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Geodetic Surveying, Earth Modeling, and the New Geodetic Datum of 2022
Geodetic Surveying, Earth Modeling, and the New Geodetic Datum of 2022 PDH330 3 Hours PDH Academy PO Box 449 Pewaukee, WI 53072 (888) 564-9098 www.pdhacademy.com [email protected] Geodetic Surveying Final Exam 1. Who established the U.S. Coast and Geodetic Survey? A) Thomas Jefferson B) Benjamin Franklin C) George Washington D) Abraham Lincoln 2. Flattening is calculated from what? A) Equipotential surface B) Geoid C) Earth’s circumference D) The semi major and Semi minor axis 3. A Reference Frame is based off how many dimensions? A) two B) one C) four D) three 4. Who published “A Treatise on Fluxions”? A) Einstein B) MacLaurin C) Newton D) DaVinci 5. The interior angles of an equilateral planar triangle adds up to how many degrees? A) 360 B) 270 C) 180 D) 90 6. What group started xDeflec? A) NGS B) CGS C) DoD D) ITRF 7. When will NSRS adopt the new time-based system? A) 2022 B) 2020 C) Unknown due to delays D) 2021 8. Did the State Plane Coordinate System of 1927 have more zones than the State Plane Coordinate System of 1983? A) No B) Yes C) They had the same D) The State Plane Coordinate System of 1927 did not have zones 9. A new element to the State Plane Coordinate System of 2022 is: A) The addition of Low Distortion Projections B) Adjoining tectonic plates C) Airborne gravity collection D) None of the above 10. The model GRAV-D (Gravity for Redefinition of the American Vertical Datum) created will replace _____________ and constitute the new vertical height system of the United States A) Decimal degrees B) Minutes C) NAVD 88 D) All of the above Introduction to Geodetic Surveying The early curiosity of man has driven itself to learn more about the vastness of our planet and the universe. -
Geodesy in the 21St Century
Eos, Vol. 90, No. 18, 5 May 2009 VOLUME 90 NUMBER 18 5 MAY 2009 EOS, TRANSACTIONS, AMERICAN GEOPHYSICAL UNION PAGES 153–164 geophysical discoveries, the basic under- Geodesy in the 21st Century standing of earthquake mechanics known as the “elastic rebound theory” [Reid, 1910], PAGES 153–155 Geodesy and the Space Era was established by analyzing geodetic mea- surements before and after the 1906 San From flat Earth, to round Earth, to a rough Geodesy, like many scientific fields, is Francisco earthquakes. and oblate Earth, people’s understanding of technology driven. Over the centuries, it In 1957, the Soviet Union launched the the shape of our planet and its landscapes has developed as an engineering discipline artificial satellite Sputnik, ushering the world has changed dramatically over the course because of its practical applications. By the into the space era. During the first 5 decades of history. These advances in geodesy— early 1900s, scientists and cartographers of the space era, space geodetic technolo- the study of Earth’s size, shape, orientation, began to use triangulation and leveling mea- gies developed rapidly. The idea behind and gravitational field, and the variations surements to record surface deformation space geodetic measurements is simple: Dis- of these quantities over time—developed associated with earthquakes and volcanoes. tance or phase measurements conducted because of humans’ curiosity about the For example, one of the most important between Earth’s surface and objects in Earth and because of geodesy’s application to navigation, surveying, and mapping, all of which were very practical areas that ben- efited society. -
NASA Space Geodesy Program: Catalogue of Site Information
