News

Call for Experts: AI, Machine Learning, Data Assimilation and paleoclimate for the CLIVAR Scientific Steering Group (SSG)

Call for Experts: AI, Machine Learning, Data Assimilation and paleoclimate for the CLIVAR Scientific Steering Group (SSG)


CLIVAR is seeking qualified experts to join our SSG with appointments starting in January 2027 and 2028. New members for the CLIVAR SSG will be approved by the...

Read More ...

CLIVAR SSG Rotation in 2026

Dr. Rym Msadek, New CLIVAR SSG Member

The CLIVAR Scientific Steering Group (SSG) is pleased to welcome Dr. Rym Msadek, a research scientist at the CNRS (Centre National de la Recherche Scientifique, France), as a new member for the 2026-2029 term.

Dr....

Read More ...

Introducing the New CLIVAR Logo

...

Read More ...

Call for Papers: Research Topic in Frontiers in Climate

You are invited to submit your work to the Research Topic in Frontiers in Climate

Background: 

This Research Topic highlights the scientific themes of the Pan-CLIVAR...

Read More ...

Position available: Director of the CLIVAR International Project Office - Deadline for application 30 November 2025

 

The Ocean University of China (OUC) and the World Climate Research Programme (WCRP) invite applications for the post of Director of the CLIVAR (Climate and Ocean - Variability, Predictability, and Change) International Project Office (CLIVAR IPO), based in Qingdao, China. The director...

Read More ...

Pan-CLIVAR Meeting and Symposium 2025 was held in Bali

The Pan-CLIVAR Meeting 2025 was held in Bali, Indonesia, from 22nd to 26th of September 2025, attended by over 150 in-person participants from more than 35 countries.  This was only the second Pan-CLIVAR Meeting after the 2014 meeting...

Read More ...

OMDP - Webinar Series

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

Subscribe here to receive notifications about future editions and reminders about joining the sessions.

...
Read More ...

Online Posters

 

              Title                                                                                                                                   Presenter                     Authors

...

Read More ...

Greenhouse Gases and Aerosols Together Shape a pIOD-like Warming Pattern in the Indian Ocean

 

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...

Read More ...

Pan-CLIVAR 2025 Side Event: Enhancing International Ocean-Climate Research Collaboration in a Changing Climate

Date and time: Thursday, 25 September, 14:00-17:30

Register your interest to participate by 22 August 2025:  https://forms.gle/z2DPAQVu1J4dG9uaA and complete this optionally anonymous...

Read More ...

Interactive Session: "Inclusive Innovation for Ocean and Climate Observations" (11 am on 26th September) Co-sponsored by Rip Curl Asia

(EVENT UPDATED)

Please fill out this registration link to attend

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

Read More ...

2025 Open Call for New Members of CLIVAR Panels and SSG

The call for nominations to the CLIVAR panels and Scientific Steering Group (SSG) with appointment starting in January 2026 and January 2027 respectively is closed. Nominations can be submitted online via the nomination form, deadline for the submission was 3 October 2025. Detailed...

Read More ...

OSM26 Sessions convened by CLIVAR members

 

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...

Read More ...

The CLIVAR-Spain Committee

The CLIVAR-Spain Committee

by Gabriel Jordà and Isabel Cacho, coordinators of the CLIVAR-Spain committee

The CLIVAR-Spain Committee (http://clivar.es/ ) was established in 1999-2000, first as a National CLIVAR Committee, sponsored by the...

Read More ...

Multiyear La Niña does not increase the likelihood of transitioning to a strong El Niño

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...

Read More ...

Pages