Long-Term Lake Area Change and Its Relationship with Climate in the Endorheic Basins of the Tibetan Plateau

Lakes are sensitive indicators of climate change in the Tibetan Plateau (TP), which have shown high temporal and spatial variability in recent decades. The driving forces for the change are still not entirely clear. This study examined the area change of the lakes greater than 1 km 2 in the endorhei...

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Bibliographic Details
Published in:Remote Sensing
Main Authors: Junxiao Wang, Mengyao Li, Liuming Wang, Jiangfeng She, Liping Zhu, Xingong Li
Format: Article in Journal/Newspaper
Language:English
Published: MDPI AG 2021
Subjects:
remote sensing
Landsat
monsoon system
El Niño/La Niña events
Science
Q
Indian
North Atlantic
North Atlantic oscillation
Online Access:https://doi.org/10.3390/rs13245125
https://doaj.org/article/51d6adbfc22647f2bbb9b596fbff4b90
Description
Summary:Lakes are sensitive indicators of climate change in the Tibetan Plateau (TP), which have shown high temporal and spatial variability in recent decades. The driving forces for the change are still not entirely clear. This study examined the area change of the lakes greater than 1 km 2 in the endorheic basins of the Tibetan Plateau (EBTP) using Landsat images from 1990 to 2019, and analysed the relationships between lake area and local and large-scale climate variables at different geographic scales. The results show that lake area in the EBTP has increased significantly from 1990 to 2019 at a rate of 432.52 km 2 ·year −1 . In the past 30 years, lake area changes in the EBTP have mainly been affected by local climate variables such as precipitation and temperature. At a large scale, Indian Summer Monsoon (ISM) has correlations with lake area in western sub-regions in the Inner Basin (IB). While Atlantic Multidecadal Oscillation (AMO) has a significant connection with lake area, the North Atlantic Oscillation (NAO) does not. We also found that abnormal drought (rainfall) brought by the El Niño/La Niña events are significantly correlated with the lake area change in most sub-regions in the IB.

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