NASA Technical Memorandum 4482 NASA Space Geodesy Program: Catalogue of Site Information M. A. Bryant and C. E. Noll March 1993 N93-2137_ (NASA-TM-4482) NASA SPACE GEODESY PROGRAM: CATALOGUE OF SITE INFORMATION (NASA) 688 p Unclas Hl146 0154175 v ,,_r NASA Technical Memorandum 4482 NASA Space Geodesy Program: Catalogue of Site Information M. A. Bryant McDonnell Douglas A erospace Seabro'ok, Maryland C. E. Noll NASA Goddard Space Flight Center Greenbelt, Maryland National Aeronautics and Space Administration Goddard Space Flight Center Greenbelt, Maryland 20771 1993 . _= _qum_ Table of Contents Introduction .......................................... ..... ix Map of Geodetic Sites - Global ................................... xi Map of Geodetic Sites - Europe .................................. xii Map of Geodetic Sites - Japan .................................. xiii Map of Geodetic Sites - North America ............................. xiv Map of Geodetic Sites - Western United States ......................... xv Table of Sites Listed by Monument Number .......................... xvi Acronyms ............................................... xxvi Subscription Application ..................................... xxxii Site Information ............................................. Site Name Site Number Page # ALGONQUIN 67 ............................ 1 AMERICAN SAMOA 91 ............................ 5 ANKARA 678 ............................ 9 AREQUIPA 98 ............................ 10 ASKITES 674 ........................... , 15 AUSTIN 400 ........................... -
Report of the Commissioner of the General Land Office, 1860
University of Oklahoma College of Law University of Oklahoma College of Law Digital Commons American Indian and Alaskan Native Documents in the Congressional Serial Set: 1817-1899 11-29-1860 Report of the Commissioner of the General Land Office, 1860 Follow this and additional works at: https://digitalcommons.law.ou.edu/indianserialset Part of the Indian and Aboriginal Law Commons Recommended Citation S. Exec. Doc. No. 2, 36th Cong., 2nd Sess.(1860) This Senate Executive Document is brought to you for free and open access by University of Oklahoma College of Law Digital Commons. It has been accepted for inclusion in American Indian and Alaskan Native Documents in the Congressional Serial Set: 1817-1899 by an authorized administrator of University of Oklahoma College of Law Digital Commons. For more information, please contact [email protected]. SECRETARY OF THE INTERIOR. 49 REPORT OF THE CO~I~IJISSIONER OF TI-IE GENER.AL LAND OFFICE. ' GENERAL LAND OFFICE, November 29, 1860. Sn-t: During the past year the operations of the land system have extended by direct administrq.tive action within the limits of all the political divisions embracing the public domain, to wit: Ohio, Indiana, Michigan, Illinois, Wisconsin, Iowa, California, Oregon, Minnesota, Florida, Alabama, Mississippi, Louisiana, Arkansas, Missouri, and to the Territories of Kansas, Nebraska, Minnesota, (known as Dacotah,) Washington, New Mexico, and Utah. Our correspondence has passed those limits, having extended within all the other members of the Confederacy where non-resident claimants hold interests, requiring adjustment under bounty land grants for services in the war of the revolution, in the last war with Great Britain, the war with Mexico, with Indian tribes, under foreign titles, and under other grants in great diversity. -
General Assembly
UNITED NATIONS Distr. GENERAL GENERAL A/AC.135/11/Add.l ASSEMBLY 13 August 1968 ORIGINAL: ENGLISH AD HCC COMMITTEE TO STUDY THE PEACEFUL USES OF THE SEA-BED AND THE CCEAN FLOOR BEYOND THE LIMITS OF NATIONAL JURISDICTION Third session SURVEY OF NATIONAL LEGISLATION CONCERNING THE SEA-BED AND THE OCEAN FLOOR, AND THE SUBSOIL THEREOF, UNDERLYING THE HIGH SEAS BEYOND THE LIMITS OF PRESENT NATIONAL JURISDICTION Document prepared by the Secretariat I ... 68-17267 A/AC.135/11/Add.l English Page 2 CONTE1"TS Ifote . 3 I. Limits of the territorial sea. 5 II. Limits and scope of national jurisdiction over the continental shelf 9 1. Brazil. 10 2. Dahomey 11 3. Dcminican Republic 12 4. Guaterr:.ala 12 5. India 13 6. Iran 14 7, Ivory Coast . 15 8. IJicaragua . 15 9. Senegal 15 10. Spain . 16 11. United Kingdom of Great Britain and Northern Ireland 20 12. Venezuela 23 III. Protection of submarine cables and pipelinesY IV. Prevention of pollution of the seaY V. Prohibition of broadcasting from ships, aircraft and marine structures y VI. List of national laws, orders and regulations comprising exploration and exploitation procedures and safety practices 25 y No additional information has been received by the United Nations Secretariat. I ... A/AC.135/11/Add.l English Page 3 NOTE The present document contains legislative texts recently provided or indicated by Governments in response to circular notes sent to them by the Secretary-General on 16 March 1967, 26 January 1968 and 9 April 1968. / ... A/AC.135/11/Add.l English Page 5 I. -
