000027847 001__ 27847
000027847 041__ $$aEnglish
000027847 100__ $$aDing, M.
000027847 245__ $$aThe Relationship between Ndvi and Precipitation on the Tibetan Plateau
000027847 260__ $$c2007
000027847 300__ $$a259-268
000027847 511__ $$aKoshi, Article
000027847 520__ $$aThe temporal and spatial changes of NDVI on the Tibetan Plateau, as well as the relationship between NDVI and precipitation, were discussed in this paper, by using 8-km resolution multi-temporal NOAA AVHRR-NDVI data from 1982 to 1999. Monthly maximum NDVI and monthly rainfall were used to analyze the seasonal changes, and annual maximum NDVI, annual effective precipitation and growing season precipitation (from April to August) were used to discuss the interannual changes. The dynamic change of NDVI and the correlation coefficients between NDVI and rainfall were computed for each pixel. The results are as follows: (1) The NDVI reached the peak in growing season (from July to September) on the Tibetan Plateau. In the northern and western parts of the plateau, the growing season was very short (about two or three months); but in the southern, vegetation grew almost all the year round. The correlation of monthly maximum NDVI and monthly rainfall varied in different areas. It was weak in the western, northern and southern parts, but strong in the central and eastern parts. (2) The spatial distribution of NDVI interannual dynamic change was different too. The increase areas were mainly distributed in southern Tibet montane shrub-steppe zone, western part of western Sichuan-eastern Tibet montane coniferous forest zone, western part of northern slopes of Kunlun montane desert zone and southeastern part of southern slopes of Himalaya montane evergreen broad-leaved forest zone; the decrease areas were mainly distributed in the Qaidam montane desert zone, the western and northern parts of eastern Qinghai-Qilian montane steppe zone, southern Qinghai high cold meadow steppe zone and Ngari montane desert-steppe and desert zone. The spatial distribution of correlation coefficient between annual effective rainfall and annual maximum NDVI was similar to the growing season rainfall and annual maximum NDVI, and there was good relationship between NDVI and rainfall in the meadow and grassland with medium vegetation cover, and the effect of rainfall on vegetation was small in the forest and desert area.
000027847 700__ $$aZhang, Y.
000027847 700__ $$aLiu, L.
000027847 700__ $$aZhang, W.
000027847 700__ $$aWang, Z.
000027847 700__ $$aBai, W.
000027847 773__ $$pJournal of Geographical Sciences
000027847 773__ $$v17 (3)
000027847 773__ $$a10.1007/s11442-007-0259-7
000027847 8564_ $$uhttp://dx.doi.org/10.1007/s11442-007-0259-7$$yWeb address
000027847 980__ $$aArticle