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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Published in | Geothermics Vol. 30; no. 5; pp. 547 - 559 |
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Main Authors | , |
Format | Journal Article |
Language | English |
Published |
Oxford
Elsevier Ltd
01.10.2001
Elsevier Science |
Subjects | |
Online Access | Get full text |
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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. |
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ISSN: | 0375-6505 1879-3576 |
DOI: | 10.1016/S0375-6505(01)00012-8 |