Title: WP6
1WP6
- Monitoring Earthquakes and Related Environmental
Hazards
2WP6 Monitoring Earthquakes and Related
Environmental Hazards
- Participants
- CDCS J.Kurths
- ENS M.Ghil
- IGRA D. Zugravescu, L.Asimopolos, N.Cadicheanu,
C.Diacopolos, M.Ivascu, A.Marin, M.Popescu,
D.Stanica, M.Tatu. - IPGP J.-L.Le Mouël, M.Mandea, C.Narteau
- MITPAN V.Kossobokov, G.Molchan, O.Novikova,
L.Romashkova, P.Shebalin, A.Soloviev, I.Vorobieva
- ULG M.Ausloos, F.Petroni
- IGPP V.Keilis-Borok, I.Zaliapin
- Constituents of the Work Package
- Models of seismicity
- Observational
- Data set network
- Earthquake Real-time
- prediction earthquake
- algorithms prediction
3WP6 Data Set (MITPAN, IGRA)
- Vrancea (Romania) is a geographical region
between Eastern and Southern Carpathian
Mountains. The region is characterized by a
rather high level of seismic activity mainly at
intermediate (up to 200 km) depths. These
intermediate-depth earthquakes occur between
45o-46oN and 26o-27oE. The shallow earthquakes
are dispersed over much broader territory. - The dataset on seismic activity has been compiled
using several available sources. This dataset
contains the earthquake catalogue for the Vrancea
region that covers period 1900-2005. Since 1962
the catalogue is complete for magnitude M 3.0
and since 1980 it is complete for M 2.5. - The comparative analysis of earthquake catalogues
available for Vrancea region has been performed
aiming at compilation of a data set, as much
complete and homogeneous as possible, which,
hopefully, will be used for prediction of strong
and possibly moderate earthquakes in the region.
The two catalogues under study are 1) Global
Hypocenter Data Base catalogue, NEIC and 2) local
Vrancea seismic catalogue. - This data set is continued by the RomPlus
earthquake catalogue that is compiled at the
National Institute of Earth Physics (Magurele
Romania). Starting from April 2006 the IGRA
provides monthly update of this catalogue.
4Earthquakes in Vrancea and vicinities reported in
GHDB, 1962-2004All events
Events at depths of 60 km or more
5The annual number of earthquakes from the local
Vrancea catalogue, 1930-2005
6Gutenberg-Richter graphs for different versions
of the Vrancea catalogue
7WP6 Earthquake Prediction Algorithms (MITPAN,
IGPP)
- The intermediate-term earthquake prediction
algorithm M8 are improved and modified to apply
it to the Vrancea region for prediction of
earthquakes with magnitude 6.5 or higher. - The new short-term prediction algorithm based on
chains of earthquakes as short-term precursors of
strong earthquakes and the earthquake prediction
methodology named Reverse Detection of
Precursors (RDP) is adapted for prediction of
Vrancea earthquakes.
8WP6 Real-time Earthquake Prediction (IGRA,
MITPAN, IGPP)
- The real-time prediction experiment by means of
M8 algorithm has been launched in the region. - Alarm for a strong (M 6.5) earthquake has been
declared for the five-year period starting from
July 2006.
9WP6 Observational Network (IGRA)
- Specific pattern recognition of the test sites
for continuous monitoring of the short-term
precursory phenomena of the tectonic activity
(earthquakes, active faults and landslides
associated) has been made. - The adequate equipment has been installed in two
relevant geodynamic test sites (Surlari
Observatory for short term precursory parameters
and Provita de Sus landslide test site). - Continuous monitoring of geophysical fields in
order to reveal the short-term precursory
phenomena of the tectonic activity (earthquakes,
active faults and landslides associated) has been
launched.
