1. 新疆师范大学地理科学与旅游学院,乌鲁木齐,830054
2. 新疆干旱区湖泊环境与资源实验室,乌鲁木齐,830054
[ "方登先(1994—),女,在读硕士研究生,主要从事干旱区资源利用与环境演变研究。E-mail:1336684770@qq.com" ]
纸质出版:2023
移动端阅览
方登先, 王勇辉. 夏尔希里自然保护区生长季NDVI变化特征及驱动力研究[J]. 水土保持学报, 2023,37(2):127-135.
FANG Dengxian, WANG Yonghui. Study on Variation Characteristics and Driving Forces of NDVI During Growing Season in Xarxili Nature Reserve[J]. 2023, 37(2): 127-135.
方登先, 王勇辉. 夏尔希里自然保护区生长季NDVI变化特征及驱动力研究[J]. 水土保持学报, 2023,37(2):127-135. DOI: 10.13870/j.cnki.stbcxb.2023.02.016.
FANG Dengxian, WANG Yonghui. Study on Variation Characteristics and Driving Forces of NDVI During Growing Season in Xarxili Nature Reserve[J]. 2023, 37(2): 127-135. DOI: 10.13870/j.cnki.stbcxb.2023.02.016.
采用趋势分析、相关分析、多元线性回归等方法
系统研究了夏尔希里自然保护区成立前(1990—2005年)和成立后(2006—2018年)不同植被类型归一化植被指数(NDVI)的时空变化特征及驱动NDVI变化的主要因素。结果表明:(1)不同海拔梯度上
保护区成立后的NDVI多年平均值均高于成立前;(2)保护区成立前后NDVI趋势均以增加为主
成立后NDVI的增加趋势为0.05~0.10/10 a的像元数量明显比成立前增多;(3)保护区成立前后大部分区域的NDVI均与气温呈现显著负相关
与降水呈现显著正相关(p<0.05)。(4)气温抑制低海拔(500~1 500 m)草地生长
降水促进中海拔(1 500~2 000 m)的植被生长
土壤有机碳、气温共同驱动高海拔(2 000~3 000 m)的植被生长。
By using the methods of trend analysis
correlation analysis and multiple linear regression
this paper systematically studied the temporal and spatial variation characteristics and the main driving factors of normalized vegetation index (NDVI) of different vegetation types changed in the establishment of Xarxili Nature Reserve before (1990—2005) and after (2006—2018).The results showed that:(1) At different altitude gradients
the annual mean of NDVI after the establishment of the nature reserve was higher than that before.(2) The trend of NDVI before and after the establishment of the NDVI was mainly increased.After the establishment of the reserve
the increasing trend of NDVI was 0.05 to 0.10/10 years
the number of pixels was significantly increased compared with that before the establishment.(3) The NDVI in most areas showed a significant negative correlation with air temperature and a significant positive correlation with precipitation (p<0.05).(4) Temperature inhibited the growth of grassland at low altitude (500~1 500 m)
precipitation promoted the growth of vegetation at middle altitude (1 500~2 000 m)
and soil organic carbon and air temperature jointly drove the growth of vegetation at high altitude (2 000~3 000 m).
Thuiller W, Lavorel S, Araújo M B, et al. Climate change threats to plant diversity in Europe[J].Proceedings of the National Academy of Sciences,2005,102(23):8245-8250.
Wang J, Meng J J, Cai Y L. Assessing vegetation dynamics impacted by climate change in the southwestern karst region of China with AVHRR NDVI and AVHRR NPP time-series[J].Environmental Geology,2008,54(6):1185-1195.
刘瑶,江辉,吴春波.鄱阳湖区植被覆盖度的遥感估算[J].南昌工程学院学报,2006,25(1):52-56.
朴世龙,方精云.最近18年来中国植被覆盖的动态变化[J].第四纪研究,2001,21(4):294-302.
马明国,董立新,王雪梅.过去21 a中国西北植被覆盖动态监测与模拟[J].冰川冻土,2003,25(2):232-236.
