What does Height Really Mean?. How We Measure Height Heights are generally measured against one of two different reference frames (datums). 1.Gravity.

Slides:



Advertisements
Similar presentations
Scheduled for HYPACK 2011 Release
Advertisements

Procedure for GPS Height Transformation within a Small Local Area
Navigation Fundamentals
The general equation for gravity anomaly is: where:  is the gravitational constant  is the density contrast r is the distance to the observation point.
Datums, Heights and Geodesy Central Chapter of the Professional Land Surveyors of Colorado 2007 Annual Meeting Daniel R. Roman National Geodetic Survey.
National report of LITHUANIA THE 4th BALTIC SURVEYORS FORUM, 2013, Ventspils, LATVIA Eimuntas Parseliunas Geodetic Institute of Vilnius Technical University.
Geographic Datums Y X Z The National Imagery and Mapping Agency (NIMA) and the Defense Mapping School Reviewed by:____________ Date:_________ Objective:
Des Éléments Importants des Systèmes de Référence et de la Géodésie au CERN Mark Jones EN\MEF-SU.
GI Systems and Science January 11, Points to Cover  Introduction  Maps and spatial data  How spatial data is represented in GIS Scale Spatial.
and IGLD 85 Hydraulic Correctors
NOAA’s National Geodetic Survey USGG2009 & GEOID09: New geoid height models for surveying/GIS ACSM-MARLS-UCLS-WFPS Conference FEB 2009 Salt Lake.
Geodesy, Map Projections and Coordinate Systems Geodesy - the shape of the earth and definition of earth datums Map Projection - the transformation of.
Juliana Blackwell, Director National Geodetic Survey, NOAA
1 Geodesy for Neutrino Physicists by Wes Smart, Fermilab Based on: “GPS Satellite Surveying” By Alfred Leick, Wiley (1990 ) Geodesy : a branch of applied.
0/27 Merriam-Webster: a branch of applied mathematics concerned with the determination of the size and shape of the earth and the exact positions of points.
VDATUM: the Vertical Datum Transformation Tool
Modern Navigation Thomas Herring MW 10:30-12:00 Room
SU 4100 GEODETIC POSITIONING Instructor: Indra Wijayratne.
Lecture 11: Geometry of the Ellipse 25 February 2008 GISC-3325.
Geography 370 Locating Positions on the Earth
1 Assessment of Geoid Models off Western Australia Using In-Situ Measurements X. Deng School of Engineering, The University of Newcastle, Australia R.
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.
Geoid Modeling at NOAA Dru A. Smith, Ph.D. National Geodetic Survey National Ocean Service, NOAA November 13, 2000.
Integrated and Collaborative Organizations Create Geospatial Solutions Geospatial Solutions by DBZ Achieving Great Heights: Toward a Better Vertical Reference.
Lecture 7 – More Gravity and GPS Processing GISC February 2009.
Gravity Methods Gravity is not a “constant” 9.78 m/s 2 Responds to local changes in rock density Widely used in oil and gas, mineral exploration, engineering.
Tide corrections from KGPS and a precise geoid John Brozena, Randy Herr, Vicki Childers.
An application of FEM to the geodetic boundary value problem Z. Fašková, R. Čunderlík Faculty of Civil Engineering Slovak University of Technology in Bratislava,
Who Needs New Datums? NGS Says… ftp://ftp.ngs.noaa.gov/pub/marti Marti Ikehara California Geodetic Advisor, Sacramento.
More observables: gravity and the geoid Isostasy “Perfect” adjustment not realistic… –Rigid crust, dynamic features in mantle mean that density anomalies.
GG 450 Lecture 3 1/22/08 Gravity Corrections Potential Geoid.
Feedback on the New Datums Reference Frames 2015 Geospatial Summit April 14, 2015 Amar Nayegandhi Dewberry Consultants LLC.
PRS92 Bonifacia Daet Sylvia Esperanza
Map Basics Lecture #3, Intro to GIS spring Topics Map definitions Types of maps Map projections Geodetic Datums Coordinate Systems.
GRAV-D Part II : Examining airborne gravity processing assumptions with an aim towards producing a better gravimetric geoid Theresa Diehl*, Sandra Preaux,
Establishing A Gravity Plan Ohio Department of Transportation October 14, 2011.
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.
Vicki Childers National Geodetic Survey GRAV-D: The Gravity for the Re- definition of the American Vertical Datum ACSM 2009 Workshop.
Geography 70  Basic Geodesy  Map Projections  Coordinate Systems  Scale Locating Positions on the Earth.
Why do Millimeters Matter? NOAA Models and Tools Support High Accuracy Positioning for Ecosystem Restoration and Ecological Research Surface too low: too.
Center for Modeling & Simulation.  It is always necessary to unify objects recorded in different coordinate system, into one system using coordinate.
The Height Modernization Program in the United States and the Future of the National Vertical Reference Frame 1 Renee Shields National Geodetic Survey,
BOT / GEOG / GEOL 4111 / Field data collection Visiting and characterizing representative sites Used for classification (training data), information.
AUSGeoid Richard Bean Robyn Stevens 26 May Geoid 3D surface of equal gravity (Equipotential) Not smooth like an ellipsoid Transformation needed.
Tide corrections from KGPS and a precise geoid
Section 9: Extracting a Shoreline from Lidar Data.
The Delta Levees Program
Catherine LeCocq SLAC USPAS, Cornell University Large Scale Metrology of Accelerators June 27 - July 1, 2005 Height Systems 1 Summary of Last Presentation.
Lecture 7 – Gravity and Related Issues GISC February 2008.
WATER LEVEL OPTIONS. Water Level Corrections Water Level Above Chart Datum = Negative Tide Correction! In Depth Mode:  Chart Sounding =  Measured Sounding.
Or : Why doesn’t my GPS elevation agree with other measurements of elevation?
GEOID03 in Louisiana and Alaska Dr. Yan M Wang and Dr. Daniel R Roman Geodesist, NGS/NOAA ACSM Annual Conference and Technology Exhibition Orlando, FL.
EE 495 Modern Navigation Systems Navigation Mathematics Earth Surface and Gravity Wednesday, Feb EE 495 Modern Navigation Systems Slide 1 of 14.
Nic Donnelly – Geodetic Data Analyst 5 March 2008 Vertical Datum Issues in New Zealand.
Surface and bottom topography of the oceans. How do we measure seafloor topography? Why is ocean bathymetry important? Questions:
Why ocean bathymetry?. How do we measure bathymetry? Why is ocean bathymetry important? Questions:
SRM Tutorial, STC 2000, Snowbird, Utah Section IIB A Few More Facts and Diagrams.
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.
Subsidence Monitoring and the GRAV-D project Dru Smith, Dan Roman, Daniel Winester, Mark Eckl NOAA’s National Geodetic Survey Subsidence Workshop -
Gravity II: Gravity anomaly due to a simple-shape buried body
Earth to Globe to Map Map Projection: Map Scale: Scale Factor, k
Maps Base maps Coordinate Systems, Datums, Projections
Lecture 2 GRAVITY CLASS WEBSITES Lectures Labs
0/27 Merriam-Webster: a branch of applied mathematics concerned with the determination of the size and shape of the earth and the exact positions of points.
to understand what is in the water…
California Geodetic Advisor,
Geoid Enhancement in the Gulf Coast Region
Fundamentals of Geodesy
Sea-Level changes.
Presentation transcript:

