太阳辐照度对蒙德极小期气候的影响

B. Mendoza, R. Garduño, J. Adem
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引用次数: 1

摘要

我们利用平均太阳总辐照度估算蒙德极小期(1645-1715)北半球平均地表温度异常约为-0.3°C。由于忽略了各种冷却效应,这个估计是一个上限,可能会发现更深的异常。太阳总辐照度是根据巴黎天文台1660年至1719年记录的太阳黑子观测资料重建的太阳自转速率得到的,发现它比现在低0.1%至0.43%。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The Impact of Solar Irradiance on the Maunder Minimum Climate
We estimate an average surface Northern Hemisphere temperature anomaly of around -0.3°C for the Maunder Minimum (1645-1715) using the average total solar irradiance. As various cooling effects were neglected this estimate is an upper limit and a deeper anomaly may be found. The total solar irradiance is obtained from the solar rotation rate reconstructed using observations of sunspots recorded at the Observatoire de Paris from 1660 to 1719, and is found to be lower than at present by 0.1% to 0.43%.
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