Articles | Volume 15, issue 12
Atmos. Chem. Phys., 15, 6981–6991, 2015

Special issue: The Boundary-Layer Late Afternoon and Sunset Turbulence (BLLAST)...

Atmos. Chem. Phys., 15, 6981–6991, 2015
Research article
29 Jun 2015
Research article | 29 Jun 2015

Lifted temperature minimum during the atmospheric evening transition

E. Blay-Carreras et al.

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The BLLAST field experiment: Boundary-Layer Late Afternoon and Sunset Turbulence
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Cited articles

Arya, S. P.: Introduction to Micrometeorology, Academic Press, San Diego, USA. 420 pp., 2001.
Bhat, G. S.: Near-surface temperature inversion over the Arabian Sea due to natural aerosols, Geophys. Res. Lett., 33, L02802,, 2006.
Campbell, G. C.: Measurement of air temperature fluctuations with thermocouples, Atmospheric Sciences Laboratory, White Sands Missile Range, ECOM-5273, 10 pp., 1969.
Campbell, G. S. and Norman, J. (Eds.): An Introduction to Enviromental Biophysics, Springer, 2 Edn., 1998.
De Coster, O. M. Y. and Pietersen, H. P.: BLLAST-uniform processing of Eddy-Covariance data, Internship Report Meteorology and Climatology, Wageningen University and Research Center, the Netherlands, 30 pp., available at:, 2011.
Short 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.
Final-revised paper