Difference between pages "IC SG5" and "IC SG9"

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<big>'''JSG 0.5: Multi-sensor combination for the separation of integral
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<big>'''Application of time-series analysis in geodesy'''</big>
geodetic signals'''</big>
 
  
Chair: ''F. Seitz (Germany)''<br>
+
Chair: ''W. Kosek (Poland)''<br>
Affiliation: ''Comm. 2, 3 and GGOS''
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Affiliation:''Comm. 1, 2, 3, 4''
  
 
__TOC__
 
__TOC__
===Objectives===
+
===Introduction===
 +
 
 +
Observations of the new space geodetic techniques (geometric and gravimetric) deliver a global picture of dynamics of the Earth usually represented in the form of  time series which describe 1) changes of the surface geometry of the Earth due to horizontal and vertical deformations of the land surface, variations of the ocean surface and ice covers, 2) the fluctuations in the orientation of the Earth divided into precession, nutation, polar motion and spin rate, and, 3) the variations of the Earth’s gravitational field as well as the variations of the centre of mass of the Earth. Geometry, Earth rotation and the gravity field are the three components of the Global Geodetic Observing System (GGOS). The vision of GGOS is to integrate all observations and elements of the Earth’s system into one unique physical and mathematical model. However, the temporal variations of Earth rotation and gravity/geoid represent the total, integral effect of all mass exchange between all elements of Earth’s system including atmosphere, ocean and hydrology.
 +
 
 +
Different time series analysis methods are applied to analyze all these geodetic time series for better understanding of the relation between all elements of the Earth’s system as well as their geophysical causes. The interactions between different components of the Earth’s system are very complex so the nature of considered signals in the geodetic time series is mostly wideband, irregular and non-stationary. Thus, it is necessary to apply time frequency analysis methods in order to analyze these time series in different frequency bands as well as to explain their relations to geophysical processes e.g. by computing time frequency coherence between Earth’s rotation or the gravity field data and data representing the mass exchange between the atmosphere, ocean and hydrology. The techniques of time frequency spectrum and coherence may be developed further to display reliably the features of the temporal or spatial variability of signals existing in various geodetic data, as well as in other data sources.
 +
 
 +
Geodetic time series may include for example variations of site positions, tropospheric delay, ionospheric total electron content, temporal variations of estimated orbit parameters.  Time series analysis methods can be also applied to analyze data on the surface including maps of the gravity field, sea level and ionosphere as well as temporal variations of such surface data. The main problems to deal with concern the estimation of deterministic (including trend and periodic variations) and stochastic (non-periodic variations and random changes) components of the geodetic time series as well as the application of digital filters for extracting specific components with a chosen frequency bandwidth. 
  
A large part of the geodetic parameters derived from space geodetic observation techniques are integral quantities of the Earth system. Among the most prominent ones are parameters related to Earth rotation and the gravity field. Variations of those parameters reflect the superposed effect of a multitude of dynamical processes and interactions in various subsystems of the Earth. The integral geodetic quantities provide fundamental and unique information for different balances in the Earth system, in particular for the balances of mass and angular momentum that are directly related to (variations of) the gravity field and Earth rotation. In respective balance equations the geodetic parameters describe the integral effect of exchange processes of mass and angular momentum in the Earth system. In contrast to many other disciplines of geosciences, geodesy is characterized by a very long observation history. Partly, the previously mentioned parameters have been determined over many decades with continuously improved space observation techniques. Thus geodesy provides an excellent data base for the analysis of long term changes in the Earth system and contributes fundamentally to an improved understanding of large-scale processes.
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The multiple methods of time series analysis may be encouraged to be applied to the preprocessing of raw data from various geodetic measurements in order to promote the quality level of enhancement of signals existing in the raw data. The topic on the improvement of the edge effects in time series analysis may also be considered, since they may affect the reliability of long-range tendency (trends) estimated from data series as well as the real-time data processing and prediction.
  
However, in general the integral parameter time series cannot be separated into contributions of specific processes without further information. Their separation and therewith their geophysical interpretation requires complementary data from observation techniques that are unequally sensitive for individual effects and/or from numerical models. Activities of the study group are focussed on the development of strategies for the separation of the integral geodetic signals on the basis of modern space-based Earth observation systems. A multitude of simultaneously operating satellite systems with different objectives is available today. They offer a broad spectrum of information on global and regional-scale processes at different temporal resolutions. Within the study group it shall be investigated in which way the combination of heterogeneous data sets allows for the quantification of individual contributors to the balances of mass and angular momentum.
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For coping with small geodetic samples one can apply simulation-based methods and if the data are sparse, Monte-Carlo simulation or bootstrap technique may be useful.
  
