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机构地区:[1]中国科学院兰州高原大气物理研究所
出 处:《高原气象》1998年第3期266-270,共5页Plateau Meteorology
基 金:国家攀登计划
摘 要:讨论了2500多年来太阳黑子周期长度(SCL)的跃变特征,发现在百年尺度上SCL基本在平均值附近变化,而其变率则存在明显的跃变现象,当SCL的变率增大时,气候随之发生冷跃变,反之,则发生暖跃变。小冰期时,太阳活动弱且不稳定,与地球气候冷且不稳定具有同时性。In this paper, the jump transition characteristic of sunspot cycle length(henceforth SCL) from 522BC upward were analyzed. Moving t-test method based results indicate that there were no appreciable change of SCL in recent 2500 years. However, the variances of SCL series (henceforth S v) show apparent jump transitions in 260BC, 31AD, 271AD, 1172AD and 1844AD, respectively. When S v jump from low to high level, the “cold” climatic jumps were occurred, and vice versa. Moreover, the highest level of S v coincide with the frequently occurrence of natural disaster in the Little Ice Age, which indicates that the instability of climate was caused by the unstable SCL (solar activity).
分 类 号:P461.1[天文地球—大气科学及气象学] P467
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