1 Observations. Sat05_71.ppt, 2005-11-28. Directions: satellite visible with stars as background. Direction to radio-source (VLBI) Directions and distances:

Slides:

Advertisements

Similar presentations

Satellite geodesy, Fall C.C.Tscherning, University of Copenhagen,

Advertisements

MR P.Durkee 5/20/2015 MR3522Winter 1999 MR Remote Sensing of the Atmosphere and Ocean - Winter 1999 Active Microwave Radar.

Time Transfert by Laser Link T2L2 On Jason 2 OCA –UMR Gemini Grasse – FRANCE E. Samain – Principal.

SURVEYING II UNIT IV PRESENTATION II.

Satellite geodesy. Basic concepts. I1.1a = geocentric latitude φ = geodetic latitude r = radial distance, h = ellipsoidal height a = semi-major axis, b.

Satellite geodesy, Fall C.C.Tscherning, University of Copenhagen,

ASIC**3 Workshop -- May 2006 Measuring Global Sea Level Rise With Satellite Radar Altimetry ASIC**3 Workshop -- May 2006 Laury Miller NOAA/NESDIS Lab for.

GRACE “Gravity Recovery and Climate Experiment” Use in measuring Earth’s gravitational field and geoids By Jacob Launder.

1 SLR Data Automatic Preprocessing BeiJing SLR Station Chinese Academy of Surveying and Mapping DING Jian QU Feng WEI Zhibin.

1 GPS processing. Sat07_82.ppt, Directly from the observations 2.From differences (especially if vectors between points are to be determined)

1 TRANSIT. Sat05_72.ppt, Doppler-effect used: In the orbit Distant observer.

1 GPS Observations and data-processing. Sat07_81.ppt, Observations: Pseudo-ranges from P-code obs. Pseudo-range differences from Doppler shift.

Active microwave systems (1) Satellite Altimetry

Environmental Geodesy

Remote Sensing: John Wilkin Active microwave systems (1) Satellite Altimetry IMCS Building Room 214C ext

Ground-Based Altimetry Using a Single- Receiver Single-Frequency GNSS Phase Ambiguity Resolution Technique G. Stienne* S. Reboul J.-B. Choquel M. Benjelloun.

Navigational Aids Know the theory and operation of modern air navigational aids.

DORIS - DAYS Toulouse May 2-3, 2000 DORIS Doppler Orbitography and Radiopositioning Integrated by Satellite  Basic system concept  Main missions  Schedules.

ESPACE Porto, June 2009 MODELLING OF EARTH’S RADIATION FOR GPS SATELLITE ORBITS Carlos Javier Rodriguez Solano Technische Universität München

Unit 11 Lesson 5 Light Technology Copyright © Houghton Mifflin Harcourt Publishing Company.

Geodesy A look at the Earth. What is Geodesy? - The Merriam Webster Dictionary defines Geodesy as, "a branch of applied mathematics concerned with the.

Satellite geodesy (ge-2112) Observation systems E. Schrama.

ODINAFRICA/GLOSS Sea Level Training Course

ET- 3rd Indo-French Workshop on Megha-Tropiques, October ALTIKA / OCEANSAT3 ISRO / CNES mission Prepared by E. Thouvenot (CNES)

Satellite geophysics. Land and Sea Ice. C.C.Tscherning, University of Copenhagen, Applications: Mapping the altitude of ice-covered areas.

Unit E: Space Exploration. Heliocentric (Sun-centered) vs. Geocentric (Earth-centered) HeliocentricGeocentric.

Observations Passive: Natural Signals Photographs Semi-Passive: Artificial Signals GPS receiver Active: Signals Controlled by Observers Radar Echo, Laser.

Contour Mapping Topographic Maps – a detailed map showing hills, valleys, and other features of a specific area.

Space Geodesy Networks to Improve the ITRF Michael Pearlman Harvard-Smithsonian Center for Astrophysics Cambridge MA USA Erricos.

The only core network station in the Arctic Photo: Rambøll.

Regional and Global Measurements: The Reference Frame for Understanding Observations Geoff Blewitt University of Nevada, Reno, USA Zuheir Altamimi IGN,

Satellite Altimetry - possibilities and limitations

VLBI2010 Reference antenna for antenna deformations and site ties East Coast Geodetic VLBI Meeting Feb, 2011, Haystack Observatory Bill Petrachenko.

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.,

March 1 & 2, 2005NC&I WG GGOS Meeting/GFZ1 International Laser Ranging Service GGOS Meeting GFZ Potsdam Germany March 1 and 2, 2005.

Using What You’ve Learned About Electromagnetic Radiation and Sound (Acoustic Energy) to Measure Speed and Distance April 2007.

IRI Workshop 2005 TEC Measurements with Dual-Frequency Space Techniques and Comparisons with IRI T. Hobiger, H. Schuh Advanced Geodesy, Institute of Geodesy.

