YANG, Bao, Chun QIN, Achim BRAUNING, Timothy J. OSBORN, Valerie TROUET, Fredrik Charpentier LJUNGQVIST, Jan ESPER, Lea SCHNEIDER, Jussi GRIESSINGER, Ulf BÜNTGEN, Sergio ROSSI, Guanghui DONG, Mi YAN, Liang NING, Jianglin WANG, Xiaofeng WANG, Beixi FAN, Suming WANG, Jürg LUTERBACHER, Edward R. COOK and Nils Chr. STENSETH. Reply to Weiss: Tree-ring stable oxygen isotopes suggest an increase in Asian monsoon rainfall at 4.2 ka BP. Proceedings of the National Academy of Sciences of the United States of America. National Academy of Sciences, 2022, vol. 119, No 20, p. 1-3. ISSN 0027-8424. Available from: https://dx.doi.org/10.1073/pnas.2204067119.
Other formats:   BibTeX LaTeX RIS
Basic information
Original name Reply to Weiss: Tree-ring stable oxygen isotopes suggest an increase in Asian monsoon rainfall at 4.2 ka BP
Authors YANG, Bao, Chun QIN, Achim BRAUNING, Timothy J. OSBORN, Valerie TROUET, Fredrik Charpentier LJUNGQVIST, Jan ESPER, Lea SCHNEIDER, Jussi GRIESSINGER, Ulf BÜNTGEN (276 Germany, belonging to the institution), Sergio ROSSI, Guanghui DONG, Mi YAN, Liang NING, Jianglin WANG, Xiaofeng WANG, Beixi FAN, Suming WANG, Jürg LUTERBACHER, Edward R. COOK and Nils Chr. STENSETH.
Edition Proceedings of the National Academy of Sciences of the United States of America, National Academy of Sciences, 2022, 0027-8424.
Other information
Original language English
Type of outcome Article in a journal
Field of Study 10500 1.5. Earth and related environmental sciences
Country of publisher United States of America
Confidentiality degree is not subject to a state or trade secret
WWW URL
Impact factor Impact factor: 11.100
RIV identification code RIV/00216224:14310/22:00127016
Organization unit Faculty of Science
Doi http://dx.doi.org/10.1073/pnas.2204067119
UT WoS 000854008900015
Keywords in English tree rings; monsoon; rainfall; Asian; oxygen isotope
Tags rivok
Tags International impact, Reviewed
Changed by Changed by: Mgr. Marie Šípková, DiS., učo 437722. Changed: 25/10/2022 15:56.
Abstract
Weiss (1) raises interesting points on our article (2). He observes that the Delingha tree-ring δ18O record matches KM-A speleothem δ18O record from the Mawmluh Cave in India, that defines the 4.2-ka event’s global-type stratum (3). This event is also manifested as a multicentennial drought in the Iranian Gol-E-Zard speleothem record (4). Weiss further argues that the Delingha record is also consistent with the 4.2-ka anomaly recorded in low-resolution proxy records from northern China despite inherent limitations of these proxies.
PrintDisplayed: 4/10/2024 16:44