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Solar cycle and long-period variations of mesospheric temperatures
Institution:1. Department of Electronic Engineering, Chang Gung University, Taoyuan, Taiwan;2. Sustainable Energy Development Center, National Taiwan University of Science & Tech., Taipei, Taiwan;3. Biosensor Group, Chang Gung University, Taoyuan, Taiwan;4. Research Unit for Clean Technology, Indonesian Institute of Sciences, Bandung, Indonesia;5. Research Center for Electronics and Telecommunications, Indonesian Institute of Sciences, Bandung, Indonesia;6. Department of Nephrology, Chang Gung Memorial Hospital, Taoyuan, Taiwan;7. Department of Electronic Engineering, Ming-Chi University of Technology, New Taipei City, Taiwan;8. Department of Materials Engineering, Ming-Chi University of Technology, New Taipei City, Taiwan;1. Department of Chemistry, University of Coimbra, 3004-535 Coimbra, Portugal;2. CFisUC, Department of Physics, University of Coimbra, Coimbra 3004-516, Portugal;3. Centre for Nanoscience and Technology, Anna University, Chennai 600-025, India;4. Division of Chemical Engineering, Konkuk University, 120 Neungdong-ro, Gwangjin-gu, Seoul 05029, Republic of Korea;1. Food Chemistry and Food Development, Department of Biochemistry, University of Turku, FI-20014 Turku, Finland;2. Department of Chemistry, University of Turku, FI-20014 Turku, Finland;3. MTT Plant Production Research, FI-31600 Jokioinen, Finland;1. Department of Electronic Engineering, Chang Gung University, Taoyuan, Taiwan;2. Biosensor Group, Chang Gung University, Taoyuan, Taiwan;3. Center for Biomedical Engineering, Chang Gung University, Taoyuan, Taiwan;4. Research Unit for Clean Technology, Indonesian Institute of Sciences, Bandung, Indonesia;5. Research Center for Electronics and Telecommunications, Indonesian Institute of Sciences, Bandung, Indonesia;6. Sustainable Energy Development Center, National Taiwan University of Science & Tech., Taipei, Taiwan;7. Department of Nephrology, Chang Gung Memorial Hospital, Taoyuan, Taiwan;8. Department of Materials Engineering, Ming-Chi University of Technology, New Taipei City, Taiwan;9. Department of Life Sciences, International Iberian Nanotechnology Laboratory, Braga, Portugal;10. Department of Nanoelectronics Engineering, International Iberian Nanotechnology Laboratory, Braga, Portugal;1. Department of Chemistry, Banasthali University, Rajasthan 304022, India;2. School of Chemical Sciences, Central University of Gujarat, Gandhinagar 382030, India
Abstract:Evidence for a temperature variation above about 55 km between years of high and low solar activity is found in rocket data of Volgograd (49°N, 44°E) 1969–1983, reaching a solar-cycle amplitude of 6K, whereas below 55 km no statistically significant solar cycle effect is detected. This mesospheric temperature variation is in qualitative agreement with a pressure variation at 80 km derived from lower ionosphere radio reflection heights near 51°N, 13°E, measured at Kühlungsborn/GDR, covering almost two solar cycles. When the solar cycle variation has been removed from these 80 km pressure data by means of a regression analysis, there remains a quasi-cycle of about 20 yr, which agrees well with observations of a general cooling of the northern mid-latitude stratosphere between 1965 and 1977, reported by other authors.
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