A Unified Plane Coordinate Reference System
This dissertation has been microfilmed exactly as received COLVOCORESSES, Alden Partridge, 1918- A UNIFIED PLANE COORDINATE REFERENCE SYSTEM. The Ohio State University, Ph.D., 1965 Geography University Microfilms, Inc., Ann Arbor, Michigan A UNIFIED PLANE COORDINATE REFERENCE SYSTEM DISSERTATION Presented in Partial Fulfillment of the Requirements for The Degree Doctor of Philosophy in the Graduate School of The Ohio State University Alden P. Colvocoresses, B.S., M.Sc. Lieutenant Colonel, Corps of Engineers United States Army * * * * * The Ohio State University 1965 Approved by Adviser Department of Geodetic Science PREFACE This dissertation was prepared while the author was pursuing graduate studies at The Ohio State University. Although attending school under order of the United States Army, the views and opinions expressed herein represent solely those of the writer. A list of individuals and agencies contributing to this paper is presented as Appendix B. The author is particularly indebted to two organizations, The Ohio State University and the Army Map Service. Without the combined facilities of these two organizations the preparation of this paper could not have been accomplished. Dr. Ivan Mueller of the Geodetic Science Department of The Ohio State University served as adviser and provided essential guidance and counsel. ii VITA September 23, 1918 Born - Humboldt, Arizona 1941 oo.oo.o BoS. in Mining Engineering, University of Arizona 1941-1945 .... Military Service, European Theatre 1946-1950 o . o Mining Engineer, Magma Copper -
Reference Systems for Surveying and Mapping Lecture Notes
Delft University of Technology Reference Systems for Surveying and Mapping Lecture notes Hans van der Marel ii The front cover shows the NAP (Amsterdam Ordnance Datum) ”datum point” at the Stopera, Amsterdam (picture M.M.Minderhoud, Wikipedia/Michiel1972). H. van der Marel Lecture notes on Reference Systems for Surveying and Mapping: CTB3310 Surveying and Mapping CTB3425 Monitoring and Stability of Dikes and Embankments CIE4606 Geodesy and Remote Sensing CIE4614 Land Surveying and Civil Infrastructure February 2020 Publisher: Faculty of Civil Engineering and Geosciences Delft University of Technology P.O. Box 5048 Stevinweg 1 2628 CN Delft The Netherlands Copyright ©20142020 by H. van der Marel The content in these lecture notes, except for material credited to third parties, is licensed under a Creative Commons AttributionsNonCommercialSharedAlike 4.0 International License (CC BYNCSA). Third party material is shared under its own license and attribution. The text has been type set using the MikTex 2.9 implementation of LATEX. Graphs and diagrams were produced, if not mentioned otherwise, with Matlab and Inkscape. Preface This reader on reference systems for surveying and mapping has been initially compiled for the course Surveying and Mapping (CTB3310) in the 3rd year of the BScprogram for Civil Engineering. The reader is aimed at students at the end of their BSc program or at the start of their MSc program, and is used in several courses at Delft University of Technology. With the advent of the Global Positioning System (GPS) technology in mobile (smart) phones and other navigational devices almost anyone, anywhere on Earth, and at any time, can determine a three–dimensional position accurate to a few meters. -
Curvilinear Coordinate Systems
