Difference between pages "IC SG5" and "IC SG7"

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<big>'''JSG 0.5: Multi-sensor combination for the separation of integral
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<big>'''JSG 0.7: Computational methods for high-resolution gravity field modelling and nonlinear dif-fusion filtering'''</big>
geodetic signals'''</big>
 
  
Chair: ''F. Seitz (Germany)''<br>
+
Chairs: ''R. Čunderlík (Slovakia), K. Mikula (Slovakia)''<br>
 
Affiliation: ''Comm. 2, 3 and GGOS''
 
Affiliation: ''Comm. 2, 3 and GGOS''
  
 
__TOC__
 
__TOC__
===Objectives===
+
===Introduction===
 
+
Efficient numerical methods and HPC (High Performance Computing) facilities provide new opportunities in many applications in geodesy. The goal of the IC SG is to apply numerical methods like the finite element method (FEM), finite volume method (FVM), boundary element method (BEM) and others mostly for gravity field modelling and non-linear filtering of data on the Earth’s surface. An advantage is that such numerical methods use finite elements as basis functions with local supports. Therefore a refinement of the discretization is very straightforward allowing adaptive refinement procedures as well.
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 rota-tion. In respective balance equations the geodetic para-meters 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 deter-mined 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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In case of gravity field modelling, a parallelization of algorithms using the standard MPI (Message Passing Interface) procedures and computations on clusters with distributed memory allows to achieve global or local gravity field models of very high-resolution, where a level of the discretization practically depends on capacity of available HPC facilities. The aforementioned numerical methods allow a detailed discretization of the real Earth’s surface considering its topography. To get precise numerical solution to the geodetic boundary-value problems (BVPs) on such complicated surface it is also necessary handle problems like the oblique derivative.
However, in general the integral parameter time series can-not 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 sensi-tive for individual effects and/or from numerical models. Activities of the study group are focussed on the develop-ment of strategies for the separation of the integral geo-detic 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 informa-tion on global and regional-scale processes at different temporal resolutions. Within the study group it shall be investigated in which way the combination of heterogene-ous data sets allows for the quantification of individual contributors to the balances of mass and angular momen-tum.
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Data filtering occurs in many applications of geosciences. A quality of filtering is essential for correct interpretations of obtained results. In geodesy we usually use methods based on the Gaussian filtering that corresponds to a linear diffusion. Such filtering has a uniform smoothing effect, which also blurs “edges” representing important structures in the filtered data. In contrary, a nonlinear diffusion allows adaptive smoothing that can preserve main structures in data, while a noise is effectively reduced. In image processing there are known at least two basic nonlinear diffusion models; (i) the regularized Perona-Malik model, where the diffusion coefficient depends on an edge detector, and (ii) the geodesic mean curvature flow model based on a geometrical diffusion of level-sets of the image intensity.
The research activities shall be coordinated between the participating scientists and shall be conducted in interdisci-plinary 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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The aim of the SG is to investigate and develop nonlinear filtering methods that would be useful for a variety of geodetic data, e.g., from satellite missions, satellite altimetry and others. A choice of an appropriate numerical technique is open to members of the SG. An example of the proposed approach is based on a numerical solution of partial differential equations using a surface finite volume method. It leads to a semi-implicit numerical scheme of the nonlinear diffusion equation on a closed surface.
  
 
===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 para-meters 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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* to develop numerical models for solving the geodetic BVPs using numerical methods like FEM, FVM, BEM and others,
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 contribu-tions of individual hydrological storage compartments, such as groundwater, surface water, soil moisture and snow.
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* to investigate the problem of oblique derivative,
Investigations in the frame of the study group will exploit the synergies of various observation systems (satellite alti-metry, 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 differ-ent observation methods.
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* to implement parallelization of numerical algorithms using the standard MPI procedures,
 
+
* to perform large-scale parallel computations on clusters with distributed memory,
In particular the research comprises the following topics:
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* to investigate methods for nonlinear filtering of data on closed surfaces using the regularized Perona-Malik model or mean curvature flow model,
* potential und usability of contemporary space-borne and terrestrial sensors for an improved understanding of pro-cesses within atmosphere and hydrosphere.
+
* to derive fully-implicit and semi-implicit numerical schemes for the linear and nonlinear diffusion equation on closed surfaces using the surface FVM,
* analysis of accuracy, temporal and spatial resolution and coverage of different data sets
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* to develop algorithms for the nonlinear filtering of data on the Earth’s surface,
* theoretical and numerical studies on the combination of heterogeneous observation types. This comprehends in-vestigations on appropriate methods for parameter esti-mation including error propagation, the analysis of linear dependencies between parameters and the solution of rank deficiency problems.
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* to summarize the developed methods and achieved numerical results in journal papers.
* mathematical methods for the enhancement of the infor-mation content (e.g. filters)
 
* quantification of variations of mass and angular momen-tum in different subsystems from multi-sensor analysis
 
* analysis of the consistencies of balances between individ-ual 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===
 
 
 
* Set-up of a SG webpage for dissemination of information (activities and a bibliographic list of references) and for presentation and communication of research results.
 
