GGOS User Requirements and Functional Specifications Richard S. Gross Jet Propulsion Laboratory, California Institute of Technology, Pasadena, USA Global.

Slides:



Advertisements
Similar presentations
Philip L. Woodworth Permanent Service for Mean Sea Level With an enormous amount of assistance from Norman Teferle and Richard Bingley University.
Advertisements

Atmospheric Loading Nicole M. Shivers.  “The Earth’s surface is perpetually being displaced due to temporally varying atmospheric oceanic and continental.
Geodetic Reference Frames In Presence of Crustal Deformations Martin Lidberg 1,2, Maaria Nordman 3, Jan M. Johansson 1,4, Glenn A Milne5, Hans-Georg Scherneck.
Reference Frames for GPS Applications and Research
Seasonal Position Variations and Regional Reference Frame Realization Jeff Freymueller Geophysical Institute University of Alaska Fairbanks.
Effect of Surface Loading on Regional Reference Frame Realization Hans-Peter Plag Nevada Bureau of Mines and Geology and Seismological Laboratory University.
2-3 November 2009NASA Sea Level Workshop1 The Terrestrial Reference Frame and its Impact on Sea Level Change Studies GPS VLBI John Ries Center for Space.
Environmental Geodesy
The Four Candidate Earth Explorer Core Missions Consultative Workshop October 1999, Granada, Spain, Revised by CCT GOCE S 43 Science and.
VieVS User Workshop 14 – 16 September, 2011 Vienna VIE_MOD Lucia Plank.
The Four Candidate Earth Explorer Core Missions consultative Workshop October 1999, Granada, Spain, Revised by CCT GOCE S 23 The gravity.
Facilitating Joint Analysis of Data From Several Systems Using Geophysical Models Hans-Peter Plag, William C. Hammond, Geoffrey Blewitt Nevada Bureau of.
Laser Ranging Contributions to Earth Rotation Studies Richard S. Gross Jet Propulsion Laboratory California Institute of Technology Pasadena, CA 91109–8099,
An optimist's 20 year look-ahead at geodesy and geophysics Dru Smith, Chief Geodesist NOAA’s National Geodetic Survey NRC Workshop on NGA future directions12010.
Mass and Volume Contribution to Twentieth-century Global Sea Level Rise L. Miller & B. C. Douglas Nature vol. 428, 2004.
Cryospheric and Hydrologic Contributions to Global Sea Level Change M. Tamisiea Proudman Oceanographic Laboratory R. Steven Nerem University of Colorado.
The Global Geodetic Observing System: Meeting the Requirements of a Global Society on a Changing Planet in 2020 Hans-Peter Plag, Reiner Rummel, Dork Sahagian,
1 Applications of the CORS System Richard Snay & Giovanni Sella National Geodetic Survey National Ocean Service, NOAA NOAA GNSS Workshop Boulder, Colorado.
NASA, CGMS-41, July 2013 Coordination Group for Meteorological Satellites - CGMS The Terrestrial Reference Frame by NASA Presented to CGMS-41 Working Group.
Task AR-07-03: Global Geodetic Reference Frames Report to ADC-5 prepared by Hans-Peter Plag (IAG/GGOS) Nevada Bureau of Mines and Geology and Seismological.
Modern Navigation Thomas Herring MW 10:30-12:00 Room
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.
Geography 370 Locating Positions on the Earth
Faculty of Applied Engineering and Urban Planning Civil Engineering Department Geographic Information Systems Spatial Referencing Lecture 4 Week 6 1 st.
Who Needs New Datums? NGS Says… ftp://ftp.ngs.noaa.gov/pub/marti Marti Ikehara California Geodetic Advisor, Sacramento.
NGS GPS ORBIT DETERMINATION Positioning America for the Future NATIONAL OCEANIC AND ATMOSPHERIC ADMINISTRATION National Ocean Service National Geodetic.
Chapter 8: The future geodetic reference frames Thomas Herring, Hans-Peter Plag, Jim Ray, Zuheir Altamimi.
Regional and Global Measurements: The Reference Frame for Understanding Observations Geoff Blewitt University of Nevada, Reno, USA Zuheir Altamimi IGN,
Space Geodesy (1/3) Geodesy provides a foundation for all Earth observations Space geodesy is the use of precise measurements between space objects (e.g.,
Geodetic Networks: The Supporting Framework Terrestrial Reference Frame is ‘Critical Infrastructure’ for all Earth science research and applications. Global.
Outline  Construction of gravity and magnetic models  Principle of superposition (mentioned on week 1 )  Anomalies  Reference models  Geoid  Figure.
Sea Level Change Measurements: Estimates from Altimeters Understanding Sea Level Rise and Variability June 6-9, 2006 Paris, France R. S. Nerem, University.
Sea-Level Change Driven by Recent Cryospheric and Hydrological Mass Flux Mark Tamisiea Harvard-Smithsonian Center for Astrophysics James Davis Emma Hill.
Sea level: measuring the bounding surfaces of the ocean by Mark E. Tamisiea, Chris W. Hughes, Simon D. P. Williams, and Richard M. Bingley Philosophical.
