海洋表面温度变暖对极地珊瑚生境扩展的预测和不确定性:一个多气候模式研究

Yumiko Yara, K. Oshima, M. Fujii, H. Yamano, Y. Yamanaka, N. Okada
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引用次数: 29

摘要

利用多种气候模式预估的21世纪月平均海温(SST)和基于海温的指数,定量评价了海温变暖对日本附近海域珊瑚生境潜在北界的影响及其在全球变暖预估中的不确定性。由于全球变暖,温带珊瑚群落形成时间的不确定性不小于30年,由于年代际气候变率的调节为±10年。据预测,到21世纪末,日本附近海域的热带-亚热带和温带珊瑚群落和珊瑚分布将向极地移动数百公里。热带-亚热带珊瑚群落、温带珊瑚群落和珊瑚分布的平均迁移速度分别为1 km/年、2 km/年和4 km/年。模拟的速度比以前观测到的速度相对较慢(高达14公里/年;Yamano et al. 2011),这表明珊瑚群落的新招募与珊瑚群落的建立之间存在时间滞后。因此,需要监测珊瑚对海温变暖的响应动态。监测和建模之间的合作将提高未来对珊瑚栖息地变化预测的可靠性。这种预测对于保护海洋生物多样性和制定人类社会适应全球变暖的计划非常重要。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Projection and uncertainty of the poleward range expansion of coral habitats in response to sea surface temperature warming: A multiple climate model study
Using projected monthly mean sea surface tem-perature (SST) in the 21st century obtained by multiple climate models and SST-based indices for the poleward range expansions of three types of coral habitats, we quantitatively evaluated the effects of SST warming on potential northern limit of coral habitats in seas close to Japan and their uncertainty in the global warming pro-jections. The uncertainty in the timing of temperate coral community formation due to global warming was no less than 30 years, with a modulation of ±10 years due to decadal climate variability. Tropical-subtropical and tem-perate coral communities and coral occurrence in seas close to Japan were predicted to shift poleward by a few hundred kilometers by the end of the 21st century. The average estimated speeds of the shifts were 1, 2, and 4 km/year for the tropical-subtropical coral community, temper-ate coral community, and coral occurrence, respectively. The simulated speeds were relatively slower than those previously observed (up to 14 km/year; Yamano et al. 2011), indicating that there are time lags between the new recruitment of coral colonies and the establishment of coral communities. Hence, monitoring of coral dynamics in response to SST warming is required. Collaboration between monitoring and modeling would enhance the reliability of future projections of changes in coral ha-bitats. Such projections are important for conserving marine biodiversity and developing plans for human societies to adapt to global warming.
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