<?xml version="1.0"?>
<oai_dc:dc xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:title>Drivers of CMIP Tropical Pacific warming pattern diversity</dc:title>
  <dc:creator>/Danielli, Vincent</dc:creator>
  <dc:creator>/Lengaigne, Matthieu</dc:creator>
  <dc:creator>Sadhvi, K.</dc:creator>
  <dc:creator>Gopika, S.</dc:creator>
  <dc:creator>/Vialard, J&#xE9;r&#xF4;me</dc:creator>
  <dc:subject>climate change</dc:subject>
  <dc:subject>tropical Pacific warming pattern</dc:subject>
  <dc:subject>CMIP models</dc:subject>
  <dc:subject>ocean dynamics</dc:subject>
  <dc:subject>evaporative feedback</dc:subject>
  <dc:subject>ocean-atmosphere coupling</dc:subject>
  <dc:description>Anthropogenic changes in sea surface temperature relative to the tropical mean (relative SST) play a pivotal role in influencing atmospheric stability and circulation. In the tropical Pacific, CMIP5/6 multi-model mean (MMM) projections by the end of the 21st century show a southeastern relative cooling and a reduced equatorial SST gradient, although individual models exhibit considerable diversity. Using a simplified heat budget framework, we analyze the processes driving these relative SST changes across 63 CMIP5/6 models under historical and most pessimistic future scenarios. In the southeastern tropical Pacific, MMM relative SST cooling is driven by intensified winds that enhance latent heat flux, with inter-model diversity explained by variations in clouds and winds. Conversely, the MMM equatorial SST gradient reduction arises from reduced evaporative cooling efficiency in the climatologically cold eastern Pacific. A heat budget covariance analysis reveals that inter-model diversity in equatorial Pacific warming is predominantly driven by ocean dynamical processes, challenging previous studies that emphasized cloud feedback mechanisms. Clouds instead mitigate inter-model spread. The inter-model spread in ocean dynamics is linked to two factors: trade wind relaxation and the cold tongue bias. Stronger trade wind relaxation amplifies western Pacific warming, while a weaker cold tongue indicates a less effective ocean thermostat, enhancing eastern Pacific warming. During the present-day period, only a subset of models captures the observed equatorial SST gradient strengthening, but the mechanisms vary across these models, complicating the identification of robust drivers of this observed trend.</dc:description>
  <dc:date>2025</dc:date>
  <dc:type>text</dc:type>
  <dc:identifier>https://www.documentation.ird.fr/hor/fdi:010094820</dc:identifier>
  <dc:identifier>fdi:010094820</dc:identifier>
  <dc:identifier>Danielli Vincent, Lengaigne Matthieu, Sadhvi K., Gopika S., Vialard J&#xE9;r&#xF4;me. Drivers of CMIP Tropical Pacific warming pattern diversity. 2025, 13 (8),  e2025EF005938 [20 p.]</dc:identifier>
  <dc:language>EN</dc:language>
  <dc:coverage>PACIFIQUE</dc:coverage>
  <dc:coverage>ATLANTIQUE</dc:coverage>
  <dc:coverage>ZONE TROPICALE</dc:coverage>
</oai_dc:dc>
