The ocean is a crucial sink for anthropogenic CO2 and experiences various biogeochemical extremes, yet it is not clear whether and to what extent such extreme events occur in air–sea CO2 fluxes. Here, we established a framework to define oceanic carbon uptake extremes (CUXs) and release extremes (CRXs) using daily air–...
Yang-Yan Cheng, Bo Han, J. Tjiputra et al.· Journal of Geophysical Resea...· 0 citations
In the Southern Ocean’s marginal ice zone (MIZ), sea ice complicates accurate estimation of air–sea fluxes, limiting the predictive skill of climate models. From December 2020 to January 2021, the 37th Chinese National Antarctic Research Expedition conducted ship-based measurements in the MIZ using an EC (eddy covarian...
Gong Zhang, Bo Han, Chang-Wei Liu et al.· Advances in Atmospheric Scie...· 0 citations
Sea ice is crucial for modulating Antarctic air–sea fluxes, and its thickness (SIT) is the primary factor controlling the exchange of heat, moisture, and momentum. Although CryoSat-2 is commonly used for SIT retrieval, conventional algorithms rely on empirical parameters and auxiliary data that introduce substantial un...
Ziqi Ma, Ya-Fei Nie, Hao Luo et al.· Advances in Atmospheric Scie...· 1 citation
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