Coordinate Conversions and Transformations Including Formulas
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Map Projections--A Working Manual
This is a reproduction of a library book that was digitized by Google as part of an ongoing effort to preserve the information in books and make it universally accessible. https://books.google.com 7 I- , t 7 < ?1 > I Map Projections — A Working Manual By JOHN P. SNYDER U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1395 _ i UNITED STATES GOVERNMENT PRINTING OFFIGE, WASHINGTON: 1987 no U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Gordon P. Eaton, Director First printing 1987 Second printing 1989 Third printing 1994 Library of Congress Cataloging in Publication Data Snyder, John Parr, 1926— Map projections — a working manual. (U.S. Geological Survey professional paper ; 1395) Bibliography: p. Supt. of Docs. No.: I 19.16:1395 1. Map-projection — Handbooks, manuals, etc. I. Title. II. Series: Geological Survey professional paper : 1395. GA110.S577 1987 526.8 87-600250 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, DC 20402 PREFACE This publication is a major revision of USGS Bulletin 1532, which is titled Map Projections Used by the U.S. Geological Survey. Although several portions are essentially unchanged except for corrections and clarification, there is consider able revision in the early general discussion, and the scope of the book, originally limited to map projections used by the U.S. Geological Survey, now extends to include several other popular or useful projections. These and dozens of other projections are described with less detail in the forthcoming USGS publication An Album of Map Projections. As before, this study of map projections is intended to be useful to both the reader interested in the philosophy or history of the projections and the reader desiring the mathematics. -
Implications for the Adoption of Global Reference Geodesic System SIRGAS2000 on the Large Scale Cadastral Cartography in Brazil
Implications for the Adoption of Global Reference Geodesic System SIRGAS2000 on the Large Scale Cadastral Cartography in Brazil Vivian de Oliveira FERNANDES and Ruth Emilia NOGUEIRA, Brazil Key words: SIRGAS2000, SAD69, Global Geodesic System SUMMARY Since 2005 Brazil is going through a singular moment into Cartography. In January 2005, SIRGAS2000 began to be the geodetic official reference system for Geodesy and Cartography, with the concomitant use of SAD69. Since January 2015, only SIRGAS2000 will be official, and all cartographical products will have to be referenced into this Datum. The adoption of a geocentric reference system happens from the technological evolution that has favored an improvement of the Geodetic Reference System – SGR. Differently of a single alternative for the improvement of the SGR, the adoption of a new geocentric reference system is a basic necessity into the world-wide scenery to activities that depend on spatialized information. The technological advancements in the global positioning methods, specially in the satellite positioning systems. This change reaches more quickly the organs that need spatialized information in their infrastructure and planning activities, like town halls and services concessionaires like Telecommunications, Sanitation, Electric Energy among others, which need the real knowledge of the urban space: use and occupation of the soil, subsoil and air space, fiscal and housing technical register, generic plant of values, block plant, register reference plant, municipal master plan, among others that are derived from a cartographical basis of quality. Officially, were adopted these geodetic reference systems in Brazil: Córrego Alegre, Astro Datum Chuá, SAD69, and now SIRGAS2000. For legislation it is in transition for the SIRGAS2000. -
Arxiv:1811.01571V2 [Cs.CV] 24 Jan 2019 Many Traditional Cnns on 3D Data Simply Extend the 2D Convolutional Op- Erations to 3D, for Example, the Work of Wu Et Al
SPNet: Deep 3D Object Classification and Retrieval using Stereographic Projection Mohsen Yavartanoo1[0000−0002−0109−1202], Eu Young Kim1[0000−0003−0528−6557], and Kyoung Mu Lee1[0000−0001−7210−1036] Department of ECE, ASRI, Seoul National University, Seoul, Korea https://cv.snu.ac.kr/ fmyavartanoo, shreka116, [email protected] Abstract. We propose an efficient Stereographic Projection Neural Net- work (SPNet) for learning representations of 3D objects. We first trans- form a 3D input volume into a 2D planar image using stereographic projection. We then present a shallow 2D convolutional neural network (CNN) to estimate the object category followed by view ensemble, which combines the responses from multiple views of the object to further en- hance the predictions. Specifically, the proposed approach consists of four stages: (1) Stereographic projection of a 3D object, (2) view-specific fea- ture learning, (3) view selection and (4) view ensemble. The proposed ap- proach performs comparably to the state-of-the-art methods while having substantially lower GPU memory as well as network parameters. Despite its lightness, the experiments on 3D object classification and shape re- trievals demonstrate the high performance of the proposed method. Keywords: 3D object classification · 3D object retrieval · Stereographic Projection · Convolutional Neural Network · View Ensemble · View Se- lection. 1 Introduction In recent years, success of deep learning methods, in particular, convolutional neural network (CNN), has urged rapid development in various computer vision applications such as image classification, object detection, and super-resolution. Along with the drastic advances in 2D computer vision, understanding 3D shapes and environment have also attracted great attention. -
