ACP Atmospheric Chemistry and Physics ACP 1680-7324 Copernicus GmbH Göttingen, Germany 10.5194/acp-4-2171-2004 Ground-based water vapour soundings by microwave radiometry and Raman lidar on Jungfraujoch (Swiss Alps) Gerber D. 1 Balin I. 2 Feist D. G. 1 Kämpfer N. 1 Simeonov V. 2 Calpini B. 2 3 van den Bergh H. 2 Institute of Applied Physics, University of Bern, Switzerland Laboratory of Air Pollution, Swiss Federal Institute of Technology – Lausanne (EPFL), Lausanne, Switzerland now at: MétéoSuisse, Payerne Station, Switzerland 10 11 2004 4 8 2171 2179 This is an open-access article ditributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited. This article is available from http://www.atmos-chem-phys.net/4/2171/2004/acp-4-2171-2004.html The full text article is available as a PDF file from http://www.atmos-chem-phys.net/4/2171/2004/acp-4-2171-2004.pdf

Water vapour has been measured from the International Scientific Station Jungfraujoch (ISSJ, 47° N, 7° E, 3580m above sea level) during the winters of 1999/2000 and 2000/2001 by microwave radiometry and Raman lidar. The abundance of atmospheric water vapour between the planetary boundary layer and the upper stratosphere varies over more than three orders of magnitude. The currently used measurement techniques are only suited to determine the abundance of water vapour in different atmospheric regimes. None can resolve the vertical distribution profile from ground level to the top of the stratosphere by itself. We present such a water vapour profile where simultaneous measurements from a Raman lidar and a microwave radiometer were combined to cover both the troposphere and the stratosphere, respectively. We also present a study of the stratospheric and tropospheric water vapour variability for the two consecutive winters.