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  • Night-time airflow within a deep and dense canopy near the top of a mountain ridge is investigated based on measurements at Bily Kriz, Czech Republic. A decoupled two-layer structure of canopy flow typically develops at night. While the above-canopy flow is most frequently an upslope-directed larger-scale flow over the ridge, the lower-canopy flow is downslope. However, the lower-canopy flow can be forced upslope when the wind speed above the canopy exceeds a well-defined limit. Less frequently, on the lee slope to the larger-scale flow, both the above-canopy and the lower-canopy flow are usually downslope, although a flow reversal in the lower canopy is also observed, accompanied with a large shear stress (friction velocity) above the canopy. We introduce a simple diagnostic model, which gives realistic values of the downslope or upslope direction and speed of the lower-canopy flow that agree well with the measurements.
  • Night-time airflow within a deep and dense canopy near the top of a mountain ridge is investigated based on measurements at Bily Kriz, Czech Republic. A decoupled two-layer structure of canopy flow typically develops at night. While the above-canopy flow is most frequently an upslope-directed larger-scale flow over the ridge, the lower-canopy flow is downslope. However, the lower-canopy flow can be forced upslope when the wind speed above the canopy exceeds a well-defined limit. Less frequently, on the lee slope to the larger-scale flow, both the above-canopy and the lower-canopy flow are usually downslope, although a flow reversal in the lower canopy is also observed, accompanied with a large shear stress (friction velocity) above the canopy. We introduce a simple diagnostic model, which gives realistic values of the downslope or upslope direction and speed of the lower-canopy flow that agree well with the measurements. (en)
Title
  • Night-time airflow in a forest canopy near a mountain crest
  • Night-time airflow in a forest canopy near a mountain crest (en)
skos:prefLabel
  • Night-time airflow in a forest canopy near a mountain crest
  • Night-time airflow in a forest canopy near a mountain crest (en)
skos:notation
  • RIV/68378289:_____/10:00348522!RIV11-AV0-68378289
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • P(IAA300420803), P(KJB3087301), Z(AV0Z30420517), Z(AV0Z60870520)
http://linked.open...iv/cisloPeriodika
  • 5
http://linked.open...vai/riv/dodaniDat
http://linked.open...aciTvurceVysledku
http://linked.open.../riv/druhVysledku
http://linked.open...iv/duvernostUdaju
http://linked.open...titaPredkladatele
http://linked.open...dnocenehoVysledku
  • 274881
http://linked.open...ai/riv/idVysledku
  • RIV/68378289:_____/10:00348522
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • Spruce forest; Canopy layer; Slope; Drainage flow; Wind profile (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • NL - Nizozemsko
http://linked.open...ontrolniKodProRIV
  • [39E1A4891101]
http://linked.open...i/riv/nazevZdroje
  • Agricultural and Forest Meteorology
http://linked.open...in/vavai/riv/obor
http://linked.open...ichTvurcuVysledku
http://linked.open...cetTvurcuVysledku
http://linked.open...vavai/riv/projekt
http://linked.open...UplatneniVysledku
http://linked.open...v/svazekPeriodika
  • 150
http://linked.open...iv/tvurceVysledku
  • Janouš, Dalibor
  • Pavelka, Marian
  • Sedlák, Pavel
  • Potužníková, Kateřina
  • Aubinet, M.
  • Heinesch, B.
  • Yernaux, M.
http://linked.open...ain/vavai/riv/wos
  • 000278244400010
http://linked.open...n/vavai/riv/zamer
issn
  • 0168-1923
number of pages
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