Appendix A Curvilinear coordinate systems Results in the main text are given in one of the three most frequently used coordinate systems: Cartesian, cylindrical or spherical. Here, we provide the material necessary for formulation of the elasticity problems in an arbitrary curvilinear orthogonal coor- dinate system. We then specify the elasticity equations for four coordinate systems: elliptic cylindrical, bipolar cylindrical, toroidal and ellipsoidal. These coordinate systems (and a number of other, more complex systems) are discussed in detail in the book of Blokh (1964). The elasticity equations in general curvilinear coordinates are given in terms of either tensorial or physical components. Therefore, explanation of the relationship between these components and the necessary background are given in the text to follow. Curvilinear coordinates ~i (i = 1,2,3) can be specified by expressing them ~i = ~i(Xl,X2,X3) in terms of Cartesian coordinates Xi (i = 1,2,3). It is as- sumed that these functions have continuous first partial derivatives and Jacobian J = la~i/axjl =I- 0 everywhere. Surfaces ~i = const (i = 1,2,3) are called coordinate surfaces and pairs of these surfaces intersects along coordinate curves. If the coordinate surfaces intersect at an angle :rr /2, the curvilinear coordinate system is called orthogonal. The usual summation convention (summation over repeated indices from 1 to 3) is assumed, unless noted otherwise. Metric tensor In Cartesian coordinates Xi the square of the distance ds between two neighboring points in space is determined by ds 2 = dxi dXi Since we have ds2 = gkm d~k d~m where functions aXi aXi gkm = a~k a~m constitute components of the metric tensor. -
The Evolution of Earth Gravitational Models Used in Astrodynamics
JEROME R. VETTER THE EVOLUTION OF EARTH GRAVITATIONAL MODELS USED IN ASTRODYNAMICS Earth gravitational models derived from the earliest ground-based tracking systems used for Sputnik and the Transit Navy Navigation Satellite System have evolved to models that use data from the Joint United States-French Ocean Topography Experiment Satellite (Topex/Poseidon) and the Global Positioning System of satellites. This article summarizes the history of the tracking and instrumentation systems used, discusses the limitations and constraints of these systems, and reviews past and current techniques for estimating gravity and processing large batches of diverse data types. Current models continue to be improved; the latest model improvements and plans for future systems are discussed. Contemporary gravitational models used within the astrodynamics community are described, and their performance is compared numerically. The use of these models for solid Earth geophysics, space geophysics, oceanography, geology, and related Earth science disciplines becomes particularly attractive as the statistical confidence of the models improves and as the models are validated over certain spatial resolutions of the geodetic spectrum. INTRODUCTION Before the development of satellite technology, the Earth orbit. Of these, five were still orbiting the Earth techniques used to observe the Earth's gravitational field when the satellites of the Transit Navy Navigational Sat were restricted to terrestrial gravimetry. Measurements of ellite System (NNSS) were launched starting in 1960. The gravity were adequate only over sparse areas of the Sputniks were all launched into near-critical orbit incli world. Moreover, because gravity profiles over the nations of about 65°. (The critical inclination is defined oceans were inadequate, the gravity field could not be as that inclination, 1= 63 °26', where gravitational pertur meaningfully estimated. -
World Geodetic System 1984
World Geodetic System 1984 Responsible Organization: National Geospatial-Intelligence Agency Abbreviated Frame Name: WGS 84 Associated TRS: WGS 84 Coverage of Frame: Global Type of Frame: 3-Dimensional Last Version: WGS 84 (G1674) Reference Epoch: 2005.0 Brief Description: WGS 84 is an Earth-centered, Earth-fixed terrestrial reference system and geodetic datum. WGS 84 is based on a consistent set of constants and model parameters that describe the Earth's size, shape, and gravity and geomagnetic fields. WGS 84 is the standard U.S. Department of Defense definition of a global reference system for geospatial information and is the reference system for the Global Positioning System (GPS). It is compatible with the International Terrestrial Reference System (ITRS). Definition of Frame • Origin: Earth’s