* Organization of conference sessions / workshops:
 
** planned in 2013: Conference Session in the Hotine Marussi Symposium
 
** planned in 2014: 2nd workshop on the Quality of Geo-detic Observing and Monitoring Systems (QuGOMS’ 14)
 
* Common publications of SG members
 
* Common fund raising activities (e.g. for PhD positions)
 
 
 
===Principal Scientific Outcome/Results===
 
  
By the end of the 4-year period 2011-2015 the following outcome shall be achieved:
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===Program of activities===
Mature experience in geodetic multi-sensor data combina-tion including data availability, formats, combination strategies and accuracy aspects
+
active participation in major geodetic conferences,
Numerical results for separated hydrological contributions to integral mass variations observed by GRACE for selected study areas.
+
working meetings at international symposia,
Numerical results for separated atmospheric/hydrospheric contributions Earth rotation parameters on seasonal to inter-annual time scales
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organization of a conference session.
Initiation of at least one common funded project with posi-tions for PhD students working in the topical field of the study group
 
  
 
===Members===
 
===Members===
  
'' '''Florian Seitz (Germany), chair'''<br />Sarah Abelen (Germany)<br />Rodrigo Abarca del Rio (Chile)<br />Andreas Güntner (Germany)
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'' '''Róbert Čunderlík (Slovakia), chair<br />
<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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Karol Mikula (Slovakia), chair'''<br />
 +
Ahmed Abdalla, New Zealand<br />
 +
Michal Beneš (Czech Republic)<br />
 +
Zuzana Fašková (Slovakia)<br />
 +
Marek Macák (Slovakia)<br />
 +
Otakar Nesvadba (Czech Republic)<br />
 +
Róbert Špir (Slovakia)<br />
 +
Róbert Tenzer (New Zealand)<br />''

Revision as of 12:28, 29 June 2012

JSG 0.7: Computational methods for high-resolution gravity field modelling and nonlinear dif-fusion filtering

Chairs: R. Čunderlík (Slovakia), K. Mikula (Slovakia)
Affiliation: Comm. 2, 3 and GGOS

Introduction

Efficient numerical methods and HPC (High Performance Computing) facilities provide new opportunities in many applications in geodesy. The goal of the IC SG is to apply numerical methods like the finite element method (FEM), finite volume method (FVM), boundary element method (BEM) and others mostly for gravity field modelling and non-linear filtering of data on the Earth’s surface. An advantage is that such numerical methods use finite elements as basis functions with local supports. Therefore a refinement of the discretization is very straightforward allowing adaptive refinement procedures as well. In case of gravity field modelling, a parallelization of algorithms using the standard MPI (Message Passing Interface) procedures and computations on clusters with distributed memory allows to achieve global or local gravity field models of very high-resolution, where a level of the discretization practically depends on capacity of available HPC facilities. The aforementioned numerical methods allow a detailed discretization of the real Earth’s surface considering its topography. To get precise numerical solution to the geodetic boundary-value problems (BVPs) on such complicated surface it is also necessary handle problems like the oblique derivative. Data filtering occurs in many applications of geosciences. A quality of filtering is essential for correct interpretations of obtained results. In geodesy we usually use methods based on the Gaussian filtering that corresponds to a linear diffusion. Such filtering has a uniform smoothing effect, which also blurs “edges” representing important structures in the filtered data. In contrary, a nonlinear diffusion allows adaptive smoothing that can preserve main structures in data, while a noise is effectively reduced. In image processing there are known at least two basic nonlinear diffusion models; (i) the regularized Perona-Malik model, where the diffusion coefficient depends on an edge detector, and (ii) the geodesic mean curvature flow model based on a geometrical diffusion of level-sets of the image intensity. The aim of the SG is to investigate and develop nonlinear filtering methods that would be useful for a variety of geodetic data, e.g., from satellite missions, satellite altimetry and others. A choice of an appropriate numerical technique is open to members of the SG. An example of the proposed approach is based on a numerical solution of partial differential equations using a surface finite volume method. It leads to a semi-implicit numerical scheme of the nonlinear diffusion equation on a closed surface.

Objectives

  • to develop numerical models for solving the geodetic BVPs using numerical methods like FEM, FVM, BEM and others,
  • to investigate the problem of oblique derivative,
  • to implement parallelization of numerical algorithms using the standard MPI procedures,
  • to perform large-scale parallel computations on clusters with distributed memory,
  • to investigate methods for nonlinear filtering of data on closed surfaces using the regularized Perona-Malik model or mean curvature flow model,
  • to derive fully-implicit and semi-implicit numerical schemes for the linear and nonlinear diffusion equation on closed surfaces using the surface FVM,
  • to develop algorithms for the nonlinear filtering of data on the Earth’s surface,
  • to summarize the developed methods and achieved numerical results in journal papers.

Program of activities

active participation in major geodetic conferences, working meetings at international symposia, organization of a conference session.

Members

'Róbert Čunderlík (Slovakia), chair
Karol Mikula (Slovakia), chair
Ahmed Abdalla, New Zealand
Michal Beneš (Czech Republic)
Zuzana Fašková (Slovakia)
Marek Macák (Slovakia)
Otakar Nesvadba (Czech Republic)
Róbert Špir (Slovakia)
Róbert Tenzer (New Zealand)