南极陆地海冰的初级生产总量:基于模型的估算

IF 3.3 2区 地球科学 Q1 OCEANOGRAPHY
P. Wongpan, K. M. Meiners, M. Vancoppenolle, A. D. Fraser, S. Moreau, B. T. Saenz, K. M. Swadling, D. Lannuzel
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引用次数: 0

摘要

南极沿岸的大部分地区被季节性陆地海冰(快冰)覆盖,是冰藻的重要栖息地。快冰藻类为浮游生物和底栖生物食物网提供了重要的早期食物来源,并有助于南极沿岸生态系统的生物地球化学循环。夏季速冻冰正在减少,导致季节性速冻冰增多,对相互关联的地球系统过程的影响尚不清楚。目前,我们对南极快冰的时空变化及其对极地生态系统的影响的了解还很有限。由于观测和模型的局限性,评估速冻冰藻类的整体生产力一直受到阻碍。通过将新的速冻冰范围图与一维海冰生物地球化学模型联系起来,我们首次估算了南极速冻冰藻类总初级生产量(GPP)的时空季节变化及其在环南极尺度上的年初级生产量。2005-2006 年季节进行的实验得出的平均快速冰藻产量估计为 2.8 兆吨碳/年。这一估计值约占南大洋海冰藻类总产量的 12%(之前的一项研究估计),平均每块区域的速冻冰藻类产量是块冰的 3.3 倍。我们对罗斯海和威德尔海扇区的南极快冰 GPP 估计值可能被低估了,因为没有考虑冰下板块层生境及其高生物量。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Gross Primary Production of Antarctic Landfast Sea Ice: A Model-Based Estimate

Gross Primary Production of Antarctic Landfast Sea Ice: A Model-Based Estimate

Much of the Antarctic coast is covered by seasonal landfast sea ice (fast ice), which serves as an important habitat for ice algae. Fast-ice algae provide a key early season food source for pelagic and benthic food webs, and contribute to biogeochemical cycling in Antarctic coastal ecosystems. Summertime fast ice is undergoing a decline, leading to more seasonal fast ice with unknown impacts on interconnected Earth system processes. Our understanding of the spatiotemporal variability of Antarctic fast ice, and its impact on polar ecosystems is currently limited. Evaluating the overall productivity of fast-ice algae has historically been hampered by limitations in observations and models. By linking new fast-ice extent maps with a one-dimensional sea-ice biogeochemical model, we provide the first estimate of the spatio-seasonal variability of Antarctic fast-ice algal gross primary production (GPP) and its annual primary production on a circum-Antarctic scale. Experiments conducted for the 2005–2006 season provide a mean fast ice-algal production estimate of 2.8 Tg C/y. This estimate represents about 12% of overall Southern Ocean sea-ice algae production (estimated in a previous study), with the mean fast-ice algal production per area being 3.3 times higher than that of pack ice. Our Antarctic fast-ice GPP estimates are probably underestimated in the Ross Sea and Weddell Sea sectors because the sub-ice platelet layer habitats and their high biomass are not considered.

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来源期刊
Journal of Geophysical Research-Oceans
Journal of Geophysical Research-Oceans Earth and Planetary Sciences-Oceanography
CiteScore
7.00
自引率
13.90%
发文量
429
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