1244 / 2024-09-20 19:43:54
GOCI-estimated air-sea CO2 fluxes in the East China Sea: Patterns and variations during summer 2011–2020
Air-sea CO2 flux,sea surface pCO2,Remote sensing (RS),east china sea,east china sea,Semi-analytical algorithm (MeSAA),Machine learning,Geostationary Ocean Color Imager(GOCI)
Session 54 - Remote sensing of coastal zone and sustainable development
Abstract Accepted
Qiling Xie / Shanghai Jiao Tong University;Second Institute of Oceanography
Yan Bai / Shanghai Jiao Tong University;Second Institute of Oceanography
Xianqiang He / Second Institute of Oceanography;Donghai Laboratory
Teng Li / Second Institute of Oceanography
Inadequate spatiotemporal representativeness of observational data can lead to the oversight of significant short-term fluctuations in sea-atmosphere carbon dioxide (CO2) flux. This oversight risks misrepresenting the ocean's CO2 source-sink dynamics, particularly in marginal seas where these fluxes can vary greatly. To address this challenge, this study combines data-driven machine learning techniques with process analysis to develop a remote sensing model for sea surface pCO2 using geostationary satellite data. This model enables large-scale, daily observations of CO2 exchange processes in the East China Sea during summer.The model's performance has been validated, showing strong results with a root mean square error (RMSE) of 27 μatm and an R² of 0.96. Additionally, SHAP values provide valuable insights into the underlying mechanisms influencing pCO2. While no significant upward trend in summer sea surface pCO2 was identified from 2011 to 2020, the carbon sink capacity of the East China Sea has gradually increased in response to rising atmospheric pCO2 levels, aligning with estimates from polar orbit satellites.However, the lack of polar satellite data in coastal regions (9.86%) has led to a 71.13% overestimation of cumulative carbon sink estimates for the East China Sea during the summers of 2011 to 2019. This study contributes important new insights into the daily variations of CO2 exchange at the sea-atmosphere interface.