Map Projection Article on Wikipedia
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Parametric Modelling of Architectural Developables Roel Van De Straat Scientific Research Mentor: Dr
MSc thesis: Computation & Performance parametric modelling of architectural developables Roel van de Straat scientific research mentor: dr. ir. R.M.F. Stouffs design research mentor: ir. F. Heinzelmann third mentor: ir. J.L. Coenders Computation & Performance parametric modelling of architectural developables MSc thesis: Computation & Performance parametric modelling of architectural developables Roel van de Straat 1041266 Delft, April 2011 Delft University of Technology Faculty of Architecture Computation & Performance parametric modelling of architectural developables preface The idea of deriving analytical and structural information from geometrical complex design with relative simple design tools was one that was at the base of defining the research question during the early phases of the graduation period, starting in September of 2009. Ultimately, the research focussed an approach actually reversely to this initial idea by concentrating on using analytical and structural logic to inform the design process with the aid of digital design tools. Generally, defining architectural characteristics with an analytical approach is of increasing interest and importance with the emergence of more complex shapes in the building industry. This also means that embedding structural, manufacturing and construction aspects early on in the design process is of interest. This interest largely relates to notions of surface rationalisation and a design approach with which initial design sketches can be transferred to rationalised designs which focus on a strong integration with manufacturability and constructability. In order to exemplify this, the design of the Chesa Futura in Sankt Moritz, Switzerland by Foster and Partners is discussed. From the initial design sketch, there were many possible approaches for surfacing techniques defining the seemingly freeform design. -
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. -
Unusual Map Projections Tobler 1999
Unusual Map Projections Waldo Tobler Professor Emeritus Geography department University of California Santa Barbara, CA 93106-4060 http://www.geog.ucsb.edu/~tobler 1 Based on an invited presentation at the 1999 meeting of the Association of American Geographers in Hawaii. Copyright Waldo Tobler 2000 2 Subjects To Be Covered Partial List The earth’s surface Area cartograms Mercator’s projection Combined projections The earth on a globe Azimuthal enlargements Satellite tracking Special projections Mapping distances And some new ones 3 The Mapping Process Common Surfaces Used in cartography 4 The surface of the earth is two dimensional, which is why only (but also both) latitude and longitude are needed to pin down a location. Many authors refer to it as three dimensional. This is incorrect. All map projections preserve the two dimensionality of the surface. The Byte magazine cover from May 1979 shows how the graticule rides up and down over hill and dale. Yes, it is embedded in three dimensions, but the surface is a curved, closed, and bumpy, two dimensional surface. Map projections convert this to a flat two dimensional surface. 5 The Surface of the Earth Is Two-Dimensional 6 The easy way to demonstrate that Mercator’s projection cannot be obtained as a perspective transformation is to draw lines from the latitudes on the projection to their occurrence on a sphere, here represented by an adjoining circle. The rays will not intersect in a point. 7 Mercator’s Projection Is Not Perspective 8 It is sometimes asserted that one disadvantage of a globe is that one cannot see all of the entire earth at one time. -
Map Projections Paper 4 (Th.) UNIT : I ; TOPIC : 3 …Introduction
FOR SEMESTER 3 GE Students , Geography Map Projections Paper 4 (Th.) UNIT : I ; TOPIC : 3 …Introduction Prepared and Compiled By Dr. Rajashree Dasgupta Assistant Professor Dept. of Geography Government Girls’ General Degree College 3/23/2020 1 Map Projections … The method by which we transform the earth’s spheroid (real world) to a flat surface (abstraction), either on paper or digitally Define the spatial relationship between locations on earth and their relative locations on a flat map Think about projecting a see- through globe onto a wall Dept. of Geography, GGGDC, 3/23/2020 Kolkata 2 Spatial Reference = Datum + Projection + Coordinate system Two basic locational systems: geometric or Cartesian (x, y, z) and geographic or gravitational (f, l, z) Mean