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Low-frequency variability of beryllium-7 surface concentrations over the Eastern Mediterranean

机译:东地中海7铍表面浓度的低频变化

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Be-7 measurements, performed in Northern Greece (40degreesN) since 1988, were analyzed, in order to investigate the variability of the surface concentrations that can be attributed to processes with frequencies below the synoptic variability. Spectral analysis on the Be-7 time series revealed three characteristic spectral regions, a 1-year periodicity corresponding to the well-established annual cycle, a periodicity between 20 and 30 months and a peak corresponding to a period of 11 years. The relationship with the 11-year cycle of solar activity was investigated through the correlation between the sunspot number and Be-7 (-0.86) and between the heliocentric potential and Be-7(-0.80). (7) Be was in coincidence with the heliocentric potential whereas it lagged the sunspot number by 5 months, expressing the time needed for the solar wind variations to be reflected on the production of Be-7 during the specific solar cycle. The amplitude of the annual cycle was not constant throughout the whole period. An anti-correlation of -0.83 was revealed between the amplitude and the sunspot number with higher amplitudes during solar minimum and smaller amplitudes during solar maximum. With the use of a simplistic model, the amplitude modulation was attributed to the changing with the 11-year cycle contribution of the upper tropospheric and lower stratospheric reservoirs to the surface concentrations. More specifically, during solar maximum the contribution of upper troposphere down to the surface via winter-mixing is as much as 55% compared to the summer-mixing contribution, whereas during solar minimum winter-mixing is no more than 35%, thus inducing a higher amplitude. The superposed epoch method revealed that the 20-30 months periodicity is related to the quasi-biennial oscillation (QBO), with the Be-7 minimum following the QBO maximum with approximate to8 months time delay, whereas for the same time lag total ozone showed a reverse behavior. Cross spectrum analysis between Be-7 and total ozone with the QBO shows a significant (90% confidence level) squared coherence, indicating that 68% and 86% of Be-7 and total ozone variability of the 20-30 months periodicity, respectively, can be explained by the QBO. (C) 2003 Elsevier Science Ltd. All rights reserved. [References: 38]
机译:分析了自1988年以来在希腊北部(40度北)进行的Be-7测量,以调查表面浓度的变化,这可以归因于频率低于天气变化的过程。对Be-7时间序列的频谱分析显示了三个特征频谱区域,一个为期1年的周期对应于完善的年周期,一个为20至30个月的周期,以及一个峰值为11年。通过太阳黑子数与Be-7(-0.86)之间以及日心势与Be-7(-0.80)之间的相关性研究了与太阳活动11年周期的关系。 (7)Be与日心中心电位一致,而Be落后太阳黑子数5个月,表示太阳风变化在特定太阳周期内反映到Be-7的产生上所需要的时间。在整个周期中,年度周期的幅度不是恒定的。在振幅和太阳黑子数之间显示出-0.83的反相关关系,在太阳最小时振幅较高,而在太阳最大时振幅较小。通过使用简化模型,振幅调制归因于对流层上部和平流层下部储层对地表浓度的11年周期贡献的变化。更具体地说,在太阳最高峰期间,冬季混合对流层对地表的贡献比夏季混合层的贡献高55%,而在太阳最低峰期间,冬季对流层的贡献不超过35%,因此导致更高的振幅。叠加时代法揭示了20-30个月的周期与准两年一次振荡(QBO)有关,Be-7最小值跟随QBO最大值之后大约有8个月的时间延迟,而同一时间总臭氧显示滞后逆向行为。使用QBO对Be-7和总臭氧之间的跨光谱分析显示出显着的平方相干性(置信度为90%),表明在20-30个月的周期内,Be-7和总臭氧变异性分别为68%和86%,可以由QBO来解释。 (C)2003 Elsevier ScienceLtd。保留所有权利。 [参考:38]

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