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Measuring Water Vapor and Ash in Volcanic Eruptions with a Millimeter-Wave Radar/Imager

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arxiv 1604.03884 v2 pith:HIMW65KX submitted 2016-04-13 physics.ins-det physics.geo-ph

Measuring Water Vapor and Ash in Volcanic Eruptions with a Millimeter-Wave Radar/Imager

classification physics.ins-det physics.geo-ph
keywords eruptionmeasuremillimeter-waveradarvolcanicwatermeasurementsvapor
verification ladder T0 review T1 audit T2 compute T3 formal T4 reserved
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Millimeter-wave remote sensing technology can significantly improve measurements of volcanic eruptions, yielding new insights into eruption processes and improving forecasts of drifting volcanic ash for aviation safety. Radiometers can measure water vapor density and temperature inside eruption clouds, improving on existing measurements with infrared cameras that are limited to measuring the outer cloud surface. Millimeter-wave radar can measure the 3D mass distribution of volcanic ash inside eruption plumes and their nearby drifting ash clouds. Millimeter wavelengths are better matched to typical ash particle sizes, offering better sensitivity than longer wavelength existing weather radar measurements, as well as the unique ability to directly measure ash particle size in-situ. Here we present sensitivity calculations in the context of developing the WAMS (Water and Ash Millimeter-wave Spectrometer) instrument. WAMS, a radar/radiometer system designed to use off-the-shelf components, would be able to measure water vapor and ash throughout an entire eruption cloud, a unique capability.

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