TY - JOUR
T1 - Probabilistic analysis of rockfall frequencies during an andesite lava dome eruption
T2 - The Soufrière Hills Volcano, Montserrat
AU - Calder, E.S.
AU - Cortés, J.A.
AU - Palma, J.L.
AU - Luckett, R.
PY - 2005/8/28
Y1 - 2005/8/28
N2 - A probabilistic analysis of rockfalls has been undertaken using seismometer-determined information on the timing and duration of rockfalls from the Soufrière Hills lava dome, Montserrat, between 1995 and 1997. Repose intervals between rockfalls fit log logistic survivor distributions. Differences in the log logistic survivor function for different sub-sets of data are accommodated by variation of the parameter k, which varies from 0.7 to 1.6, and sample median, μ. When extrusion rate is assumed to be ≈0 m/s, k is ≤1 denoting that the hazard function has a continuously decreasing form, contrasting to the hazard maximum present during periods of extrusion. This analysis illustrates a direct relationship between k, μ, and lava extrusion rate. Extrusion rate becomes increasingly significant in determining rockfall frequencies when rates are relatively high, whereas other factors become increasingly significant when rates are low.
AB - A probabilistic analysis of rockfalls has been undertaken using seismometer-determined information on the timing and duration of rockfalls from the Soufrière Hills lava dome, Montserrat, between 1995 and 1997. Repose intervals between rockfalls fit log logistic survivor distributions. Differences in the log logistic survivor function for different sub-sets of data are accommodated by variation of the parameter k, which varies from 0.7 to 1.6, and sample median, μ. When extrusion rate is assumed to be ≈0 m/s, k is ≤1 denoting that the hazard function has a continuously decreasing form, contrasting to the hazard maximum present during periods of extrusion. This analysis illustrates a direct relationship between k, μ, and lava extrusion rate. Extrusion rate becomes increasingly significant in determining rockfall frequencies when rates are relatively high, whereas other factors become increasingly significant when rates are low.
UR - http://www.scopus.com/inward/record.url?eid=2-s2.0-26844559986&partnerID=8YFLogxK
U2 - 10.1029/2005GL023594
DO - 10.1029/2005GL023594
M3 - Article
AN - SCOPUS:26844559986
SN - 0094-8276
VL - 32
SP - 1
EP - 4
JO - Geophysical Research Letters
JF - Geophysical Research Letters
IS - 16
M1 - L16309
ER -