WebThe Earth's climate is not constant, and has experienced major changes in the past on all timescales. The causes of these changes, although still incompletely understood, vary according to the timescale considered. Some of the most important causal mechanisms include continental drift, changes in the Earth's orbital parameters, volcanic activity and … WebDec 17, 2024 · 64 H. Flohn: On the meteorological interpretation of Pleistocene climate fluctuations magnitude these numbers agree satisfactorily, especially if one considers that the structure of the Antarctic ...
Tropical Origins for Recent North Atlantic Climate Change
WebFlohn H. 1963: Zur Meteorologischen Interpretation der pleistozänen Klimaschwankungen. Eiszeitalter und Gegenwart, 14, 153-160. (K163) Flohn H. 1963: Klimaschwankungen und großräumige Klimabeeinflussung. In: Bonner Meteorol. Abhandlungen, BMA 2, 7-61. (auch in Arbeitsgem. f. Forschung des Landes Nordrhein - Westfalen, Heft 115.) WebLarge-scale Aspects of the "Summer Monsoon" in South and East Asia. Flohn, H. Publication: Journal of the Meteorological Society of Japan. Pub Date: 1957. DOI: 10.2151/jmsj1923.35A.0_180. in 1932 ukrainians rebelled against
Climate and paleoclimate: What we can learn about solar
WebH. Flohn During the last decades the average temperature of the tropical troposphere (200/850 hPa layer) has steadily increased, between 1965 and 1984 by about 0.8C in the whole equatorial belt. WebA suitable nomenclature for atmospheric strata as well as a clear definition of the boundaries is proposed. The necessity of such a new classification is stressed. The atmosphere is divided into an inner and an outer atmosphere; from the latter particles may escape. The inner atmosphere is divided into three spheres—troposphere, stratosphere, and … WebClick on the article title to read more. dutch norway