Slovak Repeat Stations – 2006.5 Epoch Fridrich Valach, Peter Dolinský, Magdaléna Váczyová Hurbanovo Geomagnetic Observatory GPI SAS, Slovak Republic The.

Slides:



Advertisements
Similar presentations
DMI Development and World-wide Sale of Precision Magnetic Instruments High-Precision Magnetometers Measurement of the vertical geomagnetic component (middle)
Advertisements

Geomagnetic Measurements Workshop: DIflux: Absolute Measurement of the Geomagnetic Field orientation in Space prepared for the XIVth IAGA WORKSHOP ON.
Abnormal Analysis of Averaged Midnight F before the Ms 5.1 Chuxiong Earthquake Rong Zhu 1, Dong-mei Yang 1, Yan Zhang 2, Jian-jun Wang 3, Yu-fei He 1 1.
Repeat station crustal biases and accuracy determined from regional field models M. Korte, E. Thébault* and M. Mandea, GeoForschungsZentrum Potsdam (*now.
The German Repeat Station Survey 2006 M. Korte and M. Fredow, GeoForschungsZentrum Potsdam In 2006 a complete survey of the German repeat station network.
DEFINITION, CALCULATION, AND PROPERTIES OF THE Dst INDEX R.L. McPherron Institute of Geophysics and Planetary Physics University of California Los Angeles.
CALCULATION OF THE Dst INDEX
Separating internal geomagnetic secular variation and long-term magnetospheric field variations Monika Korte Deutsches GeoForschungsZentrum GFZ.
Petukhov I.S., Petukhov S.I. Yu.G. Shafer Institute for Cosmophysical Research and Aeronomy SB RAS 21st European Cosmic Ray Symposium in Košice, Slovakia.
ITALIAN MAGNETIC NETWORK AND GEOMAGNETIC FIELD MAPS OF ITALY AT YEAR G. Dominici¹, A. Meloni¹, M. Miconi¹, M. Pierozzi², M. Sperti² ¹Istituto Nazionale.
Study of the Effect of Auroral Substorms on the Low - Latitude Currents Inga Maslova 1, Piotr Kokoszka 1, Jan Sojka 2, Lie Zhu 2 1 Mathematics and Statistics.
Testing for Lack of Dependence in Functional Linear Model Inga Maslova, Piotr Kokoszka Department of Mathematics and Statistics, Utah State University.
Introduction The primary geomagnetic storm indicator is the Dst index. This index has a well established ‘recipe’ by which ground-based observations are.
Compass surveying.
Geomagnetic field Inclination
Geomagnetic Variations along Concurrent Latitudes due to Ionospheric Currents Inge Edvardsen – UiT & Baker Hughes Magnar Gullikstad Johnsen - UiT Unni.
An Automatic Instrument to Measure the Absolute Components of the Earth's Magnetic Field H.-U. Auster, M. Mandea, A. Hemshorn, E. Pulz, M. Korte.
INTRODUCTION TO UTM COORDINATES AND MAP DATUMS.
A Verification of Magnetometer’s Time Accuracy by using a GPS Pulse Generator Some magnetic observatories are exchanging one-minute geomagnetic field data.
ISWI in Slovakia ABSTRACT I. DOROTOVIČ ISWI National Coordinator in the Slovak Republic Slovak Central Observatory, Hurbanovo, Slovak Republic,
Croatian Geomagnetic Network for Field Mapping Croatian Geomagnetic Network for Field Mapping (CGNFM) was similarly designed as the repeat stations network.
COST Action 724 "Developing the basis for monitoring, modelling and predicting Space Weather", Sofia, Bulgaria, May 2007 Atmospheric emissions and.
Geomagnetism: Earth’s magnetic field Dipole Field.
Chapter 3 Section 1- Finding Locations on Earth
Secular variation in Germany from repeat station data and a recent global field model Monika Korte and Vincent Lesur Helmholtz Centre Potsdam, German Research.
