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过去40年大型海洋生态系统中持久性锋面的全球绘图与演变

Global mapping and evolution of persistent fronts in Large Marine Ecosystems over the past 40 years.

作者信息

Xing Qinwang, Yu Haiqing, Wang Hui

机构信息

Institute of Marine Science and Technology, Shandong University, Qingdao, 266237, China.

Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai), Zhuhai, 519080, China.

出版信息

Nat Commun. 2024 May 14;15(1):4090. doi: 10.1038/s41467-024-48566-w.

Abstract

Ocean fronts, characterized by narrow zones with sharp changes in water properties, are vital hotspots for ecosystem services and key regulators of regional and global climates. Global change is reshaping the distribution of material and energy in the ocean; however, it remains unclear how fronts have varied in the last few decades. Here, we present a global, fine-scale digital atlas of persistent fronts around Large Marine Ecosystems and demonstrate significant global increases in both their occurrence and intensity. In subtropical regions (around boundary currents and upwelling systems) and polar regions, persistent frontal occurrence and intensity are rapidly increasing, while in tropical regions, they remain stable or slightly decrease. These enhancements may be respectively related to changes in boundary currents, upwelling, and sea ice retreat. This spatially heterogeneous trend holds important implications for the redistribution of front-related ecosystem services and air-sea interactions but has not been captured by representative high-resolution climate projections models or observation-assimilated ocean models.

摘要

海洋锋面以水属性急剧变化的狭窄区域为特征,是生态系统服务的重要热点以及区域和全球气候的关键调节器。全球变化正在重塑海洋中物质和能量的分布;然而,在过去几十年里海洋锋面如何变化仍不清楚。在此,我们展示了一份关于大型海洋生态系统周围持续锋面的全球精细数字地图集,并证明其出现频率和强度在全球范围内都显著增加。在亚热带地区(围绕边界流和上升流系统)以及极地地区,持续锋面的出现频率和强度正在迅速增加,而在热带地区,它们保持稳定或略有下降。这些增强可能分别与边界流、上升流和海冰退缩的变化有关。这种空间异质性趋势对与锋面相关的生态系统服务重新分配和气 - 海相互作用具有重要意义,但尚未被代表性的高分辨率气候预测模型或观测同化海洋模型所捕捉。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/38e0/11094120/daba48115724/41467_2024_48566_Fig1_HTML.jpg

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