Barbara Scherllin-Pirscher

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[1] The vertical and spatial structure of the atmospheric El Niño-Southern Oscillation (ENSO) signal is investigated using radio occultation (RO) data from August 2006 to December 2010. Due to their high vertical resolution and global coverage, RO data are well suited to describe the full 3-dimensional ENSO structure in the troposphere and lower(More)
Key Points: • Extratropical wind fields were derived from GPS radio occultation (RO) data • RO geostrophic and gradient winds well represent actual 3-D wind fields • The monthly mean RO wind fields are, in general, accurate to within 2 m/s (2014), Deriving dynamics from GPS radio occultation: Three-dimensional wind fields for monitoring the climate,(More)
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