Lake area and volume variation data in the endorheic basin of the Tibetan Plateau from 1989 to 2019

Junxiao Wang, Liuming Wang, Mengyao Li, Liping Zhu, Xingong Li
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引用次数: 3

Abstract

Abstract. The Tibetan Plateau, known as "the third pole of the Earth", is a region susceptible to climate change. With little human disturbance, lake storage changes serve as a unique indicator of climate change, but comprehensive lake storage data are rare in the region, especially for the lakes with an area less than 10 km2 which are the most sensitive to environmental changes. In this paper, we completed a census of annual lake volume change for 976 lakes larger than 1 km2 in the endorheic basin of the Tibetan Plateau (EBTP) during 1989–2019 using Landsat imagery and digital terrain models. Validation and comparison with several existing studies indicate that our data are more reliable. Lake volume in the EBTP exhibited a net increase of 193.45 km3 during the time period with an increasing rate of 6.45 km3 year−1. In general, the larger the lake area, the greater the lake volume change, though there are some exceptions. Lakes with an area less than 10 km2 have more severe volume change whether decreasing or increasing. This research complements existing lake studies by providing a comprehensive and long-term lake volume change data for the region. The dataset is available on Zenodo ( https://doi.org/10.5281/zenodo.5543615 , Wang et al., 2021).
1989 - 2019年青藏高原内陆河流域湖泊面积和体积变化数据
摘要被称为“地球第三极”的青藏高原是一个易受气候变化影响的地区。在人为干扰较小的情况下,湖泊蓄水量变化是气候变化的独特指标,但该地区湖泊蓄水量的综合数据较少,特别是对环境变化最敏感的面积小于10 km2的湖泊。本文利用陆地卫星图像和数字地形模型,对1989-2019年青藏高原内陆河流域976个大于1 km2的湖泊进行了湖泊体积变化的普查。与几个现有研究的验证和比较表明,我们的数据更可靠。在此期间,青藏高原湖泊体积净增加193.45 km3,年增长率为6.45 km3。一般来说,湖泊面积越大,湖泊体积变化越大,尽管也有一些例外。面积小于10平方公里的湖泊,无论是减少还是增加,其体积变化都更为剧烈。本研究补充了现有的湖泊研究,为该地区提供了全面和长期的湖泊体积变化数据。该数据集可在Zenodo上获得(https://doi.org/10.5281/zenodo.5543615, Wang et al., 2021)。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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