center of mass being defined for the whole Earth including oceans and atmosphere • Axes: o Z-Axis = The direction of the IERS Reference Pole (IRP). This direction corresponds to the direction of the BIH Conventional Terrestrial Pole (CTP) (epoch 1984.0) with an uncertainty of 0.005″ o X-Axis = Intersection of the IERS Reference Meridian (IRM) and the plane passing through the origin and normal to the Z-axis. The IRM is coincident with the BIH Zero Meridian (epoch 1984.0) with an uncertainty of 0.005″ o Y-Axis = Completes a right-handed, Earth-Centered Earth-Fixed (ECEF) orthogonal coordinate system • Scale: Its scale is that of the local Earth frame, in the meaning of a relativistic theory of gravitation. Aligns with ITRS • Orientation: Given by the Bureau International de l’Heure (BIH) orientation of 1984.0 • Time Evolution: Its time evolution in orientation will create no residual global rotation with regards to the crust Coordinate System: Cartesian Coordinates (X, Y, Z). -
Mission Conventions Document
Earth Observation Mission CFI Software CONVENTIONS DOCUMENT Code: EO-MA-DMS-GS-0001 Issue: 4.19 Date: 29/05/2020 Name Function Signature Prepared by: Fabrizio Pirondini Project Engineer José Antonio González Abeytua Project Manager Juan José Borrego Bote Project Engineer Carlos Villanueva Project Manager Checked by: Javier Babe Quality A. Manager Approved by: Carlos Villanueva Project Manager DEIMOS Space S.L.U. Ronda de Poniente, 19 Edificio Fiteni VI, Portal 2, 2ª Planta 28760 Tres Cantos (Madrid), SPAIN Tel.: +34 91 806 34 50 Fax: +34 91 806 34 51 E-mail: [email protected] © DEIMOS Space S.L.U. All Rights Reserved. No part of this document may be reproduced, stored in a retrieval system, or transmitted, in any form or by any means, electronic, mechanical, photocopying, recording or otherwise, without the prior written permission of DEIMOS Space S.L.U. or ESA. Code: EO-MA-DMS-GS-0001 Date: 29/05/2020 Issue: 4.19 Page: 2 DOCUMENT INFORMATION Contract Data Classification Internal Contract Number: 4000102614/1O/NL/FF/ef Public Industry X Contract Issuer: ESA / ESTEC Confidential External Distribution Name Organization Copies Electronic handling Word Processor: LibreOffice 5.2.3.3 Archive Code: P/MCD/DMS/01/026-003 Electronic file name: eo-ma-dms-gs-001-12 Earth Observation Mission CFI Software. CONVENTIONS DOCUMENT Code: EO-MA-DMS-GS-0001 Date: 29/05/2020 Issue: 4.19 Page: 3 DOCUMENT STATUS LOG Issue Change Description Date Approval 1.0 New Document 27/10/09 • Issue in-line wit EOCFI libraries version 4.1 • Section 8.2.4 Refractive -
IERS Annual Report 2000
International Earth Rotation Service (IERS) Service International de la Rotation Terrestre Member of the Federation of the Astronomical and Geophysical data analysis Service (FAGS) IERS Annual Report 2000 Verlag des Bundesamts für Kartographie und Geodäsie Frankfurt am Main 2001 IERS Annual Report 2000 Edited by Wolfgang R. Dick and Bernd Richter Technical support: Alexander Lothhammer International Earth Rotation Service Central Bureau Bundesamt für Kartographie und Geodäsie Richard-Strauss-Allee 11 60598 Frankfurt am Main Germany phone: ++49-69-6333-273/261/250 fax: ++49-69-6333-425 e-mail: [email protected] URL: www.iers.org ISSN: 1029-0060 (print version) ISBN: 3-89888-862-2 (print version) An online version of this document is available at: http://www.iers.org/iers/publications/reports/2000/ © Verlag des Bundesamts für Kartographie und Geodäsie, Frankfurt am Main, 2001 Table of Contents I Forewords............................................................................................. 4 II Organisation of the IERS in 2000............................................................. 7 III Reports of Coordination Centres III.1 VLBI Coordination Centre.............................................................. 10 III.2 GPS Coordination Centre.............................................................. 13 III.3 SLR and LLR Coordination Centre................................................. 16 III.4 DORIS Coordination Centre........................................................... 19 IV Reports of Bureaus, Centres and