The Middle Bronze Age Cold Epoch was a period of unusually cold climate in the North Atlantic region that lasted about from 1800 BC to 1500 BC. [1] [2] It was followed by the Bronze Age Optimum (1500—900 BC).
During the Middle Bronze Age Cold Epoch, a series of severe volcanic eruptions occurred, including Mount Vesuvius ( Avellino eruption, about 1660 BC), [3] Mount Aniakchak (about 1645 BC), [4] and Thera ( Minoan eruption, about 1620 BC). [5]
References
- ^ Siklosy, Z.; et al. (2007). "Middle bronze age climate change recorded in a Hungarian stalagmite: triggering by volcanic activity?" (PDF). Geophysical Research Abstracts. 11 (777).
- ^ VINTHER, B., et al., 2009, “Holocene thinning of the Greenland ice sheet”, Nature, volume 461, (p 385-388). See: https://www.carbonbrief.org/factcheck-what-greenland-ice-cores-say-about-past-and-present-climate-change
- ^ Vogel, J. S.; et al. (1990). "Vesuvius/Avellino, one possible source of seventeenth century BC climatic disturbances". Nature. 344 (6266): 534–537. Bibcode: 1990Natur.344..534V. doi: 10.1038/344534a0. S2CID 4368499.
-
^ Pearce, N. J. G., J. A. Westgate, S. J. Preece, W. J. Eastwood, and W. T. Perkins (2004).
"Identification of Aniakchak (Alaska) tephra in Greenland ice core challenges the 1645 BC date for Minoan eruption of Santorini". Geochem. Geophys. Geosyst. 5 (3): Q03005.
Bibcode:
2004GGG.....5.3005P.
doi:
10.1029/2003GC000672.
{{ cite journal}}: CS1 maint: multiple names: authors list ( link) - ^ Friedrich, Walter L.; et al. (2006). "Santorini Eruption Radiocarbon Dated to 1627-1600 B.C.". Science. 312 (5773): 548. doi: 10.1126/science.1125087. PMID 16645088. S2CID 35908442.
 | This article about atmospheric science is a stub. You can help Wikipedia by expanding it. |
The Middle Bronze Age Cold Epoch was a period of unusually cold climate in the North Atlantic region that lasted about from 1800 BC to 1500 BC. [1] [2] It was followed by the Bronze Age Optimum (1500—900 BC).
During the Middle Bronze Age Cold Epoch, a series of severe volcanic eruptions occurred, including Mount Vesuvius ( Avellino eruption, about 1660 BC), [3] Mount Aniakchak (about 1645 BC), [4] and Thera ( Minoan eruption, about 1620 BC). [5]
References
- ^ Siklosy, Z.; et al. (2007). "Middle bronze age climate change recorded in a Hungarian stalagmite: triggering by volcanic activity?" (PDF). Geophysical Research Abstracts. 11 (777).
- ^ VINTHER, B., et al., 2009, “Holocene thinning of the Greenland ice sheet”, Nature, volume 461, (p 385-388). See: https://www.carbonbrief.org/factcheck-what-greenland-ice-cores-say-about-past-and-present-climate-change
- ^ Vogel, J. S.; et al. (1990). "Vesuvius/Avellino, one possible source of seventeenth century BC climatic disturbances". Nature. 344 (6266): 534–537. Bibcode: 1990Natur.344..534V. doi: 10.1038/344534a0. S2CID 4368499.
-
^ Pearce, N. J. G., J. A. Westgate, S. J. Preece, W. J. Eastwood, and W. T. Perkins (2004).
"Identification of Aniakchak (Alaska) tephra in Greenland ice core challenges the 1645 BC date for Minoan eruption of Santorini". Geochem. Geophys. Geosyst. 5 (3): Q03005.
Bibcode:
2004GGG.....5.3005P.
doi:
10.1029/2003GC000672.
{{ cite journal}}: CS1 maint: multiple names: authors list ( link) - ^ Friedrich, Walter L.; et al. (2006). "Santorini Eruption Radiocarbon Dated to 1627-1600 B.C.". Science. 312 (5773): 548. doi: 10.1126/science.1125087. PMID 16645088. S2CID 35908442.
|
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