首页> 美国卫生研究院文献>Scientific Reports >Vegetation dynamics at the upper elevational limit of vascular plants in Himalaya
【2h】

Vegetation dynamics at the upper elevational limit of vascular plants in Himalaya

机译:喜马拉雅山维管植物海拔高度的植被动态

代理获取
本网站仅为用户提供外文OA文献查询和代理获取服务,本网站没有原文。下单后我们将采用程序或人工为您竭诚获取高质量的原文,但由于OA文献来源多样且变更频繁,仍可能出现获取不到、文献不完整或与标题不符等情况,如果获取不到我们将提供退款服务。请知悉。

摘要

A rapid warming in Himalayas is predicted to increase plant upper distributional limits, vegetation cover and abundance of species adapted to warmer climate. We explored these predictions in NW Himalayas, by revisiting uppermost plant populations after ten years (2003–2013), detailed monitoring of vegetation changes in permanent plots (2009–2012), and age analysis of plants growing from 5500 to 6150 m. Plant traits and microclimate variables were recorded to explain observed vegetation changes. The elevation limits of several species shifted up to 6150 m, about 150 vertical meters above the limit of continuous plant distribution. The plant age analysis corroborated the hypothesis of warming-driven uphill migration. However, the impact of warming interacts with increasing precipitation and physical disturbance. The extreme summer snowfall event in 2010 is likely responsible for substantial decrease in plant cover in both alpine and subnival vegetation and compositional shift towards species preferring wetter habitats. Simultaneous increase in summer temperature and precipitation caused rapid snow melt and, coupled with frequent night frosts, generated multiple freeze-thaw cycles detrimental to subnival plants. Our results suggest that plant species responses to ongoing climate change will not be unidirectional upward range shifts but rather multi-dimensional, species-specific and spatially variable.
机译:喜马拉雅山脉的快速变暖预计将增加植物的上限分布,植被覆盖以及适应气候变暖的物种的丰富性。我们在喜马拉雅山西北部探索了这些预测,方法是重新审视十年(2003-2013年)之后的最上层植物种群,详细监测永久性地块中的植被变化(2009-2012年),并对从5500到6150 m生长的植物进行年龄分析。记录植物性状和微气候变量以解释观察到的植被变化。几个物种的海拔极限移动到6150 m,比连续植物分布的极限高约150垂直米。植物年龄分析证实了变暖驱动的上坡迁移的假说。但是,变暖的影响与降水增加和物理干扰有关。 2010年夏季极端降雪事件可能是造成高山和亚热带植被的植物覆盖率大幅下降,以及向偏爱湿润生境物种的成分转变的原因。夏季温度和降水的同时增加导致积雪迅速融化,再加上频繁的夜间霜冻,产生了多个不利于亚热带植物的冻融循环。我们的结果表明,植物物种对持续的气候变化的响应将不是单向的向上范围变化,而是多维的,特定物种的和空间可变的。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
代理获取

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号