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Study of a prototypical convective boundary layer observed during BLLAST: contributions by large-scale forcings
by
de Coster, O.
, Pietersen, H. P.
, Hartogensis, O.
, Augustin, P.
, Delbarre, H.
, Pino, D.
, Ouwersloot, H. G.
, Lohou, F.
, Vilà-Guerau de Arellano, J.
, Reuder, J.
, Fourmentin, M.
, Gioli, B.
, van de Boer, A.
, Durand, P.
, Lothon, M.
in
Analysis
/ decay
/ Dynamic meteorology
/ entrainment
/ large-eddy simulation
/ radiation
/ transition
/ turbulence
/ Turbulence (Fluid dynamics)
2015
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Study of a prototypical convective boundary layer observed during BLLAST: contributions by large-scale forcings
by
de Coster, O.
, Pietersen, H. P.
, Hartogensis, O.
, Augustin, P.
, Delbarre, H.
, Pino, D.
, Ouwersloot, H. G.
, Lohou, F.
, Vilà-Guerau de Arellano, J.
, Reuder, J.
, Fourmentin, M.
, Gioli, B.
, van de Boer, A.
, Durand, P.
, Lothon, M.
in
Analysis
/ decay
/ Dynamic meteorology
/ entrainment
/ large-eddy simulation
/ radiation
/ transition
/ turbulence
/ Turbulence (Fluid dynamics)
2015
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Study of a prototypical convective boundary layer observed during BLLAST: contributions by large-scale forcings
by
de Coster, O.
, Pietersen, H. P.
, Hartogensis, O.
, Augustin, P.
, Delbarre, H.
, Pino, D.
, Ouwersloot, H. G.
, Lohou, F.
, Vilà-Guerau de Arellano, J.
, Reuder, J.
, Fourmentin, M.
, Gioli, B.
, van de Boer, A.
, Durand, P.
, Lothon, M.
in
Analysis
/ decay
/ Dynamic meteorology
/ entrainment
/ large-eddy simulation
/ radiation
/ transition
/ turbulence
/ Turbulence (Fluid dynamics)
2015
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Study of a prototypical convective boundary layer observed during BLLAST: contributions by large-scale forcings
Journal Article
Study of a prototypical convective boundary layer observed during BLLAST: contributions by large-scale forcings
2015
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Overview
We study the influence of the large-scale atmospheric contribution to the dynamics of the convective boundary layer (CBL) in a situation observed during the Boundary Layer Late Afternoon and Sunset Turbulence (BLLAST) field campaign. We employ two modeling approaches, the mixed-layer theory and large-eddy simulation (LES), with a complete data set of surface and upper-air atmospheric observations, to quantify the contributions of the advection of heat and moisture, and subsidence. We find that by only taking surface and entrainment fluxes into account, the boundary-layer height is overestimated by 70%. Constrained by surface and upper-air observations, we infer the large-scale vertical motions and horizontal advection of heat and moisture. Our findings show that subsidence has a clear diurnal pattern. Supported by the presence of a nearby mountain range, this pattern suggests that not only synoptic scales exert their influence on the boundary layer, but also mesoscale circulations. LES results show a satisfactory correspondence of the vertical structure of turbulent variables with observations. We also find that when large-scale advection and subsidence are included in the simulation, the values for turbulent kinetic energy are lower than without these large-scale forcings. We conclude that the prototypical CBL is a valid representation of the boundary-layer dynamics near regions characterized by complex topography and small-scale surface heterogeneity, provided that surface- and large-scale forcings are representative for the local boundary layer.
Publisher
Copernicus GmbH,Copernicus Publications
Subject
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