Increased heat fluxes near a forest edge
Observations of sensible and latent heat flux above forest downwind of a forest edge show these fluxes to be larger than the available energy over the forest. The enhancement averages to 56 W m(-2), or 16% of the net radiation, at fetches less than 400 m, equivalent to fetch to height ratios less than 15. The enhancement of turbulent energy fluxes is explained by advection and increases with the difference in temperature and humidity of the air over the upwind area as compared to the forest. The relatively high temperature and humidity of the upwind air are not caused by high surface heat flux... Mehr ...
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Dokumenttyp: | Artikel |
Erscheinungsdatum: | 2002 |
Reihe/Periodikum: | Klaassen , W , van Breugel , PB , Moors , EJ & Nieveen , JP 2002 , ' Increased heat fluxes near a forest edge ' , Theoretical and Applied Climatology , vol. 72 , no. 3-4 , pp. 231-243 . https://doi.org/10.1007/s00704-002-0682-8 |
Schlagwörter: | ROUGHNESS PARAMETERS / EXCHANGE / TURBULENCE / NETHERLANDS / VARIABILITY / INTERFACE / MODELS |
Sprache: | Englisch |
Permalink: | https://search.fid-benelux.de/Record/base-28779003 |
Datenquelle: | BASE; Originalkatalog |
Powered By: | BASE |
Link(s) : | https://hdl.handle.net/11370/717fb612-762f-4f96-ba0f-f1f5768b9d98 |