Geographical Position of Kyushu Island on Inoh Map and Magnetic Declination

IF 0.2 Q4 GEOGRAPHY, PHYSICAL
M. Nogami
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引用次数: 0

Abstract

M. Hoyanagi pointed out a position deviation of Kyushu Island on an Inoh map with a scale of 1 to 216000. He explained it referring to the map projection adopted by Inoh and the magnetic declination at the beginning of 19 th century. In this study, the correlation between the coordinate value of an astronomical observation point on the map and the corresponding location ( latitude and longitude ) on the actual map is statistically analyzed. The coefficients of determination ( R 2 ) are calculated for maps rotated by small degrees. As a result, anticlockwise rotation of the map by 0.975 degree gave the max value of R 2 ( 0.9995 ) . This value corresponds to a magnetic declination of about 1.0 degree to the west at that time in the central region of Kyushu Island. It is concluded that the position deviation on the map is caused by magnetic declination, because Inoh considered magnetic north to be true north when surveying and mapping.
九州岛在伊诺图上的地理位置与磁偏角
M.Hoyanagi在一张比例尺为1-216000的Inoh地图上指出了九州岛的位置偏差。他参照19世纪初伊诺采用的地图投影和磁偏角进行了解释。在这项研究中,对地图上天文观测点的坐标值与实际地图上相应位置(经纬度)之间的相关性进行了统计分析。确定系数(R2)是为小角度旋转的地图计算的。结果,地图逆时针旋转0.975度得到R2的最大值(0.9995)。该值对应于当时九州岛中部地区向西约1.0度的磁偏角。结果表明,地图上的位置偏差是由磁偏角引起的,因为Inoh在测绘时认为磁北是正北。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
CiteScore
1.50
自引率
33.30%
发文量
28
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