长江流域生长季NDVI对昼夜不对称增温及降水的响应

靖娟利, 唐兵, 赵婷, 欧红飞, 王永锋

中国环境科学 ›› 2025, Vol. 45 ›› Issue (10) : 5756-5768.

PDF(5466 KB)
PDF(5466 KB)
中国环境科学 ›› 2025, Vol. 45 ›› Issue (10) : 5756-5768.
环境生态

长江流域生长季NDVI对昼夜不对称增温及降水的响应

  • 靖娟利, 唐兵, 赵婷, 欧红飞, 王永锋
作者信息 +

Response of the NDVI to asymmetric diurnal temperature increases and precipitation changes during the growing season in the Yangtze River Basin

  • JING Juan-li, TANG Bing, ZHAO Ting, OU Hong-fei, WANG Yong-feng
Author information +
文章历史 +

摘要

长江流域作为关键的生态安全屏障,深入理解其生长季NDVI对气候变化的响应,对于长江流域生态环境保护策略的有效实施至关重要.本文利用2000~2020年MODIS NDVI数据以及同期气象数据,运用趋势分析法、偏相关分析等方法并结合GIS空间统计分析等方法,探讨了长江流域生长季NDVI对昼夜温度及降水的响应特征.结果表明:2000~2020年长江流域生长季NDVI整体呈波动增加趋势,增速为0.021/10a;除太湖流域外,其他子流域NDVI均呈极显著增加趋势.NDVI呈增加趋势的面积占比为84.19%,太湖流域超过60%的区域呈减少趋势,其余子流域以增加趋势为主.生长季Tmax、Tmin和降水量均呈不显著上升趋势,Tmin的增加速率约为Tmax的1.55倍,昼夜增温速率表现出不对称性,除金沙江流域外,其他子流域与研究区变化趋势相似.空间上,生长季Tmax、Tmin和降水量呈增加趋势的区域占比为68%~79%,以太湖和乌江流域增加趋势最为明显.生长季NDVI对Tmax、Tmin和降水量的响应表现出一定空间异质性,植被生长受Tmin和降水量显著影响的范围较Tmax更广泛.生长季NDVI对Tmin、降水量和Tmax的平均滞后响应时间分别为1.3个月、1.4个月和1.6个月;不同子流域及不同植被类型NDVI对Tmax、Tmin和降水量的响应有一定差异.

Abstract

The Yangtze River Basin is an important ecological barrier in China. Understanding the response of the NDVI to climate change during the growing season is important for the effective implementation of ecological and environmental protection strategies. In this study, on the basis of MODIS NDVI data and meteorological data from 2000 to 2020, the response of the NDVI to diurnal temperature and precipitation changes during the growing season was studied through trend analysis, partial correlation analysis and GIS spatial statistical analysis methods. The results revealed the following: from 2000~2020, the growing season NDVI exhibited a fluctuating increasing trend in the Yangtze River Basin, with a growth rate of 0.021/10a. The NDVI exhibited an increasing trend in all subbasins except for Taihu Lake. The overall NDVI exhibited an increasing trend, accounting for 84.19% of the study area, and all subbasins exhibited increasing trends, with the exception of the Taihu Basin, which showed a decreasing trend (60%). (2) During the growing season, Tmax, Tmin and precipitation showed insignificant upward trends, and the increase rate of Tmin was approximately 1.55 times that of Tmax, indicating asymmetric diurnal warming. At the subbasin scale, the change trend was similar to that in the study area except for the Jinsha River Basin. Spatially, Tmax, Tmin and precipitation showed increasing trends, with proportions ranging from 68% to 79%, especially in the Taihu and Wujiang River Basins. The responses of the NDVI to Tmax, Tmin and precipitation during the growing season exhibited spatial heterogeneity, and the range of vegetation growth significantly affected by Tmin and precipitation was greater than that affected by Tmax. The average lag times of the responses of the NDVI to Tmax, Tmin and precipitation during the growing season were 1.6, 1.3 and 1.4 months, respectively. The response characteristics differed across subbasins and vegetation types.

