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Time‐averaged SO 2 fluxes of subduction‐zone volcanoes: Example of a 32‐year exhaustive survey for Japanese volcanoes
Author(s) -
Mori Toshiya,
Shinohara Hiroshi,
Kazahaya Kohei,
Hirabayashi Junichi,
Matsushima Takeshi,
Mori Takehiko,
Ohwada Michiko,
Odai Masanobu,
Iino Hideki,
Miyashita Makoto
Publication year - 2013
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
eISSN - 2169-8996
pISSN - 2169-897X
DOI - 10.1002/jgrd.50591
Subject(s) - volcano , flux (metallurgy) , geology , subduction , seismology , tectonics , chemistry , organic chemistry
All available SO 2 flux data for 32 years (1975–2006) of Japanese volcanoes, accounting for about 10% of the world's arc volcanoes, were compiled to evaluate the temporal variation of the flux of each volcano and to estimate the time‐averaged SO 2 flux. The compiled data revealed that 6 volcanoes (Tokachi, Asama, Aso, Sakurajima, Satsuma‐Iwojima, and Suwanosejima volcanoes) out of 17 significantly degassing volcanoes usually contributed more than 94% of the total flux. The time‐averaged annual flux was 2.2 Tg a −1 , which includes intense degassing of Miyakejima volcano after 2000, which raised the figure from 1.4 Tg a −1 , indicating that a single huge emitter is capable of significantly skewing regional time‐averaged degassing totals and indicating that the time‐averaged flux assessments for infrequent huge emitters are important for accurate estimation. The regional SO 2 flux distribution in cumulative frequency‐flux plot does not obey a power law distribution. It shows a roll‐off curve bending at about 500 t d −1 , implying that it is misleading to assume the power law distribution for estimation of the global flux. Because the contribution of the major degassing volcanoes including the six volcanoes and additional sporadically degassing volcanoes during eruptive and posteruptive periods to the total flux is more than 95%, measurement of all large flux volcanoes can approximate the global flux.