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Stratospheric warmings and the geomagnetic lunar tide: 1958-2007

机译:平流层也和地磁太阴潮:1958 - 2007

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摘要

A quantitative comparison of the geomagnetic lunar tide and lower stratospheric parameters (zonal mean air temperature T and zonal mean zonal wind U) is carried out for the period 1958-2007. The correlation between the amplitude of the geomagnetic lunar tide at an equatorial station, Addis Ababa, and the lower stratospheric parameters from the National Centers for Environmental Prediction—National Center for Atmospheric Research (NCEP-NCAR) reanalysis is examined. It is found that the lunar tidal amplitude tends to be positively and negatively correlated with the stratospheric T and U, respectively, in high latitudes of the Northern Hemisphere during December and January. High correlations are observed in approximately 70% of stratospheric sudden warming (SSW) events. The results suggest that variability of the geomagnetic lunar tide during the northern winter is closely linked with dynamical changes in the lower stratospheric parameters associated with SSWs.
机译:地磁太阴的定量比较潮流和低平流层参数(纬向平均空气温度T和纬向平均纬向风U) 1958 - 2007年期间进行。的振幅之间的相关性地磁太阴潮赤道站,亚的斯亚贝巴,低平流层从国家中心参数环境Prediction-National中心大气研究(NCEP-NCAR)再分析检查。振幅往往是积极的和消极的与平流层T和U,分别在北部高纬度地区半球在12月和1月。相关性在大约70%的观察平流层突然变暖(f)事件。结果表明,变异的在北方冬天地磁太阴潮与动态变化密切相关低平流层参数相关SSWs。

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