sea level surface or geoid is approximated by an ellipsoid to define an earth datum which gives (f, l) and distance above geoid gives (z) 3/23/2020 Dept. of Geography, GGGDC, Kolkata 3 3/23/2020 Dept. of Geography, GGGDC, Kolkata 4 Classifications of Map Projections Criteria Parameter Classes/ Subclasses Extrinsic Datum Direct / Double/ Spherical Triple Surface Spheroidal Plane or Ist Order 2nd Order 3rd Order surface of I. Planar a. Tangent i. Normal projection II. Conical b. Secant ii. Transverse III. Cylindric c. Polysuperficial iii. Oblique al Method of Perspective Semi-perspective Non- Convention Projection perspective al Intrinsic Properties Azimuthal Equidistant Othomorphic Homologra phic Appearance Both parallels and meridians straight of parallels Parallels straight, meridians curve and Parallels curves, meridians straight meridians Both parallels and meridians curves Parallels concentric circles , meridians radiating st. lines Parallels concentric circles, meridians curves Geometric Rectangular Circular Elliptical Parabolic Shape 3/23/2020 Dept. -
Title CLAD HELICES and DEVELOPABLE SURFACES( Fulltext )
CLAD HELICES AND DEVELOPABLE SURFACES( Title fulltext ) Author(s) TAKAHASHI,Takeshi; TAKEUCHI,Nobuko Citation 東京学芸大学紀要. 自然科学系, 66: 1-9 Issue Date 2014-09-30 URL http://hdl.handle.net/2309/136938 Publisher 東京学芸大学学術情報委員会 Rights Bulletin of Tokyo Gakugei University, Division of Natural Sciences, 66: pp.1~ 9 ,2014 CLAD HELICES AND DEVELOPABLE SURFACES Takeshi TAKAHASHI* and Nobuko TAKEUCHI** Department of Mathematics (Received for Publication; May 23, 2014) TAKAHASHI, T and TAKEUCHI, N.: Clad Helices and Developable Surfaces. Bull. Tokyo Gakugei Univ. Div. Nat. Sci., 66: 1-9 (2014) ISSN 1880-4330 Abstract We define new special curves in Euclidean 3-space which are generalizations of the notion of helices. Then we find a geometric invariant of a space curve which is related to the singularities of the special developable surface of the original curve. Keywords: cylindrical helices, slant helices, clad helices, g-clad helices, developable surfaces, singularities Department of Mathematics, Tokyo Gakugei University, 4-1-1 Nukuikita-machi, Koganei-shi, Tokyo 184-8501, Japan 1. Introduction In this paper we define the notion of clad helices and g-clad helices which are generalizations of the notion of helices. Then we can find them as geodesics on the tangent developable(cf., §3). In §2 we describe basic notions and properties of space curves. We review the classification of singularities of the Darboux developable of a space curve in §4. We introduce the notion of the principal normal Darboux developable of a space curve. Then we find a geometric invariant of a clad helix which is related to the singularities of the principal normal Darboux developable of the original curve. -
Exploring Locus Surfaces Involving Pseudo Antipodal Points
Proceedings of the 25th Asian Technology Conference in Mathematics Exploring Locus Surfaces Involving Pseudo Antipodal Points Wei-Chi YANG [email protected] Department of Mathematics and Statistics Radford University Radford, VA 24142 USA Abstract The discussions in this paper were inspired by a college entrance practice exam from China. It is extended to investigate the locus curve that involves a point on an ellipse and its pseudo antipodal point with respect to a xed point. With the help of technological tools, we explore 2D locus for some regular closed curves. Later, we investigate how a locus curve can be extended to the corresponding 3D locus surfaces on surfaces like ellipsoid, cardioidal surface and etc. Secondly, we use the de nition of a developable surface (including tangent developable surface) to construct the corresponding locus surface. It is well known that, in robotics, antipodal grasps can be achieved on curved objects. In addition, there are many applications already in engineering and architecture about the developable surfaces. We hope the discussions regarding the locus surfaces can inspire further interesting research in these areas. 1 Introduction Technological tools have in uenced our learning, teaching and research in mathematics in many di erent ways. In this paper, we start with a simple exam problem and with the help of tech- nological tools, we are able to turn the problem into several challenging problems in 2D and 3D. The visualization bene ted from exploration provides us crucial intuition of how we can analyze our solutions with a computer algebra system. Therefore, while implementing techno- logical tools to allow exploration in our curriculum is de nitely a must. -
