Case study on heterogeneous geoid/ quasigeoid based on space borne and terrestrial data combination with special consideration of GOCE mission data impact.

Slides:



Advertisements
Similar presentations
KARTDATA TIL NYTTE FOR SAMFUNNET POSITIONING DATA – FOR SOCIETY’S BENEFIT DETERMINATION OF THE GRAVITY FIELD OVER NORWEGIAN TERRITORIES.
Advertisements

The OCTAS Project, the geoid, the mean sea surface and and the mean dynamic topography By Dag Solheim Norwegian Mapping Authority Co-authors A. Hunegnaw,
Geodetic monitoring of crustal deformation in Dronning Maud Land, Antarctica Hannu Koivula, Jaakko Mäkinen, Joel Ahola and Markku Poutanen Finnish Geodetic.
From TOPEX-POSEIDON to JASON Science Working Team Meeting GRACE Mission Status Arles, France November 18-21, 2003 Byron D. Tapley (Principal Investigator)
Satellite geodesy. Basic concepts. I1.1a = geocentric latitude φ = geodetic latitude r = radial distance, h = ellipsoidal height a = semi-major axis, b.
The Four Candidate Earth Explorer Core Missions Consultative Workshop October 1999, Granada, Spain, Revised by CCT GOCE S 43 Science and.
An example of gravimetric geoid computation: The Iberian Gravimetric Geoid of 2005.
The Four Candidate Earth Explorer Core Missions Consultative Workshop October 1999, Granada, Spain, Revised by CCT GOCE S 59 Performance.
COMBINED MODELING OF THE EARTH’S GRAVITY FIELD FROM GOCE AND GRACE SATELLITE OBSERVATIONS Robert Tenzer 1, Pavel Ditmar 2, Xianglin Liu 2, Philip Moore.
The Four Candidate Earth Explorer Core Missions consultative Workshop October 1999, Granada, Spain, Revised by CCT GOCE S 23 The gravity.
The Four Candidate Earth Explorer Core Missions Consultative Workshop October 1999, Granada, Spain, Revised by CCT GOCE S 1 Gravity Field.
Dynamic Planet 2005 Cairns, Australia August 2005
Monitoring the Global Sea Level Rise Budget with Jason, Argo and GRACE Observations Eric Leuliette and Laury Miller NOAA/Laboratory for Satellite Altimetry.
NOAA’s National Geodetic Survey USGG2009 & GEOID09: New geoid height models for surveying/GIS ACSM-MARLS-UCLS-WFPS Conference FEB 2009 Salt Lake.
Motivation: much of the deep ocean floor is uncharted by ships high spatial resolution gravity can reveal tectonic fabric, uncharted seamounts, and seafloor.
DORIS - DAYS Toulouse May 2-3, 2000 DORIS Doppler Orbitography and Radiopositioning Integrated by Satellite  Basic system concept  Main missions  Schedules.
Use of G99SSS to evaluate the static gravity geopotential derived from the GRACE, CHAMP, and GOCE missions Daniel R. Roman and Dru A. Smith Session: GP52A-02Decade.
Figure and Gravity Figure of a planet (Earth) Geoid Gravity field
Sea-ice freeboard heights in the Arctic Ocean from ICESat and airborne laser H. Skourup, R. Forsberg, S. M. Hvidegaard, and K. Keller, Department of Geodesy,
Advances and Best Practices in Airborne Gravimetry from the U.S. GRAV-D Project Theresa M. Damiani 1, Vicki Childers 1, Sandra Preaux 2, Simon Holmes 3,
Puerto Rico Airborne Gravity Data Modeling
Institut für Erdmessung (IfE), Leibniz Universität Hannover, Germany Quality Assessment of GOCE Gradients Phillip Brieden, Jürgen Müller living planet.
GRAV-D Project Update Vicki Childers, Ph.D. GRAV-D Project Manager.
Using GRACE to estimate changes in land water storage: present limitations and future potential John Wahr, Sean Swenson, Isabella Velicogna University.
1 Assessment of Geoid Models off Western Australia Using In-Situ Measurements X. Deng School of Engineering, The University of Newcastle, Australia R.
ESA Living Planet Symposium, Bergen, T. Gruber, C. Ackermann, T. Fecher, M. Heinze Institut für Astronomische und Physikalische Geodäsie (IAPG)
A spherical Fourier approach to estimate the Moho from GOCE data Mirko Reguzzoni 1, Daniele Sampietro 2 2 POLITECNICO DI MILANO, POLO REGIONALE DI COMO.
Geoid Modeling at NOAA Dru A. Smith, Ph.D. National Geodetic Survey National Ocean Service, NOAA November 13, 2000.
CryoSat Workshop, March 9, CryoSat: showing the way to a future of improved ocean mapping Walter H. F. Smith NOAA Lab for.
Center for Satellite Applications and Research (STAR) Review 09 – 11 March 2010 Altimetric Bathymetry Model Excels Global bathymetry model combines depths.
Last Time: Ground Penetrating Radar Radar reflections image variations in Dielectric constant  r ( = relative permittivity )  3-40 for most Earth materials;
