Study on the spatial differences and its time lag effect on climatic factors of the vegetation in the Longitudinal Range-Gorge Region

被引:14
作者
Bao YaJing [1 ]
Song GuoBao [1 ,2 ]
Li ZhengHai [1 ,3 ]
Gao Jixi [3 ]
Lue, HaiYan [4 ]
Wang HaiMei [6 ]
Cheng Yan [5 ]
Xu Tian [7 ]
机构
[1] Dalian Natl Univ, Coll Life Sci, Inst Bioresources & Environm, Dalian 116600, Peoples R China
[2] Beijing Normal Univ, Coll Resources Sci & Technol, Beijing 100875, Peoples R China
[3] Chinese Res Inst Environm Sci, Beijing 100012, Peoples R China
[4] Chinese Acad Agr Sci, Inst Agr Resources & Reg Planning, Beijing 100081, Peoples R China
[5] Inner Mongolia Agr Univ, Hohhot 010018, Peoples R China
[6] Inner Mongolia Municipal Observ, Hohhot 010051, Peoples R China
[7] Inner Mongolia Univ, Coll Life Sci, Hohhot 010021, Peoples R China
来源
CHINESE SCIENCE BULLETIN | 2007年 / 52卷
关键词
land cover; meteorological factors; effect of time lag; spatial correlation; population density; Longitudinal Range-Gorge Region (LRGR);
D O I
10.1007/s11434-007-7005-5
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
This article analyzes the correlation of NDVI and two meteorological data including temperature and precipitation, and probes the spatial pattern of responding sensitivity of the vegetation to temperature and precipitation change. By constructing the NDVI, index, the relation between vegetation cover and land use in the Longitudinal Range-Gorge Region (LRGR) is revealed. The conclusion is as follows: (1) The time lag effect that vegetation responds to temperature and precipitation change is proven. Different regions have different delay time corresponding to maximum correlation coefficient. According to response time of precipitation and temperature combination, three kinds of temperature-precipitation forms are defined, namely, precipitation and temperature in the same time, precipitation prior to temperature and temperature prior to precipitation. (2) The spatial distribution of sensitivity, of which vegetation responses to temperature, is characterized by several high and low scattered correlation centers. Different from temperature, two insensitive regions and two sensitive belts are formed to present the response of vegetation to precipitation. (3) The NDVIr is constructed, which can perfectly reflect the corresponding relationship between meteorological factors and land use condition in the LRGR.
引用
收藏
页码:42 / 49
页数:8
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