Reply to Weiss: Tree-ring stable oxygen isotopes suggest an increase in Asian monsoon rainfall at 4.2 ka BP

0561661 - ÚVGZ 2023 RIV US eng J - Článek v odborném periodiku
Yang, B. - Qin, Ch. - Braeuning, A. - Osborn, T. J. - Trouet, V. - Ljungqvist, F. C. - Esper, J. - Schneider, L. - Griessinger, J. - Büntgen, Ulf - Rossi, S. - Dong, G. - Yan, M. - Ning, L. - Wang, J. - Wang, X. - Fan, B. - Wang, S. - Luterbacher, J. - Cook, E.R. - Stenseth, N.Ch.
Reply to Weiss: Tree-ring stable oxygen isotopes suggest an increase in Asian monsoon rainfall at 4.2 ka BP.
2022. Proceedings of the National Academy of Sciences of the United States of America. Roč. 119, č. 20 (2022), č. článku e2204067119. ISSN 0027-8424. E-ISSN 1091-6490
Výzkumná infrastruktura: CzeCOS III - 90123
Institucionální podpora: RVO:86652079
Klíčová slova: hydroclimate * tree-ring * monsoon rainfall
Obor OECD: Meteorology and atmospheric sciences
Impakt faktor: 11.1, rok: 2022
Způsob publikování: Open access
https://www.pnas.org/doi/full/10.1073/pnas.2204067119

Weiss raises interesting points on our article . Heobserves that the Delingha tree-ringδ18O record matchesKM-A speleothemδ18O record from the Mawmluh Cave inIndia, that defines the 4.2-ka event’s global-type stratum. This event is also manifested as a multicentennialdrought in the Iranian Gol-E-Zard speleothem record.Weiss further argues that the Delingha record is alsoconsistent with the 4.2-ka anomaly recorded in low-resolution proxy records from northern China despiteinherent limitations of these proxies.
Trvalý link: https://hdl.handle.net/11104/0334195