1 Geoid and Geoid Change: Discussion Topics Roger Haagmans, Boulder, 21October 2009.
Overview of CEOS Virtual Constellations Andrew Mitchell NASA CEOS SIT Team / WGISS NASA ESRIN – Frascati, Italy September 20, 2013 GEOSS Vision and Architecture.
Shape of the Earth, Geoid, Global Positioning System, Map Coordinate Systems, and Datums Or how you can impress your friend on a hike D. Ravat University.
Lecture 21 – The Geoid 2 April 2009 GISC-3325.
A Brief Introduction to Gravity UT Intro to Geophysics Class March 10, 2009 Austin-Bergstrom Airport Theresa Diehl, Ph.D. Research Geodesist NOAA National.
Progress in Geoid Modeling from Satellite Missions
Regional Enhancement of the Mean Dynamic Topography using GOCE Gravity Gradients Matija Herceg 1 and Per Knudsen 1 1 DTU Space, National Space Institute,
Data for Plate Tectonics Earthquakes –World wide network for detecting nuclear tests Magnetic stripes –From World War 2 submarine detection Bathymetry.
International Symposium on Gravity, Geoid and Height Systems GGHS 2012, Venice, Italy 1 GOCE data for local geoid enhancement Matija Herceg Per Knudsen.
Full Resolution Geoid from GOCE Gradients for Ocean Modeling Matija Herceg & Per Knudsen Department of Geodesy DTU Space living planet symposium 28 June.
Recent Investigations Towards Achieving a One Centimeter Geoid Daniel R. Roman & Dru A. Smith U.S. National Geodetic Survey GGG 2000, Session 9 The Challenge.
Catherine LeCocq SLAC USPAS, Cornell University Large Scale Metrology of Accelerators June 27 - July 1, 2005 Height Systems 1 Summary of Last Presentation.
C H A M P International Laser Ranging Service - General Assembly, October 2005 Eastbourne, UK L. Grunwaldt, R. Schmidt, D. König, R. König, F.-H. Massmann.
A comparison of different geoid computation procedures in the US Rocky Mountains YM Wang 1, H Denker 2, J Saleh 3, XP Li 3, DR Roman 1, D Smith 1 1 National.
Improved Marine Gravity from CryoSat and Jason-1 David T. Sandwell, Emmanuel Garcia, and Walter H. F. Smith (April 25, 2012) gravity anomalies from satellite.
Investigation of the use of deflections of vertical measured by DIADEM camera in the GSVS11 Survey YM Wang 1, X Li 2, S Holmes 3, DR Roman 1, DA Smith.
Improving Regional Geoid by optimal Combination of GRACE Gravity Model and Surface Gravity Data YM Wang, DR Roman and J Saleh National Geodetic Survey.
Mayer-Gürr et al.ESA Living Planet, Bergen Torsten Mayer-Gürr, Annette Eicker, Judith Schall Institute of Geodesy and Geoinformation University.
ESA Living Planet Symposium 28 June - 2 July 2010, Bergen, Norway A. Albertella, R. Rummel, R. Savcenko, W. Bosch, T. Janjic, J.Schroeter, T. Gruber, J.
1 NGA Mission - Data – Collaboration 2009 Workshop on Monitoring North American Geoid Change 21 Oct 2009 NGA Mission - Data – Collaboration 2009 Workshop.
4.Results (1)Potential coefficients comparisons Fig.3 FIR filtering(Passband:0.005~0.1HZ) Fig.4 Comparison with ESA’s models (filter passband:0.015~0.1HZ)
The OC in GOCE: A review The Gravity field and Steady-state Ocean Circulation Experiment Marie-Hélène RIO.
An oceanographic assessment of the GOCE geoid models accuracy S. Mulet 1, M-H. Rio 1, P. Knudsen 2, F. Siegesmund 3, R. Bingham 4, O. Andersen 2, D. Stammer.
GOCE/GRACE GGM evaluation over Greece with GPS/Leveling and gravity data G.S. Vergos, V.D. Grigoriadis, I.N. Tziavos, D.A. Natsiopoulos, E.A. Tzanou.
Last Time: Introduction to Gravity Governed by LaPlace’s equation: with solution of the form: If we have a spherical body with mass M and constant (or.
1st Steering Committee Meeting activities from WP3 –
ESA’s Earth Observation Programmes and GOCE
Satlevel Collocation Model for Adapting GEM 2008 to Regional Geoid: A case Study of Yanbu Industrial City in Saudi Arabia Kamorudeen Aleem Department of.
Satellite Altimetry for Gravity, geoid and marine applications (MSS + LAT) Dr Ole B. Andersen, DTU Space, Denmark,
Dynamic Planet 2005 Cairns, Australia August 2005
Satellite Gravity Report Offshore SRI LANKA May, 2003
Geodesy & Crustal Deformation
1st Steering Committee Meeting activities from WP3 –
Chairs: H. Sünkel, P. Visser
GOCE in Ocean Modelling and the GOCINO project.
D. Rieser *, R. Pail, A. I. Sharov
Session 6 Aeronomy/ Novel applications
Daniel Rieser, Christian Pock, Torsten Mayer-Guerr
Advances and Best Practices in Airborne Gravimetry from the U. S
Presentation transcript:

