Wsl Institute For Schnee Und Lawinenforschung Slf

Davos, Switzerland

Wsl Institute For Schnee Und Lawinenforschung Slf

Davos, Switzerland
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Huber R.,Eidgenossische Forschungsanstalt fur Wald | Bebi P.,Wsl Institute For Schnee Und Lawinenforschung Slf | Briner S.,ETH Zurich | Bugmann H.,ETH Zurich | And 7 more authors.
Agrarforschung Schweiz | Year: 2012

The research project MOUNTLAND addresses the impacts of climate- and land-use changes on the provision of ecosystem services in mountain regions. The project applies an integrative approach by combining field experiments, ecological modeling, land-use modeling and the analysis societal and political decision making processes. The conceptual approach taken allows for the consideration of feedback effects in human-nature interactions in three different mountain regions in Switzerland.


Steeneveld G.J.,Wageningen University | Wokke M.J.J.,Meteogroup B.V | Groot Zwaaftink C.D.,Wsl Institute For Schnee Und Lawinenforschung Slf | Pijlman S.,Royal Haskoning | And 3 more authors.
Journal of Geophysical Research: Atmospheres | Year: 2010

This paper presents the results of 5 months of in situ observations of the diurnal cycle of longwave radiative heating rate in the lower part of the atmospheric boundary layer over grassland, with a particular focus on nighttime conditions. The observed longwave radiative heating is minimal at the evening transition, with a median value of -1.8 K h-1 between 1.3 and 10 m and -0.5 K h-1 between 10 and 20 m, respectively. After the transition, its magnitude gradually decreases during the night. For individual clear calm nights, a minimal radiative heating rate of -3.5 and -2.0 K h -1 was found for the two indicated layers. The total radiative heating rate appears dominantly controlled by the upward longwave flux divergence. Surprisingly, at noon a radiative heating rate of ∼1 Kh -1 was found between 1.3 and 10m for clear calm days. The availability of these radiation divergence measurements enables evaluation of the model performance for the temperature tendency caused by radiation divergence. The mesoscale model MM5 performs poorly for the stable boundary layer, because it overestimates the surface temperature and wind speed, while it underestimates the magnitude of radiative cooling. Some computationally efficient methods based on physical modeling, statistical modeling, and dimensional analysis are proposed by examining the gathered data set. The physical modeling approach appears to perform best. Copyright 2010 by the American Geophysical Union.

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