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  1. Assessing and optimizing the performance of infrasound networks to monitor volcanic eruptions

    We propose a numerical modeling technique based on a frequency-dependent attenuation relation to ...

    D Tailpied, A Le Pichon, E Marchetti, JD Assink, S Vergniolle | Status: published | Journal: Geophys. J. Int. | Volume: 208 | Year: 2017 | First page: 437 | Last page: 448 | doi: 10.1093/gji/ggw400

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  2. Origin of aerosol particles in the mid-latitude and subtropical upper troposphere and lowermost stratosphere from cluster analysis of CARIBIC data

    The origin of aerosol particles in the upper troposphere and lowermost stratosphere over the Eura...

    M Koppe, M Hermann, CAM Brenninkmeijer, J Heintzenberg, H Schlager, T Schuck, F Slemr, D Sprung, PFJ van Velthoven, A Wiedensohler, A Zahn, H Ziereis | Status: published | Journal: Atm. Chem. Phys. | Year: 2009 | First page: 8413 | Last page: 8430 | doi: /www.atmos-chem-phys.net/9/8413/2009/

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  3. Global changes in indices describing moderate temperature extremes from daily climate model data

    S Russo, A Sterl | Status: published | Journal: J. Geophys. Res. | Volume: 116 | Year: 2011 | First page: D03104 | doi: 10.1029/2010JD014727

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  4. Monthly, seasonal and annual temperature reconstructions for Central Europe derived from documentary evidence and instrumental records since AD 1500

    Monthly temperature series for Central Europe back to AD 1500 are developed from documentary inde...

    P Dobrovolny, A Moberg, R Brazdil, C Pfister, R Glaser, R Wilson, A van Engelen, D Limanowka, A Kiss, M Halickova, J Mackova, D Riemann, J Luterbacher, R Bohm | Status: accepted | Journal: Climatic Change | Year: 2009 | doi: DOI 10.1007/s10584-009-9724-x

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  5. The infrasonic signature of the 2009 major Sudden Stratospheric Warming

    The study of infrasound is experiencing a renaissance since it was chosen as a verification techn...

    LG Evers, P Siegmund | Status: published | Journal: Geophys. Res. Lett. | Volume: 36 | Year: 2009 | doi: 10.1029/2009GL041323

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