1 Geoid and Geoid Change: Discussion Topics Roger Haagmans, Boulder, 21October 2009.
01/0000 HEO and Daylight Ranging “Reality and Wishes” Ramesh Govind ILRS Fall Workshop, 4 th October 2005.
NASA GNSS Applications & Geosciences Ruth E. Neilan Jet Propulsion Laboratory California Institute of Technology International GNSS Central Bureau Pasadena,
National Geodetic Survey – Continuously Operating Reference Stations & Online Positioning User Service (CORS & OPUS) William Stone Southwest Region (UT,
State-of-the-art physical models for calculating atmospheric pressure loading effects 1 Geodätische Woche October, Köln, Germany Dudy D.
Environmental Geodesy Lecture 11 (April 4, 2011): Loading - Predicting loading signals - Atmospheric loading - Ocean tidal loading - Non-tidal ocean loading.
Geography 70  Basic Geodesy  Map Projections  Coordinate Systems  Scale Locating Positions on the Earth.
Gravimetry Geodesy Rotation
Reference Frame Theory & Practice: Implications for SNARF SNARF Workshop 1/27/04 Geoff Blewitt University of Nevada, Reno.
An Overview of the Observations of Sea Level Change R. Steven Nerem University of Colorado Department of Aerospace Engineering Sciences Colorado Center.
Earth Surface and Interior Focus Area Space Geodetic Networks for Maintaining the Reference Frame Geodesy's Critical Contributions to NASA (Earth Science)
Global VLBI Solution IGG05R01 1 Institute of Geodesy and Geophysics (IGG), Vienna, Austria 2 German Geodetic Research Institute (DGFI), Munich, Germany.
Data for Plate Tectonics Earthquakes –World wide network for detecting nuclear tests Magnetic stripes –From World War 2 submarine detection Bathymetry.
Don Chambers Center for Space Research, The University of Texas at Austin Josh Willis Jet Propulsion Laboratory, California Institute of Technology R.
LLR Analysis – Relativistic Model and Tests of Gravitational Physics James G. Williams Dale H. Boggs Slava G. Turyshev Jet Propulsion Laboratory California.
(c) 2009 California Institute of Technology. Government sponsorship acknowledged. Improving Predictions of the Earth’s Rotation Using Oceanic Angular Momentum.
View on GPS and Galileo ‘From across the Atlantic…’ Ruth E. Neilan International GNSS Service (IGS) Central Bureau Jet Propulsion Laboratory/California.
Earth System Data Record of mass transport from time-variable gravity data Victor Zlotnicki 1, Matthieu Talpe 2, F. Lemoine 3, R. Steven Nerem 2, Felix.
1. The International Terrestrial Reference Frame (ITRF) needs to be made more robust and stable over multi-decadal time scales. –target accuracy is 0.1.
SPP Mass Transport and Mass Distribution in the Earth System Contribution of the New Generation of Satellite Gravity and Altimetry Missions to Geosciences.
Water vapour estimates over Antarctica from 12 years of globally reprocessed GPS solutions Ian Thomas, Matt King, Peter Clarke Newcastle University, UK.
A proposal for a consistent model of air pressure loading as part of the International Terrestrial Reference System (ITRS) Conventions Plag, H.-P. (1),
Geodetic Networks: The Supporting Framework Terrestrial Reference Frame is ‘Critical Infrastructure’ for all Earth science research and applications. Global.
Earth Surface and Interior Focus Area Space Geodetic Networks for Maintaining the Reference Frame Geodesy's Critical Contributions to NASA (Earth Science)
12/12/01Fall AGU Vertical Reference Frames for Sea Level Monitoring Thomas Herring Department of Earth, Atmosphere and Planetary Sciences
IVS High Accuracy Products for the Maintenance of the Global Reference Frames as a Contribution to GGOS VLBI provides high accuracy and unique products.
IGARSS 2011, Vancuver, Canada July 28, of 14 Chalmers University of Technology Monitoring Long Term Variability in the Atmospheric Water Vapor Content.
11-12 April 2005NASA Sea Level Workshop1 SPACE GEODETIC MEASUREMENT SYSTEM FOR GLOBAL SEA LEVEL CHANGE "In all things it is a good idea to hang a question.
29 August 2005Geosciences Australia1 Space Geodesy, SLR and Global Sea Level Change John Ries Canberra, Australia August 29,,2005.
Earth Surface and Interior Focus Area Space Geodetic Networks for Maintaining the Reference Frame Geodesy's Critical Contributions to NASA (Earth Science)
How Convection Currents Affect Weather and Climate.
THE NATURE OF SCIENCE Earth Science is the study of the Earth Processes and Forces that change it The materials from which it is made Its long history.
Unit D: Energy Flow in Global Systems. The Biosphere.
THE EARTH’S CLIMATE SYSTEM
The DNSC08ERR Interpolatsion Error
Presentation transcript:

