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Updated: Sep 16, 2025

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Simulating Impacts of Ice Storms on Forest Ecosystems
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冬季降雪量减少,抵消了北方温带森林生态系统生长季节变暖导致的碳储量增加
Emerson Conrad-Rooney1, Andrew B Reinmann2,3,4, Pamela H Templer1
1Department of Biology, Boston University, Boston, MA 02215.
概括
气候变化影响温带森林的碳汇. 变暖会增加碳储存,但降低积雪和土壤结解周期会减轻这种效应,可能会在模型中高估森林碳吸收.
科学领域:
- 生态生态学 生态生态学
- 林业林业 林业 林业 林业
- 气候科学 气候科学
背景情况:
- 美国东北部温带森林是重要的碳汇,对抵消人类排放至关重要.
- 预计的气候变化,包括气候变暖和降雪,可能会改变森林的碳储存能力.
- 气候变化对森林碳汇的全年综合影响尚未完全理解.
研究的目的:
- 调查生长季节变暖和冬季降雪对北方温带森林碳储存的十年影响.
- 确定这些气候变化因素对森林碳捕获的净影响.
- 评估当前地球系统模型在预测未来森林碳汇行为的准确性.
主要方法:
- 在哈伯德布鲁克实验森林利用跨季气候变化实验 (CCASE).
- 应用了模拟生长季节变暖和减少冬季积雪量的处理方法.
- 在十年内监测累积树干生物质碳.
主要成果:
- 生长季节的变暖使树干生物质的累积碳增加了63%.
- 冬季的土壤结/解周期,由降低的积雪造成,抵消了大约一半的气候变暖引起的碳储量增加.
- 与对照片相比,联合处理导致茎生物质碳增加31%,但不显著.
结论:
- 必须考虑降低积雪和增加土壤融周期对树木活力和碳吸收的负面影响.
- 当前的地球系统模型可能高估了北方温带森林的碳沉积能力.
- 准确的气候变化影响评估需要纳入改变冬季条件对森林生态系统的影响.
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