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赤道平流层中下层纬向风准2 a振荡与行星运动
引用本文:叶更新,刘国禹.赤道平流层中下层纬向风准2 a振荡与行星运动[J].气象科学,2015,35(3):323-327.
作者姓名:叶更新  刘国禹
作者单位:通化市气象局, 吉林 通化 134001,通化市气象局, 吉林 通化 134001
基金项目:吉林省气象局科技创新基金(201054)
摘    要:利用实况资料和小波分析方法研究了赤道平流层中下层纬向风准2 a振荡(简称QBO)周期变化与行星运动之间的联系, 结果表明, QBO周期以火星冲日(25.68月)周期为基准, 时而变长, 时而变短。当地球、土星、天王星3星一线时, 火星冲日月份30 hPa纬向风由东风向西风转换;而3星成直角时, 则从西风向东风的转换。QBO周期变化与木星冲日时的视赤纬存在明显的对应关系。当木星冲日视赤纬达到正极值时(此时为北半球的冬季), QBO周期达到最大;当木星冲日视赤纬达到负极值时(此时为北半球的夏季), QBO周期达到最小。QBO周期与木星冲日视赤纬之间的相关系数高达0.496, 并通过0.001显著性检验。QBO强度与周期、木星冲日时的视赤纬呈现反相变化, 即QBO强度的强(弱), 对应于QBO周期的短(长)。木星冲日负(正)视赤纬, 在过去60 a中, QBO的强度总体呈现增加的趋势, 与天王星的视赤纬减小存在一定的联系。

关 键 词:纬向风  平流层  周期变化  行星运动  视赤纬
收稿时间:2013/9/29 0:00:00
修稿时间:4/3/2014 12:00:00 AM

Relation between QBO periodic variation and planetary motion
YE Gengxin and LIU Guoyu.Relation between QBO periodic variation and planetary motion[J].Scientia Meteorologica Sinica,2015,35(3):323-327.
Authors:YE Gengxin and LIU Guoyu
Institution:Tonghua Meteorological Bureau, Jilin Tonghua 134001, China and Tonghua Meteorological Bureau, Jilin Tonghua 134001, China
Abstract:By using the recorded data and the wavelet analysis method, the relation between QBO periodic variation and planetary motion is studied. Results show that QBO cycle is based on Mars opposition period (25.68 months), and sometimes it is longer, sometimes it is shorter. When the Earth, Saturn, Uranus were in a line, the 30 hPa zonal easterly wind converts to the westerly; when the three celestial bodies were at right angle, the westerly wind converts to the easterly. A significant connection exists between QBO cycle and Jupiter at opposition declination, when Jupiter opposition declination reaches the positive extreme (the winter of northern hemisphere), QBO cycle reaches its maximum, while Jupiter opposition declination reaches its negative extreme (the summer of northern hemisphere), QBO cycle approaches to its minimum. The correlation coefficient between QBO cycle and Jupiter opposition declination amounts to 0.496, it means confidence correlation test greater than 0.001. QBO intensity is in inverse phase with QBO cycle and Jupiter opposition declination, that is, strong (weak) QBO intensity corresponds to the short (long) QBO period and negative (positive) Jupiter opposition declination. In the past 60 years, QBO intensity has been increasing with Uranus declination decreasing.
Keywords:Latitudinal  Wind  Stratosphere  Periodic change  Planetary motion  Apparent declination
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