Field Observations of Canopy Flows over Complex Terrain

被引:23
作者
Grant, Eleanor R. [1 ,2 ]
Ross, Andrew N. [1 ]
Gardiner, Barry A. [3 ,4 ,5 ]
Mobbs, Stephen D. [6 ,7 ]
机构
[1] Univ Leeds, Sch Earth & Environm, Inst Climate & Atmospher Sci, Leeds LS2 9JT, W Yorkshire, England
[2] British Antarctic Survey, High Cross, Cambridge CB3 0ET, England
[3] No Res Stn, Forest Res, Roslin EH25 9SY, Midlothian, Scotland
[4] INRA, UMR ISPA 1391, F-33140 Villenave Dornon, France
[5] Bordeaux Sci Agro, UMR ISPA 1391, F-33170 Gradignan, France
[6] Univ Leeds, Natl Ctr Atmospher Sci, Leeds LS2 9JT, W Yorkshire, England
[7] Univ Leeds, Sch Earth & Environm, Leeds LS2 9JT, W Yorkshire, England
关键词
Atmospheric boundary layer; Complex terrain; Flow separation; Forest canopy; Hills; LARGE-EDDY SIMULATION; NEUTRAL TURBULENT-FLOW; AIR-FLOW; HILL; TRANSPORT; LAYER;
D O I
10.1007/s10546-015-0015-y
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
The investigation of airflow over and within forests in complex terrain has been, until recently, limited to a handful of modelling and laboratory studies. Here, we present an observational dataset of airflow measurements inside and above a forest situated on a ridge on the Isle of Arran, Scotland. The spatial coverage of the observations all the way across the ridge makes this a unique dataset. Two case studies of across-ridge flow under near-neutral conditions are presented and compared with recent idealized two-dimensional modelling studies. Changes in the canopy profiles of both mean wind and turbulent quantities across the ridge are broadly consistent with these idealized studies. Flow separation over the lee slope is seen as a ubiquitous feature of the flow. The three-dimensional nature of the terrain and the heterogeneous forest canopy does however lead to significant variations in the flow separation across the ridge, particularly over the less steep western slope. Furthermore, strong directional shear with height in regions of flow separation has a significant impact on the Reynolds stress terms and other turbulent statistics. Also observed is a decrease in the variability of the wind speed over the summit and lee slope, which has not been seen in previous studies. This dataset should provide a valuable resource for validating models of canopy flow over real, complex terrain.
引用
收藏
页码:231 / 251
页数:21
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