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Volume 15, issue 12 | Copyright

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

Atmos. Chem. Phys., 15, 6981-6991, 2015
https://doi.org/10.5194/acp-15-6981-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 29 Jun 2015

Research article | 29 Jun 2015

Lifted temperature minimum during the atmospheric evening transition

E. Blay-Carreras1, E. R. Pardyjak2, D. Pino1,3, S. W. Hoch4, J. Cuxart5, D. Martínez6, and J. Reuder7 E. Blay-Carreras et al.
  • 1Department of Applied Physics, Universitat Politècnica de Catalunya, BarcelonaTech, Barcelona, Spain
  • 2Department of Mechanical Engineering, University of Utah, Salt Lake City, UT, USA
  • 3Institute for Space Studies of Catalonia (IEEC–UPC), Barcelona, Spain
  • 4Department of Atmospheric Sciences, University of Utah, Salt Lake City, UT, USA
  • 5Grup de Meteorologia, Departament de Física, Universitat de les Illes Balears, Palma de Mallorca, Spain
  • 6Center for Applied Geoscience, University of Tübingen, Tübingen, Germany
  • 7Geophysical Institute, University of Bergen, Bergen, Norway

Abstract. Observations of lifted temperature minimum (LTM) profiles in the nocturnal boundary layer were first reported in 1932. It was defined by the existence of a temperature minimum some centimetres above the ground. During the following decades, several research studies analysed this phenomenon verifying its existence and postulating different hypotheses about its origin.

The aim of this work is to study the existence and characteristics of LTM during the evening transition by using observations obtained during the Boundary Layer Late Afternoon and Sunset Turbulence (BLLAST) campaign. Data obtained from two masts instrumented with thermocouples and wind sensors at different heights close to the ground and a mast with radiometers are used to study the role of mechanical turbulence and radiation in LTM development.

The study shows that LTM 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 when the local flow shifts associated with a mountain–plain circulation in relatively complex orography. Under these special conditions, turbulence becomes a crucial parameter in determining the ideal conditions for observing LTM. Additionally, LTM observed profiles are also related to a change in the atmospheric radiative characteristics under calm conditions.

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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.
The study shows that lifted temperature minimum can be detected under calm conditions during the...
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