Pāhoehoe flow cooling, discharge, and coverage rates from thermal image chronometry

Andrew J.L. Harris, Jonathan Dehn, Mike R. James, Christopher Hamilton, Richard Herd, Luigi Lodato, Andrea Steffke

Research output: Contribution to journalArticle

23 Scopus citations

Abstract

Theoretically- and empirically-derived cooling rates for active pāhoehoe lava flows show that surface cooling is controlled by conductive heat loss through a crust that is thickening with the square root of time. The model is based on a linear relationship that links log(time) with surface cooling. This predictable cooling behavior can be used assess the age of recently emplaced sheet flows from their surface temperatures. Using a single thermal image, or image mosaic, this allows quantification of the variation in areal coverage rates and lava discharge rates over 48 hour periods prior to image capture. For pāhoehoe sheet flow at Kīlauea (Hawai'i) this gives coverage rates of 1-5 m2/min at discharge rates of 0.01-0.05 m3/s, increasing to ∼40 m2/min at 0.4-0.5 m3/s. Our thermal chronometry approach represents a quick and easy method of tracking flow advance over a three-day period using a single, thermal snap-shot.

Original languageEnglish (US)
Article numberL19303
JournalGeophysical Research Letters
Volume34
Issue number19
DOIs
StatePublished - Oct 16 2007
Externally publishedYes

ASJC Scopus subject areas

  • Geophysics
  • Earth and Planetary Sciences(all)

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    Harris, A. J. L., Dehn, J., James, M. R., Hamilton, C., Herd, R., Lodato, L., & Steffke, A. (2007). Pāhoehoe flow cooling, discharge, and coverage rates from thermal image chronometry. Geophysical Research Letters, 34(19), [L19303]. https://doi.org/10.1029/2007GL030791