Oscillations in atmospheric water above Switzerland

Cloud fraction (CF), integrated liquid water (ILW) and integrated water vapour (IWV) were continuously measured from 2004 to 2016 by the TROpospheric WAter RAdiometer (TROWARA) in Bern, Switzerland. There are indications for interannual variations of CF and ILW. A spectral analysis shows that IW...

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Main Authors: K. Hocke, F. Navas-Guzmán, L. Moreira, L. Bernet, C. Mätzler
Format: Article
Language:English
Published: Copernicus Publications 2017-10-01
Series:Atmospheric Chemistry and Physics
Online Access:https://www.atmos-chem-phys.net/17/12121/2017/acp-17-12121-2017.pdf
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spelling doaj-17d2a96cb2544ef8857cf7718c069c422020-11-24T23:24:45ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242017-10-0117121211213110.5194/acp-17-12121-2017Oscillations in atmospheric water above SwitzerlandK. Hocke0K. Hocke1F. Navas-Guzmán2L. Moreira3L. Bernet4L. Bernet5C. Mätzler6C. Mätzler7Institute of Applied Physics, University of Bern, Bern, SwitzerlandOeschger Centre for Climate Change Research, University of Bern, Bern, SwitzerlandInstitute of Applied Physics, University of Bern, Bern, SwitzerlandInstitute of Applied Physics, University of Bern, Bern, SwitzerlandInstitute of Applied Physics, University of Bern, Bern, SwitzerlandOeschger Centre for Climate Change Research, University of Bern, Bern, SwitzerlandInstitute of Applied Physics, University of Bern, Bern, SwitzerlandOeschger Centre for Climate Change Research, University of Bern, Bern, SwitzerlandCloud fraction (CF), integrated liquid water (ILW) and integrated water vapour (IWV) were continuously measured from 2004 to 2016 by the TROpospheric WAter RAdiometer (TROWARA) in Bern, Switzerland. There are indications for interannual variations of CF and ILW. A spectral analysis shows that IWV is dominated by an annual oscillation, leading to an IWV maximum of 24 kg m<sup>−2</sup> in July to August and a minimum of 8 kg m<sup>−2</sup> in February. The seasonal behaviour of CF and ILW is composed by both the annual and the semiannual oscillation. However, the annual oscillation of CF has a maximum in December while the annual oscillation of ILW has a maximum in July. The semiannual oscillations of CF and ILW are strong from 2010 to 2014. The normalized power spectra of ILW and CF show statistically significant spectral components with periods of 76, 85, 97 and 150 days. We find a similarity between the power spectra of ILW and CF with those of zonal wind at 830 hPa (1.5 km) above Bern. Particularly, the occurrence of higher harmonics in the CF and ILW spectra is possibly forced by the behaviour of the lower-tropospheric wind. The mean amplitude spectra of CF, ILW and IWV show increased short-term variability on timescales less than 40 days from spring to fall. We find a weekly cycle of CF and ILW from June to September with increased values on Saturday, Sunday and Monday.https://www.atmos-chem-phys.net/17/12121/2017/acp-17-12121-2017.pdf
collection DOAJ
language English
format Article
sources DOAJ
author K. Hocke
K. Hocke
F. Navas-Guzmán
L. Moreira
L. Bernet
L. Bernet
C. Mätzler
C. Mätzler
spellingShingle K. Hocke
K. Hocke
F. Navas-Guzmán
L. Moreira
L. Bernet
L. Bernet
C. Mätzler
C. Mätzler
Oscillations in atmospheric water above Switzerland
Atmospheric Chemistry and Physics
author_facet K. Hocke
K. Hocke
F. Navas-Guzmán
L. Moreira
L. Bernet
L. Bernet
C. Mätzler
C. Mätzler
author_sort K. Hocke
title Oscillations in atmospheric water above Switzerland
title_short Oscillations in atmospheric water above Switzerland
title_full Oscillations in atmospheric water above Switzerland
title_fullStr Oscillations in atmospheric water above Switzerland
title_full_unstemmed Oscillations in atmospheric water above Switzerland
title_sort oscillations in atmospheric water above switzerland
publisher Copernicus Publications
series Atmospheric Chemistry and Physics
issn 1680-7316
1680-7324
publishDate 2017-10-01
description Cloud fraction (CF), integrated liquid water (ILW) and integrated water vapour (IWV) were continuously measured from 2004 to 2016 by the TROpospheric WAter RAdiometer (TROWARA) in Bern, Switzerland. There are indications for interannual variations of CF and ILW. A spectral analysis shows that IWV is dominated by an annual oscillation, leading to an IWV maximum of 24 kg m<sup>−2</sup> in July to August and a minimum of 8 kg m<sup>−2</sup> in February. The seasonal behaviour of CF and ILW is composed by both the annual and the semiannual oscillation. However, the annual oscillation of CF has a maximum in December while the annual oscillation of ILW has a maximum in July. The semiannual oscillations of CF and ILW are strong from 2010 to 2014. The normalized power spectra of ILW and CF show statistically significant spectral components with periods of 76, 85, 97 and 150 days. We find a similarity between the power spectra of ILW and CF with those of zonal wind at 830 hPa (1.5 km) above Bern. Particularly, the occurrence of higher harmonics in the CF and ILW spectra is possibly forced by the behaviour of the lower-tropospheric wind. The mean amplitude spectra of CF, ILW and IWV show increased short-term variability on timescales less than 40 days from spring to fall. We find a weekly cycle of CF and ILW from June to September with increased values on Saturday, Sunday and Monday.
url https://www.atmos-chem-phys.net/17/12121/2017/acp-17-12121-2017.pdf
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