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  • 1
    Online Resource
    Online Resource
    Wiley ; 2013
    In:  Quarterly Journal of the Royal Meteorological Society Vol. 139, No. 672 ( 2013-04), p. 607-624
    In: Quarterly Journal of the Royal Meteorological Society, Wiley, Vol. 139, No. 672 ( 2013-04), p. 607-624
    Abstract: A field campaign, the Slope Experiment near La Fouly (SELF‐2010), was conducted to monitor the evening transition of slope flows on clear‐sky days from July to September 2010 in a narrow valley of the Swiss Alps. A steep west‐facing slope with inclinations ranging from 25° to 45° was instrumented from 1900 m to 2200 m above sea‐level. Detailed measurements were made along a linear transect of the slope with two turbulence towers, two weather stations, five surface temperature measurement stations and a tethered balloon system. The present study focuses on nine exemplary ‘convective’ days, characterized by weak synoptic flow and clear‐sky conditions, during which thermal circulations prevail. The analysis of the observational data shows that topographic shading triggers the evening transition. The topographic configuration around the experimental site results in a sharply defined ‘shading front’ propagating upslope, causing a sudden decrease in incoming short‐wave radiation on the order of several hundreds of W m −2 within a few minutes. The slope surface rapidly responds to the advancing shading front; in some cases, reductions in surface temperatures of some 10°C in less than 10 min are observed. This is rapidly followed by an early‐evening calm period with very small turbulent kinetic energy (TKE 〈 0.05 m 2 s −2 ) and extremely light wind speeds ( 〈 0.5 m s −1 ). When the inertia‐driven upslope flow is fully stopped by the katabatic acceleration, a shallow local drainage flow forms and reaches a quasi‐equilibrium 1.5 h after the local sunset. An analysis of the TKE budget close to the surface shows that the buoyancy flux is much greater than the shear production in the last hours before the local sunset, possibly due to valley curvature effects. Copyright © 2012 Royal Meteorological Society
    Type of Medium: Online Resource
    ISSN: 0035-9009 , 1477-870X
    URL: Issue
    RVK:
    RVK:
    Language: English
    Publisher: Wiley
    Publication Date: 2013
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    detail.hit.zdb_id: 2089168-4
    SSG: 14
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  • 2
    Online Resource
    Online Resource
    Cambridge University Press (CUP) ; 2010
    In:  Journal of Fluid Mechanics Vol. 665 ( 2010-12-25), p. 480-515
    In: Journal of Fluid Mechanics, Cambridge University Press (CUP), Vol. 665 ( 2010-12-25), p. 480-515
    Abstract: A field experiment – the Snow Horizontal Array Turbulence Study (SnoHATS) – has been performed over an extensive glacier in Switzerland in order to study small-scale turbulence in the stable atmospheric surface layer, and to investigate the role, dynamics and modelling of the subgrid scales (SGSs) in the context of large-eddy simulations. The a priori data analysis aims at comparing the role and behaviour of the SGSs under stable conditions with previous studies under neutral or unstable conditions. It is found that the SGSs in a stable surface layer remain an important sink of temperature variance and turbulent kinetic energy from the resolved scales and carry a significant portion of the fluxes when the filter scale is larger than the distance to the wall. The fraction of SGS fluxes (out of the total fluxes) is found to be independent of stability. In addition, the stress–strain alignment is similar to the alignment under neutral and unstable conditions. The model coefficients vary considerably with stability but in a manner consistent with previous findings, which also showed that scale-dependent dynamic models can capture this variation. Furthermore, the variation of the coefficients for both momentum and heat SGS fluxes can be shown to be better explained by stability parameters based on vertical gradients, rather than vertical fluxes. These findings suggest that small-scale turbulence dynamics and SGS modelling under stable conditions share many important properties with neutral and convective conditions, and that a unified approach is thus possible. This paper concludes with a discussion of some other challenges for stable boundary-layer simulations that are not encountered in the neutral or unstable cases.
    Type of Medium: Online Resource
    ISSN: 0022-1120 , 1469-7645
    Language: English
    Publisher: Cambridge University Press (CUP)
    Publication Date: 2010
    detail.hit.zdb_id: 1472346-3
    detail.hit.zdb_id: 218334-1
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  • 3
    In: Water Resources Research, American Geophysical Union (AGU), Vol. 47, No. 9 ( 2011-09)
    Type of Medium: Online Resource
    ISSN: 0043-1397
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 2011
    detail.hit.zdb_id: 2029553-4
    detail.hit.zdb_id: 5564-5
    SSG: 13
    SSG: 14
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  • 4
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 2012
    In:  Geophysical Research Letters Vol. 39, No. 2 ( 2012-01), p. n/a-n/a
    In: Geophysical Research Letters, American Geophysical Union (AGU), Vol. 39, No. 2 ( 2012-01), p. n/a-n/a
    Type of Medium: Online Resource
    ISSN: 0094-8276
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 2012
    detail.hit.zdb_id: 2021599-X
    detail.hit.zdb_id: 7403-2
    SSG: 16,13
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