Rapid development of thermokarst lakes and driving factors along a highway in Northeast China (2000–2020)

IF 3.5 4区 地球科学 Q4 GEOGRAPHY, PHYSICAL
Research in Cold and Arid Regions Pub Date : 2026-04-01 Epub Date: 2025-03-12 DOI:10.1016/j.rcar.2025.03.004
JunHe Liang , Shuai Huang , XiaoYing Jin , XiaoYing Li , AnYuan Li , Lin Yang , WenHui Wang , JianJun Tang , Ze Zhang , YongPing Wang , ShanZhen Li , XiangLong Li , JinBang Zhai , Xue Yang , HongWei Wang , LanZhi Lü , RuiXia He , Raul-David Şerban , HuiJun Jin
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引用次数: 0

Abstract

In the northern Da Xing'anling Mountains of Northeast China, thermokarst lakes have undergone significant changes. These changes are particularly evident along the Highway X302, which stretches from Yakeshi in the south to Yitulihe in the north, across zones of discontinuous to patchy Xing'an permafrost (XAP). Thermokarst lakes are highly sensitive to both climate warming and human activities. However, changes in their areal extent and number over the past two decades remain unclear. To identify the drivers of thermokarst lake changes in the XAP region, this study analyzes the relationship among lake dynamics, climate change, and human activities. Rich data on lake changes were extracted using the modified normalized difference water index (MNDWI) from the Google Earth Engine (GEE) and verified against the Joint Research Centre (JRC) global surface water datasets. The results show a net increase in both the number and areal extent of thermokarst lakes along the Highway X302 from 2000 to 2020. Larger lakes (greater than 0.01 km2) expanded in surface area. Meanwhile, smaller lakes (less than 0.01 km2) increased in number. A bell-shaped trend was observed, with an initial increase in lake area followed by a decline around 2013. Before 2013, climate factors such as precipitation, air temperature, and potential evapotranspiration (PET) strongly influenced lake changes. After 2013, annual precipitation became the dominant driver of lake expansion. Human activities also contributed to changes in permafrost thermal regimes, further influencing lake dynamics. These findings provide valuable insights into the management of thermokarst lakes and wetlands in the region, and offer a reference for mitigating frost-related hazards along the Highway X302.
东北高速公路沿线热岩溶湖快速发展及其驱动因素分析(2000-2020年)
在东北大兴安岭北部,热岩溶湖泊发生了显著的变化。这些变化在X302高速公路沿线尤其明显,这条公路从南部的雅克石延伸到北部的伊图里河,穿过不连续的区域到零散的兴安永久冻土带(XAP)。热岩溶湖对气候变暖和人类活动都非常敏感。然而,它们的面积范围和数量在过去二十年中的变化仍不清楚。为了确定XAP地区热岩溶湖泊变化的驱动因素,本文分析了湖泊动态、气候变化和人类活动之间的关系。利用谷歌地球引擎(GEE)的修正归一化差水指数(MNDWI)提取了丰富的湖泊变化数据,并与联合研究中心(JRC)全球地表水数据集进行了验证。结果表明:2000 ~ 2020年,X302高速公路沿线热岩溶湖数量和面积均呈净增加趋势;较大的湖泊(大于0.01平方公里)表面积扩大。与此同时,较小的湖泊(小于0.01平方公里)数量增加。2013年前后湖泊面积呈钟形变化趋势,呈先增大后减小的趋势。2013年以前,降水、气温、潜在蒸散(PET)等气候因子对湖泊变化影响较大。2013年以后,年降水量成为湖泊扩张的主导驱动力。人类活动还导致了永久冻土热状态的变化,进一步影响了湖泊动态。这些发现为该地区热岩溶湖泊和湿地的管理提供了有价值的见解,并为减轻X302高速公路沿线的霜冻相关灾害提供了参考。
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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