10WP6 Models of Seismicity (CDCS, ENS, IPGP,
MITPAN, ULG, IGPP)
- cellular automata that include long-range, as
well as nearest-neighbour interactions - scaling organization of fracture tectonics
(SOFT) - colliding cascades model
- model of block-and-fault system dynamics
- accounting for the fracture growth process and
interactions between different faulting
mechanisms in the determining the seismogenic
potential of active tectonic zones
11Study of Vrancea seismicity
- Temporal properties of seismicity in Vrancea have
been studied in order to estimate the hazard rate
distribution of the largest seismic events. - The average return period of the largest events
has been estimated on the basis of Generalized
Extreme Value techniques. Then, scaling
properties of recurrence times between
earthquakes have been studied in appropriate
spatial volumes. - It has been found that the seismicity is
temporary clustered, and the distribution of
recurrence times is significantly different from
a Poisson process even for times largely
exceeding corresponding periods of foreshock and
aftershock activity. - Modelling such a clustering by gamma distribution
of recurrence times gives possibility to estimate
hazard rates now depending on the time elapsed
from the last large earthquake.
12Simplified SOFT model
- Strain accumulation rates inferred from
aftershocks have been studied. - The Limited Power Law (LPL) model of the
aftershock decay derived from the SOFT model
suggests that the delay of the power-law decay
of aftershocks depends on the heterogeneity of
the stress field the larger stresses exist, the
shorter is this delay. This delay has been
estimated by considering stacked aftershock
sequences from moderate main shocks in some
volume (for example, a system of faults,
different time intervals). - A strong correlation of this delay with the focal
mechanism (rake angle) of the main shocks has
been found.
13A new model of rupture
- A hierarchical model of rupture incorporating
healing and faulting has been developed. - The seismicity obtained in the model demonstrates
the main characteristics of the observed
seismicity Gutenberg-Richter law for the
frequency-magnitude relationship, Omori law for
the aftershock decay rate, clustering of major
events, swarms of earthquakes, seismicity of
creeping segment and seismic noise. - A new multiscale cellular automation model of
rupture has been designed to reproduce structural
patterns observed in the formation and evolution
of a population of strike-slip faults.
14BLOCK MODEL OF THE VRANCEA REGION
KINEMATIC MODEL (after V.I.Mocanu)
BLOCK STRUCTURE
15COMPARISON BETWEEN MODEL AND OBSERVED SEISMICITY
MAP OF VRANCEA SEISMICITY
MODEL EPICENTERS
16New Version of the Block Model for Vrancea
17WP7
Socio-Economic Barometer
18WP7 Socio-Economic Barometer
- Participants
- CDCS J.Kurths
- CEPS G.Schaber, P.Liégeois, P.Van Kerm
- ENS M.Ghil
- MITPAN I.Kuznetsov, A.Mostinskii, M.Rodkin,
A.Soloviev, T.Tseplinskaya, F.Winberg - ULG M.Ausloos, F.Petroni
- IGPP V.Keilis-Borok
- Objective
- Development of a socio-economic barometer that
is the methodology and relevant algorithms and
software for forecasting crises (or stable
development) in socio-economic systems. -
- The forecast will be based on analysis of
relevant socio-economic indicators, which are the
input for the algorithms - The output of the algorithms is a forecast
whether a crisis is or is not approaching the
forecasts will include probabilities of false
alarms and failures to predict - Different algorithms will be needed for
prediction of different crisis types, but for a
given crisis type we plan to develop a
self-adaptive algorithm and relevant software
that can be applied without readaptation in
different territories.
19WP7 Approaches
- At each moment an algorithm indicates whether a
crisis should or should not be expected within
subsequent ? months, ? being duration of alarm.
