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    Please use this identifier to cite or link to this item: https://ir.lib.ncu.edu.tw/handle/987654321/99797


    Title: Observations of stratosphere-troposphere coupling during major solar eclipses from FORMOSAT-3/COSMIC constellation
    Authors: 王國英;Wang, Kuo-Ying;Liu, Chao-Han;Lee, Lou-Chuang;Braesicke, Peter
    Contributors: 地球科學學院大氣科學學系
    Keywords: Aerospace Technology and Astronautics;Astrophysics and Astroparticles;Cooling;Earth, ocean, space;Exact sciences and technology;External geophysics;General properties of the high atmosphere;Global positioning systems;GPS;Meteorology;Physics;Physics and Astronomy;Physics of the high neutral atmosphere;Planetology;Solar eclipses;Space Exploration and Astronautics;Space Sciences (including Extraterrestrial Physics;Stratosphere;Troposphere;Weather forecasting
    Date: 2012-06-01
    Issue Date: 2026-04-21 13:35:46 (UTC+8)
    Publisher: Springer Netherlands;Dordrecht: Springer Netherlands
    Abstract: 摘要: Sudden tropospheric cooling and induced stratospheric warming were found during the 22 July 2009 total solar eclipse. Can the 22 July 2009 hallmark also be seen in other major solar eclipses? Here we hypothesize that the tropospheric cooling and the stratospheric warming can be predicted to occur during a major solar eclipse event. In this work we use the FORMOSAT-3/COSMIC (F3C) Global Positioning System (GPS) radio occultation (RO) data to construct eclipse-time temperature profiles before, during, and after the passages of major solar eclipses for the years 2006–2010. We use four times a day of meteorological analysis from the European Centre for Medium Range Weather Forecast (ECMWF) global meteorological analysis to construct non-eclipse effect temperature profiles for the same eclipse passages. The eclipse effects were calculated based on the difference between F3C and ECMWF profiles. A total of five eclipse cases and thirteen non-eclipse cases were analyzed and compared. We found that eclipses cause direct thermal cooling in the troposphere and indirect dynamic warming in the stratosphere. These results are statistically significant. Our results show −0.6 to −1.2°C cooling in the troposphere and 0.4 to 1.3°C warming in the middle to lower stratosphere during the eclipses. This characteristic stratosphere-troposphere coupling in temperature profiles represent a distinctive atmospheric responses to the solar eclipses.
    其他題名: Space Sci Rev
    出版者: Dordrecht: Springer Netherlands
    出版日期: 2012-06-01
    出處: Space science reviews, 2012-06, Vol.168 (1-4), p.261-282
    資源來源: EBSCOhost Academic Search Premier
    版權: The Author(s) 2011
    版權: 2015 INIST-CNRS
    版權: Springer Science+Business Media B.V. 2012
    識別號: ISSN: 0038-6308
    識別號: ISSN: 1572-9672
    識別號: EISSN: 1572-9672
    識別號: DOI: 10.1007/s11214-011-9829-1
    識別號: CODEN: SPSRA4
    Appears in Collections:[Department of Atmospheric Sciences] journal & Dissertation

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