postulated hypotheses and momentum equations. The exponential Reynolds stress profiles were successfully predicted by the leaf area index (LAI) profile alone. The characteristics of the S-shaped wind profile were theoretically explained by the plant morphology and local drag coefficient distribution. Predictions of maximum drag coefficient were located around the maximum leaf area level for most forest canopies but lower than the maximum leaf area level for a corn canopy. A universal relationship of the Reynolds stress between the top and bottom of the canopy is predicted for all canopies. This universal relationship can be used to understand what percentage of the Reynolds stress at the top of canopy is absorbed by the whole canopy layer from the observed LAI values alone. All of these predictions are consistent with the conclusions from dimensional analysis and satisfy the continuity requirement of Reynolds stress, mean wind speed, and local drag coefficient at the top of canopy.
publisherAmerican Meteorological Society
titleMomentum Transfer within Canopies
typeJournal Paper
journal volume47
journal issue1
journal titleJournal of Applied Meteorology and Climatology
identifier doi10.1175/2007JAMC1667.1
journal fristpage262
journal lastpage275
treeJournal of Applied Meteorology and Climatology:;2008:;volume( 047 ):;issue: 001
contenttypeFulltext


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