在坦博拉火山爆发后,全球树木生长对极端寒冷的抵御力
Shan Gao1, J Julio Camarero2, Flurin Babst3,4
1State Key Laboratory of Tibetan Plateau Earth System, Environment and Resources (TPESER), Institute of Tibetan Plateau Research, Chinese Academy of Sciences, 100101, Beijing, China.
Nature communications
|October 19, 2023
概括
像坦博拉火山这样的爆炸性火山喷发会导致全球显著降温,并严重影响森林生长,特别是在高度地区. 了解这些影响对于管理自然资源和减轻未来风险至关重要.
科学领域:
- 气候学 气候学 气候学
- 生态生态学 生态生态学
- 林业林业 林业 林业 林业
背景情况:
- 全球变暖正在发生,但爆炸性火山喷发可以引发突然,显著的冷却事件.
- 像1809年和1815年的坦博拉火山这样的历史性喷发,在全球范围内造成了长期的极端寒冷.
- 森林生态系统在火山冷却事件后表现出不同的弹性和恢复模式.
研究的目的:
- 调查火山冷却对全球森林弹性和恢复的影响.
- 量化1809年和1815年的坦博拉火山喷发对树木生长的影响.
- 评估火山事件对森林生态系统的长期影响.
主要方法:
- 分析树环数据以推断生长弹性.
- 在不同度和高度的树木生长减少的比较.
- 对严重增长减缓的区域概率的统计评估.
主要成果:
- 由于火山的冷却,树木的生长弹性受到严重影响,特别是在高度和高海拔地区.
- 平均树木生长率下降了高达31.8%,树林的生长率显著下降.
- 严重增长减缓的区域概率增加了高达1390%.
结论:
- 火山冷却事件显著损害了森林生长,特别是在脆弱的高度和高海拔地区.
- 火山冷却的长期影响,包括寒冷和干旱压力,影响森林恢复.
- 评估火山爆发的影响对于自然资源管理和减轻对生态系统的不利影响至关重要.
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