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'''James Croll''' (2 January 1821 – 15 December 1890) was a [[Scotland|Scottish]] physical scientist who was the leading proponent of an astronomical theory of [[climate change]] in the 19th century. The son of a stonemason and crofter from Cargill in Scotland, he started work as a millwright, but became caretaker at Anderson's College, [[Glasgow]], in 1859. He was later appointed resident geologist in the [[Edinburgh]] office of the Geological Survey, where he remained until he retired in 1880.<ref>International Commission on History of Meteoro, James Fleming (Lead Author);Cutler Cleveland (Topic Editor) "James Croll and the astronomical theory of climate change". In: Encyclopedia of Earth. Eds. Cutler J. Cleveland (Washington, D.C.: Environmental Information Coalition, National Council for Science and the Environment). [First published in the Encyclopedia of Earth May 5, 2007; Last revised Date May 5, 2007; Retrieved December 19, 2010 </ref>
'''James Croll''' (2 January 1821 – 15 December 1890) was a [[Scotland|Scottish]] physical scientist who was the leading proponent of an astronomical theory of [[climate change]] in the 19th century. The son of a stonemason and crofter from Cargill in Scotland, he started work as a millwright, but became caretaker at Anderson's College, [[Glasgow]], in 1859. He was later appointed resident geologist in the [[Edinburgh]] office of the Geological Survey, where he remained until he retired in 1880.<ref>International Commission on History of Meteoro, James Fleming (Lead Author);Cutler Cleveland (Topic Editor) "James Croll and the astronomical theory of climate change". In: Encyclopedia of Earth. Eds. Cutler J. Cleveland (Washington, D.C.: Environmental Information Coalition, National Council for Science and the Environment). [First published in the Encyclopedia of Earth May 5, 2007; Last revised Date May 5, 2007; Retrieved December 19, 2010 </ref>
Croll, who was effectively self-taught, is best known for his work on the astronomical theory of the [[ice age]]s, but he also made major contributions on the glacial geology of Scotland, on the mechanisms that drive ocean circulation and the impact of that circulation on climate, tidal theory and the rotation of the Earth.  
Croll, who was effectively self-taught, is best known for his work on the astronomical theory of the [[ice age]]s, but he also made major contributions on the glacial geology of Scotland, on the mechanisms that drive ocean circulation and the impact of that circulation on climate, tidal theory and the rotation of the Earth. <ref>[http://www.nature.com/nature/journal/v43/n1104/abs/043180b0.html James Croll F.R.S.]
''Nature'' 43:180-181 (1890)</ref>


His insights into the interplay between [[astronomy|astronomical]] and [[geology|geological factors]] – into cosmic [[physics]] and [[climate dynamics]] -- were extremely influential. In 1875 Croll published his major book ''Climate and Time'' which had a profound influence on geologists around the world.<ref>Croll, James, 1875. [http://books.google.com/books?id=JBsAAAAAQAAJ&pg=PA1&dq=Climate+and+Time+in+Their+Geological+Relations Climate and Time in Their Geological Relations]. A theory of secular changes of the earth's climate. New York. </ref> [[Charles Lyell]], the leading geologist of the time, revised his ''Principles of Geology'' in response to Croll’s theory. His view was notably followed by [[James Geikie]] in ''The Great Ice Age'' (1874–84),  
His insights into the interplay between [[astronomy|astronomical]] and [[geology|geological factors]] – into cosmic [[physics]] and [[climate dynamics]] -- were extremely influential. In 1875 Croll published his major book ''Climate and Time'' which had a profound influence on geologists around the world.<ref>Croll, James, 1875. [http://books.google.com/books?id=JBsAAAAAQAAJ&pg=PA1&dq=Climate+and+Time+in+Their+Geological+Relations Climate and Time in Their Geological Relations]. A theory of secular changes of the earth's climate. New York. </ref> [[Charles Lyell]], the leading geologist of the time, revised his ''Principles of Geology'' in response to Croll’s theory. His view was notably followed by [[James Geikie]] in ''The Great Ice Age'' (1874–84),  
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In 1864, Croll published an article entitled ''On the Physical Cause of the Change of Climate During Geological Epochs,'' where he proposed that periodic variations in the earth’s orbit around the sun accounted for the periodic variations in [[climate]] evidenced by [[geology|geological]] evidence of [[ice age]]s , and alternating cold and warm periods in each hemisphere (i.e. that ice ages in the Northern Hemisphere coincided with interglacials in the Southern Hemisphere). He proposed that feedback mechanisms, including the radiative effects of the ice fields, enhanced formation of [[cloud]] and [[fog]], changes in [[sea level]], and the mixing and redirection of warm and cold [[ocean current]]s enhanced the climatic changes initiated by the orbital changes. Because of uncertainties in the timing of ice ages, and because Croll’s theory predicted glaciation in only one hemisphere at a time, his theory was disregarded at first.  
In 1864, Croll published an article entitled ''On the Physical Cause of the Change of Climate During Geological Epochs,'' where he proposed that periodic variations in the earth’s orbit around the sun accounted for the periodic variations in [[climate]] evidenced by [[geology|geological]] evidence of [[ice age]]s , and alternating cold and warm periods in each hemisphere (i.e. that ice ages in the Northern Hemisphere coincided with interglacials in the Southern Hemisphere). He proposed that feedback mechanisms, including the radiative effects of the ice fields, enhanced formation of [[cloud]] and [[fog]], changes in [[sea level]], and the mixing and redirection of warm and cold [[ocean current]]s enhanced the climatic changes initiated by the orbital changes. Because of uncertainties in the timing of ice ages, and because Croll’s theory predicted glaciation in only one hemisphere at a time, his theory was disregarded at first.  


