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000189736 037__ $$aFZJ-2015-02768
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000189736 1001_ $$0P:(DE-HGF)0$$aLothon, M.$$b0$$eCorresponding Author
000189736 245__ $$aThe BLLAST field experiment: Boundary-Layer Late Afternoon and Sunset Turbulence
000189736 260__ $$aKatlenburg-Lindau$$bEGU$$c2014
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000189736 520__ $$aDue to the major role of the sun in heating the earth's surface, the atmospheric planetary boundary layer over land is inherently marked by a diurnal cycle. The afternoon transition, the period of the day that connects the daytime dry convective boundary layer to the night-time stable boundary layer, still has a number of unanswered scientific questions. This phase of the diurnal cycle is challenging from both modelling and observational perspectives: it is transitory, most of the forcings are small or null and the turbulence regime changes from fully convective, close to homogeneous and isotropic, toward a more heterogeneous and intermittent state.These issues motivated the BLLAST (Boundary-Layer Late Afternoon and Sunset Turbulence) field campaign that was conducted from 14 June to 8 July 2011 in southern France, in an area of complex and heterogeneous terrain. A wide range of instrumented platforms including full-size aircraft, remotely piloted aircraft systems, remote-sensing instruments, radiosoundings, tethered balloons, surface flux stations and various meteorological towers were deployed over different surface types. The boundary layer, from the earth's surface to the free troposphere, was probed during the entire day, with a focus and intense observation periods that were conducted from midday until sunset. The BLLAST field campaign also provided an opportunity to test innovative measurement systems, such as new miniaturized sensors, and a new technique for frequent radiosoundings of the low troposphere.Twelve fair weather days displaying various meteorological conditions were extensively documented during the field experiment. The boundary-layer growth varied from one day to another depending on many contributions including stability, advection, subsidence, the state of the previous day's residual layer, as well as local, meso- or synoptic scale conditions.Ground-based measurements combined with tethered-balloon and airborne observations captured the turbulence decay from the surface throughout the whole boundary layer and documented the evolution of the turbulence characteristic length scales during the transition period.Closely integrated with the field experiment, numerical studies are now underway with a complete hierarchy of models to support the data interpretation and improve the model representations.
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000189736 536__ $$0G:(GEPRIS)139819005$$aDFG project 139819005 - Links between local scale and catchment scale measurements and modelling of gas exchange processes over land surfaces (139819005)$$c139819005$$x2
000189736 588__ $$aDataset connected to CrossRef, juser.fz-juelich.de
000189736 7001_ $$0P:(DE-HGF)0$$aLohou, F.$$b1
000189736 7001_ $$00000-0002-4512-0175$$aPino, D.$$b2
000189736 7001_ $$0P:(DE-HGF)0$$aCouvreux, F.$$b3
