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Edward Sabine KCB FRS ( Dublin, 14 de outubro de 1788 — Londres, 26 de junho de 1883) foi um astrônomo, geofísico, ornitólogo e explorador irlandês. [ 1][ 2][ 3] Dois caminhos do trabalho de Sabine merecem destaque: Pesquisas extensivas relacionadas ao campo magnético terrestre.
Sir Edward Sabine KCB FRS FRSE FRAS (/ ˈ s eɪ b ɪ n /; 14 October 1788 – 26 June 1883) was an Irish astronomer, geophysicist, ornithologist, explorer, soldier and the 30th president of the Royal Society. He led the effort to establish a system of magnetic observatories in various parts of British territory all over the globe.
- 14 October 1788, Dublin, Kingdom of Ireland
- Sir Benjamin Brodie
- 26 June 1883 (aged 94), East Sheen, London, England
- Sir George Airy
5 de abr. de 2024 · Edward Sabine, Anglo-Irish astronomer and geodesist noted for his experiments in determining the shape of Earth and for his studies of Earth’s magnetic field. He discovered that the periodic variation of sunspots correlates with certain changes in magnetic disturbances on Earth.
- The Editors of Encyclopaedia Britannica
Edward Sabine was an Irish geophysicist, astronomer, and explorer, who made extensive pendulum measurements to determine the shape of the earth, and established magnetic observatories to relate sunspot activity with disturbances in terrestrial magnetism.
14 de out. de 2021 · On October 14, 1788, Irish astronomer, geophysicist, ornithologist, explorer, soldier and the 30th President of the Royal Society Sir Edward Sabine was born. His aim was to study the shape of the Earth and its magnetic field.
26 de mai. de 2008 · Sir Edward Sabine, soldier, scientist (b at Dublin, Ire 14 Oct 1788; d at Richmond, Eng 26 June 1883). He fought along the St Lawrence River in Upper and Lower Canada in 1813-14, and then, within the army, went on to a distinguished career in science.
12 de mai. de 2014 · by Timothy Oleson. Monday, May 12, 2014. Geophysicist and astronomer Edward Sabine (1788–1883). Credit: Bibliothèque Nationale de France, public domain. At the beginning of the 19th century, little was understood about Earth’s magnetic field, but interest in its workings had begun to grow, especially in Europe.
