WANG B X, SUN W F, CHEN X Y, et al, 2026. Vertical Chlorophyll-a profile reconstruction in the North Indian Ocean using deep neural networksJ. Advances in Marine Science, 44(2): 420-433. DOI: 10.12362/j.issn.1671-6647.20241010003
Citation: WANG B X, SUN W F, CHEN X Y, et al, 2026. Vertical Chlorophyll-a profile reconstruction in the North Indian Ocean using deep neural networksJ. Advances in Marine Science, 44(2): 420-433. DOI: 10.12362/j.issn.1671-6647.20241010003

Vertical Chlorophyll-a Profile Reconstruction in the North Indian Ocean Using Deep Neural Networks

  • To gain an in-depth understanding of the distribution patterns of marine primary productivity and support the monitoring of marine ecological environment changes, this paper integrates Biogeochemical-Argo (BGC-Argo) float data with satellite remote sensing data to construct a deep learning model for retrieving the vertical distribution characteristics of Chlorophyll-a (Chl-a) mass concentration in the North Indian Ocean. The model combines the vertical temperature and salinity profile features extracted by the 1DCNN-Transformer module, the spatiotemporal continuous vectors transformed by the Embedding module, and satellite remote sensing data, which are then fed into a Deep Neural Network (DNN) to reconstruct the vertical distribution of Chl-a mass concentration in the North Indian Ocean. Sensitivity analysis identified Sea Surface Temperature (SST), sea surface Chl-a mass concentration, and vertical temperature and salinity profiles as the optimal input variables for the model. The results show that the model achieves an RMSE of 0.106 μg/L and an R2 of 0.81 in reconstructing Chl-a mass concentration profiles. Within the 0-140 m depth range, the maximum RMSE for Chl-a concentration retrieval is approximately 0.4 μg/L, while errors decrease significantly below 140 m. In terms of spatial distribution, the maximum Chl-a concentration (A) in the Arabian Sea is significantly higher than that in the Bay of Bengal and equatorial regions. In terms of temporal variation, the A values and their corresponding depths (Zmax) in the Arabian Sea, Bay of Bengal, and equatorial regions exhibit seasonal variations, with a certain negative correlation observed between Zmax and A.
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