Properties of great circle chart.

Expansion formulae about geodesic line on chart of Mercator projection are derived. In section 2, lengths of tangent and normal to projected geodesic, length of rectilinear chord, and angle between rectilinear chord and tangent to the projected geodesic are expanded in power series of true length S of the geodesic ( eqs. ( 8)~(11)). In section 3, curvature σ of projected geodesic 〔eq.(22)) on Mercator projection and its derivatives σ', σ",σ''' are given 〔eqs.(27)~(30)〕 with their respective values at the beginning point of the geodesic〔eqs.(31)~(37)〕. Similar quantities for scale k are also obtained 〔eqs.(39)~〔42) and (43〕~(49〕〕. In section 4, some examples of applications of quantities obtained in section 3 are shown. ( i ) For given length m of projected geodesic on chart, minimum limit of scale by which great circle can be approximated by straight line and that by which geodesic can be approximated by great circle are derived for standard parallel〔eqs.(57) and (58)〕. Both of these limits hold for enough larger scales. In TABLES 1 (for m = 1 metre〕and 2 (for 111=0.1 metre〕examples of these scale limits are shown. 〔ii〕 Correction formulae to obtain the terminal of geodesicfrom a point, which is plotted on chart by employing directly given azimuth T of the geodesic and its true length S, are derived〔eqs.(59)~(62)〕 and their auxiliary quantities are given in TABLES 3 and 4. (iii) Maximum displacement of rectilinear chord from the projected geodesic occurs at about mid-point of the projected geodesic when the geodesic is not too large. Formulae to evaluate this mid-point displacement h 1/2 and its corresponding distance on the earth surface H 1/2 are also derived 〔eqs.(65)~(67)〕 and examples are shown in TABLE 5 for latitudes 25° to 45°.

Saved in:
Bibliographic Details
Main Authors: Sinzi, M. Akira, Kubo, Yoshio
Format: Journal Contribution biblioteca
Language:Japanese
Published: 1967
Online Access:http://hdl.handle.net/1834/16434
Tags: Add Tag
No Tags, Be the first to tag this record!
id dig-aquadocs-1834-16434
record_format koha
spelling dig-aquadocs-1834-164342021-05-19T06:54:37Z Properties of great circle chart. Sinzi, M. Akira Kubo, Yoshio Expansion formulae about geodesic line on chart of Mercator projection are derived. In section 2, lengths of tangent and normal to projected geodesic, length of rectilinear chord, and angle between rectilinear chord and tangent to the projected geodesic are expanded in power series of true length S of the geodesic ( eqs. ( 8)~(11)). In section 3, curvature σ of projected geodesic 〔eq.(22)) on Mercator projection and its derivatives σ', σ",σ''' are given 〔eqs.(27)~(30)〕 with their respective values at the beginning point of the geodesic〔eqs.(31)~(37)〕. Similar quantities for scale k are also obtained 〔eqs.(39)~〔42) and (43〕~(49〕〕. In section 4, some examples of applications of quantities obtained in section 3 are shown. ( i ) For given length m of projected geodesic on chart, minimum limit of scale by which great circle can be approximated by straight line and that by which geodesic can be approximated by great circle are derived for standard parallel〔eqs.(57) and (58)〕. Both of these limits hold for enough larger scales. In TABLES 1 (for m = 1 metre〕and 2 (for 111=0.1 metre〕examples of these scale limits are shown. 〔ii〕 Correction formulae to obtain the terminal of geodesicfrom a point, which is plotted on chart by employing directly given azimuth T of the geodesic and its true length S, are derived〔eqs.(59)~(62)〕 and their auxiliary quantities are given in TABLES 3 and 4. (iii) Maximum displacement of rectilinear chord from the projected geodesic occurs at about mid-point of the projected geodesic when the geodesic is not too large. Formulae to evaluate this mid-point displacement h 1/2 and its corresponding distance on the earth surface H 1/2 are also derived 〔eqs.(65)~(67)〕 and examples are shown in TABLE 5 for latitudes 25° to 45°. Published 2020-02-20T10:39:09Z 2020-02-20T10:39:09Z 1967 Journal Contribution Refereed http://hdl.handle.net/1834/16434 ja https://www1.kaiho.mlit.go.jp/GIJUTSUKOKUSAI/KENKYU/report/rhr02/rhr02-05.pdf pp.61-75
institution UNESCO
collection DSpace
country Francia
countrycode FR
component Bibliográfico
access En linea
databasecode dig-aquadocs
tag biblioteca
region Europa del Oeste
libraryname Repositorio AQUADOCS
language Japanese
description Expansion formulae about geodesic line on chart of Mercator projection are derived. In section 2, lengths of tangent and normal to projected geodesic, length of rectilinear chord, and angle between rectilinear chord and tangent to the projected geodesic are expanded in power series of true length S of the geodesic ( eqs. ( 8)~(11)). In section 3, curvature σ of projected geodesic 〔eq.(22)) on Mercator projection and its derivatives σ', σ",σ''' are given 〔eqs.(27)~(30)〕 with their respective values at the beginning point of the geodesic〔eqs.(31)~(37)〕. Similar quantities for scale k are also obtained 〔eqs.(39)~〔42) and (43〕~(49〕〕. In section 4, some examples of applications of quantities obtained in section 3 are shown. ( i ) For given length m of projected geodesic on chart, minimum limit of scale by which great circle can be approximated by straight line and that by which geodesic can be approximated by great circle are derived for standard parallel〔eqs.(57) and (58)〕. Both of these limits hold for enough larger scales. In TABLES 1 (for m = 1 metre〕and 2 (for 111=0.1 metre〕examples of these scale limits are shown. 〔ii〕 Correction formulae to obtain the terminal of geodesicfrom a point, which is plotted on chart by employing directly given azimuth T of the geodesic and its true length S, are derived〔eqs.(59)~(62)〕 and their auxiliary quantities are given in TABLES 3 and 4. (iii) Maximum displacement of rectilinear chord from the projected geodesic occurs at about mid-point of the projected geodesic when the geodesic is not too large. Formulae to evaluate this mid-point displacement h 1/2 and its corresponding distance on the earth surface H 1/2 are also derived 〔eqs.(65)~(67)〕 and examples are shown in TABLE 5 for latitudes 25° to 45°.
format Journal Contribution
author Sinzi, M. Akira
Kubo, Yoshio
spellingShingle Sinzi, M. Akira
Kubo, Yoshio
Properties of great circle chart.
author_facet Sinzi, M. Akira
Kubo, Yoshio
author_sort Sinzi, M. Akira
title Properties of great circle chart.
title_short Properties of great circle chart.
title_full Properties of great circle chart.
title_fullStr Properties of great circle chart.
title_full_unstemmed Properties of great circle chart.
title_sort properties of great circle chart.
publishDate 1967
url http://hdl.handle.net/1834/16434
work_keys_str_mv AT sinzimakira propertiesofgreatcirclechart
AT kuboyoshio propertiesofgreatcirclechart
_version_ 1756076653209976832