The Influence of the Projected Coordinate System on Animal Home Range Estimation Area
University of South Florida Scholar Commons Graduate Theses and Dissertations Graduate School 11-4-2014 The nflueI nce of the Projected Coordinate System on Animal Home Range Estimation Area Michael Barr University of South Florida, [email protected] Follow this and additional works at: https://scholarcommons.usf.edu/etd Part of the Physical and Environmental Geography Commons Scholar Commons Citation Barr, Michael, "The nflueI nce of the Projected Coordinate System on Animal Home Range Estimation Area" (2014). Graduate Theses and Dissertations. https://scholarcommons.usf.edu/etd/5343 This Thesis is brought to you for free and open access by the Graduate School at Scholar Commons. It has been accepted for inclusion in Graduate Theses and Dissertations by an authorized administrator of Scholar Commons. For more information, please contact [email protected]. The Influence of the Projected Coordinate System on Animal Home Range Estimation Area by Michael R. Barr A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science School of Geosciences College of Arts and Sciences University of South Florida Major Professor: Joni Downs, Ph.D. Lori Collins, Ph.D. Elizabeth Walton, Ph.D. Date of Approval: November 4, 2014 Keywords: map distortion, GIS, characteristic hull polygon, map projections Copyright © 2014, Michael R. Barr ACKNOWLEDGEMENTS I would like to thank my committee members Dr. Walton and Dr. Collins for all of their valuable feedback and encouragement during this process. I would also like to thank the researchers whose data I have used in this thesis for making their work available. Special thanks to my advisor Dr. -
A Bevy of Area Preserving Transforms for Map Projection Designers.Pdf
Cartography and Geographic Information Science ISSN: 1523-0406 (Print) 1545-0465 (Online) Journal homepage: http://www.tandfonline.com/loi/tcag20 A bevy of area-preserving transforms for map projection designers Daniel “daan” Strebe To cite this article: Daniel “daan” Strebe (2018): A bevy of area-preserving transforms for map projection designers, Cartography and Geographic Information Science, DOI: 10.1080/15230406.2018.1452632 To link to this article: https://doi.org/10.1080/15230406.2018.1452632 Published online: 05 Apr 2018. Submit your article to this journal View related articles View Crossmark data Full Terms & Conditions of access and use can be found at http://www.tandfonline.com/action/journalInformation?journalCode=tcag20 CARTOGRAPHY AND GEOGRAPHIC INFORMATION SCIENCE, 2018 https://doi.org/10.1080/15230406.2018.1452632 A bevy of area-preserving transforms for map projection designers Daniel “daan” Strebe Mapthematics LLC, Seattle, WA, USA ABSTRACT ARTICLE HISTORY Sometimes map projection designers need to create equal-area projections to best fill the Received 1 January 2018 projections’ purposes. However, unlike for conformal projections, few transformations have Accepted 12 March 2018 been described that can be applied to equal-area projections to develop new equal-area projec- KEYWORDS tions. Here, I survey area-preserving transformations, giving examples of their applications and Map projection; equal-area proposing an efficient way of deploying an equal-area system for raster-based Web mapping. projection; area-preserving Together, these transformations provide a toolbox for the map projection designer working in transformation; the area-preserving domain. area-preserving homotopy; Strebe 1995 projection 1. Introduction two categories: plane-to-plane transformations and “sphere-to-sphere” transformations – but in quotes It is easy to construct a new conformal projection: Find because the manifold need not be a sphere at all. -
Bibliography of Map Projections
AVAILABILITY OF BOOKS AND MAPS OF THE U.S. GEOlOGICAL SURVEY Instructions on ordering publications of the U.S. Geological Survey, along with prices of the last offerings, are given in the cur rent-year issues of the monthly catalog "New Publications of the U.S. Geological Survey." Prices of available U.S. Geological Sur vey publications released prior to the current year are listed in the most recent annual "Price and Availability List" Publications that are listed in various U.S. Geological Survey catalogs (see back inside cover) but not listed in the most recent annual "Price and Availability List" are no longer available. Prices of reports released to the open files are given in the listing "U.S. Geological Survey Open-File Reports," updated month ly, which is for sale in microfiche from the U.S. Geological