Spatial—temporal pattern of GIMMS NDVI and its dynamics in Mongolian Plateau

Y. Ban, Qian Zhang, Yunfeng Hu, Xueyan Zhang, Jiyuan Liu, D. Zhuang
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引用次数: 1

Abstract

The physical geography of Mongolian Plateau plays an important role in the East Asian climate ecology system. In this research, GIMMS NDVI, the third generation of NDVI dataset, was processed using the MVC method first, then the spatial-temporal patterns of GIMMS NDVI in Mongolian Plateau during 1982-2003 was investigated, and the transect from Tariat to Xilin Gol was also selected to analyze the NDVI dynamic processes in detail. The results demonstrated that: (1) the general spatial distribution pattern of NDVI showed a clear spatial differentiation. The high value pixels were mainly distributed in the east and north of Mongolian Plateau with forest and meadow steppe land cover, while the low value pixels were mainly distributed in the west and centre part of Mongolian Plateau with desert and Gobi land cover. However, the annual NDVI variability was relative small either in the high-covered regions (i.e. forest, forest steppe, and meadow steppe) or in low-covered regions (i.e. steppe desert, desert and Gobi), while the region with typical steppe normally had higher annual NDVI variability. (2) During 1982-2003, the dynamic evolution process of NDVI in Mongolian Plateau also showed an evident spatial differentiation. About 12.4% of total area featured a significant increase, 4.8% of total area featured an increase but without significance, and 9.3% of total area featured decrease without significance. The other part, about 73.5% of total area, had no obvious change. The NDVI increased significantly in the South-East, South and of Mongolian Plateau, while it decreased in the North-East and North of Mongolian Plateau. Further, the NDVI-increased regions were those typical steppe and farming-pastoral regions before, while the NDVI-decreased regions were those well-covered forest, forest steppe and meadow steppe regions before.
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蒙古高原GIMMS NDVI时空格局及其动态分析
蒙古高原自然地理在东亚气候生态系统中占有重要地位。本文首先采用MVC方法对第三代NDVI数据集GIMMS NDVI进行处理,研究了1982-2003年蒙古高原GIMMS NDVI的时空格局,并选取塔里塔市至锡林郭勒市的样带对NDVI的动态过程进行了详细分析。结果表明:(1)NDVI总体空间分布格局呈现明显的空间分异。高值像元主要分布在蒙古高原东部和北部,有森林和草甸草原覆盖;低值像元主要分布在蒙古高原西部和中部,有沙漠和戈壁覆盖。高覆盖度地区(森林、森林草原、草甸草原)和低覆盖度地区(草原荒漠、荒漠、戈壁)的NDVI年变率相对较小,而典型草原地区的NDVI年变率通常较高。(2) 1982—2003年,蒙古高原NDVI的动态演变过程也表现出明显的空间分异。12.4%的面积显著增加,4.8%的面积增加但不显著,9.3%的面积减少但不显著。其余部分(约占总面积的73.5%)变化不明显。蒙古高原东南部、南部和北部NDVI显著增加,东北部和北部NDVI显著减少。ndvi增加的区域为以前的典型草原和农牧区,而减少的区域为以前的覆盖良好的森林、森林草原和草甸草原区。
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