融冰期主导着北极清水湖泊每年的二氧化碳逃逸量

IF 5.1 2区 地球科学 Q1 LIMNOLOGY
J. Karlsson, H. A. Verheijen, D. A. Seekell, D. Vachon, M. Klaus
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引用次数: 0

摘要

目前对北极湖泊二氧化碳(CO2)蒸发量的估计非常不确定,因为很少有研究结合季节性变化,特别是春季融冰期的蒸发量。我们通过质量平衡(融冰期)和高频率记录仪(开阔水域期)对瑞典北部 14 个清水北极湖泊的二氧化碳年度蒸发量进行了量化。平均而言,80%(SD:± 18)的年度二氧化碳蒸发发生在融冰后的 10 d 内。与之前的北极湖泊研究相比,融冰期对年度二氧化碳蒸发的贡献率较高(47% ± 32%)。在所有湖泊中,融冰期:年二氧化碳蒸发量的比例与溶解有机碳浓度呈负相关,与湖泊的平均深度呈正相关。结果表明,需要测量融冰时的二氧化碳交换量,以准确量化北极湖泊的二氧化碳蒸发量。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Ice-melt period dominates annual carbon dioxide evasion from clear-water Arctic lakes

Ice-melt period dominates annual carbon dioxide evasion from clear-water Arctic lakes

Current estimates of carbon dioxide (CO2) evasion from Arctic lakes are highly uncertain because few studies integrate seasonal variability, specifically evasion during spring ice-melt. We quantified annual CO2 evasion for 14 clear-water Arctic lakes in Northern Sweden through mass balance (ice-melt period) and high-frequency loggers (open-water period). On average, 80% (SD: ± 18) of annual CO2 evasion occurred within 10 d following ice-melt. The contribution of the ice-melt period to annual CO2 evasion was high compared to earlier studies of Arctic lakes (47% ± 32%). Across all lakes, the proportion of ice-melt : annual CO2 evasion was negatively related to the dissolved organic carbon concentration and positively related to the mean depth of the lakes. The results emphasize the need for measurements of CO2 exchange at ice-melt to accurately quantify CO2 evasion from Arctic lakes.

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来源期刊
CiteScore
10.00
自引率
3.80%
发文量
63
审稿时长
25 weeks
期刊介绍: Limnology and Oceanography Letters (LO-Letters) serves as a platform for communicating the latest innovative and trend-setting research in the aquatic sciences. Manuscripts submitted to LO-Letters are expected to present high-impact, cutting-edge results, discoveries, or conceptual developments across all areas of limnology and oceanography, including their integration. Selection criteria for manuscripts include their broad relevance to the field, strong empirical and conceptual foundations, succinct and elegant conclusions, and potential to advance knowledge in aquatic sciences.
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