a core project of
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...
Applications are invited for groups within, or linked to CLIVAR communities across the globe to propose “Research Foci” (RF) Studies.
In response to the rapid pace of scientific advances and recognizing the need for the project to be flexible and...
Dr. Antonietta Capotondi received the AGU Harald Svedrup Lecture 2024
The co-chair of CLIVAR Marine Heatwaves in the Global Ocean Research Focus, Antonietta Capotondi is the 2024 recipient for the Harald Sverdrup Lecture at AGU. She presented a talk: "Understanding Tropical Pacific Decadal Variability in the Presence of Anthropogenic Climate...
As part of the Brazilian scientific delegation to COP29, Prof. Regina Rodrigues (Atlantic Region Panel and Marine Heatwaves co-chair) participated in various events. Representing the Brazilian Ministry of Environment and Climate Change...
Figure: Geographical distribution of Summer School participants, located by their institutional affiliations. For the distribution by nationality, see the image below
Figure 1. Schematic diagram representing the factors contributing to the spatial dipole pattern of below-normal and above-normal rainfall during ELLA and LALA episodes. The oceanic and atmospheric conditions over the Indo-Pacific region are shown. Over the ocean, the red...
Meet the New Staff of the International CLIVAR Project Office
After nearly a year of transition, we are excited to announce that the staff team at the International CLIVAR Project Office is now fully complete! Based in Qingdao, China, and hosted by the Ocean University of China, our team is made up of passionate professionals from Indonesia, Mexico, and...
Figure 1. Mean intensity of marine heatwaves (MHWs) and total heat exposures (THEs) during 2071–2100 based on CMIP6 multi-model mean (MMM) under the SSP585 scenario. (a), (b) MHW mean intensity in the global ocean and the Arctic Ocean, respectively. (c), (d) As (a) and (b) but for the changes in MHW mean intensity during 2071-2100 relative to 1985-2014. (e)–(h) As (a)–(d),...
We would like to draw your attention to submit abstracts to two upcoming Southern Ocean sessions convene by CLIVAR members at the
EGU General Assembly 2025 in Vienna, 27 April to 2...
We are excited to announce the publication of a new paper by the Marine Heatwaves in the Global Ocean Research Foci Group, titled:
"A Global Overview of...
Fig. 1. Weakening of equatorial Pacific warming due to the decoupling of Indian and Atlantic Oceans. (A) Composite equatorial (5°S-5°N) SST (shading, °C, with stippling indicating significance at the 95...
Highlights from the International Indian Ocean Science Conference (IIOSC) 2024, March 4-8, 2024, Lombok, Indonesia
This year’s International Indian Ocean Science Conference (IIOSC) marked a significant milestone. The event hosted the 20th Session of the CLIVAR/IOC-GOOS Indian Ocean Region Panel (IORP) and annual...
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