Abstract
The source of external forces on the earth surface is solar activity. In the short time scale, direct solar activity may be more related to external forcing, whereas solar radiation (insolation) is essential in the long time scale. Galaxy cosmic ray was addressed in the recent discussions on the effect of solar activity on climate. The Milankovitch forcing have been also discussed with the long-term climatic changes related to landform changes. Long-term external forcing (Milankovitch cycles) has been recorded in long lacustrine sediments of Lake Baikal and Lake Biwa, showing different responses to the forcing due to the environmental conditions.
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Kashiwaya, K. (2017). Long-Term External Forcing and Limnogeomorphology. In: Geomorphology of Lake-Catchment Systems. Environmental Earth Sciences. Springer, Singapore. https://doi.org/10.1007/978-981-10-5110-4_9
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