Gierens, Rosa T., Henriksson, Svante, Josipovic, Micky, Vakkari, Ville, van Zyl, Pieter G., Beukes, Johan P., Wood, Curtis R. and O'Connor, Ewan J. (2019). Observing continental boundary-layer structure and evolution over the South African savannah using a ceilometer. Theor. Appl. Climatol., 136 (1-2). S. 333 - 347. WIEN: SPRINGER WIEN. ISSN 1434-4483

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Abstract

The atmospheric boundary layer (BL) is the atmospheric layer coupled to the Earth's surface at relatively short timescales. A key quantity is the BL depth, which is important in many applied areas of weather and climate such as air-quality forecasting. Studying BLs in climates and biomes across the globe is important, particularly in the under-sampled southern hemisphere. The present study is based on a grazed grassland-savannah area in northwestern South Africa during October 2012-August 2014. Ceilometers are probably the cheapest method for measuring continuous aerosol profiles up to several kilometers above ground and are thus an ideal tool for long-term studies of BLs. A ceilometer-estimated BL depth is based on profiles of attenuated backscattering coefficients from atmospheric aerosols; the sharpest drop often occurs at BL top. Based on this, we developed a new method for layer detection that we call the signal-limited layer method. The new algorithm was applied to ceilometer profiles which thus classified BL into classic regime types: daytime convective mixing, and a double layer at night of surface-based stable with a residual layer above it. We employed wavelet fitting to increase successful BL estimation for noisy profiles. The layer-detection algorithm was supported by an eddy-flux station, rain gauges, and manual inspection. Diurnal cycles were often clear, with BL depth detected for 50% of the daytime typically being 1-3 km, and for 80% of the night-time typically being a few hundred meters. Variability was also analyzed with respect to seasons and years. Finally, BL depths were compared with ERA-Interim estimates of BL depth to show reassuring agreement.

Item Type: Journal Article
Creators:
CreatorsEmailORCIDORCID Put Code
Gierens, Rosa T.UNSPECIFIEDUNSPECIFIEDUNSPECIFIED
Henriksson, SvanteUNSPECIFIEDUNSPECIFIEDUNSPECIFIED
Josipovic, MickyUNSPECIFIEDUNSPECIFIEDUNSPECIFIED
Vakkari, VilleUNSPECIFIEDUNSPECIFIEDUNSPECIFIED
van Zyl, Pieter G.UNSPECIFIEDUNSPECIFIEDUNSPECIFIED
Beukes, Johan P.UNSPECIFIEDUNSPECIFIEDUNSPECIFIED
Wood, Curtis R.UNSPECIFIEDUNSPECIFIEDUNSPECIFIED
O'Connor, Ewan J.UNSPECIFIEDUNSPECIFIEDUNSPECIFIED
URN: urn:nbn:de:hbz:38-151814
DOI: 10.1007/s00704-018-2484-7
Journal or Publication Title: Theor. Appl. Climatol.
Volume: 136
Number: 1-2
Page Range: S. 333 - 347
Date: 2019
Publisher: SPRINGER WIEN
Place of Publication: WIEN
ISSN: 1434-4483
Language: English
Faculty: Unspecified
Divisions: Unspecified
Subjects: no entry
Uncontrolled Keywords:
KeywordsLanguage
MIXING-HEIGHT; DOPPLER LIDAR; RETRIEVAL; PROFILES; AEROSOLS; VARIABILITY; PARTICLES; POLLUTION; TRENDS; CLOUDMultiple languages
Meteorology & Atmospheric SciencesMultiple languages
Refereed: Yes
URI: http://kups.ub.uni-koeln.de/id/eprint/15181

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