大气与环境光学学报 ›› 2025, Vol. 20 ›› Issue (4): 503-519.doi: 10.3969/j.issn.1673-6141.2025.04.008

• 光学遥感 • 上一篇    下一篇

热环境下高原湖泊水体冷岛效应机制分析

何志斌 1, 姜永利 1, 王盼 1,2, 杨晓娇 1, 赵芮 1, 郝英杰 1*   

  1. 1 云南省生态环境工程评估中心, 云南 昆明 650228; 2 昆明理工大学环境科学与工程学院, 云南 昆明 650500
  • 收稿日期:2023-05-18 修回日期:2023-09-09 出版日期:2025-07-28 发布日期:2025-07-25
  • 通讯作者: E-mail: 491783083@qq.com E-mail:643839467@qq.com
  • 作者简介:何志斌 (1994- ), 云南曲靖人, 硕士, 工程师, 主要从事生态环境与地理信息方面的研究。E-mail: 643839467@qq.com
  • 基金资助:
    省级部门决策咨询研究课题 (ZFKKT-2021-060)

Mechanism analysis of cold island effect in plateau lake gathering area in thermal environment

HE Zhibin 1, JIANG Yongli 1, WANG Pan 1,2, YANG Xiaojiao 1, ZHAO Rui 1, HAO Yingjie 1*   

  1. 1 Yunnan Appraisal Center for Ecological and Environmental Engineering, Kunmin 650228, China; 2 College of Environmental Science and Engineering, Kunming University of Science and Technology, Kunmin 650500, China
  • Received:2023-05-18 Revised:2023-09-09 Online:2025-07-28 Published:2025-07-25
  • Contact: 何志斌 HE Zhin-bin E-mail:643839467@qq.com

摘要: 为了研究高原湖泊水体的冷岛效应机制, 以云南玉溪抚仙湖、星云湖、杞麓湖为研究对象, 首先基于遥感技术 完成了2015、2017、2019、2021 年该研究区的地表温度反演, 并运用地理信息技术对湖泊区域进行温度等级划分;在此 基础上, 对湖泊的降温范围、降温强度的时空变化特征进行分析, 并利用社会科学统计分析软件 (SPSS) 对温度和多个 景观指数进行相关性分析以判断温度变化影响因素; 最终, 创新采用岭回归分析构建拟合模型。结果表明: (1) 2015 ―2021 年间该研究区的高温区、次高温区面积均呈现先升后降的态势, 低温区与次低温区的面积变化与前者相反, 中 温区面积持续减少; (2) 抚仙湖降温范围约为水体边线外扩150~200 m之间, 星云湖与杞麓湖降温范围约为水体边线 外扩100~150 m之间, 抚仙湖、星云湖、杞麓湖各自的平均降温强度约为7.5、5.5、5.4 ℃; (3) 抚仙湖的冷岛效应受水体 分布、植被分布和建筑分布影响显著, 杞麓湖则受水体分布、植被分布和距离因素影响显著, 星云湖受全部因素影响 显著; (4) 岭回归关系模型的分析结果表明模型估算值与反演值的拟合度指数R2均高于0.8, 拟合度与精度检验结果均 在可接受范围内。总之, 本工作发现被研究的湖泊区域地表温度呈现高温与低温的两极分化态势, 植被、建筑、水体、 距离对湖泊冷岛效应均有影响, 并且基于岭回归分析的温度拟合方法具有实操性。

关键词: 冷岛效应, 高原湖泊, 温度反演, 岭回归分析

Abstract: In order to investigate the mechanism of cold island effect in plateau lakes, Fuxian Lake, Xingyun Lake and Qilu Lake in Yuxi, Yunnan Province, China, were taken as research objects. Firstly, the land surface temperature inversion of the study area in 2015, 2017, 2019 and 2021 was completed based on remote sensing technology, and Geographic Information System (GIS) technology was used to classify the temperature of the lake region. Then on this basis, the temporal and spatial variation characteristics of the cooling range and cooling intensity of the lakes were analyzed, and Statistical Package for the Social Sciences (SPSS) was used to analyze the correlation between temperature and multiple landscape indices to determine the influencing factors of temperature change. Finally, ridge regression analysis was innovatively adopted to build a fitting model. The results showed that: (1) From 2015 to 2021, the areas of high temperature and sub high temperature zones increased firstly and then decreased, while the areas of low temperature and sub low temperature zones were opposite to the former, and the area of middle temperature zone continued to decrease. (2) The cooling range of Fuxian Lake was about 150–200 m beyond the water boundary, and the cooling ranges of Xingyun Lake and Qilu Lake were about 100–150 m beyond the water boundary. The average cooling intensity of Fuxian Lake, Xingyun Lake and Qilu Lake is about 7.5 ℃, 5.5 ℃ and 5.4 ℃ respectively. (3) The cold island effect of Fuxian Lake was significantly affected by water distribution, vegetation distribution and building distribution, while that of Qilu Lake was significantly affected by water distribution, vegetation distribution and distance factors, and that of Xingyun Lake is significantly affected by all factors. (4) The results of ridge regression relationship model showed that the fitting index R2 of the estimated value of the model and the inversion value are all above 0.8, indicating that the fit degree and the accuracy test results are within an acceptable range. In brief, the surface temperature in the studied lake region presented a polarizing trend of high temperature and low temperature, and vegetation, architecture, water body and distance all had influence on the cold island effect of the lakes. Moreover, the temperature fitting method based on ridge regression analysis demonstrated its practical applicability.

Key words: cold island effect, plateau lake, temperature inversion, ridge regression analysis

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