Background to >10 years of BIFROST activities Jan M. Johansson 1, Hans-Georg Scherneck 1, Rüdiger Haas 1, Sten Bergstrand 1 Martin Lidberg 1,2, Lotti Jivall.
© NERC All rights reserved Measuring the Earth’s Magnetic Field Chris Turbitt.
Outline Magnetic dipole moment Magnetization Magnetic induction
© NERC All rights reserved UK Repeat Station Report T J G Shanahan and S Macmillan June 2009 MagNetE Workshop Helsinki, Finland.
© NERC All rights reserved Chris Turbitt Observatories Manager Geomagnetism Team British Geological Survey BGS Observatory Network.
Tom Wilson, Department of Geology and Geography Environmental and Exploration Geophysics II tom.h.wilson Department of Geology.
Models of the Earth Chapter 3. Ch03\80017.html.
Geomagnetism: Lecture 1 This lecture is based largely on:
Tom Wilson, Department of Geology and Geography Environmental and Exploration Geophysics I tom.h.wilson Department of Geology and.
Geology 5660/6660 Applied Geophysics 28 Mar 2014 © A.R. Lowry 2014 For Mon 31 Mar: Burger (§7.4–7.6) Last Time: Earth’s Main Magnetic Field Earth’s.
Tom Wilson, Department of Geology and Geography Environmental and Exploration Geophysics I tom.h.wilson Department of Geology and.
Tom Wilson, Department of Geology and Geography Environmental and Exploration Geophysics I tom.h.wilson Department of Geology and.
Cosmic Rays2 The Origin of Cosmic Rays and Geomagnetic Effects.
Environmental and Exploration Geophysics I tom.h.wilson Department of Geology and Geography West Virginia University Morgantown,
Geomagnetic Charts of Southern Part of Korean Peninsula as of LIM, Mutaek* 1, MOON, Jiyoung 2, PARK, Youngsue 1, SHIN, Younghong 1, RIM, Hyoungrae.
1 Yongliang Song & Mei Zhang (National Astronomical Observatory of China) The effect of non-radial magnetic field on measuring helicity transfer rate.
Environmental and Exploration Geophysics I tom.h.wilson Department of Geology and Geography West Virginia University Morgantown,
AUTOMATED QUALITY CONTROL OF GEOPHYSICAL TIME SERIES The algorithmic systems developed at Geophysical Center of Russian Academy of Sciences are intended.
Figure 2. Spatial Distribution ISOPORIC MODELLING OF THE GEOMAGNETIC FIELD COMPONENTS AT THE EPOCH PENINSULA AND BALEARIC ISLANDS. V.M. Marin(1),
Measuring the Gravity and Magnetic Anomaly of a Rising Lava Plume Chris Jaeger December 3, 2015.
MAGNETOMETERS IN HYPACK® Data Collection & Data Processing.
Recall that the proton precession magnetometer makes measurements of the total field, not the vector components of the field. Recall also that the total.
Tom Wilson, Department of Geology and Geography Environmental and Exploration Geophysics I tom.h.wilson Department of Geology and.
Tom Wilson, Department of Geology and Geography Environmental and Exploration Geophysics I tom.h.wilson Department of Geology and.
Geology 5660/6660 Applied Geophysics 1 Apr 2016 © A.R. Lowry 2016 For Mon 4 Apr: Burger (§ ) Last Time: Magnetics (Measurement, Anomalies)
Environmental and Exploration Geophysics I tom.h.wilson Department of Geology and Geography West Virginia University Morgantown, WV.
SOUTHERN REGIONAL SPACE RESEARCH CENTER – CRS/INPE-MCT SPACE SCIENCE LABORATORY OF SANTA MARIA – LACESM/CT-UFSM LOW COST FLUXGATE MAGNETOMETER DEVELOPMENT.
Geology 5660/6660 Applied Geophysics 30 Mar 2016
Environmental and Exploration Geophysics I tom.h.wilson Department of Geology and Geography West Virginia University Morgantown,
Compass surveying.
What is the magnetic potential of a dipole?