关键词

生长季NDVI / 昼夜增温 / 不对称变化 / 时滞效应 / 长江流域

Key words

growing season NDVI / diurnal temperature increase / asymmetric changes / time lag effect / Yangtze River Basin

引用本文

导出引用
靖娟利, 唐兵, 赵婷, 欧红飞, 王永锋. 长江流域生长季NDVI对昼夜不对称增温及降水的响应[J]. 中国环境科学. 2025, 45(10): 5756-5768
JING Juan-li, TANG Bing, ZHAO Ting, OU Hong-fei, WANG Yong-feng. Response of the NDVI to asymmetric diurnal temperature increases and precipitation changes during the growing season in the Yangtze River Basin[J]. China Environmental Science. 2025, 45(10): 5756-5768
中图分类号: X173   

参考文献

[1] Piao S L, Wang X H, Park T. et al. Characteristics, drivers and feedbacks of global greening [J]. Nature Reviews Earth & Environment, 2020,1(1):14-27.
[2] Cui L F, Wang Z D, Deng L H, et al. Vegetation dynamics and their relations with climate change at seasonal scales in the Yangtze River Basin, China [J]. Applied Ecology & Environmental Research, 2020, 18(2):3543-3556.
[3] 孙 颖.人类活动对气候系统的影响-解读IPCC第六次评估报告第一工作组报告第三章 [J]. 大气科学学报, 2021,44(5):654-657. Sun Y. Impact of humanactivities on climate system: an interpretation of Chapter Ⅲ of WGⅠreport of IPCC AR6 [J]. Transactions of Atmospheric Sciences, 2021,44(5):654-657.
[4] Vose R S, Easterling D R, Gleason B. Maximum and minimum temperature trends for the globe: an update through 2004 [J]. Geophys, 2005,32(23):L23822.
[5] Davy R, Esau I, Chernokulsky A, et al. Diurnal asymmetry to the observed global warming [J]. International Journal of Climatology, 2017,37(1):79-93.
[6] Peng S S, Piao S L, Ciais P, et al. Asymmetric effects of daytime and night-time warming on northern hemisphere vegetation [J]. Nature, 2013,501:88-94.
[7] Wan S Q, Xia J Y, Liu W X, et al. Photosynthetic overcompensation under nocturnal warming enhances grassland carbon sequestration [J]. Ecology, 2009,90(10):2700-2710.
[8] Zheng Z T, Zhang Y J, Zhu J T, et al. Daytime temperature contributes more than nighttime temperature to the weakened relationship between climate warming and vegetation growth in the extratropical northern hemisphere [J]. Ecological Indicators, 2021,131:108203.
[9] Zhu G F, Wang X F, Xiao J F, et al. Daytime and nighttime warming has no opposite effects on vegetation phenology and productivity in the northern hemisphere [J]. Science of the Total Environment, 2022, 822:153386.
[10] 赵 杰,杜自强,张 红,等.中国季节性昼夜增温的不对称性及其对植被活动的影响 [J]. 生态学报, 2018,38(11):3909-3919. Zhao J, Du Z Q, Zhang H, et al. Asymmetric seasonal variability in day-and night-time warming and their effects on vegetation activity in China [J]. Acta Ecologica Sinica, 2018,38(11):3909-3919.
[11] 赵 杰,刘雪佳,杜自强,等.昼夜增温速率的不对称性对新疆地区植被动态的影响 [J]. 中国环境科学, 2017,37(6):2316-2321. Zhao J, Liu X J, Du Z Q, et al. Effects of the asymmetric diurnal- warming on vegetation dynamics in Xinjiang [J]. China Environmental Science, 2017,37(6):2316-2321.
[12] Xu B N, Li J J, Pei X J, et al. Decoupling the response of vegetation dynamics to asymmetric warming over the Qinghai-Tibet plateau from 2001 to 2020 [J]. Journal of Environmental Management, 2023,347: 119131.
