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dc.contributor.authorÁgústsson, Hálfdán
dc.contributor.authorÓlafsson, Haraldur
dc.contributor.authorJonassen, Marius Opsanger
dc.contributor.authorRögnvaldsson, Ólafur
dc.description.abstractOrographic winds near a 914 m high mountain in Southwest-Iceland are explored using unique observations made aloft with a small remotely piloted aircraft, as well as with traditional observations and high-resolution atmospheric simulations. There was an inversion well above mountain top level at about 2 km with weak winds below. Observed winds in the lee of the mountain were indicative of flow locally enhanced by wave activity aloft. Winds descended along the lee slope with a prevailing direction away from the mountain. They were relatively strong and gusty at the surface close to the mountain, with a maximum at low levels, and weakening and becoming more diffuse a short distance further downstream. The winds weakened further aloft, with a minimum on average near mountain top level. This situation is reproduced in a high-resolution atmospheric simulation forced with atmospheric analysis as well as with the observed lee-side profiles of wind and temperature below 1.4 km. Without the additional observations consisting of the lee-side profiles, the model fails to reproduce the winds aloft as well as at the surface in a region in the lee of the mountain, as was also the case for the operational numerical models at that time. A sensitivity simulation indicates that this poor performance is a result of the poorly captured strength and sharpness of the inversion aloft. The study illustrates, firstly, that even at very low wind speed, in a close to neutral low-level flow, gravity waves may still be a dominating feature of the flow. Secondly, the study presents an example of the usefulness of lee-side atmospheric profiles, retrieved by simple model aircraft, for improving numerical simulations and short-term weather forecasting in the vicinity of mountains. Thirdly, the study confirms the sensitivity of downslope flow to only moderate change in the sharpness of an upstream inversion.en_US
dc.publisherTaylor and Francisen_US
dc.rightsNavngivelse 4.0 Internasjonal*
dc.titleThe impact of assimilating data from a remotely piloted aircraft on simulations of weak-wind orographic flowen_US
dc.typeJournal articleen_US
dc.typePeer revieweden_US
dc.rights.holderCopyright 2014 H. Ágústsson et al.en_US
dc.source.journalTellus A: Dynamic Meteorology and Oceanographyen_US
dc.identifier.citationTellus A: Dynamic Meteorology and Oceanography. 2014, 66 (1), 1-15.en_US

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