Relation of Changes in CO2 Concentration over Large Water Areas of the Boreal and Subarctic Zones of the Northern Hemisphere with Their Phenological Phases Determined from SMOS Satellite Data

V. Tikhonov, E. Pashinov, D. M. Ermakov, I. Khvostov, A. Romanov
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Abstract

The paper presents the results of comparing the atmospheric carbon dioxide reanalysis data and phenological phases of large freshwater areas located in the boreal and subarctic zone for 2012–2020. The data from the CAMS global greenhouse gas reanalysis, which are three-dimensional fields of aerosols and chemical constituents in the atmosphere, with full coverage of the globe, were used in this work. The data used in this study were the average CO2 content in the air column over the water areas. The phenological phases of freshwater bodies (water surface, ice cover, ice destruction) were determined using data from the MIRAS microwave radiometer of the SMOS satellite. The comparison and analysis showed that the CO2 concentration in the atmosphere over the studied water areas has a seasonal cyclic character. The minimum concentration corresponds to the summer period due to strong photosynthesis in water areas, as a result of which carbon dioxide is absorbed in the water column. The maximum concentration of CO2 over water areas corresponds to the period of destruction of the ice cover, leading to the release of carbon dioxide accumulated during the winter period, which is “sealed” in the ice and in the water column under the ice. In freezing lakes located in the boreal zone, in addition to the stable spring CO2 maximum, a strong short-term release of carbon dioxide is sometimes observed, also corresponding to the stage of ice cover destruction. This emission is explained by the higher bioproductivity of water bodies in the boreal zone compared to water areas in the subarctic zone.
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根据 SMOS 卫星数据确定的北半球北方和亚北极区大面积水域二氧化碳浓度变化与其物候期的关系
本文介绍了 2012-2020 年大气二氧化碳再分析数据与北方和亚北极地区大型淡水区域物候期的比较结果。本研究采用了 CAMS 全球温室气体再分析数据,该数据是大气中气溶胶和化学成分的三维场,完全覆盖全球。本研究使用的数据是水域上空气柱中二氧化碳的平均含量。淡水水体的物候期(水面、冰覆盖、冰破坏)是利用 SMOS 卫星的 MIRAS 微波辐射计的数据确定的。比较和分析表明,研究水域上空大气中的二氧化碳浓度具有季节性周期特征。最低浓度出现在夏季,原因是水域光合作用旺盛,水体吸收了二氧化碳。水域二氧化碳浓度最高时,冰盖被破坏,导致冬季积累的二氧化碳释放出来,这些二氧化碳被 "封存 "在冰层和冰下水体中。在北方地区的冰冻湖泊中,除了稳定的春季二氧化碳最大值外,有时还会观察到二氧化碳的短期强烈释放,这也与冰盖破坏阶段相对应。与亚北极区的水域相比,北方区水体的生物生产率较高,这就是这种排放的原因。
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