Download presentation
Presentation is loading. Please wait.
Published byDale Thomas Modified over 9 years ago
1
Bucharest, 14-16 May 2007 1 Gerald Duma Central Institute for Meteorology and Geodynamics Vienna, Austria GEOMAGNETIC VARIATIONS AND EARTHQUAKE ACTIVITY 3 rd MagNetE Workshop on European Geomagnetic Repeat Station Survey
2
Bucharest, 14-16 May 2007 2 Observations (1996) – daily range AUSTRIA M 2.5, 1901-1990 Geomagnetic Observatory
3
Bucharest, 14-16 May 2007 3 Duma, Vilardo (INGV), 1998 Geomagnetic Observatory Observations (1997) – daily range Mt. VESUVIUS volcanic eqs, area 10 x 10 km, 1.8 M 3.1, 1972-1996, 1400 events
4
Bucharest, 14-16 May 2007 4 A seismic daily cycle Greek philosophers Pliny the Elder, 79 A.D. eruption of Mt.Vesuvius Conrad, 1932 Shimshoni, 1972 Rarely investigated in recent decades
5
Bucharest, 14-16 May 2007 5 A seismic daily cycle 3 sub-periods 20th century AUSTRIA M 2.5 May 31 – June 18, 1997 Earthquake swarm in Austria, region IMST
6
Bucharest, 14-16 May 2007 6 A seismic daily cycle Observed also in many other regions Earthquakes M 5 and 6 A very powerful geodynamic process acting!
7
Bucharest, 14-16 May 2007 7 Geomagnetic Observatory Obs WIK, comp N AUSTRIA M 3.1 (Io 5°) Observations (1996) – long term
8
Bucharest, 14-16 May 2007 8 Mechanism, models? Dependence on Local Time Process related to sun A mechanism which penetrates the whole Earth‘s lithosphere Tides ? -> No! High energy mechanism Can a few nT influence tectonic performance?
9
Bucharest, 14-16 May 2007 9 The electromagnetic model Geomagnetic variations reach deep into the Earth‘s interior, 100s and 1000s of km! (magnetotellurics) Maxwell‘s equations : E - H relation ( ) Earth‘s conductive lithosphere: „telluric currents“ associated with all geomagnetic variations Applies to all natural variations in a broad frequency range (from Hz – solar cycle)
10
Bucharest, 14-16 May 2007 10 The electromagnetic model Telluric currents and forces F = e. [ v e. B ] F... mechanic force vector e... electron charge v e... velocity vector B... magnetic field vector ‚Lorentz force‘ F B veve e
11
Bucharest, 14-16 May 2007 11 The electromagnetic model Magnetic observatories monitor vertical force Fv (t)
12
Bucharest, 14-16 May 2007 12 The electromagnetic model r P1 P2 I2 ≠ I1 Regional mechanic moment, torque Tr
13
Bucharest, 14-16 May 2007 13 A new meaning of variation H H: monitors change ( t) of vertical force F v in P gradient H: monitors change ( t) of regional mechanic moment Tr ( azimuth Az) Torque axis P
14
Bucharest, 14-16 May 2007 14 Energy – diurnal variation Sq: solar controlled, heating, ionization, tides (Chapman, Bartels, 1940)
15
Bucharest, 14-16 May 2007 15 Energy – diurnal variation T = MM x H A large scale current field, covering 1/3 of the northern Earth‘s hemisphere The dayside Sq lithospheric current vortex (Matsushita, 1968)
16
Bucharest, 14-16 May 2007 16 Energy – diurnal variation The mechanic moment of Sq for a single loop (Duma, Ruzhin, 2003) The example demonstrates: The deformation energy provided to the lithosphere by a single current loop, radius 1500 km and current 10 kA, is equivalent to the energy of an earthquake M 5,1.
17
Bucharest, 14-16 May 2007 17 Energy – diurnal variation 60% of total moment concentrates in a 30° segment H I
18
Bucharest, 14-16 May 2007 18 Modelling the electromagnetic effect Data for H(lat,long) to compute gradient Hourly values (diurnal variation): Model simulating Sq telluric current vortex Regional observatory data (average Sq-var.) Annual values (long term, secular variation): Retrieved from IGRF, 1900-2010 (grid data) Regional observatory data (annual means, SV)
19
Bucharest, 14-16 May 2007 19 Case studies – Regions AustriaTaiwan CaliforniaBaikal region
20
Bucharest, 14-16 May 2007 20 Case studies – Austria (M ≥ 3.2, Gradient H – N10W) Gradient H from IGRF10 (1900-2010) Diurnal range Long term 1900 - 2003 Gradient H from Sq-Model
21
Bucharest, 14-16 May 2007 21 Case studies – Taiwan (M ≥ 5, Gradient H – N55E) Gradient H from IGRF10 (1900-2010) Diurnal range Long term Gradient H from Sq-Model 1973 - 1998
22
Bucharest, 14-16 May 2007 22 Case studies – Baikal area (M ≥ 5, Gradient H – N00E) Gradient H from IGRF10 (1900-2010) Diurnal range Long term Gradient H from Sq-Model 1900 - 1980 2001 - 2006
23
Bucharest, 14-16 May 2007 23 Case studies – California (M ≥ 6, Gradient H – N30E) Gradient H from IGRF10 (1900-2010) Diurnal range Long term Gradient H from Sq-Model 1970 - 2005
24
Bucharest, 14-16 May 2007 24 Novel aspects Geomagnetic variations modulate (trigger) seismic activity Answer to daily rhythm of seismic activity Activity ‚controlled‘ by external sources (sun, magnetic dynamo) Monitoring: directly by geomagnetic observatories Predictability: systematic diurnal, seasonal, secular variations (IGRF 2010) Not yet investigated: influence of magnetic storms
25
Bucharest, 14-16 May 2007 25 Thank your for your attention !
26
Bucharest, 14-16 May 2007 26 A surprising but plausible model Magnetic observatories monitor horizontal force Fh C (t)
27
Bucharest, 14-16 May 2007 27 Mt. VESUVIUS – long term volcanic eqs, area 10 x 10 km, 1.8 M 3.1, 1972-1996, 1400 events Observations – sun spot cycles Duma, Vilardo (INGV), 1998 n: annual number of eqs M 1.8, 1972-1996 sf: annual number of solar flares (10 3 ) Duma, Vilardo (INGV), 1998
28
Bucharest, 14-16 May 2007 28 ITALY, 4 subregions / IONIAN ILANDS (G4) 1910 – 1980, M 5 Observations – daily range I1 I2 I3 I4 all Italy G4
29
Bucharest, 14-16 May 2007 29 The regional torque Tr – Energy > lithosphere block model <
30
Bucharest, 14-16 May 2007 30 Model of Sq telluric current vortex Fits observed Sq-variations at observatories Computes grad H(LT)
31
Bucharest, 14-16 May 2007 31 H – current density
32
Bucharest, 14-16 May 2007 32 Case studies – Austria (M ≥ 2.5, gradient H – N10W) Seasonal range, 2001 - 2005 H data from observatories - monthly mean values
33
Bucharest, 14-16 May 2007 33 Case studies – Austria (M ≥ 2.5, gradient H – N10W) Seasonal range, 2001 - 2005 Gradient H from observatories - monthly mean values 2002 2001 2003 2004
34
Bucharest, 14-16 May 2007 34 Case studies – Austria (M ≥ 2.5, gradient H – N10W) Seasonal range, 2001 - 2005 Gradient H from observatories - monthly mean values 2005
Similar presentations
© 2025 SlidePlayer.com. Inc.
All rights reserved.