What does Height Really Mean?

How We Measure Height Heights are generally measured against one of two different reference frames (datums). 1.Gravity (geopotential height) 2.Ellipsoid (ellipsoid height) These heights are not interchangeable. Without site specific gravitation measurements no transformation between them. Orthometric Height

Ellipsoid Height (I know these pictures are spheroids but they look good!) Height above a mathematical surface Simple, cost effective, time invariant reference surface Geocentric Datum: Regularly used for height measurements particularly by GPS devices Local Datum: Not generally used for height measurements

Geoid in Height Measurements Initially Mean Sea Level used as the reference surface Discovery that MSL is not the same height in all places Requirement to find a new reference surface…. Geoid Geoid is “the equipotential surface of the Earth’s gravity field that nominally defines mean sea level” Meyer et al Geoid is perpendicular to gravity at all points Traditional measurement techniques (e.g. levelling) are heights above this surface

Relating Ellipsoid Height to Orthometric Height h = H + N Important to note that h and N are reference ellipsoid specific In Australia the value of N can be obtained from AUSGeoid98 GPS heights less the value of N provide the orthometric height This technique is referred to as GPS levelling Not yet regarded as being as accurate as traditional levelling

Why don’t we just use GPS heights? Reference Ellipsoid lacks the subtle variation of the geoid  Water flowing uphill GPS levelling will improve as geoid models improve (sampling at a finer spatial resolution) If everyone used the same reference ellipsoid and it did not change, isn’t that enough? 60% of GPS users do not come from a surveying background. (Waite 2005) Why should they doubt height readings from their GPS device. Answer to these problems: Real time correction for orthometric height within GPS devices. (Connectivity)

Questions? Meyer, Thomas H.; Roman, Daniel R.; Zilkoski, David B. (2005) What does height really mean? Part II: Physics and Gravity, Surveying and Land Information Science, 65(1), pp Waite, Lucan (2005) Geoid Modelling, Survey Quarterly, 43 pp REFERENCES