The research activities shall be coordinated between the participating scientists and shall be conducted in interdisciplinary collaboration. At all times the group is open for new contacts and members in order to embed the activities in a wide context. The study group is primarily affiliated with the IAG commissions 2 (Gravity field) and 3 (Earth rotation and geodynamics).
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Understanding the nature of geodetic time series is very important from the point of view of appropriate spectral analysis as well as application of filtering and prediction methods.
  
 
===Objectives===
 
===Objectives===
  
The primary objective of the study group is the development of strategies for multi-sensor combinations with the aim of separating time series of integral geodetic parameters related to Earth rotation and gravity field. The separation of the parameter time series into contributions of individual underlying effects fosters the understanding of dynamical processes and interactions in the Earth system. This is of particular interest in the view of global change.
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Study of the nature of geodetic time series to choose optimum time series analysis methods  for filtering, spectral analysis, time frequency analysis and prediction.
 +
 
 +
Study of Earth rotation and gravity field variations and their geophysical causes in different frequency bands.
 +
 
 +
Evaluation of appropriate covariance matrices for the time series by applying the law of error propagation to the original measurements, including weighting schemes, regularization, etc.
  
Individual contributions from various subsystems of the Earth shall be quantified and balanced. In particular our investigations focus on the separation of the Earth rotation parameters (polar motion and variations of length-of-day) into contributions of atmospheric and hydrospheric angular momentum variations, and on the separation of GRACE gravity field observations over continents into the contributions of individual hydrological storage compartments, such as groundwater, surface water, soil moisture and snow.
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Determination of the statistical significance levels of the results obtained by different time series analysis methods and algorithms applied to geodetic time series.  
Investigations in the frame of the study group will exploit the synergies of various observation systems (satellite altimetry, optical and radar remote sensing, SMOS, and others) for the separation of the signals and combine their output with numerical models. Among the most important steps are compilation and assessment of background information for individual observation systems and sensors (mode of operation, sensitivity, accuracy, deficiencies) as well as theoretical studies which (new) information on the Earth system can be gained from a combination of different observation methods.
 
  
In particular the research comprises the following topics:
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Comparison of different time series analysis methods in order to point out their advantages and disadvantages.  
* potential und usability of contemporary spaceborne and terrestrial sensors for an improved understanding of processes within atmosphere and hydrosphere,
 
* analysis of accuracy, temporal and spatial resolution and coverage of different data sets,
 
* theoretical and numerical studies on the combination of heterogeneous observation types; this comprehends investigations on appropriate methods for parameter estimation including error propagation, the analysis of linear dependencies between parameters and the solution of rank deficiency problems,
 
* mathematical methods for the enhancement of the information content (e.g., filters),
 
* quantification of variations of mass and angular momentum in different subsystems from multi-sensor analysis,
 
* analysis of the consistencies of balances between individual effects and integral geodetic parameters on different spatial scales,
 
* formulation of recommendations for future research and (if possible) for future satellite missions on the basis of balance inconsistencies.
 
  
===Planned Activities===
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Recommendations of different time series analysis methods for solving problems concerning specific geodetic time series.
  
* Set-up of a JSG webpage for dissemination of information (activities and a bibliographic list of references) and for presentation and communication of research results.
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===Program of activities===
* Organization of conference sessions / workshops:
 
** planned in 2013: Conference Session in the Hotine Marussi Symposium,
 
** planned in 2014: 2nd workshop on the Quality of Geodetic Observing and Monitoring Systems (QuGOMS’ 14).
 
* Common publications of SG members.
 
* Common fund raising activities (e.g., for PhD. positions).
 
  
===Principal Scientific Outcome/Results===
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Launching of a web page with information concerning time series analysis and it application to geodetic time series with special emphasis on exchange of ideas, providing and updating bibliographic list of references of research results and relevant publications from different disciplines as well as unification of terminology applied in time series analysis.
  
By the end of the 4-year period 2011-2015 the following outcome shall be achieved:
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Working meetings at the international symposia and presentation of research results at the appropriate sessions.  
Mature experience in geodetic multi-sensor data combina-tion including data availability, formats, combination strategies and accuracy aspects.
 
Numerical results for separated hydrological contributions to integral mass variations observed by GRACE for selected study areas.
 
Numerical results for separated atmospheric/hydrospheric contributions Earth rotation parameters on seasonal to inter-annual time scales.
 
Initiation of at least one common funded project with positions for PhD students working in the topical field of the study group.
 
