Samudra: An AI Global Ocean Emulator for Climate

Abstract AI emulators for forecasting have emerged as powerful tools that can outperform conventional numerical predictions. The next frontier is to build emulators for long climate simulations with skill across a range of spatiotemporal scales, a particularly important goal for the ocean. Our work builds a skillful global emulator of the ocean component of a state‐of‐the‐art climate model. We emulate key ocean variables, sea surface height, horizontal velocities, temperature, and salinity, across their full depth. We use a modified ConvNeXt UNet architecture trained on multi‐depth levels of ocean data. We show that the ocean emulator— Samudra —which exhibits no drift relative to the truth, can reproduce the depth structure of ocean variables and their interannual variability. Samudra is stable for centuries and 150 times faster than the original ocean model. Samudra struggles to capture the correct magnitude of the forcing trends and simultaneously remain stable, requiring further work.

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Publication Details

Journal
Geophysical Research Letters
Published
2025-05-24
DOI
https://doi.org/10.1029/2024gl114318
Citations
10
Primary Topic
Oceanographic and Atmospheric Processes
Type
article
Field-Weighted Citation Impact
17.94
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article

Samudra: An AI Global Ocean Emulator for Climate

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10 citations
Geophysical Research Letters
Oceanographic and Atmospheric Processes
17.94
article

Samudra: An AI Global Ocean Emulator for Climate

Alistair Adcroft, Adam Subel, Laure Zanna, Carlos Fernandez‐Granda, Julius Busecke, Surya Dheeshjith, Shubham Gupta
article en
10 citations

Abstract

Abstract AI emulators for forecasting have emerged as powerful tools that can outperform conventional numerical predictions. The next frontier is to build emulators for long climate simulations with skill across a range of spatiotemporal scales, a particularly important goal for the ocean. Our work builds a skillful global emulator of the ocean component of a state‐of‐the‐art climate model. We emulate key ocean variables, sea surface height, horizontal velocities, temperature, and salinity, across their full depth. We use a modified ConvNeXt UNet architecture trained on multi‐depth levels of ocean data. We show that the ocean emulator— Samudra —which exhibits no drift relative to the truth, can reproduce the depth structure of ocean variables and their interannual variability. Samudra is stable for centuries and 150 times faster than the original ocean model. Samudra struggles to capture the correct magnitude of the forcing trends and simultaneously remain stable, requiring further work.

Geophysical Research LettersVol. 52(10)
Lamont-Doherty Earth Observatory (US), Princeton University (US), Courant Institute of Mathematical Sciences (US), New York University (US), Columbia University (US)
Openalex Percentile: Top 1%
Oceanographic and Atmospheric Processes
17.94
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