Identification of the impact of climate change and human activities on rainfall-runoff relationship variation in the Three-River Headwaters region

•The rainfall-runoff relationship has changed under climate change and human activities in the TRH region.•The impacts climate indicators of rainfall-runoff ratio in the sub-basins of TRH region were different.•The contribution rates of human activity in the YRB were a little higher than that in the...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Ecological indicators 2019-11, Vol.106, p.105516, Article 105516
Hauptverfasser: Chu, Haibo, Wei, Jiahua, Qiu, Jun, Li, Qiong, Wang, Guangqian
Format: Artikel
Sprache:eng
Schlagworte:
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
Beschreibung
Zusammenfassung:•The rainfall-runoff relationship has changed under climate change and human activities in the TRH region.•The impacts climate indicators of rainfall-runoff ratio in the sub-basins of TRH region were different.•The contribution rates of human activity in the YRB were a little higher than that in the YARB. Identifying the impact of climate change and human activities on rainfall-runoff relationship in the Three-River Headwaters (TRH) region is essential for water source conservation, ecological security, and biodiversity maintenance of China and East Asia. In this paper, the runoff-rainfall ratio was used as the index of rainfall-runoff relationship. Different methods were employed to identify the impact indicators and quantitative assessment of rainfall-runoff relationship from 1957 to 2016. The results are the following: (1) the rainfall-runoff relationship has changed in the source regions of Yangtze River basin (YARB) and Yellow River (YRB), and runoff-rainfall ratio has increased by 2.9% and decreased by 3.2%, respectively; (2) the main climate indicators of runoff-rainfall ratio were rainfall, potential evaporation and sunshine hours in the YARB, and rainfall, potential evaporation and temperature in the YRB; (3) the contribution rates of human activity in the YRB were a little higher than that in the YARB, and the contribution rates of climate change and human activity were 90.9% and 9.1% in the YARB and 42.9% and 57.1% in the YRB. The results can provide invaluable information for managing water resources and taking ecological protection measures.
ISSN:1470-160X
1872-7034
DOI:10.1016/j.ecolind.2019.105516