Case study on heterogeneous geoid/ quasigeoid based on space borne and terrestrial data combination with special consideration of GOCE mission data impact Proj. ID Dr. Kirco Arsov, Prof. Wen Hanjiang and rest of the Dragon 3 team

Objectives Assesment of GOCE mission with respect to ground gravity data in China and Finland; GOCE mission validation Computation od one geoid solution for part of China and Finland with inclusion of GOCE and ground - based data in one model Inclusion of GOCE models in the upcoming Nordic Geoid computation Performance test of the HY-2 altimetry mission; gravity anomalies from altimeter data computation Optimal filtering and combination of long wavelength satellite based models, special accent on GOCE mission Asessment of different geoid solutions based on combination of different satellite models ; insight on GOCE performance

Project partners and roles Dr. Kirco Arsov (FGI): Geoid techniques, data, numerics, data reductions, GOCE modelling, Assessment of techniques Prof. Wen Hanjiang (CASM) marine and terrestrial geoid, altimetry processing, spectral methods, data acquisition coordination, computation techniques MSc. Hannu Ruotsalainen (FGI) gravity data acquisition, field campaigns, data smoothing, DEM, Seismic data, Density data MSc. Mirjam-Biker Koivula (FGI) : Geoid modelling, Spectral methods, GOCE models computation, Geoid assessment, Spectral geoid calculations: PhD thesis as outcome

Project partners and roles (cnt) Dr. Yanhui Cai (CASM): GPS processing and acquisition, GPS/Leveling preparation and screening, software coding MSc Huanling Liu (CASM): Ph.D earth’s gravity field model derivation from GOCE observations, altimeter data processing Yantian Xu(CASM): Ph.D, geoid determination and software coding Wei Li (CASM) : Ph.D, GPS processing, software coding

Project partners and roles (cnt) CASM: Chinese data acquisition, chinese data preparation, screening, smoothing, Chinese geoid computation and assessment of satellite models with respect to ground data, processing and assessment of altimetry data and determination of gravity anomalies on sea, screening of chinese land gravity data, assessment of GOCE models, GOCE models inclusion in the final geoid solution, comparing with nordic solution, publishing results

