USGS ScienceSearch

Geology topics

Andrew J.S. McGonigle

Publications and source records attributed to Andrew J.S. McGonigle.

2 recordsLinked to original sources

A new permanent, low-cost, low-power SO2 camera for continuous measurement of volcanic emissions

Since its introduction to volcanology in the mid-2000 s, the SO 2 camera has become an important instrument for the acquisition of accurate and high time-resolution SO 2 emission rates, aiding in hazard assessment and volcanological research. However, with the exception of a few locations (Stromboli, Etna, Kīlauea), hitherto the majority of measurements have been made on discrete field campaigns, which provide only brief snapshots into a volcano’s activity. Here, we present the development of a new, low-cost, low-power SO 2 camera for permanent deployment on volcanoes, facilitating long-term, quasi-continuous (daylight hours only) measurements. We then discuss preliminary datasets from Lascar and Kīlauea volcanoes, where instruments are now in continuous operation. Further proliferation of such instrumentation has the potential to greatly improve our understanding of the transient nature of volcanic activity, as well as aiding volcano monitoring/eruption forecasting.

Frontiers in Earth Science

Comparison of COSPEC and two miniature ultraviolet spectrometer systems for SO 2 measurements using scattered sunlight

The correlation spectrometer (COSPEC), the principal tool for remote measurements of volcanic SO 2 , is rapidly being replaced by low-cost, miniature, ultraviolet (UV) spectrometers. We compared two of these new systems with a COSPEC by measuring SO 2 column amounts at Kīlauea Volcano, Hawaii. The two systems, one calibrated using in-situ SO 2 cells, and the other using a calibrated laboratory reference spectrum, employ similar spectrometer hardware, but different foreoptics and spectral retrieval algorithms. Accuracy, signal-to-noise, retrieval parameters, and precision were investigated for the two configurations of new miniature spectrometer. Measurements included traverses beneath the plumes from the summit and east rift zone of Kīlauea, and testing with calibration cells of known SO 2 concentration. The results obtained from the different methods were consistent with each other, with <8% difference in estimated SO 2 column amounts up to 800 ppm m. A further comparison between the COSPEC and one of the miniature spectrometer configurations, the &lsquo;FLYSPEC&rsquo;, spans an eight month period and showed agreement of measured emission rates to within 10% for SO 2 column amounts up to 1,600 ppm m. The topic of measuring high SO 2 burdens accurately is addressed for the Kīlauea measurements. In comparing the foreoptics, retrieval methods, and resultant implications for data quality, we aim to consolidate the various experiences to date, and improve the application and development of miniature spectrometer systems.`

Bulletin of Volcanology