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Tree-ring indications of recent glacier fluctuations in Gangotri, western Himalaya, India

机译:印度喜马拉雅山西部甘戈特里最近的冰川波动的年轮迹象

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A 410-year-old (AD 1590-1999) ring-width chronology of Himalayan pine (Pinus wallichiana) based on large replication of samples derived from a pure, mixed age stand growing on thick soil with almost even topography near Chirbasa, Gangotri has been developed. This makes the longest chronology of this species developed so far from the Indian region. The chronology shows abrupt surge in tree growth during the late 20th century, with the highest growth indices recorded in the 1990s. Strong correlation noted between tree growth and winter temperature shows that the winter warmth is one of the main factors responsible for the twentieth century growth surge. This growth surge is closely associated with the area vacated by the Gangotri glacier. Low growth prior to the 1950s reflecting cooler conditions indicates that the glacier should have been stationary for a long time with some episodic advances. [References: 26]
机译:喜马拉雅松(Pinus wallichiana)的410年(公元1590-1999年)环宽年表,是基于大量纯净,混合年龄林分样品的复制,这些样品生长在厚厚的土壤上,地势奇尔巴萨附近的地形几乎均匀,甘戈特里已开发。这使得该物种从印度地区发展至今的时间最长。年表显示,树木生长在20世纪后期突然激增,在1990年代记录了最高的生长指数。树木生长与冬季温度之间存在很强的相关性,表明冬季温暖是导致20世纪生长激增的主要因素之一。这种增长激增与甘戈特里冰川腾空的面积密切相关。 1950年代之前的低增长反映了天气转凉,这表明冰川应该长期处于静止状态,并取得了一些积极的进展。 [参考:26]

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