[13] 李 理,刘俊杰,赵 芳,等.昼夜不对称性增温对秦巴山地植被NDVI的影响研究 [J]. 地域研究与开发, 2023,42(1):161-166,173. Li L, Liu J J, Zhao F, et al. Effects of day and night asymmetric warming on different vegetation types in Qinling-Daba Mountains [J]. Areal Research and Development, 2023,42(1):161-166,173.
[14] Wang Y J, Shen X J, Jiang M, et al. Daytime and nighttime temperatures exert different effects on vegetation net primary productivity of marshes in the western Songnen plain [J]. Ecological Indicators, 2022,137:108789.
[15] 李忠良,何光鑫,李 勋.高寒气候区生长季NDVI与昼夜不对称增温的Copula分析 [J]. 大气科学学报, 2024,47(3):407-424. Li Z L, He G X, Li X. Copula analysis of NDVI and diurnal-nocturnal asymmetric warming during the growing season in typical plateau climatic region [J]. Transactions of Atmospheric Sciences, 2024,47(3): 407-424.
[16] Wen Y Y, Liu X P, Pei F S, et al. Non-uniform time-lag effects of terrestrial vegetation responses to asymmetric warming [J]. Agricultural and Forest Meteorology, 2018,252:130-143.
[17] 崔利芳,王伦澈,屈 赛,等.气温、降水量和人类活动对长江流域植被NDVI的影响 [J]. 地球科学, 2020,45(6):1905-1917. Cui L F, Wang L C, Qu S, et al. Impacts of temperature, precipitation and human activity on vegetation NDVI in Yangtze River Basin, China [J]. Earth Science, 2020,45(6):1905-1917.
[18] Zhang W, Wang L C, Xiang F F, et al. Vegetation dynamics and the relations with climate change at multiple time scales in the Yangtze River and Yellow River Basin, China [J]. Ecological Indicators, 2020, 110:105892.
[19] Stow D A, Hope A, McGuire D, et al. Remote sensing of vegetation and land-cover change in arctic tundra ecosystems [J]. Remote Sensing of Environment, 2004,89(3):281-308.
[20] 王永锋,靖娟利,刘海红,等.顾及时滞和累积效应的西南喀斯特地区植被变化归因分析 [J]. 环境科学, 2025,46(7):4382-4391. Wang Y F, Jing J L, Liu H H, et al. Attribution analysis of vegetation variation in the karst region of southwest China considering time lag and accumulation effects [J]. Environmental Science, 2025,46(7): 4382-4391.
[21] 易 浪,孙 颖,尹少华,等.2000~2019年长江流域植被覆盖时空演化及其驱动因素 [J]. 生态学报, 2023,43(2):798-811. Yi L, Sun Y, Yin S H, et al. Spatial-temporal variations of vegetation coverage and its driving factors in the Yangtze River Basin from 2000 to 2019 [J] Acta Ecologica Sinica, 2023,43(2):798-811.
[22] Ding Y X, Li Z, Peng S Z. Global analysis of time-lag and accumulation effects of climate on vegetation growth [J]. International Journal of Applied Earth Observation and Geoinformation, 2020,92: 102179.
[23] Ma M Y, Wang Q M, Liu R, et al. Effects of climate change and human activities on vegetation coverage change in northern China considering extreme climate and time-lag and accumulation effects [J]. Science of the Total Environment, 2023,860:160527.
[24] 崔浩楠,罗海江,张学珍.1982~2019年长江经济带植被覆盖变化的时空特征 [J]. 生态学杂志, 2021,40(8):2517-2529. Cui H N, Luo H H, Zhang X Z. Temporal and spatial characteristics of green vegetation cover changes in the Yangtze River Economic Belt from 1982 to 2019 [J]. Chinese Journal of Ecology, 2021,40(8):2517- 2529.
