Research output: Chapter in Book/Report/Conference proceeding › Other chapter contribution › Research › peer-review
On the Cooperation of Wladimir Köppen, Alfred Wegener and Milutin Milankovitch in Paleoclimate Research and the Revival of the Milankovitch Hypothesis. / Thiede, J.
Геология морей и океанов: Материалы XXIII Международной научной конференции (Школы) по морской геологии. ed. / А.П. Лисицын; Н.В. Политова; В.П. Шевченко. Vol. II М. : Институт Океанологии РАН, 2019. p. 195.Research output: Chapter in Book/Report/Conference proceeding › Other chapter contribution › Research › peer-review
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TY - CHAP
T1 - On the Cooperation of Wladimir Köppen, Alfred Wegener and Milutin Milankovitch in Paleoclimate Research and the Revival of the Milankovitch Hypothesis
AU - Thiede, J.
PY - 2019
Y1 - 2019
N2 - Wladimir Köppen (1846–1940, originally from St. Petersburg), Alfred Wegener (1880–1930, originally from Berlin) and Milutin Milankovitch (1879– 1958, originally from Dalj/ then Austria-Hungary, today eastern Croatia) made very important contributions to paleoclimatology during the early years of the 20th century. Köppen described the global climate zonation, Wegener defined the continental drift during the Phanerozoic, using Köppen´s climate zonations applied to paleogeographic scenarios of the geological past, and Milankovitch introduced regularly changing orbital parameters as controls of past climatic changes providing a precise time scale for Glacials and Interglacials during the Quaternary. By combining their scientific efforts, they succeeded to change our understanding of Earth history in a fundamental way, each of them with their specific expertise and their wide scientific horizons.
AB - Wladimir Köppen (1846–1940, originally from St. Petersburg), Alfred Wegener (1880–1930, originally from Berlin) and Milutin Milankovitch (1879– 1958, originally from Dalj/ then Austria-Hungary, today eastern Croatia) made very important contributions to paleoclimatology during the early years of the 20th century. Köppen described the global climate zonation, Wegener defined the continental drift during the Phanerozoic, using Köppen´s climate zonations applied to paleogeographic scenarios of the geological past, and Milankovitch introduced regularly changing orbital parameters as controls of past climatic changes providing a precise time scale for Glacials and Interglacials during the Quaternary. By combining their scientific efforts, they succeeded to change our understanding of Earth history in a fundamental way, each of them with their specific expertise and their wide scientific horizons.
UR - http://geoschool.ocean.ru/index.php?option=com_k2&view=item&id=29:oglavlenie-toma-ii-sbornika-dokladov-konferentsii-2019-g&Itemid=272
UR - http://geoschool.ocean.ru/images/reports_2019/Volume_2_MarineGeology_2019.pdf
M3 - Other chapter contribution
SN - 9785990144965
VL - II
SP - 195
BT - Геология морей и океанов
A2 - Лисицын, А.П.
A2 - Политова, Н.В.
A2 - Шевченко, В.П.
PB - Институт Океанологии РАН
CY - М.
Y2 - 18 November 2019 through 22 November 2019
ER -
ID: 53743796