首页|2000-2022年长江流域地表温度时空变化特征研究

2000-2022年长江流域地表温度时空变化特征研究

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地表温度(land surface temperature,LST)是地表和大气能量交互的重要媒介,在维持两者动态平衡中起着重要调节作用.长江流域作为中国综合发展水平较高的地区之一,近年来夏季LST上升日益显著.利用多源数据集,如MODIS数据和气象数据,揭示了 2000-2022年长江流域夏季LST时空变化、影响因素及热环境特征.结果显示:过去23年长江流域夏季平均LST呈显著上升.LST超过80%的地区有上升趋势,其中显著和极显著上升的区域约占整个流域的31.34%,显著和极显著下降趋势占0.37%.长江流域LST变化趋势具有明显的地域差异性,在中游和下游尤其明显.促使LST出现增长趋势的原因可能与NDVI和气候因子有关.NDVI是LST变化的主导驱动因素,以抑制LST上升为主.气温与降水对LST影响次之,前者以正主导为主,后者则以负主导为主.一定程度上,日照的增长和相对湿度的减少提高了 LST,而风速的增长会导致LST下降.长江流域LST未来在不同情景下的增长速率存在差异,但整体上均呈极显著上升(P<0.01).且在高排放情景下增长更显著.本研究结果有助于深入了解长江流域热环境的时空变化及其潜在驱动因素,为区域管理者提供应对高温的决策支持.
Study on the Temporal and Spatial Variation Characteristics of Surface Temperature in the Yangtze River Basin From 2000 to 2022
Land surface temperature(LST)is an important medium for the interaction between surface and at-mospheric energy,and plays an important role in maintaining the dynamic balance between the two.As one of the regions with a high level of comprehensive development in China,the summer LST in the Yangtze River Basin has increased significantly in recent years.In this study,multi-source data sets,such as MODIS data,meteoro-logical data and statistical data,were used to reveal the spatial and temporal changes,influencing factors and ther-mal environment characteristics of summer LST in the Yangtze River Basin from 2000 to 2022.The results show that the average summer LST in the Yangtze River Basin has increased significantly in the past 23 years.There is an upward trend in more than 80%of the areas with LST,of which the areas with significant and extremely sig-nificant increases account for about 31.34%of the entire basin,and the significant and extremely significant downward trends account for 0.37%.The variation trend of LST in the Yangtze River Basin has obvious regional differences,especially in the middle and lower reaches.The reason for the growth trend of LST may be related to NDVI and climatic factors.NDVI is the dominant driving factor of LST change,mainly to inhibit the rise of LST.The influence of temperature and precipitation on LST is the second.The former is dominated by positive,while the latter is dominated by negative.To a certain extent,the increase of sunshine and the decrease of relative hu-midity increase LST,while the increase of wind speed leads to the decrease of LST.The growth rate of LST in the Yangtze River Basin in the future is different under different scenarios,but the overall increase is extremely sig-nificant(P<0.01).And the growth is more significant under high emission scenarios.The results of this study are helpful to understand the spatial and temporal changes of thermal environment in the Yangtze River Basin and its potential driving factors,and provide decision support for regional managers to cope with high temperature.

land surface temperaturetemporal and spatial changesdriving forceYangtze River Basinfuture trends

郭贤、张玉平、张永灵、符静

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衡阳师范学院地理与旅游学院,湖南衡阳 421002

湖南环境生物职业技术学院公共基础课部,湖南衡阳 421005

地表温度 时空变化 驱动力 长江流域 未来趋势

2024

绿色科技
花木盆景杂志社

绿色科技

影响因子:0.365
ISSN:1674-9944
年,卷(期):2024.26(17)