Explaining the convector effect in canopy turbulence by means of large-eddy simulation
- Karlsruhe Inst. of Technology (KIT), Garmisch-Partenkirchen (Germany). Inst. of Meteorology and Climate Research. Atmospheric Environmental Research (IMK-IFU)
Semi-arid forests are found to sustain a massive sensible heat flux in spite of having a low surface to air temperature difference by lowering the aerodynamic resistance to heat transfer (rH) – a property called the canopy convector effect (CCE). In this work large-eddy simulations are used to demonstrate that the CCE appears more generally in canopy turbulence. It is indeed a generic feature of canopy turbulence: rH of a canopy is found to reduce with increasing unstable stratification, which effectively increases the aerodynamic roughness for the same physical roughness of the canopy. This relation offers a sufficient condition to construct a general description of the CCE. In addition, we review existing parameterizations for rH from the evapotranspiration literature and test to what extent they are able to capture the CCE, thereby exploring the possibility of an improved parameterization.
- Research Organization:
- Karlsruhe Inst. of Technology (KIT), Garmisch-Partenkirchen (Germany); Los Alamos National Lab. (LANL), Los Alamos, NM (United States)
- Sponsoring Organization:
- USDOE; German Research Foundation (DFG); Helmholtz Association (Germany)
- Grant/Contract Number:
- AC52-06NA25396
- OSTI ID:
- 1369206
- Report Number(s):
- LA-UR-17-22651
- Journal Information:
- Hydrology and Earth System Sciences (Online), Vol. 21, Issue 6; ISSN 1607-7938
- Publisher:
- European Geosciences Union (EGU)Copyright Statement
- Country of Publication:
- United States
- Language:
- English
Web of Science
A Column Canopy‐Air Turbulent Diffusion Method for Different Canopy Structures
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journal | January 2019 |
Turbulent transport of energy across a forest and a semiarid shrubland
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Effect of Secondary Circulations on the Surface–Atmosphere Exchange of Energy at an Isolated Semi-arid Forest
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The influence of idealized surface heterogeneity on virtual turbulent flux measurements
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Turbulent transport of energy across a forest and a semiarid shrubland
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