[25] Jia X Q, Fu B J, Feng X M, et al. The tradeoff and synergy between ecosystem services in the Grain-for-Green areas in Northern Shaanxi, China [J]. Ecological Indicators, 2014,43:103–113.
[26] Tong X W, Wang K L, Yue Y M, et al. Quantifying the effectiveness of ecological restoration projects on long-term vegetation dynamics in the karst regions of Southwest China [J]. International Journal of Applied Earth Observation and Geoinformation, 2017,54:105–113.
[27] Qu S, Wang L C, Lin A W, et al. What drives the vegetation restoration in Yangtze River Basin, China: Climate change or anthropogenic factors? [J]. Ecological Indicators, 2018,90:438-450.
[28] 覃庆锋,陈 晨,曾宪芷,等.长江流域防护林体系工程建设30年回顾与展望 [J]. 中国水土保持科学, 2018,16(5):145-152. Qin Q F, Chen C, Zeng X Z, et al. Review and prospect of protection forest system construction in the Yangtze River Basin in the past 30 years [J]. Science of Soil and Water Conservation, 2018,16(5):145- 152.
[29] Chen S S, Wen Z F, Zhang S L, et al. Effects of long-term and large-scale ecology projects on forest dynamics in Yangtze River Basin, China [J]. Forest Ecology and Management, 2021,496:119463.
[30] 张 亮,丁明军,张华敏,等.1982~2015年长江流域植被覆盖度时空变化分析 [J]. 自然资源学报, 2018,33(12):2084-2097. Zhang L, Ding M J, Zhang H M, et al. Spatiotemporal variation of the vegetation coverage in Yangtze River Basin during 1982~2015 [J]. Journal of Natural Resources, 2018,33(12):2084-2097.
[31] Yin J, Yao M Z, Yuan Z, et al. Spatial-temporal variations in vegetation and their responses to climatic and anthropogenic factors in upper reaches of the Yangtze River during 2000 to 2019 [J]. Watershed Ecology and the Environment, 2023,5:114–124.
[32] Solomon S, Qin D, Manning M, et al. Climate change 2007-the physical science basis: Working group I contribution to the fourth assessment report of the IPCC [M]. Cambridge university press, 2007.
[33] Yu LX, Liu Y, Yan FQ, et al. Vegetation-induced asymmetric diurnal land surface temperatures changes across global climate zones [J]. Science of the Total Environment, 2023,896:165255.
[34] Zhang S Q, Ren G Y, Zheng X, et al. Changes in the mean and extreme temperature in the Yangtze River Basin over the past 120 years [J]. Weather and Climate Extremes, 2023,40:100557.
[35] Zhang S Q, Ren G Y, Ren Y Y, et al. Linkage of extreme temperature change with atmospheric and locally anthropogenic factors in China mainland [J]. Atmospheric research, 2022,277:106307.
[36] Ma L Q, Xia H M, Meng Q M. Spatiotemporal variability of asymmetric daytime and night-time warming and its effects on vegetation in the Yellow River Basin from 1982 to 2015 [J]. Sensors, 2019,19:1832.
[37] Turnbull M H, Murthy R, Griffin K L. The relative impacts of day-time and night-time warming on photosynthetic capacity in Populus deltoides [J]. Plant Cell Environ, 2002,25:1729–1737.
[38] Melillo J M, Steudler P A, Aber J D, et al. Soil warming and carbon- cycle feedbacks to the climate system [J]. Science, 2022,298: 2173–2176.