Project partners and roles (cnt) FGI: Update of the FGI gravity database, measurements screening and preparation, measurements reduction, GOCE models extraction, reduction and computation, GOCE models enhancements and filtering of local grav. Data, GOCE assessment with Finnish data (and possibly nordic), filtering of terrestrial measurements, study on combination of different long wavelength models with GOCE models, Finnish (and nordic) geoid computation by usage of stand alone and combined GOCE models, numerical investigations, justification of results with Chinese data and publication of results

FGI (and nordic) gravity database

FGI gravity database

FGI gravity database: vertical deflections

Gravity measurements 590,000 ( 500,000 on land , 90,000 in ocean ) The accuracy of 5′×5′mean free- air gravity anomalies is ±9mGal Number of GPS/Leveling points : 1000 Order-I leveling network : 93,360km Order-II leveling network : 136,369km Chinese data description Distribution of GPS/Leveling points

study area for geoid determination in China: Longitude: 118°00′ ~ 123°00′ Latitude: 27°00′ ~ 31°10′ The topography changes from 2.5m to 1800 Data collection: Gravity data Marine gravity anomalies derived from altimeter data GPS/Leveling measurements The topography of the study area Chinese data description (cnt)

Data collection in China collection of altimeter data(including HY-2 altimeter data), GPS/Leveling data, gravity measurements, DEM,marine gravity measurements near Zhejiang province,

ESA GOCE data ESA gravity field models to be used ESA GOCE PSO_2 data for orbit determination tests and gravity extraction from orbits Error var/cov of GOCE models GRACE models Altimetry: altimeter data from Jason-2, Envisat,and HY-2,marine gravity measurements GOCE gradiometry measurements :GOCE EGG Level 1b/L2 (excluded EGM_GVC_2

Project schedule and expected results 06/ /2013 terrestrial data screening, collection, filtering, reduction, study on methodology and software preparation, use of seismic and geological data for reductions. 06/ /2013 Marine gravity anomalies from altimeter data, marine geoid determination, validation of earth's gravity field models from GOCE 01/ /2015 Methods study for the derivation of the earth's gravity field model from GOCE gravity gradient data, validation of earth's gravity field models from GOCE, geoid determination in Zhejing province of China and Finland

Project schedule and expected results 01/ /2015 Study and reporting on the analysis of the influences of long-wavelength earth's gravity field to the accuracy of geoid in Zhejiang province of China and in Finland. Jan Dec.2015 cross-validation of HY-2 altimeter data, optimal combination of different altimiter missions for marine gravity anomalies and marine geoid.

01/ /2014 Study and reporting on the analysis of the influences of long-wavelength earth's gravity field to the accuracy of marine gravity anomalies in China sea by comparing to the marine gravity measurements. 01/ /2015 optimal combination of geoid improvements by using GOCE,altimeter,gravity measurements,DEM, GPS/Leveling Project schedule and expected results

Young scientists training Mirjam Biker-Koivula will work toward her PhD dealing with geoid modelling. She will be actively involved into Finnish data preparation, screening and GOCE model inclusion. This project will be part of her PhD study Three Ph.D students from China are going to be involved in this project: Ms. Liu will focus on the marine gravity anomalies derivation and marine geoid determination by using heterogeneous observations, and the study of long- wavelength earth's gravity field contribution to geoid accuracy

Young scientists training (cnt) Ms. Li will focus on the validation of earth's gravity field models from GOCE by using the GPS/Leveling data in Chinese territory and the validation of marine gravity anomalies derived from altimeter data Mr. Xu will focus on cross-validation of HY-2 altimeter data by comparing to altimeter data from other missions, such as Jason-2, Envisat, etc. He will also study the gravity filtering techniques and optimal methods of data fusion

Young scientists training (cnt) As outcome of this project we expect that our young colleagues will present their results obtained in the course of this project in scientific meetings and conferences and that this will contribute to a great extent into their scientific career goals. 4 PhD theses are also furthermore expected as outcome of this project

Expected Project results Assessment of GOCE products with terrestrial data from China and Finland, maps of discrepancies, GOCE models accuracy tests, documentation of filtering/spectral enhancement methods and their usability Geoid solution for Finnland and part of China by inclusion of GOCE models Assessment of HY-2 Chinese altimeter mission. 4+ Peer reviewed publications dealing with abovementioned results. 5 PhD theses of students involved in the project Attending scientific conferences and assemblies and presenting the project results

Thank you for your attention