Abstract
Chronologically-secure volcanic event histories are important for improving our understanding of volcano-climate responses, and securing ice core chronologies. We present an exploratory case-study that attempts to reconcile the chemical fingerprints of major volcanism in Greenland ice-cores for the years 670-730 CE. This period experienced considerable volcanic perturbation with multiple volcanic signals registered in all 8 Greenland ice-core datasets studied, including some comparable in magnitude to the great 1815 Tambora eruption, but reconciling signals with divergent dating between datasets presents a number of challenges. To further our understanding of the volcanic history of this period, frost-rings, tree-ring growth width and density minima from Europe, Siberia and China are considered together with Western European, Near Eastern and Chinese documentary evidence. These reveal a striking sequence of co-occurring inter-regional climatic extremes and social crises. We further examine a recently proposed 7-year adjustment to the GICC05 chronology used by many Greenland ice cores, and find that this results in a more coherent volcanic history for these years, and an improved agreement with tree-ring and written records. Three major volcanic events can now be identified, dated to 681, 684 -686 and 706-707, with several moderate events further contributing to a sustained climate perturbation reflected in prolonged temperature reductions in high-resolution reconstructions. (C) 2015 Elsevier Ltd and INQUA. All rights reserved.
Dokumententyp: | Zeitschriftenartikel |
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Fakultätsübergreifende Einrichtungen: | Nanosystems Initiative Munich (NIM) |
Themengebiete: | 500 Naturwissenschaften und Mathematik > 530 Physik |
ISSN: | 1040-6182 |
Sprache: | Englisch |
Dokumenten ID: | 49081 |
Datum der Veröffentlichung auf Open Access LMU: | 27. Apr. 2018, 08:16 |
Letzte Änderungen: | 04. Nov. 2020, 13:26 |