000189736 7001_ $$0P:(DE-HGF)0$$aPardyjak, E. R.$$b4
000189736 7001_ $$0P:(DE-HGF)0$$aReuder, J.$$b5
000189736 7001_ $$0P:(DE-HGF)0$$aVilà-Guerau de Arellano, J.$$b6
000189736 7001_ $$0P:(DE-HGF)0$$aDurand, P.$$b7
000189736 7001_ $$0P:(DE-HGF)0$$aHartogensis, O.$$b8
000189736 7001_ $$0P:(DE-HGF)0$$aLegain, D.$$b9
000189736 7001_ $$0P:(DE-HGF)0$$aAugustin, P.$$b10
000189736 7001_ $$0P:(DE-HGF)0$$aGioli, B.$$b11
000189736 7001_ $$0P:(DE-HGF)0$$aLenschow, D. H.$$b12
000189736 7001_ $$0P:(DE-HGF)0$$aFaloona, I.$$b13
000189736 7001_ $$0P:(DE-HGF)0$$aYagüe, C.$$b14
000189736 7001_ $$0P:(DE-HGF)0$$aAlexander, D. C.$$b15
000189736 7001_ $$0P:(DE-HGF)0$$aAngevine, W. M.$$b16
000189736 7001_ $$0P:(DE-HGF)0$$aBargain, E.$$b17
000189736 7001_ $$0P:(DE-HGF)0$$aBarrié, J.$$b18
000189736 7001_ $$0P:(DE-HGF)0$$aBazile, E.$$b19
000189736 7001_ $$0P:(DE-HGF)0$$aBezombes, Y.$$b20
000189736 7001_ $$0P:(DE-HGF)0$$aBlay-Carreras, E.$$b21
000189736 7001_ $$0P:(DE-HGF)0$$avan de Boer, A.$$b22
000189736 7001_ $$0P:(DE-HGF)0$$aBoichard, J. L.$$b23
000189736 7001_ $$0P:(DE-HGF)0$$aBourdon, A.$$b24
000189736 7001_ $$0P:(DE-HGF)0$$aButet, A.$$b25
000189736 7001_ $$0P:(DE-HGF)0$$aCampistron, B.$$b26
000189736 7001_ $$0P:(DE-HGF)0$$ade Coster, O.$$b27
000189736 7001_ $$0P:(DE-HGF)0$$aCuxart, J.$$b28
000189736 7001_ $$0P:(DE-HGF)0$$aDabas, A.$$b29
000189736 7001_ $$0P:(DE-HGF)0$$aDarbieu, C.$$b30
000189736 7001_ $$0P:(DE-HGF)0$$aDeboudt, K.$$b31
000189736 7001_ $$0P:(DE-HGF)0$$aDelbarre, H.$$b32
000189736 7001_ $$0P:(DE-HGF)0$$aDerrien, S.$$b33
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000189736 7001_ $$0P:(DE-HGF)0$$aFourmentin, M.$$b35
000189736 7001_ $$0P:(DE-HGF)0$$aGarai, A.$$b36
000189736 7001_ $$0P:(DE-HGF)0$$aGibert, F.$$b37
000189736 7001_ $$0P:(DE-Juel1)129461$$aGraf, Alexander$$b38
000189736 7001_ $$0P:(DE-HGF)0$$aGroebner, J.$$b39
000189736 7001_ $$0P:(DE-HGF)0$$aGuichard, F.$$b40
000189736 7001_ $$0P:(DE-HGF)0$$aJiménez, M. A.$$b41
000189736 7001_ $$0P:(DE-HGF)0$$aJonassen, M.$$b42
000189736 7001_ $$0P:(DE-HGF)0$$avan den Kroonenberg, A.$$b43
000189736 7001_ $$0P:(DE-HGF)0$$aMagliulo, V.$$b44
000189736 7001_ $$0P:(DE-HGF)0$$aMartin, S.$$b45
000189736 7001_ $$0P:(DE-HGF)0$$aMartinez, D.$$b46
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000189736 7001_ $$0P:(DE-Juel1)130270$$aMoulin, E.$$b50
000189736 7001_ $$0P:(DE-HGF)0$$aPietersen, H. P.$$b51
000189736 7001_ $$00000-0002-8070-7924$$aPiguet, B.$$b52
000189736 7001_ $$0P:(DE-HGF)0$$aPique, E.$$b53
000189736 7001_ $$0P:(DE-HGF)0$$aRomán-Cascón, C.$$b54
000189736 7001_ $$0P:(DE-HGF)0$$aRufin-Soler, C.$$b55
000189736 7001_ $$0P:(DE-HGF)0$$aSaïd, F.$$b56
000189736 7001_ $$0P:(DE-HGF)0$$aSastre-Marugán, M.$$b57
000189736 7001_ $$0P:(DE-HGF)0$$aSeity, Y.$$b58
000189736 7001_ $$00000-0002-5922-8179$$aSteeneveld, G. J.$$b59
000189736 7001_ $$0P:(DE-HGF)0$$aToscano, P.$$b60
000189736 7001_ $$0P:(DE-HGF)0$$aTraullé, O.$$b61
000189736 7001_ $$0P:(DE-HGF)0$$aTzanos, D.$$b62
000189736 7001_ $$0P:(DE-HGF)0$$aWacker, S.$$b63
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000189736 773__ $$0PERI:(DE-600)2069847-1$$a10.5194/acp-14-10931-2014$$gVol. 14, no. 20, p. 10931 - 10960$$n20$$p10931 - 10960$$tAtmospheric chemistry and physics$$v14$$x1680-7324$$y2014
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