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The relationship between plant stable carbon isotope composition, precipitation and satellite data, Tibet Plateau, China

机译:青藏高原植物稳定碳同位素组成,降水与卫星资料的关系

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摘要

Stable carbon isotope composition (δ ~(13)C) of C3 plant leaves from the Tibet Plateau was analyzed to detect the relationship between stable carbon isotope composition (δ ~(13)C) and precipitation. In northern Tibet, δ ~(13)C increases by 0.46 per thousand with an increase of 100 mm in precipitation, while in the southern plateau δ ~(13)C decreases by 1.82 per thousand with an increase of 100 mm in precipitation. Because field sampling is limited by funds and traffic conditions, while remote sensing has no limitations, satellite data was introduced as a new data source to study the relationship between δ ~(13)C and normalized difference vegetation index (NDVI). NDVI has the same trend with δ ~(13)C, as does precipitation. So NDVI can be used to indicate δ ~(13)C approximately.
机译:分析了青藏高原C3植物叶片的稳定碳同位素组成(δ〜(13)C),以检测稳定碳同位素组成(δ〜(13)C)与降水之间的关系。在西藏北部,δ〜(13)C每增加千毫米增加0.46,而降水量增加100毫米;而在南部高原,δ〜(13)C每增加千毫米减少100毫米,千分之1.82。由于野外采样受到资金和交通条件的限制,而遥感没有限制,因此引入卫星数据作为新的数据源来研究δ〜(13)C与归一化植被指数(NDVI)之间的关系。 NDVI在δ〜(13)C时具有与降水相同的趋势。因此,NDVI可以近似表示δ〜(13)C。

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