JOURNAL ARTICLE
Prediction of seasonal sea surface temperature based on temperature and salinity of subsurface ocean using machine learning.
Published In: International Journal of Climatology, 2024, v. 44, n. 5. P. 1326 1 of 3
Database: Academic Search Ultimate 2 of 3
Authored By: Wei, Sentao; Wang, Chenghai; Zhang, Feimin; Yang, Kai 3 of 3
Abstract
The sea surface temperature (SST) is not only a crucial external factor in the evolution of the atmosphere, but also a primary factor and premonition signal used in climate prediction. It is challenging to obtain a precise SST for generating accurate initial and boundary conditions in numerical models. This study employs a machine learning approach, that is, a convolutional neural network (CNN) algorithm, to predict SST on a seasonal scale. In particular, the subsurface ocean temperature (OT) and ocean salinity (OS) at depths of 5.02, 15.08, 25.16, 35.28, 45.45 and 76.55 m were used as training factors in developing a CNN prediction model. The results indicate that subsurface OT and OS can persist for 6 months or longer, with a maximum persistence of up to 12 months. Using the CNN prediction model, the SST can be reliably predicted 6 months in advance in most cases. The predicted SST has a mean bias of approximately 0–0.8 K on the globe. The bias is small (below 0.5 K) in the open ocean. The root mean square errors (RMSEs) of hindcasting for Interdecadal Pacific Oscillation, North Atlantic Oscillation (NAO) and Atlantic Multidecadal Oscillation indices are all less than 1.0 K. Specifically, the RMSE for El Niño prediction is less than 0.5 K. This study provides a viable method for establishing initial and boundary conditions for climate prediction. [ABSTRACT FROM AUTHOR]
Additional Information
- Source:International Journal of Climatology. 2024/04, Vol. 44, Issue 5, p1326
- Document Type:Article
- Subject Area:Power and Energy
- Publication Date:2024
- ISSN:0899-8418
- DOI:10.1002/joc.8384
- Accession Number:176586126
- Copyright Statement:Copyright of International Journal of Climatology is the property of Wiley-Blackwell and its content may not be copied or emailed to multiple sites without the copyright holder's express written permission. Additionally, content may not be used with any artificial intelligence tools or machine learning technologies. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)
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