![]() Have been confirmed with tephra preserved in ice cores. None of the candidate volcanoes for the mid-17th century sulfate peaks Potentially attributed to the eruptions of Hekla (63 ∘ N, Iceland)Īnd Shiveluch (56 ∘ N, Russia), respectively. Has potentially also contributed to the sulfate concentrations observed in Mount Parker (6 ∘ N, Philippines) on 26 December 1640, but sulfateĮmitted from Komaga-take (42 ∘ N, Japan) volcano on 31 July 1641 The resultingīipolar sulfur peak in 1641–1642 can likely be ascribed to the eruption of Unambiguous sulfate spike is recorded, peaking in 1642. Three distinct sulfur peaks are found in the Greenland Socio-political context in which they occurred and the human responses they This contribution investigates the sources of the eruptions of the 1630s and 1640s and their possible impact on contemporary climate using ice core, tree-ring, and historical evidence but will also look into the ![]() Of explosive volcanic eruptions in the 1630s and 1640s, climatic conditionsĬulminating in the Maunder Minimum, and political instability andįamine in regions of western and northern Europe as well as China and Japan. The mid-17th century is characterized by a cluster ![]()
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