Uon Digital Repository Home
University of Nairobi School of Engineering Building a QGIS Helper Application to Overcome the Challenges of Cassini to UTM Coordinate System Conversions in Kenya BY Ajanga Dissent Ingati F56/81982/2015 A Project submitted in partial fulfillment for the Degree of Master of Science in Geographical Information Systems, in the Department of Geospatial & Space Technology of the University of Nairobi October 2017 I Declaration I, Ajanga Dissent Ingati, hereby declare that this project is my original work. To the best of my knowledge, the work presented here has not been presented for a degree in any other Institution of Higher Learning. ……………………………………. ……………………… .……..……… Name of student Signature Date This project has been submitted for examination with my approval as university supervisor. ……………………………………. ……………………… .……..……… Name of Supervisor Signature Date I Dedication I dedicate this work to my family for their support throughout the entire process of pursuing this degree and to the completion of the project. Your encouragement has been instrumental in ensuring the success of this project; may God truly bless you. II Acknowledgement I would like to show my heartfelt appreciation to all the people who saw me through the process of preparing this report. These thanks go to all those who provided technical support, talked through the issues I studied, read, wrote, gave comments, and also those who assisted in editing and proof reading of this project report before submission. I would like to thank Steve Firsake for his technical support through Python Programing. Special thanks also go to Dr.-Ing. Musyoka for his technical advice and support for the entire project. -
Portraying Earth
A map says to you, 'Read me carefully, follow me closely, doubt me not.' It says, 'I am the Earth in the palm of your hand. Without me, you are alone and lost.’ Beryl Markham (West With the Night, 1946 ) • Map Projections • Families of Projections • Computer Cartography Students often have trouble with geographic names and terms. If you need/want to know how to pronounce something, try this link. Audio Pronunciation Guide The site doesn’t list everything but it does have the words with which you’re most likely to have trouble. • Methods for representing part of the surface of the earth on a flat surface • Systematic representations of all or part of the three-dimensional Earth’s surface in a two- dimensional model • Transform spherical surfaces into flat maps. • Affect how maps are used. The problem: Imagine a large transparent globe with drawings. You carefully cover the globe with a sheet of paper. You turn on a light bulb at the center of the globe and trace all of the things drawn on the globe onto the paper. You carefully remove the paper and flatten it on the table. How likely is it that the flattened image will be an exact copy of the globe? The different map projections are the different methods geographers have used attempting to transform an image of the spherical surface of the Earth into flat maps with as little distortion as possible. No matter which map projection method you use, it is impossible to show the curved earth on a flat surface without some distortion. -
Arcgis 10.1 Geographic and Vertical Transformation Tables
ArcGIS 10.1 Geographic and Vertical Transformation Tables Note: Some numbers have been rounded for display. Area of use values are in degrees based upon WGS 1984. Table 1: Geographic (datum) transformations: well-known IDs, accuracies and areas of use ........................................................................................... 1 Table 2: Geographic (datum) transformations: Longitude rotation and unit change methods ......................................................................................... 43 Table 3: Geographic (datum) transformations: Geographic 2D offset method ................................................................................................................ 44 Table 4: Geographic (datum) transformations: Geocentric translation method ............................................................................................................... 44 Table 5: Geographic (datum) transformations: Coordinate frame (CF) and position vector (PV) methods .................................................................... 60 Table 6: Geographic (datum) transformations: Molodensky-Badekas method ................................................................................................................ 70 Table 7: Geographic (datum) transformations: HARN, NADCON, and NTv2 methods ................................................................................................. 71 Table 8: Geographic transformation methods: well-known IDs ...................................................................................................................................... -
