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As seen in: Frontiers in Marine Science

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Validation of forecasted surface sensible and latent heat fluxes by GFS and GEFS against saildrone observations in the Arctic

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By Hope Hunter, Chidong Zhang, Dongxiao Zhang, Hannah Horowitz
| Frontiers in Marine Science
1 Introduction The Arctic is warming at a rate approximately four times faster than the global average, a phenomenon known as Arctic amplification, driving significant changes within the Arctic environment and throughout the world (Rantanen et al., 2022). Sensible and latent heat fluxes at the air-sea interface are critical components of energy balance in the Arctic.
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