20WP7 Predicting the End of an Economic Recession
- The problem of predicting the end of an American
economic recession by analysis of macroeconomic
indicators within the recession period has been
considered. The study is a technical analysis
that is a heuristic search of phenomena preceding
the recession end. The methodology of pattern
recognition of infrequent events is used. The
goal is to identify by an analysis of
macroeconomic indicators a robust and rigidly
defined prediction algorithm of the yes or no
variety indicating at any time moment, whether
the recession end should be expected or not
within the subsequent months. A specific
premonitory pattern of six macroeconomic
indicators that may predict algorithmically the
recession end has been found for six economic
recessions in the U.S. between 1960 and 2000. The
ends of all six recessions under consideration
are preceded within 5 months by this pattern that
appears at no other time. The end of the last
recession occurred in 2001 has been also
predicted.
21WP7 Analysis of Time Series Behaviour
- The problems that arise in data processing (i)
what kind of change of the examined time series
should be treated as a non-random and (ii) what
kind of change (events) could be tried to be
forecasted were studied. The approaches to
development of some formal procedure(s) to
distinguish random and non-random features and
random and non-random time-frequency domains in
the regime of the time series under examination
have been analyzed.
22WP7 New approaches to prediction of extreme
events
- The algorithms use background activity that is
introduced for the systems under consideration
the economy (the U.S. economy) and the megacity
(Los Angeles or New York). Economic recessions in
the U.S., homicide surges in Los Angeles and New
York City, and episodes of a sharp increase in
the unemployment rate in the U.S. are considered
as the extreme events. Events forming background
activity are determined from monthly series of
the U.S. industrial production index (in the case
of recessions), of the grand total of all actual
offences in Los Angeles or New York City (in the
case of homicide surges), and of index of help
wanted advertising (in the case of episodes of a
sharp increase in the unemployment rate).
23Definition of events of the background activity
- Monthly series of Index f is considered.
- Let the general trend of f before the extreme
events characterised by (a) decline, µf(m/s,u)
Kf(m-s-u,m-s) - Kf(m-s,m), (b) surge, µf(m/s,u)
Kf(m-s,m) Kf(m-s-u,m-s). Dots show monthly
values of index f, straight lines are the linear
least-square regressions on segments (m-s-u, m-s)
and (m-s, m).
24Transformation of scaling relation before extreme
events
- Extreme event the start of American economic
recession. D-periods periods before extreme
events. - Scaling relation is defined for events of the
background activity determined by means of
monthly industrial production - N(M) is the number of events with µ M.
25Scheme of a prediction algorithm
A(m/s,u,µ,v) is the number of events with
µf(m/s,u) µ occurred within a time window of v
months m-v1, m
26Economic recessions in the U.S. f industrial
production index
27Episodes of a sharp increase in the unemployment
rate in the U.S. f index of help wanted
advertising
28Periods of the homicide surge in Los Angeles f
the grand total of all actual offences
29Periods of the homicide surge in New York City
30WP7 Prediction of the rise of unemployment rate
in the US civilian labour force
- Precursory trends of the indicators used for
prediction of the rise of unemployment rate. - Brown curves show smoothed indicators S-
short-term interest rate on 90-day U.S. treasury
bills, at an annual rate L - long-term interest
rate on 10-year U.S. treasury bonds, at an annual
rate IP - total U.S. industrial production
defined in to 2002. - Red bars show time intervals when the trend of an
indicator was large (i.e. above the respective
threshold). - An alarm for the rise of the unemployment rate is
declared for 6 months after each month when the
trends of all three indicators are large
(regardless of whether this month belongs or not
to an already determined alarm). - A yellow bar shows the period of the alarm
starting in May 2007 and reported in September
2006.
31Unemployment rate in USA, 199909-200801
conforming the prediction
- A thin blue curve shows the data of Bureau of
Labor Statistics, U.S. Department of Labor
(http//data.bls.gov), and a thick curve the
smoothed data. Yellow bars indicate the alarm
periods, vertical red lines starting months of
the rise of unemployment rate (the rise of
unemployment started in December 2006 has
confirmed the prediction), a grey bar the
period of the unemployment growth in 2000-2003.
32Unemployment rate in the U.S., 1964-2007