Abstract
The Boiling Lake of Dominica has exhibited stable high-temperature behavior for at least 150 a. This stability is punctuated by occasional crises involving rapid filling and
draining of the lake and changes in water temperature. The most recent such crisis occurred in December 2004 to April 2005. Using the results of previous theoretical and experimental work on analogue models, we present a combined thermal, hydrological, and fluid mechanical model of the Boiling Lake. This reveals that the lake appears to be suspended above the local water table by a constant supply of rising steam bubbles sourced from the boiling of groundwater near an igneous intrusion. The bubbles condense
in the Boiling Lake, maintaining the temperature at
Translated title of the contribution | Boiling Lake of Dominica, West Indies: High-temperature volcanic crater lake dynamics |
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Original language | English |
Pages (from-to) | B02203 |
Number of pages | 17 |
Journal | Journal of Geophysical Research |
Volume | 114 |
DOIs | |
Publication status | Published - Feb 2009 |