金凯,王飞,韩剑桥,等.1982—2015年中国气候变化和人类活动对植被NDVI变化的影响[J].地理学报,2020,75(5):961-974.
张江,袁昱舒,张婧,等.近30年来青藏高原高赛草地NDVI动态变化对自然及人为因子的响应[J].生态学报,2020,40(18):6269-6281.
陈舒婷,郭兵,杨飞,等.2000—2015年青藏高原植被NPP时空变化格局及其对气候变化的响应[J].自然资源学报,2020,35(10):2511-2527.
Wu D H, Zhao X, Liang S L, et al. Time-lag effects of global vegetation responses to climate change[J].Global Change Biology,2015,21(9):3520-3531.
郑艺,张丽,周宇,等.1982—2012年全球干旱区植被变化及驱动因子分析[J].干旱区研究,2017,34(1):59-66.
候静,杜灵通,刘可,等.1982—2012年北半球荒漠草原过渡带植被物候特征及其与气候因子的关系[J].气候变化研究进展,2017,13(5):473-482.
马蓉,夏春林,张佳琦,等.中国温带草原植被NDVI时空变化及其对气候变化的响应.生态学杂志. http://kns.cnki.net/kcms/detail/21.1148.Q.20220617.1531.022.html.
Militino A F, Ugarte M D, Pérez-Goya U. Stochastic spatio-temporal models for analysing NDVI distribution of GIMMS NDVI3g images[J].Remote Sensing,2017,9(1):e76.
李红英,张存桂,汪生珍,等.近40年青藏高原植被动态变化对水热条件的响应[J].生态学报,2022,42(12):4770-4783.
解晗,同小娟,李俊,等.2000—2018年黄河流域生长季植被指数变化及其对气候因子的响应[J].生态学报,2022,42(11):4536-4549.
黄豪奔,徐海量,林涛,等.2001—2020年新疆阿勒泰地区归一化植被指数时空变化特征及其对气候变化的响应[J].生态学报,2022,42(7):2798-2809.
周淑琴,荆耀栋,张青峰,等.毛乌素沙地南缘植被景观格局演变与空间分布特征[J].生态学报,2013,33(12):3774-3782.
林玉英,胡喜生,邱荣祖,等.基于Landsat影像的NDVI对植被与影响因子交互耦合的响应[J].农业机械学报,2018,49(10):212-219.
高庆,艾里西尔·库尔班,肖昊.塔里木河下游区域植被时空变化[J].自然资源学报,2019,34(3):624-632.
刘西刚,王勇辉,焦黎.夏尔希里自然保护区草地表层土壤理化性质与海拔高度的关系[J].生态与农村环境学报,2019,35(6):773-780.
刘西刚,王勇辉,焦黎.夏尔希里自然保护区典型植被土壤水源涵养功能探究[J].水土保持学报,2019,33(3):121-128.
王勇辉,焦黎.中国夏尔希里土壤环境背景值特征及评价[J].土壤通报,2015,46(3):754-761.
曹永强,周姝含,杨雪婷.近20年辽宁省植被动态特征及其对气候变化的响应[J].生态学报,2022,42(14):5966-5979.
Yang J, Huang X. 30 m annual land cover and its dynamics in China from 1990 to 2019[J].Earth System Science Data,2021,13:3907-3925.
Hawker L, Bates P, Neal J, et al. Perspectives on digital elevation model (DEM) simulation for flood modeling in the absence of a high-accuracy open access global DEM[J].Frontiers in Earth Science,2018,6:e233.
姜萍,胡列群,肖静,等.新疆植被NDVI时空变化及定量归因[J].水土保持研究,2022,29(2):212-220,242.
王涛,白红英.秦岭山地植被NDVI对气候变化与人类活动的响应[J].山地学报,2017,35(6):778-789.
程昌武.黄河流域1982—2015年植被变化及其影响因素分析[D].西安:长安大学,2020.
