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Seismometer Self-Noise and Measuring Methods
Seismometer self-noise is usually not considered when selecting and using seismic waveform data i...
AT Ringler, R Sleeman, CR Hutt, LS Gee | Status: published | Journal: Encyclopedia of Earthquake Engineering | Year: 2014 | doi: /10.1007/978-3-642-36197-5_175-1
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The stratospheric arrival pair in infrasound propagation
The ideal case of a deep and well-formed stratospheric duct for long range infrasound propagation...
R Waxler, L Evers, J Assink, P Blom | Status: published | Journal: J.A.S.A. | Volume: 137 | Year: 2015 | First page: 1846 | doi: /10.1121/1.4916718
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On gustiness and growth of ocean waves
The effect of gustiness on the growth of ocean waves in the WAM model, a third generation ocean ...
G Burgers, R Kraan, W Oost, L Cavaleri | Year: 1990 | Pages: 17
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How big is an OMI pixel?
The Ozone Monitoring Instrument (OMI) is a
push-broom imaging spectrometer, observing solar...
M de Graaf, H Sihler, LG Tilstra, P Stammes | Status: published | Journal: Atmospheric Measurement Techniques | Volume: 9 | Year: 2016 | First page: 3607 | Last page: 3618 | doi: 10.5194/amt-9-3607-2016
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Future changes in atmospheric rivers and extreme precipitation in Norway
Flooding events associated with extreme precipitation have had large impacts in Norway. It is wel...
K Whan, J Sillmann, N Schaller, R Haarsma | Status: published | Journal: Clim. Dyn. | Year: 2020 | doi: https://doi.org/10.1007/s00382-019-05099-z
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