Killet Software Ing.-Gbr
History of the program TRANSDATpro Changes and Supplements of the last five years Worldwide geodetic Coordinate Transformations Detailed Information about the program TRANSDATpro: https://www.killetsoft.de/p_trda_e.htm Translation of this history to other languages: https://translate.google.com/ 01. 01. 2021: Program release TRANSDATpro 24.00 Changes and Supplements during the version TRANSDATpro 24.xx: 24.14: New help chapter "Selection of a Meridian Strip". 24.13: New round button to call the help "Selection of a Meridian Strip". 24.12: New Help link "What actually is a Coordinate Reference System?" 24.11: For calculations with the Mercator projection (1SP / 2SP) the International Date Line is considered. 24.10: New coordinate system "PDC Mercator (Pacific)". 24.10: EPSG code 3832 "WGS84 / PDC Mercator" implemented. 24.09: RefSys "ETRS89 (EU GPS measurements)" renamed to "ETRS89 (EU ITRS epoch 1989)". 24.09: RefSys "NAD83(US+CA GPS measurements)" renamed to "NAD83(US+CA ITRS epoch 1988)". 24.09: RefSys "GDA2020 (AU GPS measurements)" renamed to "GDA2020 (AU ITRS epoch 2020)". 24.08: Automatic language detection at the first program call adjusted. 24.07: Increased stability and speed with a new development system. 24.07: Delivered with new Dynamic Link Libraries (DLLs). 24.06: Error handling improved. 24.05: New NTv2 reference system for Belgium added. 24.05: New NTv2 reference systems for Portugal added. 24.03: New Language interface file for Bosnian, Croatian and Serbian added. 24.02: New language interface file for Italian added. 24.01: Restricted access to functions of the underlying GeoDLL fixed. 24.01: Link to the worldwide NTv2 files collection corrected. -
Cylindrical Projections 27
MAP PROJECTION PROPERTIES: CONSIDERATIONS FOR SMALL-SCALE GIS APPLICATIONS by Eric M. Delmelle A project submitted to the Faculty of the Graduate School of State University of New York at Buffalo in partial fulfillments of the requirements for the degree of Master of Arts Geographical Information Systems and Computer Cartography Department of Geography May 2001 Master Advisory Committee: David M. Mark Douglas M. Flewelling Abstract Since Ptolemeus established that the Earth was round, the number of map projections has increased considerably. Cartographers have at present an impressive number of projections, but often lack a suitable classification and selection scheme for them, which significantly slows down the mapping process. Although a projection portrays a part of the Earth on a flat surface, projections generate distortion from the original shape. On world maps, continental areas may severely be distorted, increasingly away from the center of the projection. Over the years, map projections have been devised to preserve selected geometric properties (e.g. conformality, equivalence, and equidistance) and special properties (e.g. shape of the parallels and meridians, the representation of the Pole as a line or a point and the ratio of the axes). Unfortunately, Tissot proved that the perfect projection does not exist since it is not possible to combine all geometric properties together in a single projection. In the twentieth century however, cartographers have not given up their creativity, which has resulted in the appearance of new projections better matching specific needs. This paper will review how some of the most popular world projections may be suited for particular purposes and not for others, in order to enhance the message the map aims to communicate. -
Supported Coordinate Systems and Geographic Transformations
Supported coordinate systems and geographic transformations This document contains information about the coordinate systems and geographic (datum) transformations supported in ArcGIS. The information is current as of version 8.1.2 of the Projection Engine. The tables include supported units of measure, spheroids, datums, and prime meridians. The supported map projections and their parameters are listed in one table. The geographic and projected coordinate system areas of interest are available. The geographic transformation tables include the method and parameters as well as the areas of interest. Earlier versions of the Projection Engine will not include all objects listed in these tables. Geographic (datum) transformations, three parameter Name Code Method dX dY dZ Abidjan_1987_To_WGS_1984 8414 Geocentric Translation -124.76 53.0 466.79 Accra_To_WGS_1972_BE 1570 Geocentric Translation -171.16 17.29 323.31 Accra_To_WGS_1984 1569 Geocentric Translation -199 32 322 Adindan_To_WGS_1984_1 8000 Geocentric Translation -166 -15 204 Adindan_To_WGS_1984_2 8001 Geocentric Translation -118 -14 218 Adindan_To_WGS_1984_3 8002 Geocentric Translation -134 -2 210 Adindan_To_WGS_1984_4 8003 Geocentric Translation -165 -11 206 Adindan_To_WGS_1984_5 8004 Geocentric Translation -123 -20 220 Adindan_To_WGS_1984_6 8005 Geocentric Translation -128 -18 224 Adindan_To_WGS_1984_7 8006 Geocentric Translation -161 -14 205 Afgooye_To_WGS_1984 8007 Geocentric Translation -43 -163 45 AGD_1966_To_GDA_1994 8189 Geocentric Translation -127.8 -52.3 152.9 AGD_1966_To_WGS_1984 -