  
===Members===
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===Membership===
  
'' '''Florian Seitz (Germany), chair''' <br /> Sarah Abelen (Germany) <br /> Rodrigo Abarca del Rio (Chile) <br /> Andreas Güntner (Germany) <br /> Karin Hedman (Germany) <br /> Franz Meyer (USA) <br /> Michael Schmidt (Germany) <br /> Manuela Seitz (Germany) <br /> Alka Singh (India) <br />''
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'' '''Wieslaw Kosek, Poland, chair'''<br /> Michael Schmidt, Germany<br /> Jan Vondrák, Czech Republic<br /> Waldemar Popinski, Poland<br /> Tomasz Niedzielski, Poland<br />Johannes Boehm, Austria<br />Rudolf Widmer-Schnidrig, Germany<br />Dawei Zheng, China<br />Yonghong Zhou, China<br />Mahmut O. Karslioglu, Turkey<br />Orhan Akyilmaz, Turkey<br />Laura Fernandez, Argentina<br />Richard Gross, USA<br />Olivier de Viron, France<br />
 +
Michel van Camp, Belgium<br/>''

Revision as of 14:19, 23 July 2008

Application of time-series analysis in geodesy

Chair: W. Kosek (Poland)
Affiliation:Comm. 1, 2, 3, 4

Introduction

Observations of the new space geodetic techniques (geometric and gravimetric) deliver a global picture of dynamics of the Earth usually represented in the form of time series which describe 1) changes of the surface geometry of the Earth due to horizontal and vertical deformations of the land surface, variations of the ocean surface and ice covers, 2) the fluctuations in the orientation of the Earth divided into precession, nutation, polar motion and spin rate, and, 3) the variations of the Earth’s gravitational field as well as the variations of the centre of mass of the Earth. Geometry, Earth rotation and the gravity field are the three components of the Global Geodetic Observing System (GGOS). The vision of GGOS is to integrate all observations and elements of the Earth’s system into one unique physical and mathematical model. However, the temporal variations of Earth rotation and gravity/geoid represent the total, integral effect of all mass exchange between all elements of Earth’s system including atmosphere, ocean and hydrology.

Different time series analysis methods are applied to analyze all these geodetic time series for better understanding of the relation between all elements of the Earth’s system as well as their geophysical causes. The interactions between different components of the Earth’s system are very complex so the nature of considered signals in the geodetic time series is mostly wideband, irregular and non-stationary. Thus, it is necessary to apply time frequency analysis methods in order to analyze these time series in different frequency bands as well as to explain their relations to geophysical processes e.g. by computing time frequency coherence between Earth’s rotation or the gravity field data and data representing the mass exchange between the atmosphere, ocean and hydrology. The techniques of time frequency spectrum and coherence may be developed further to display reliably the features of the temporal or spatial variability of signals existing in various geodetic data, as well as in other data sources.

Geodetic time series may include for example variations of site positions, tropospheric delay, ionospheric total electron content, temporal variations of estimated orbit parameters. Time series analysis methods can be also applied to analyze data on the surface including maps of the gravity field, sea level and ionosphere as well as temporal variations of such surface data. The main problems to deal with concern the estimation of deterministic (including trend and periodic variations) and stochastic (non-periodic variations and random changes) components of the geodetic time series as well as the application of digital filters for extracting specific components with a chosen frequency bandwidth.

The multiple methods of time series analysis may be encouraged to be applied to the preprocessing of raw data from various geodetic measurements in order to promote the quality level of enhancement of signals existing in the raw data. The topic on the improvement of the edge effects in time series analysis may also be considered, since they may affect the reliability of long-range tendency (trends) estimated from data series as well as the real-time data processing and prediction.

For coping with small geodetic samples one can apply simulation-based methods and if the data are sparse, Monte-Carlo simulation or bootstrap technique may be useful.

Understanding the nature of geodetic time series is very important from the point of view of appropriate spectral analysis as well as application of filtering and prediction methods.

Objectives

Study of the nature of geodetic time series to choose optimum time series analysis methods for filtering, spectral analysis, time frequency analysis and prediction.

Study of Earth rotation and gravity field variations and their geophysical causes in different frequency bands.

Evaluation of appropriate covariance matrices for the time series by applying the law of error propagation to the original measurements, including weighting schemes, regularization, etc.

Determination of the statistical significance levels of the results obtained by different time series analysis methods and algorithms applied to geodetic time series.

Comparison of different time series analysis methods in order to point out their advantages and disadvantages.

Recommendations of different time series analysis methods for solving problems concerning specific geodetic time series.

Program of activities

Launching of a web page with information concerning time series analysis and it application to geodetic time series with special emphasis on exchange of ideas, providing and updating bibliographic list of references of research results and relevant publications from different disciplines as well as unification of terminology applied in time series analysis.

Working meetings at the international symposia and presentation of research results at the appropriate sessions.

Membership

Wieslaw Kosek, Poland, chair
Michael Schmidt, Germany
Jan Vondrák, Czech Republic
Waldemar Popinski, Poland
Tomasz Niedzielski, Poland
Johannes Boehm, Austria
Rudolf Widmer-Schnidrig, Germany
Dawei Zheng, China
Yonghong Zhou, China
Mahmut O. Karslioglu, Turkey
Orhan Akyilmaz, Turkey
Laura Fernandez, Argentina
Richard Gross, USA
Olivier de Viron, France
Michel van Camp, Belgium