Sea Level Change Measurements: Estimates from Altimeters Understanding Sea Level Rise and Variability June 6-9, 2006 Paris, France R. S. Nerem, University.

Satellite Oceanography and Applications 2: Altimetry, scatterometry, SAR, GRACE RMU Summer Program (AUGUST 24-28, 2015)

Pioneer Anomaly Test – Jonathan Fitt 1 Design Assessment of Lunar, Planetary and Satellite Ranging Applied to Fundamental Physics Jonathan Fitt Friday,

SPACE GEODESY NETWORK & ITRF Z Minchul LEE 1.

Faculty of Applied Engineering and Urban Planning Civil Engineering Department Introduction to Geodesy and Geomatics Position, Positioning Modes, and the.

Data management: Data sources & Quality control. Sea level measurements.

Monitoring of altimeter measurements against a global tide gauge network F. Lefèvre, G. Valladeau, E. Sénant, J. Dorandeu F. Lefèvre, G. Valladeau, E.

remote sensing electromagnetic spectrum frequency Landsat satellite Objectives Compare and contrast the different forms of radiation in the electromagnetic.

(a) Pre-earthquake and (b) post-earthquake Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) images of North Sentinel Island. The.

Seasonal Terrestrial Water Storage Change and Global Mean Sea Level Variation Jianli Chen 1 and Clark Wilson 1,2 Center for Space Research, The University.

SLR in the age of GPS Frank G. Lemoine, Scott B. Luthcke, Nikita P Zelensky Brian D. Beckley Code 697, Space Geodesy Laboratory NASA Goddard Space Flight.

AOGS 5 th Annual Meeting 2008, June 16-20, 2008, Busan, Korea GG S Global Geodetic Observing System (GGOS): Status and Future Markus Rothacher, Ruth Neilan,

Choose a category. You will be given the answer. You must give the correct question. Click to begin.

Sun Controls Earth’s Climate System Earth has a global climate system that includes air, land, liquid water, ice, and living things.climate system The.

Chapter 9.1 Notes Electromagnetic Waves Part 1. A changing electric field can produce a changing Magnetic Field.Magnetic Field. A changing magnetic field.

Earth Surface and Interior Focus Area Space Geodetic Networks for Maintaining the Reference Frame Geodesy's Critical Contributions to NASA (Earth Science)

What Channel is That?.  Visible light is a form of electromagnetic radiation.  Others include:  Radio waves  Infrared waves (heat)  Ultraviolet waves.

1 Satellite geodesy (ge-2112) Applications E. Schrama.

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.

Center for Satellite Applications and Research (STAR) Review 09 – 11 March 2010 Image: MODIS Land Group, NASA GSFC March 2000 Closing the Global Sea Level.

Electromagnetic Spectrum. -is the range of all possible frequencies of electromagnetic radiation. The "electromagnetic spectrum" of an object is the characteristic.

Earth Surface and Interior Focus Area Space Geodetic Networks for Maintaining the Reference Frame Geodesy's Critical Contributions to NASA (Earth Science)

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.

Doppler Effect Moving source, stationary observer:

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.

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.

SVY207 Lecture 8: The Carrier Phase Observable

How Do we Estimate Gravity Field? Terrestrial data –Measurements of surface gravity –Fit spherical harmonic coefficients Satellite data –Integrate equations.

Unit 3 Lesson 5 Light Technology

Chapter Using Technology to See the Visible

Unit 3 Lesson 5 Light Technology

Remote Sensing.

Laser Interferometry for a future GRACE follow-on mission

Presentation transcript:

1 Observations. Sat05_71.ppt, Directions: satellite visible with stars as background. Direction to radio-source (VLBI) Directions and distances: if satellite carries reflectors

2 Stellar-triangulation. Sat05_71.ppt

3 Global network. Sat05_71.ppt

4 West-European Network. sat05_71.ppt

5 North-American Network: First results for Greenland

6 Distances. Sat05_71.ppt, Reflected light: Lasers – 2-ways. SLR= Satellite Laser Ranging. aus.com/satellite_laser_ranging.htm Satellite emits signal: 1 way or two ways.

7 Laser

8 LAGEOS

9 Earth-Moon system

10 Distance measurements. Sat05_71.ppt, Signal: Impuls: Phase: λ Δλ

11 Integer ambiguity. Sat05_71.ppt, N may be determined using Signal with several frequencies Several observations

12 Distance-differences. Doppler. Sat05_71.ppt, Observations:

13 Satellite Altimetry. Sat05_71.ppt, Geos-3, GSFO SEASAT Topex/Poseidon, Jason, ERS1 + 2, Envisat and CRYOSAT Satellite Water – Ice - Plains

14 Satellite-to-Satellite Tracking. Sat05_71.ppt, CHAMP, from GPS to satellite GRACE. from GPS to two satellites and ranging between the satellites GOCE, from GPS to the satellite.

15 Interferometry. Sat05_71.ppt,

16 VLBI. Sat05_71.ppt,

17 Results. Sat05_71.ppt,