MDT Versión 4
Customization Manual Version 7.5 Aplitop, 2016 C/ Sumatra, 9 E-29190 MÁLAGA (SPAIN) web: www.aplitop.com e-mail: [email protected] Customization ............................................................. 3 Introduction ................................................................................. 3 General ........................................................................................ 4 Angles ........................................................................... 4 Measurement ................................................................ 5 User Blocks .................................................................. 5 Layers ........................................................................... 5 Project ........................................................................... 5 Printer ........................................................................... 5 Print in MS Word ......................................................... 6 Printing on Drawing ..................................................... 7 PDF Printing ................................................................. 7 Menus ......................................................................................... 7 Surveying .................................................................................... 8 Coordinate Reference Systems (CRS) .......................... 8 Corrections ................................................................... 9 Admissible Errors ........................................................ -
Guidance Note 7 Part 2
IOGP Publication 373-7-2 – Geomatics Guidance Note number 7, part 2 – September 2019 To facilitate improvement, this document is subject to revision. The current version is available at www.epsg.org. Geomatics Guidance Note Number 7, part 2 Coordinate Conversions and Transformations including Formulas Revised - September 2019 Page 1 of 162 IOGP Publication 373-7-2 – Geomatics Guidance Note number 7, part 2 – September 2019 To facilitate improvement, this document is subject to revision. The current version is available at www.epsg.org. Table of Contents Preface ............................................................................................................................................................5 1 IMPLEMENTATION NOTES ................................................................................................................. 6 1.1 ELLIPSOID PARAMETERS ......................................................................................................................... 6 1.2 ARCTANGENT FUNCTION ......................................................................................................................... 6 1.3 ANGULAR UNITS ....................................................................................................................................... 7 1.4 LONGITUDE 'WRAP-AROUND' .................................................................................................................. 7 1.5 OFFSETS ................................................................................................................................................... -
Datum Transformations Using the Ntv2 Grid by Julie Lovesay, Chief Directorate: National Geo-Spatial Information (CD:NGI)
Visualisation technical Datum transformations using the NTv2 grid by Julie Lovesay, Chief Directorate: National Geo-spatial Information (CD:NGI) Prior to 1999, all geospatial data in South Africa was referenced to the Cape datum (Modified Clarke 1880 ellipsoid). Since the introduction of the Hartebeesthoek 94 datum (utilising the WGS84 ellipsoid) in 1999, GIS practitioners have faced challenges combining historical data in the Cape datum and more modern data in the Hartebeesthoek 94 datum. I have investigated an approach that can easily be used to transform data from the Cape datum to Hatebeesthoek 94. This is called the NTv2 grid which is software independent. However, it was tested within the ARC environment as this is one of the most widely used platforms. he transformation of point files from one datum to another is Trelatively simple, and can be done with a Helmert transformation, provided the area is smaller than 40 km and at least two points are known in both systems. In smaller areas of only a few kilometres, a straight shift is acceptable if surrounding trigonometrical (trig) beacons or town survey marks are consistent. However the transformation of GIS vector data such as shapefiles does not involve only point conversion, but rather points, polygons and lines. This makes the transformation more complicated as the polygons and lines may contain many vertices and can possibly be geographically extensive. Currently, the vast majority of GIS projects utilise WGS84/ Hartebeesthoek94 as the default Fig. 1: Left - Water pipes in Mossel Bay in Cape Datum overlaid on an image rectified in the datum. GIS practitioners are regularly Hartebeesthoek94 datum.