Role of the residual layer and large-scale subsidence on the development and evolution of the convective boundary layer
Atmos. Chem. Phys., 14, 4515-4530, 2014
Land surface spinup for episodic modeling
Atmos. Chem. Phys., 14, 8165-8172, 2014
Countergradient heat flux observations during the evening transition period
Atmos. Chem. Phys., 14, 9077-9085, 2014
The BLLAST field experiment: Boundary-Layer Late Afternoon and Sunset Turbulence
Atmos. Chem. Phys., 14, 10931-10960, 2014
Study of a prototypical convective boundary layer observed during BLLAST: contributions by large-scale forcings
Atmos. Chem. Phys., 15, 4241-4257, 2015
Lifted temperature minimum during the atmospheric evening transition
Summary: The study shows that lifted temperature minimum can be detected under calm conditions during the day-night transition, several hours earlier than reported in previous work. These conditions are fulfilled under weak synoptic forcing during local flow shifts associated with a mountain-plain complex orography. Under these special conditions, turbulence and radiation becomes a crucial parameter in determining the ideal conditions for observing LTM measurements.
Atmos. Chem. Phys., 15, 6981-6991, 2015
A comprehensive investigation on afternoon transition of the atmospheric boundary layer over a tropical rural site
Summary: The afternoon-evening transition (AET) in the atmospheric boundary layer has been studied in an integrated approach using 3 years of tower, sodar and wind profiler measurements. Such a long-term data set has been used for the first time to understand the behavior of AET. It allowed us to study the seasonal variation. In contrast to the common belief that the transition evolves from bottom to top, the present study clearly showed that the start time of transition follows top-to-bottom evolution.
Atmos. Chem. Phys., 15, 7605-7617, 2015
Interactions among drainage flows, gravity waves and turbulence: a BLLAST case study
Summary: Stable-boundary-layer processes have been analysed using BLLAST data. Shallow drainage flows were formed at some locations after the near calm stage of the late afternoon. This stage ended with the arrival of a deeper wind associated with the mountain-plain circulation. At the same time, gravity waves were detected with an array of microbarometers. The interaction of these processes with turbulence was studied through multi-resolution flux decomposition at different sites and heights.
Atmos. Chem. Phys., 15, 9031-9047, 2015