Articles | Volume 9, issue 3
https://doi.org/10.5194/amt-9-929-2016
https://doi.org/10.5194/amt-9-929-2016
Research article
 | 
07 Mar 2016
Research article |  | 07 Mar 2016

Controlled weather balloon ascents and descents for atmospheric research and climate monitoring

Andreas Kräuchi, Rolf Philipona, Gonzague Romanens, Dale F. Hurst, Emrys G. Hall, and Allen F. Jordan

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Cited articles

Forster, P. M. F. and Shine, K. P.: Assessing the climate impact of trends in stratospheric water vapour, Geophys. Res. Lett., 29, 1086, https://doi.org/10.1029/2001GL013909, 2002.
GCOS-112: GCOS Reference Upper-Air Network (GRUAN): Justification, requirements, siting and instrumentation options, Technical Document 112, WMO TD No. 1379, 25 pp., https://www.wmo.int/pages/prog/gcos/Publications/gcos-112.pdf, 2007.
Hergesell, H.: Ballon-Aufstiege über dem freien Meere zur Erforschung der Temperatur und der Feuchtigkeitsverhältnisse sowie der Luftströmung bis zu sehr grossen Höhen der Atmosphäre, Beitr. Phys. frei. Atmos., 1, 200–204, 1906.
Hermite, G.: Exploration des hautes régions de l'atmosphère à l'aide de ballons non montés, pourvus d'enregistreurs automatiques, Compt. Rend. Séances Acad. Sci., Paris, 115, 862–864, 1892.
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Short summary
In situ upper-air measurements are often made with instruments attached to weather balloons launched at the surface and lifted into the stratosphere. It has been demonstrated that ascending weather balloons can perturb the air measured by very sensitive humidity and temperature sensors trailing behind them. The use of controlled balloon descent for such measurements has therefore been investigated and is described here. We present two different methods and show advantages and disadvantages.
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