Steam cloud characteristics and heat output of fumaroles

The heat transferred to the atmosphere by fumarole clouds is linearly proportional to the cloud area that is visible in vertical air-photos. Using measured outputs of a few accessible fumaroles, the total heat output of all fumaroles in a fumarole field can be assessed from the total area of the ste...

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Bibliographic Details
Published inGeothermics Vol. 30; no. 5; pp. 547 - 559
Main Authors Hochstein, Manfred P, Bromley, Chris J
Format Journal Article
LanguageEnglish
Published Oxford Elsevier Ltd 01.10.2001
Elsevier Science
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Summary:The heat transferred to the atmosphere by fumarole clouds is linearly proportional to the cloud area that is visible in vertical air-photos. Using measured outputs of a few accessible fumaroles, the total heat output of all fumaroles in a fumarole field can be assessed from the total area of the steam clouds. Normalised heat outputs, Q j , and normalised cloud areas, A j , were used as variables. Two surveys of the large Karapiti fumarole field (Wairakei, New Zealand) show that the total heat discharged by fumaroles with cloud areas >10 m 2 was 99 MW and 88 MW in 1999 and 2000, respectively. The output of vents with smaller cloud areas has to be obtained from ground surveys. The method also gives a representative (order of magnitude) estimate of the total heat discharged by fumarole clouds if measurements from a single, large fumarole can be used in conjunction with a recent air-photo.
ISSN:0375-6505
1879-3576
DOI:10.1016/S0375-6505(01)00012-8