Abstract
Holocene climate was strongly determined by changing solar insolation (millennial scale) as well as by changing solar activity, large tropical volcanic eruptions, and the dynamics of the ocean thermohaline circulation (multi-decadal to multi-century scale).
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APA
Wanner, H. (2014). Holocene climate. In Global Environmental Change (pp. 55–59). Springer Netherlands. https://doi.org/10.1007/978-94-007-5784-4_28
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