[39] 焦珂伟,高江波,吴绍洪,等.植被活动对气候变化的响应过程研究进展 [J]. 生态学报, 2018,38(6):2229-2238. Jiao K W, Gao J B, Wu S H, et al. Research progress on the response processes of vegetation activity to climate change [J]. Acta Ecologica Sinica, 2018,38(6):2229-2238.
[40] 梁春玲,于泉洲,刘煜杰,等.昼夜增温对南四湖湿地植被NDVI的影响差异 [J]. 热带地理, 2015,35(3):422-426,436. Liang C L, Yu Q Z, Liu Y J, et al. Effects of air temperature circadian on the NDVI of Nansi Lake wetland vegetation [J]. Tropical Geography, 2015,35(3):422-426,436.
[41] Su H X, Feng J C, Axmacher J C, et al. Asymmetric warming significantly affects net primary production, but not ecosystem carbon balances of forest and grassland ecosystems in northern China [J]. Scientific Reports, 2015,5:9115.
[42] 王逸玮,赵 林,刘广岳,等.青藏高原沱沱河源多年冻土区NDVI时空变化及影响因素分析 [J]. 冰川冻土, 2024,46(4):1386-1402. Wang Y W, Zhao L, Liu G Y, et al. Analysis of spatiotemporal changes and influencing factors of NDVI in the permafrost area of the Tuotuo River source area on the Qinghai-Xizang Plateau [J]. Journal of Glaciology and Geocryology, 2024,46(4):1386-1402.
[43] 武丹丹,井 新,林 笠,等.青藏高原高寒草甸土壤无机氮对增温和降水改变的响应 [J]. 北京大学学报:自然科学版, 2016,52(5):959- 966. Wu D D, Jing X, Lin L, et al. Responses of soil inorganic nitrogen to warming and altered precipitationin an alpine meadow on the Qinghai- Tibetan Plateau [J]. Acta Scientiarum Naturalium Universitatis Pekinensis, 2016,52(5):959-966.
[44] Ding Y, Xu J, Wang X, et al. Spatial and temporal effects of drought on Chinese vegetation under different coverage levels. Science of the Total Environment, 2020,716:137166.doi:10.1016/j.scitotenv.2020. 137166.
[45] 马炳鑫,和彩霞,靖娟利,等.1982~2019年中国西南地区植被变化归因研究 [J]. 地理学报, 2023,78(3):714-728. Ma B X, He C X, Jing J L, et al. Attribution of vegetation dynamics in Southwest China from 1982 to 2019 [J]. Acta Geographica Sinica, 2023,78(3):714-728.
[46] 徐 勇,盘钰春,邹 滨,等.定量评估气候变化对长江中下游地区植被GPPGS变化的影响 [J]. 环境科学, 2024,45(3):1615-1628. Xu Y, Pan Y C, Zou B, et al. Quantitative assessment of the impact of climate change on the growing season of vegetation gross primary productivity in the middle and lower reaches of the Yangtze River [J]. Environmental Science, 2024,45(3):1615-1628.
[47] 张峰源,苏远航,刘滨辉.东北森林生长季NDVI对昼夜不对称增温及降水变化的响应特征 [J]. 北京林业大学学报, 2023,45(2):34-48. Zhang F Y, Su Y H, Liu B H. Response characteristics of NDVI to asymmetric diurnal temperature increase and precipitation changes during the forest growing season in Northeast China [J]. Journal of Beijing Forestry University, 2023,45(2):34-48.
[48] 张钧泳,丁建丽,黄 帅,等.新疆自然植被对非对称性昼夜增温的时滞响应 [J]. 中国环境科学, 2020,40(1):392-400. Zhang J Y, Ding J L, Huang S, et al. Time lags responses of terrestrial natural vegetation to asymmetric diurnal warming in Xinjiang [J]. China Environmental Science, 2020,40(1):392-400.
[49] Wu Z J, Yao F M, Ahmad A, et al. Spatiotemporal evolution and driving mechanisms of kNDVI in different sections of the Yangtze River Basin using multiple statistical methods and the PLSPM model [J]. Remote Sensing. 2025,17:299.

基金

国家自然科学基金资助项目(42161028)

PDF(5466 KB)