Airborne detection of diffuse carbon dioxide emissions at Mammoth Mountain, California

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Abstract

We report the first airborne detection of CO2 degassing from diffuse volcanic sources. Airborne measurement of diffuse CO2 degassing offers a rapid alternative for monitoring CO2 emission rates at Mammoth Mountain. CO2 concentrations, temperatures, and barometric pressures were measured at ~2,500 GPS-referenced locations during a one-hour, eleven-orbit survey of air around Mammoth Mountain at ~3 km from the summit and altitudes of 2,895-3,657 m. A volcanic CO2 anomaly 4-5 km across with CO2 levels ~1 ppm above background was revealed downwind of tree-kill areas. It contained a 1-km core with concentrations exceeding background by >3 ppm. Emission rates of ~250 t d-1 are indicated. Orographic winds may play a key role in transporting the diffusely degassed CO2 upslope to elevations where it is lofted into the regional wind system.

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Gerlach, T. M., Doukas, M. P., McGee, K. A., & Kessler, R. (1999). Airborne detection of diffuse carbon dioxide emissions at Mammoth Mountain, California. Geophysical Research Letters, 26(24), 3661–3664. https://doi.org/10.1029/1999GL008388

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