Colaba–Alibag magnetic observatory and Nanabhoy Moos: the influence of one over the other

The first permanent magnetic observatories in colonial India were established by the East India Company and under the Göttingen Magnetic Union. One of the world's longest running observatories was set up at Colaba (Bombay) in 1841, which was shifted to Alibag in 1904 to avoid electric traction...

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Main Authors: P. B. Gawali, M. G. Doiphode, R. N. Nimje
Format: Article
Language:English
Published: Copernicus Publications 2015-09-01
Series:History of Geo- and Space Sciences
Online Access:http://www.hist-geo-space-sci.net/6/107/2015/hgss-6-107-2015.pdf
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spelling doaj-fcbd8dc1e8ba4ce19286cda04ebe9de22020-11-24T23:04:28ZengCopernicus PublicationsHistory of Geo- and Space Sciences2190-50102190-50292015-09-016210713110.5194/hgss-6-107-2015Colaba–Alibag magnetic observatory and Nanabhoy Moos: the influence of one over the otherP. B. Gawali0M. G. Doiphode1R. N. Nimje2Indian Institute of Geomagnetism, Plot No. 5, Sector 18, Kalamboli Highway, New Panvel, Navi Mumbai – 410 218, IndiaIndian Institute of Geomagnetism, Plot No. 5, Sector 18, Kalamboli Highway, New Panvel, Navi Mumbai – 410 218, IndiaIndian Institute of Geomagnetism, Plot No. 5, Sector 18, Kalamboli Highway, New Panvel, Navi Mumbai – 410 218, IndiaThe first permanent magnetic observatories in colonial India were established by the East India Company and under the Göttingen Magnetic Union. One of the world's longest running observatories was set up at Colaba (Bombay) in 1841, which was shifted to Alibag in 1904 to avoid electric traction effects on magnetic recordings. The observatory is located at the northwestern tip of Maharashtra, India, on the Arabian Sea. The magnetic data at Colaba were collected through eye-observation instruments from 1841 to 1872 and by photographic (magnetograph) instruments from 1872 to 1905, which reveal seasonal and other periodic effects on geomagnetic elements. Seasonal influence can be deciphered on the <i>H</i> minimum, but not on the maximum; the disturbances in March and April were opposite to those in December and January. <i>D</i> was maximum in 1880 (57' E) and minimum in 1904 (10' E). The data from 1882 to 1905 revealed that <i>H</i> annual inequality was influenced by 5.5-year periodicity, <i>D</i> by 13.5 days from 1888 to 1905, and <i>I</i> and <i>Z</i> by 11-year periodicity from 1894 to 1905 and 1873 to 1905, respectively. Secular variation of <i>Z</i> was parallel to that of <i>I</i>. <i>Z</i> exhibited an increasing trend from 1868 (12 874 nT) to 1905 (15 083 nT). The plan and location of Colaba–Alibag as well as the instruments used are discussed. The initial Colaba magnetic data containing "magnetic disturbances" was harnessed to identify the "disturbing point" on Earth. Nanabhoy Moos, the first Indian director, presciently hinted at a solar origin for magnetic disturbances, revealed the dependence of magnetic elements on the sunspot cycle, unraveled disturbance daily variation, and tried to understand the association, if any, between geomagnetic, seismological and meteorological phenomena. The two giant volumes published in 1910 attest to Moos' seminal work and his inventiveness in organizing and analyzing long series data. He also had a major role in moving Colaba magnetic observatory to Alibag. Thus, the observatory and Moos had a synergestic relationship influencing each other. The long data series has as much historical significance as scientific, which can bring out short- as well as long-term trends in geomagnetic data.http://www.hist-geo-space-sci.net/6/107/2015/hgss-6-107-2015.pdf
collection DOAJ
language English
format Article
sources DOAJ
author P. B. Gawali
M. G. Doiphode
R. N. Nimje
spellingShingle P. B. Gawali
M. G. Doiphode
R. N. Nimje
Colaba–Alibag magnetic observatory and Nanabhoy Moos: the influence of one over the other
History of Geo- and Space Sciences
author_facet P. B. Gawali
M. G. Doiphode
R. N. Nimje
author_sort P. B. Gawali
title Colaba–Alibag magnetic observatory and Nanabhoy Moos: the influence of one over the other
title_short Colaba–Alibag magnetic observatory and Nanabhoy Moos: the influence of one over the other
title_full Colaba–Alibag magnetic observatory and Nanabhoy Moos: the influence of one over the other
title_fullStr Colaba–Alibag magnetic observatory and Nanabhoy Moos: the influence of one over the other
title_full_unstemmed Colaba–Alibag magnetic observatory and Nanabhoy Moos: the influence of one over the other
title_sort colaba–alibag magnetic observatory and nanabhoy moos: the influence of one over the other
publisher Copernicus Publications
series History of Geo- and Space Sciences
issn 2190-5010
2190-5029
publishDate 2015-09-01
description The first permanent magnetic observatories in colonial India were established by the East India Company and under the Göttingen Magnetic Union. One of the world's longest running observatories was set up at Colaba (Bombay) in 1841, which was shifted to Alibag in 1904 to avoid electric traction effects on magnetic recordings. The observatory is located at the northwestern tip of Maharashtra, India, on the Arabian Sea. The magnetic data at Colaba were collected through eye-observation instruments from 1841 to 1872 and by photographic (magnetograph) instruments from 1872 to 1905, which reveal seasonal and other periodic effects on geomagnetic elements. Seasonal influence can be deciphered on the <i>H</i> minimum, but not on the maximum; the disturbances in March and April were opposite to those in December and January. <i>D</i> was maximum in 1880 (57' E) and minimum in 1904 (10' E). The data from 1882 to 1905 revealed that <i>H</i> annual inequality was influenced by 5.5-year periodicity, <i>D</i> by 13.5 days from 1888 to 1905, and <i>I</i> and <i>Z</i> by 11-year periodicity from 1894 to 1905 and 1873 to 1905, respectively. Secular variation of <i>Z</i> was parallel to that of <i>I</i>. <i>Z</i> exhibited an increasing trend from 1868 (12 874 nT) to 1905 (15 083 nT). The plan and location of Colaba–Alibag as well as the instruments used are discussed. The initial Colaba magnetic data containing "magnetic disturbances" was harnessed to identify the "disturbing point" on Earth. Nanabhoy Moos, the first Indian director, presciently hinted at a solar origin for magnetic disturbances, revealed the dependence of magnetic elements on the sunspot cycle, unraveled disturbance daily variation, and tried to understand the association, if any, between geomagnetic, seismological and meteorological phenomena. The two giant volumes published in 1910 attest to Moos' seminal work and his inventiveness in organizing and analyzing long series data. He also had a major role in moving Colaba magnetic observatory to Alibag. Thus, the observatory and Moos had a synergestic relationship influencing each other. The long data series has as much historical significance as scientific, which can bring out short- as well as long-term trends in geomagnetic data.
url http://www.hist-geo-space-sci.net/6/107/2015/hgss-6-107-2015.pdf
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