some challenges in modelling volcanic occurrence datambebbing/talks/volcanoes.pdf · completeness...
TRANSCRIPT
Some Challenges in Modelling Volcanic Occurrence Data
Mark BebbingtonIIST & Volcanic Risk Solutions, Massey University
What is an Eruption?• Arrival of solid volcanic products at surface• Events ranging from an individual explosion to
eruptive periods lasting centuries– Includes quiet periods of up to 3 months– Often `stop’ dates go unrecorded.
• `Historical’ eruptions– Presence of observers, monitoring, weather
• `Pre-historical’ eruptions– Dated, radio-carbon (to 50ka, with error ~ 25 to 1000
yr), K-Ar dating (from 50ka, with error ~ 10 to 100 ka).• VEI (Volcanic Explosivity Index)
– a logarithmic `size’ assigned to historical eruptions on the basis of: explosion size; volume; column height; classification; duration; …
CompletenessGlobally, the observance probability rises from 10% in 1500 to 100% in 1980 (assumed).
BUT
– some volcanoes are much better observed
- Big eruptions are much better observed
- what is an eruption?
Data: The good,
Etna flank eruptions: 1970 –Stationary behaviour?
Are time and size of next eruption `predictable’?
Etna: Flank eruptions 1600-Non-stationary?
60 flank eruptions- “known” onset
dates, duration, and volume
- Complete since ~1600 AD
Etna: Summit + Flank 1970-Independence?
12 summit eruptions, onset dates, durations and volumes, complete since 1970?
Any relation to the flank eruptions?
Data: The Bad,
A prediction?- The past behaviour of a volcano is the best predictor of its future activity.
“The repetitive nature of the eruptive activity at Mt St Helens during the last 4000 years, with dormant intervals typically of a few centuries or less, suggests that the current quiet period will not last a 1000 years. Instead, an eruption is likely within the next hundred years, possibly before the end of this century”
- Crandell et al., “Mt St Helens volcano: Recent and future behavior”. Science 187:438-441, 1975
- Mt St Helens erupted in 1980, having been quiescent since 1857
Data: The Ugly
VEI > 3
Vesuvius
Cycles initiated by (sub-) plinian event and terminated by repose of several centuries?
Periodicities
20151050
50
40
30
20
10
0
i
tau
_i
S 14.0130R-Sq 22.0%R-Sq(adj) 11.6%
Fitted Line Plottau_i = 30.32 - 5.096 i + 0.2796 i**2
Radiocarbon Dating• Volcanic products cannot be directly
carbon dated – they were never alive.• Date organic material in (or more often just
under) an eruptive layer. • Dates are given as
N(mu,sigma)• Conversion to
calendar years • Stratigraphic
ordering
Taveuni, Fiji
101 eruptive episodes, individually datedBUT - considerable “rounding”, large error bars
rift volcano – only one spatial dimension
120001000080006000400020000
100
80
60
40
20
0
Years BP
Co
un
t
meanup_bndlow_bnd
Variable
Eruption dates
Taranaki 103 tephras in single core –depths on all, 10 dated individually
Stars = core dates, lines 95% confidence limits
`DODGY’DATE
Taranaki II – 2 cores plus near source
Umutekai104 tephras, c. 1550BP –10100BP
Rotokare45 tephras, c.500BP – 6200BP
Near-source23 tephras, c.90BP – 2200BP
Related cycles of magma-feeding pulses, large eruptions and
eruption frequencyTaranaki
Yucca Mountain40 eruptions in last 10.5Ma. Last 80ka ago.Large error bars, and multiple eruptions with the same estimated age.Widely varying sizes- Probability of disruption of repository in 10ka?
Auckland
49 cones in last 250ka, last two much bigger, especially last (Rangitoto) – 59% of total volume.
Is there any pattern?