Periodicity in the BrO/SO2 molar ratios in the volcanic gas plume of Cotopaxi and its correlation with the Earth tides during the eruption in 2015
Artikel i vetenskaplig tidskrift, 2018
time series is too short to rule out a chance recurrence of transient geological or meteorological events as a possible origin for the periodic signal, we nevertheless took this observation
as a motivation to examine the influence of natural forcings with periodicities of around 2 weeks on volcanic gas emissions. One strong aspirant with such a periodicity are the
Earth tides, which are thus central in this study. We present the BrO=SO2 data, analyse the reliability of the periodic signal, discuss a possible meteorological or eruption-induced origin of this signal, and compare the signal with the theoretical ground surface displacement pattern caused by the Earth tides. Our central result is the observation of a significant correlation between the BrO=SO2 molar ratios with the north–south and vertical components of the calculated tideinduced surface displacement with correlation coefficients of 47 and 36 %, respectively. From all other investigated parameters, only the correlation between the BrO=SO2 molar ratios and the relative humidity in the local atmosphere resulted in a comparable correlation coefficient of about 33 %.
Författare
Florian Dinger
Universität Heidelberg
Nicole Bobrowski
Universität Heidelberg
Simon Warnach
Universität Heidelberg
Stefan Bredemeyer
Helmholtz
Silvana Hidalgo
Santiago Arellano
Chalmers, Rymd-, geo- och miljövetenskap, Mikrovågs- och optisk fjärranalys
Bo Galle
Chalmers, Rymd-, geo- och miljövetenskap, Mikrovågs- och optisk fjärranalys
Ulrich Platt
Universität Heidelberg
Thomas Wagner
Max-Planck-Gesellschaft
Solid Earth
1869-9510 (ISSN) 1869-9529 (eISSN)
Vol. 9 2 247-266Fundament
Grundläggande vetenskaper
Ämneskategorier
Geovetenskap och miljövetenskap
Geofysik
DOI
10.5194/se-9-247-2018