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The CLIVAR Ocean Model Development Panel is pleased to invite you to join its Webinar Series.

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Figure 1: Emergence and attribution of the pIOD-like warming pattern in the tropical Indian Ocean during 1979–2020.

(a–d) Relative sea surface temperature...

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This 90-minute side event will bring together scientists, innovators, surfers, fishers, and...

We would like to draw your attention to upcoming sessions convened by CLIVAR members at the Ocean Sciences Meeting 2026, which will take place on 22-27 February 2026 in Glasgow, Scotland. S...

Figure 1. More persistent cold conditions in boreal spring and early summer after a multiyear La Niña, compared to those before a strong El Niño (left, a, c), inhibit an eastward movement and enhancement of atmosphere deep convection (right, b, d), leading to a decoupled ocean and atmosphere that delay the growth of a subsequent El Niño.

In a paper published in Science...