Survey, Books and Open-File Reports Section, Federal Center, Box 25425, Denver, CO 80225. Reports released through the NTIS may be obtained by writing to the National Technical Information Service, U.S. Department of Commerce, Springfield, VA 22161; please include NTIS report number with inquiry. Order U.S. Geological Survey publications by mail or over the counter from the offices given below. BY MAIL OVER THE COUNTER Books Books Professional Papers, Bulletins, Water-Supply Papers, Techniques of Water-Resources Investigations, Circulars, publications of general in Books of the U.S. Geological Survey are available over the terest (such as leaflets, pamphlets, booklets), single copies of Earthquakes counter at the following Geological Survey Public Inquiries Offices, all & Volcanoes, Preliminary Determination of Epicenters, and some mis of which are authorized agents of the Superintendent of Documents: cellaneous reports, including some of the foregoing series that have gone out of print at the Superintendent of Documents, are obtainable by mail from • WASHINGTON, D.C.--Main Interior Bldg., 2600 corridor, 18th and C Sts., NW. -
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. -
Estimation of an Unknown Cartographic Projection and Its Parameters from the Map
Estimation of an Unknown Cartographic Projection and its Parameters from the Map Faculty of Sciences, Charles University in Prague , Tel.: ++420-221-951-400 Abstract This article presents a new off-line method for the detection, analysis and estimation of an unknown carto- graphic projection and its parameters from a map. Several invariants are used to construct the objective function φ that describes the relationship between the 0D, 1D, and 2D entities on the analyzed and reference maps. It is min- imized using the Nelder-Mead downhill simplex algorithm. A simplified and computationally cheaper version of the objective function φ involving only 0D elements is also presented. The following parameters are estimated: a map projection type, a map projection aspect given by the meta pole K coordinates [ϕk,λk], a true parallel latitude ϕ0, central meridian longitude λ0, a map scale, and a map rotation. Before the analysis, incorrectly drawn elements on the map can be detected and removed using the IRLS. Also introduced is a new method for computing the L2 distance between the turning functions Θ1, Θ2 of the corresponding faces using dynamic programming. Our ap- proach may be used to improve early map georeferencing; it can also be utilized in studies of national cartographic heritage or land use applications. The results are presented both for real cartographic data, representing early maps from the David Rumsay Map Collection, and for the synthetic tests. Keywords: digital cartography, map projection, analysis, simplex method, optimization, Voronoi diagram, outliers detection, early maps, georeferencing, cartographic heritage, meta data, Marc 21, MapAnalyst. 1 Introduction the proposed solution, this step can be performed semi- automatically and with a higher degree of relevance us- ing our method. -
2 Regular Surfaces
2 Regular Surfaces In this half of the course we approach surfaces in E3 in a similar way to which we considered curves. A parameterized surface will be a function1 x : U ! E3 where U is some open subset of the plane R2. Our purpose is twofold: 1. To be able to measure quantities such as length (of curves), angle (between curves on a surface), area using the parameterization space U. This requires us to create some method of taking tangent vectors to the surface and ‘pulling-back’ to U where we will perform our calculations.2 2. We want to find ways of defining and measuring the curvature of a surface. Before starting, we recall some of the important background terms and concepts from other classes. Notation Surfaces being functions x : U ⊆ R2 ! E3, we will preserve some of the notational differences between R2 and E3. Thus: • Co-ordinate points in the parameterization space U ⊂ R2 will be written as lower case letters or, more commonly, row vectors: for example p = (u, v) 2 R2. • Points in E3 will be written using capital letters and row vectors: for example P = (3, 4, 8) 2 E3. 2 • Vectors in E3 will be written bold-face or as column-vectors: for example v = −1 . p2 Sometimes it will be convenient to abuse notation and add a vector v to a point P, the result will be a new point P + v. Open Sets in Rn The domains of our parameterized functions will always be open 2 sets in R . These are a little harder to describe than open intervals rp in R: the definitions are here for reference.