Insolation During Interglacial

Insolation During Interglacial
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DOI:
10.1016/s1571-0866(07)80027-3
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发表时间:
2007-01-01
期刊:
CLIMATE OF PAST INTERGLACIALS
影响因子:
--
通讯作者:
Lorenz, S. J.
Lorenz, S. J.
中科院分区:
其他
文献类型:
--
作者:
Berger, A.;Loutre, M. F.;Lorenz, S. J.

文献摘要

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回顾了主要的太阳辐射参数,特别是整个地球全年接收的能量和24小时平均辐照度。强调了它们的光谱特征,并对大气顶部和地球表面的日照、热量季节和天文季节、热带和高纬度的日照、月中日照和日历日照的差异作了一些评论。描述了间冰期海洋同位素阶段(MIS1~MIS11)的日照特征,并讨论了它们的共同特征。
The main insolation parameters are reviewed, in particular the energy received by the whole Earth over a full year and the 24-hour mean irradiance. Their spectral characteristics are underlined, and some remarks are made about the differences between insolation at the top of the atmosphere and at the Earth's surface, the caloric and the astronomical seasons, the insolations in the tropical and in the high latitudes, the mid-month and the calendar insolations. The insolations characterizing interglacials marine isotope stage (MIS) 1 to MIS 11 are described, and their common features are discussed.