首页> 外文期刊>Physics and chemistry of the earth >Long-term changes in atmospheric circulation, earth rotation rate and north-south solar asymmetry
【24h】

Long-term changes in atmospheric circulation, earth rotation rate and north-south solar asymmetry

机译:大气环流,地球自转速率和南北太阳不对称的长期变化

获取原文
获取原文并翻译 | 示例
           

摘要

Earlier studies have demonstrated a relation between long-term changes in the Earth's rotation rate and the prevalence of zonal or meridional types of circulation. The results, however, have been confined to the 20th century and to the Northern hemisphere. In the present paper we compare the long-term changes in the length of the day (LOD) and the temperature contrast between the equator and the pole in the Northern and the Southern hemispheres as an indirect measure for the zonality of the atmospheric circulation. In the 20th century in the Northern hemisphere we find a high negative correlation between the rotation rate and the equator/pole temperature contrast, while in the 19th century the correlation is positive. For the Southern hemisphere, the situation is opposite. The correlation changes when the North-South asymmetry of solar activity also changes sign. The decadal changes in LOD are shown to be related to the changes in the North-South asymmetry of solar equatorial rotation rate supposedly induced by planetary-driven changes in the angular momentum of the solar system, with both quantities showing pronounced periodicities and high squared coherence at 47 years. It is hypothesized that decadal changes in LOD are driven by core-mantle coupling processes regulated by solar wind transferring solar magnetic fields and angular momentum modulated by planetary influences. The atmospheric circulation in the Northern and Southern hemispheres is found to be different not only on decadal time-scales but also in the 11-year solar cycle, and different in even and odd cycles. While long-term changes in geomagnetic activity closely follow sunspot activity changes, the correlation between the two in the 11-year cycle has been decreasing in the last century with the increase of the North-South solar activity asymmetry which modulates also the asymmetry of galactic cosmic rays flux considered a candidate mediator between solar activity and climate.
机译:早期的研究表明,地球自转速率的长期变化与纬向或经向类型环流的流行之间存在联系。然而,结果仅限于20世纪和北半球。在本文中,我们比较了日长(LOD)的长期变化以及北半球和南半球赤道与极点之间的温度对比,以此间接测量了大气环流的分区性。在20世纪的北半球,我们发现旋转速度与赤道/极点温度反差之间存在很高的负相关性,而在19世纪,这是正相关的。对于南半球,情况则相反。当太阳活动的南北不对称性也改变符号时,相关性也会改变。 LOD的年代际变化显示与推测由行星驱动的太阳系角动量引起的太阳赤道旋转率南北不对称性的变化有关,两个量都显示出明显的周期性和高平方相干性在47岁。假设LOD的年代际变化是由芯—幔耦合过程驱动的,该过程受太阳风传递太阳磁场和受行星影响调制的角动量的调节。发现北半球和南半球的大气环流不仅在年代际尺度上不同,而且在11年的太阳周期中也不同,在偶数和奇数周期中也不同。尽管地磁活动的长期变化紧随太阳黑子的活动而变化,但随着北南太阳活动不对称性的增加,上个世纪11年周期中两者之间的相关性一直在下降,这也调节了银河系的不对称性宇宙射线通量被认为是太阳活动与气候之间的候选媒介。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号