GGOS User Requirements and Functional Specifications Richard S. Gross Jet Propulsion Laboratory, California Institute of Technology, Pasadena, USA Global Geodetic Observing System Forum April 17, 2007 Vienna, Austria

Products of GGOS Celestial reference frame Catalog of celestial radio sources including their coordinates Terrestrial reference frame Catalog of terrestrial sites Including their coordinates and parameters (trend, periodic terms) describing their temporal evolution Time series of coordinates of additional terrestrial sites Including necessary models and/or observations Needed to densify TRF to provide access to TRF anywhere on Earth’s surface Earth orientation parameters Time series of values and their rates-of-change Geodetic reference system Values of defining constants Values of derived physical and geometrical parameters

Products of GGOS, cont. Gravity field Values of parameters describing static component Time series of parameters describing time-dependent component Total electron content of ionosphere Time-dependent maps Water vapor content of troposphere Time series of zenith path delays Mass transport within Earth system Time series of angular momentum of Atmosphere, oceans, continental water, mantle, core Shape of land surface Time series of site displacements caused by loading effects Atmospheric surface pressure, ocean-bottom pressure, continental water

Products of GGOS, cont. Shape of ocean surface Time series of sea surface height measurements Altimetry Time series of sea level measurements Tide gauge Shape of ice surface Time series of ice sheet and glacier elevations Other planets and celestial bodies in solar system Time-dependent, body-fixed site coordinates Orientation parameters Gravity parameters

Accuracy of GGOS Products Focus on most demanding user Requirements of all other users will be automatically met Terrestrial Reference Frame Most demanding user: Studies of sea level change Sea level rising at a few mm/yr Reference frame should be at least an order of magnitude more accurate TRF should be accurate to 1 mm, stable to 0.1 mm/yr (including geocenter) Scale should be accurate to 0.01 ppb, stable to ppb/yr Earth orientation parameters Most demanding user: Tracking and navigating interplanetary spacecraft Capability driven: Uses most accurate EOPs available Needs EOPs consistent with TRF and CRF Thus, for consistency with TRF, EOPs should be: accurate to 1 mm with 2-week latency, to 3 mm in near real-time, daily resolution

Accuracy of GGOS Products, cont. Celestial reference frame To be consistent with TRF and EOPs Should be accurate to 30  as, stable to 3  as/yr Gravity field Most demanding users of geoid: (1) Ocean modeling (2) GNSS determinations of height above geoid Static geoid should be accurate to 1 mm, stable to 0.1 mm/yr with spatial resolution of 10 km Time varying geoid should be accurate to 1 mm, stable to 0.1 mm/yr with spatial resolution of 50 km and temporal resolution of 10 days