Croll's otherworks included ''The Philosophy of Theism'' (1857), ''Climate and Cosmology'' (1885) and ''The Philosophic Basis of Evolution'' (1890). In 1876, Croll was elected as a Fellow of the Royal Society and was awarded an honorary doctorate from the University of St Andrews.
Croll's otherworks included ''The Philosophy of Theism'' (1857), ''Climate and Cosmology'' (1885) and ''The Philosophic Basis of Evolution'' (1890). In 1876, Croll was elected as a Fellow of the Royal Society and was awarded an honorary doctorate from the University of St Andrews. His 1889 book ''Stellar Evolution and Its Relations to Geological Time'' <ref>James Croll (1889) [http://books.google.co.uk/books?id=gNm45VaNlBkC&printsec=frontcover&dq=james+croll&source=bl&ots=PmUnyCQiYr&sig=MSJXJ6GgA6AXW55yk-U2krkmGAs&hl=en&ei=uj0PTaP1HKCqhAfE2My3Dg&sa=X&oi=book_result&ct=result&resnum=9&ved=0CDgQ6AEwCDgK#v=onepage&q&f=false  Stellar Evolution and Its Relations to Geological Time]: New York, Appleton </ref>contains "the first modern attempt to explain the chemical composition of the stars"<ref>''A concise history of solar and stellar physics'' By Jean Louis Tassoul, Monique Tassoul</ref>


==References==
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James Croll (2 January 1821 – 15 December 1890) was a Scottish physical scientist who was the leading proponent of an astronomical theory of climate change in the 19th century. The son of a stonemason and crofter from Cargill in Scotland, he started work as a millwright, but became caretaker at Anderson's College, Glasgow, in 1859. He was later appointed resident geologist in the Edinburgh office of the Geological Survey, where he remained until he retired in 1880.[1] Croll, who was effectively self-taught, is best known for his work on the astronomical theory of the ice ages, but he also made major contributions on the glacial geology of Scotland, on the mechanisms that drive ocean circulation and the impact of that circulation on climate, tidal theory and the rotation of the Earth. [2]

His insights into the interplay between astronomical and geological factors – into cosmic physics and climate dynamics -- were extremely influential. In 1875 Croll published his major book Climate and Time which had a profound influence on geologists around the world.[3] Charles Lyell, the leading geologist of the time, revised his Principles of Geology in response to Croll’s theory. His view was notably followed by James Geikie in The Great Ice Age (1874–84),

In 1864, Croll published an article entitled On the Physical Cause of the Change of Climate During Geological Epochs, where he proposed that periodic variations in the earth’s orbit around the sun accounted for the periodic variations in climate evidenced by geological evidence of ice ages , and alternating cold and warm periods in each hemisphere (i.e. that ice ages in the Northern Hemisphere coincided with interglacials in the Southern Hemisphere). He proposed that feedback mechanisms, including the radiative effects of the ice fields, enhanced formation of cloud and fog, changes in sea level, and the mixing and redirection of warm and cold ocean currents enhanced the climatic changes initiated by the orbital changes. Because of uncertainties in the timing of ice ages, and because Croll’s theory predicted glaciation in only one hemisphere at a time, his theory was disregarded at first.

Croll's otherworks included The Philosophy of Theism (1857), Climate and Cosmology (1885) and The Philosophic Basis of Evolution (1890). In 1876, Croll was elected as a Fellow of the Royal Society and was awarded an honorary doctorate from the University of St Andrews. His 1889 book Stellar Evolution and Its Relations to Geological Time [4]contains "the first modern attempt to explain the chemical composition of the stars"[5]

References

  1. International Commission on History of Meteoro, James Fleming (Lead Author);Cutler Cleveland (Topic Editor) "James Croll and the astronomical theory of climate change". In: Encyclopedia of Earth. Eds. Cutler J. Cleveland (Washington, D.C.: Environmental Information Coalition, National Council for Science and the Environment). [First published in the Encyclopedia of Earth May 5, 2007; Last revised Date May 5, 2007; Retrieved December 19, 2010
  2. James Croll F.R.S. Nature 43:180-181 (1890)
  3. Croll, James, 1875. Climate and Time in Their Geological Relations. A theory of secular changes of the earth's climate. New York.
  4. James Croll (1889) Stellar Evolution and Its Relations to Geological Time: New York, Appleton
  5. A concise history of solar and stellar physics By Jean Louis Tassoul, Monique Tassoul