陈强,陈云浩,王萌杰,等.2001—2010年黄河流域生态系统植被净第一性生产力变化及气候因素驱动分析[J].应用生态学报,2014,25(10):2811-2818.
陈春波,李刚勇,彭建.1981—2018年新疆草地归一化植被指数时空特征及其对气候变化的响应.生态学报,2023,43(4). https://kns.cnki.net/kcms/detail/11.2031.Q.202209.
陈建东.多元回归模型在基坑地下水位预测中的应用[J].矿山测量,2021,49(1):52-55,73.
Du J Q, Shu J M, Yin J Q, et al. Analysis on spatio-temporal trends and drivers in vegetation growth during recent decades in Xinjiang, China[J].International Journal of Applied Earth Observation and Geoinformation,2015,38:216-228.
Zhao X, Tan K, Zhao S, et al. Changing climate affects vegetation growth in the arid region of the northwestern China[J].Journal of Arid Environments,2011,75(10):946-952.
彭凯锋,蒋卫国,侯鹏,等.三江源国家公园植被时空变化及其影响因子[J].生态学杂志,2020,39(10):3388-3396.
Schofield C J. Biogeography: An ecological and evolutionary approach (6th edn) by C.Barry Cox and Peter D [J].Parasitology Today,2000,16(9):406.
Ling Y, Mahfouz M M, Zhou S. Pre-mRNA alternative splicing as a modulator for heat stress response in plants[J].Trends in Plant Science,2021,26(11):1153-1170.
陈宸,井长青,邢文渊,等.近20年新疆荒漠草地动态变化及其对气候变化的响应[J].草业学报,2021,30(3):1-14.
张艳静,郑宏伟,于瑞德,等.天山中西段不同地区雪岭云杉径向生长对气候变暖的响应差异[J].植物研究,2017,37(3):340-350.
李广起,白帆,桑卫国.长白山红松和鱼鳞云杉在分布上限的径向生长对气候变暖的不同响应[J].植物生态学报,2011,35(5):500-511.
陈海存,李晓东,李凤霞,等.黄河源玛多县退化草地土壤温湿度变化特征[J].干旱区研究,2013,30(1):35-40.
杨瑞红,王新军.伊犁河谷山地北坡土壤特性及植被群落多样性垂直分布格局[J].水土保持研究,2016,23(6):32-39,44.
刘厚田.湿地的定义和类型划分[J].生态学杂志,1995,14(4):73-77.
刘建新.不同农田土壤酶活性与土壤养分相关关系研究[J].土壤通报,2004,35(4):523-525.
张慧,邵雪海,张永.不同海拔高度树木径向生长对气候要素响应的研究进展[J].地球环境学报,2012,3(3):845-854.
Peng J F, Li J B, Wang T, et al. Effect of altitude on climate-growth relationships of Chinese white pine (
Pinus armandii
) in the northern Fu niu Mountain, central China[J].Climate Change,2019,154(1):273-288.
李媛媛,任少华,黄宗胜,等.贵州喀斯特地区不同海拔常见树种枯落物分解及养分释放特征.生态学杂志. http://kns.cnki.net/kcms/detail/21.1148.Q.20220630.1409.004.html.
李相楹,张维勇,刘峰,等.不同海拔高度下梵净山土壤碳、氮、磷分布特征[J].水土保持研究,2016,23(3):19-24.
张彦军,郁耀闯,牛俊杰,等.秦岭太白山北坡土壤有机碳储量的海拔梯度格局[J].生态学报,2020,40(2):629-639.
Gutierrez-Giron A, Diaz-Pines E, Rubio A, et al. Both altitude and vegetation affect temperature sensitivity of soil organic matter decomposition in Mediterranean high mountain soils[J].Geoderma,2015,237:1-8.
程浩,张厚喜,黄智军,等.武夷山不同海拔高度土壤有机碳含量变化特征[J].森林与环境学报,2018,38(2):135-141.
0
浏览量
906
下载量
3
CSCD
关联资源
相关文章
相关作者
相关机构
京公网安备11010802024621