Runoff reconstruction for the Bailong River from tree rings back to AD 1601, reveals changing hydrological signals of China north–south transition zone-Reference-Cited by-同舟云学术

Runoff reconstruction for the Bailong River from tree rings back to AD 1601, reveals changing hydrological signals of China north–south transition zone

Published:2021-11 Issue:11 Volume:35 Page:
ISSN:0885-6087
Container-title:Hydrological Processes
language:en
Short-container-title:Hydrological Processes

Author:

Gao Zhihong¹,Chen Feng¹²^ORCID,Fang Keyan³

Affiliation:

1. Yunnan Key Laboratory of International Rivers and Transboundary Eco‐Security, Institute of International Rivers and Eco‐Security Yunnan University Kunming China

2. Key Laboratory of Tree‐ring Physical and Chemical Research of China Meteorological Administration/Xinjiang Laboratory of Tree‐ring Ecology, Institute of Desert Meteorology China Meteorological Administration China

3. Key Laboratory of Humid Subtropical Eco‐geographical Process (Ministry of Education), College of Geographical Sciences Fujian Normal University Fuzhou China

Funder

National Natural Science Foundation of China

Publisher

Wiley

Subject

Water Science and Technology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/hyp.14417

Reference79 articles.

1. Reconstruction of the March–August PDSI since 1703 AD based on tree rings of Chinese pine (<i>Pinus tabulaeformis</i> Carr.) in the Lingkong Mountain, southeast Chinese loess Plateau

2. Warm season temperature in the Qinling Mountains (north-central China) since 1740 CE recorded by tree-ring maximum latewood density of Shensi fir

3. Reconstruction of a long streamflow record using tree rings in the upper Kurshab River (Pamir-Alai Mountains) and its application to water resources management