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作 者:Nicodeme Djiedeu Esther C. Modi-Mbog Laurent Nana Nicodeme Djiedeu;Esther C. Modi-Mbog;Laurent Nana(CEPAMOQ, Faculty of Science, University of Douala, Douala, Cameroon;Pure Physics Laboratory, Group of Nonlinear Physics and Complex Systems, Department of Physics, Faculty of Science, University of Douala, Douala, Cameroon;Department of National Meteorology, Ministry of Transport, Yaounde, Cameroon)
机构地区:[1]CEPAMOQ, Faculty of Science, University of Douala, Douala, Cameroon [2]Pure Physics Laboratory, Group of Nonlinear Physics and Complex Systems, Department of Physics, Faculty of Science, University of Douala, Douala, Cameroon [3]Department of National Meteorology, Ministry of Transport, Yaounde, Cameroon
出 处:《Atmospheric and Climate Sciences》2024年第4期474-483,共10页大气和气候科学(英文)
摘 要:In this work, we present a general theoretical study leading to analytical expression of the seasonal temperature at the near surface that is expected to evaluate any area seasonal temperature of the world using the least square method to fit the hourly data to the theoretical curve of the temperature. It is shown that the temperature is globally the result of two contributions: the contribution of the revolution movement of the terrestrial globe on its elliptical orbit around the sun, the contribution of the spin-orbit coupling for the rotation movement of the terrestrial globe around its polar axis and its revolution movement. The orbital behavior of the temperature is used to find the seasonal divisions of the climate for the local area considered. The whole expression of the temperature is very useful for the meteorological needs. The contribution of the human activities and natural instabilities are the results of discrepancies which increase errors (standard deviations).In this work, we present a general theoretical study leading to analytical expression of the seasonal temperature at the near surface that is expected to evaluate any area seasonal temperature of the world using the least square method to fit the hourly data to the theoretical curve of the temperature. It is shown that the temperature is globally the result of two contributions: the contribution of the revolution movement of the terrestrial globe on its elliptical orbit around the sun, the contribution of the spin-orbit coupling for the rotation movement of the terrestrial globe around its polar axis and its revolution movement. The orbital behavior of the temperature is used to find the seasonal divisions of the climate for the local area considered. The whole expression of the temperature is very useful for the meteorological needs. The contribution of the human activities and natural instabilities are the results of discrepancies which increase errors (standard deviations).
关 键 词:Seasonal Temperature Orbital Temperature Spin-Orbit Temperature Hourly Data Seasonal Divisions
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