Rapid core field variations just before Swarm
Analysis of ground magnetometer coverage
A snapshot of the 3D magnetic field structure simulated with the Glatzmaier-Roberts geodynamo model. Magnetic field lines are blue where the field is directed.
Magnetic Methods- continued
Final review sessions - II
MAGNETOMETERS IN HYPACK® Data Collection & Data Processing.
Principles & Elements of Design
DI3 – A new Procedure for Absolute Directional Measurements
Color Theory Study Guide
Recent results from Odessa Observatory
REPEAT STATIONS MEASUREMENTS IN UKRAINE IN 2006
Magnetism – Learning Outcomes
G.R. Vorobeva, A.V. Vorobev Ufa State Aviation Technical University
Presentation transcript:

Slovak Repeat Stations – Epoch Fridrich Valach, Peter Dolinský, Magdaléna Váczyová Hurbanovo Geomagnetic Observatory GPI SAS, Slovak Republic The Slovak repeat station network consists of six stations. It was reoccupied in the middle of The magnetic measurements were carried out using DI-flux theodolite (Zeiss Theo 015B theodolite with Elsec 810 magnetometer) and EDA proton precession magnetometer (PPM). The data were reduced to the epoch using magnetograms of the Hurbanovo Magnetic Observatory. We assumed the transient variations of the magnetic field to be identical on the territory of Slovakia and to be equal to the variation at Hurbanovo. An arbitrary element of the geomagnetic field at a station for the is E st, = E st,t – (E HRB,t – E HRB, ), where E st,t and E HRB,t are the values of the element at the time of measurement for the station and Hurba-novo Observatory, respectively, whereas E HRB, is Hurbanovo’s element for the epoch. The geographical positions and altitudes of the stations are the following: Hurabnovo 47.88˚N, 18.20˚E, 112 m; Očkov 48.65˚N, ˚E, 160 m; Rajec 49.09˚N, 18.65˚E, 487 m; Rimavská Sobota ˚N, 20.02˚E, 239 m; Spišské Podhradie 49.00˚N, 20.73˚E, 520 m; Úbrež 48.79˚N, ˚E, 140 m.StationDeclinationInclination Total Field Hurbanovo 3˚ 11.86΄ 64˚ 13.8΄ nT Očkov 3˚ 07.18΄ 64˚ 53.5΄ nT Rajec 3˚ 22.27΄ 65˚ 18.1΄ nT Rim. Sobota 3˚ 46.59΄ 64˚ 49.6΄ nT Spiš. Podhr. 3˚ 55.29΄ 65˚ 22.1΄ nT Úbrež 4˚ 13.35΄ 65˚ 12.8΄ nT Geomagnetic field elements D, I and F measured at the Slovak repeat stations, reduced to the epoch: Magnetic declination at the repeat stations since the 19 th century Horizontal component at the repeat stations since the 19th century Magnetic inclination at the repeat stations since the 19th century Total magnetic field at the repeat stations since the 19th century Linear model of the distribution of magnetic declination for epoch [in °], red lines, and its secular variation between epochs and [in ´/year], black lines, over the territory of Slovakia. Linear model of the distribution of horizontal component for epoch [in nT], black lines, and its secular variation between epochs and [in nT/year], violet lines, over the territory of Slovakia. Linear model of the distribution of magnetic inclination for epoch [in °], black lines, and its secular variation between epochs and [in ˝/year], blue lines, over the territory of Slovakia. Linear model of the distribution of total magnetic field for epoch [in nT], black lines, and its secular variation between epochs and [in nT/year], green lines, over the territory of Slovakia. References: L. R. Newitt, C. E. Barton, J. Bitterly: Guide for Magnetic Repeat Station Surveys. IAGA, Working Group V-8, F. Valach, M. Váczyová, P. Dolinský: New Slovak geomagnetic repeat station network. Earth, Planets and Space, 58/6, , Acknowledgments. This work was supported by grants VEGA 2/7008/27 and APVV Contact to the authors: