永久土融化导致加拿大西北部的植被生产率短期增加
Emily L Ogden1, Steven G Cumming2, Sharon L Smith3
1Biology Department, Wilfrid Laurier University, Waterloo, Ontario, Canada.
Global change biology
|June 19, 2023
概括
永久土的融化最初提高了北极-北极植被的生产力,但这种绿化效应随着长时间的融化而减少,超过了植物植根深度. 生产力增长在中跨度度处是最高的,这表明对不断变化的永久土条件的复杂反应.
科学领域:
- 生态生态学 生态生态学
- 环境科学 环境科学
- 气候变化研究 气候变化研究
背景情况:
- 北极-北极生态系统表现出不同的植被生产力趋势.
- 气候变暖和气候干扰影响了这些趋势.
- 永久土融化的对植被生产力的影响仍然不太清楚.
研究的目的:
- 量化永久土条件的变化对植被生产力的影响.
- 为了研究活性层厚度和植被绿化之间的关系.
- 评估永久土融化引起的生产率变化的长期可持续性.
主要方法:
- 利用来自135个永久土监测地点的活性层厚度数据.
- 从1984年到2019年分析了Landsat时间序列的正常化差异植被指数 (NDVI).
- 在加拿大西北领地的10度度横断线上检查数据.
主要成果:
- 活性层的厚度显著影响了植被生产力的变化.
- 最高的绿化率发生在近地表永久土最近解的地方.
- 当解深度超过植物根植区时,持续的绿化减少了.
- 绿化峰值在中断点 (62.4°北65.2°北) 观察到.
结论:
- 永久土融化的对植被生产力的影响取决于活性层加厚程度.
- 由于解而导致的初始生产率增加可能不会长期持续.
- 南方的地点可能已经经过了最佳的融化条件,而北方的地点可能还没有达到它们.
- 由于永久土融化,未来植物生产率的增加是不确定的.
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