Pantropical climate interactions - Archive ouverte HAL
Article Dans Une Revue Science Année : 2019

Pantropical climate interactions

Matthieu Lengaigne
Shayne Mcgregor
Jin-Yi Yu
  • Fonction : Auteur
Xichen Li
  • Fonction : Auteur
Yoo-Geun Ham
  • Fonction : Auteur
Benjamin Ng
  • Fonction : Auteur
Yan Du
  • Fonction : Auteur
  • PersonId : 907205
Xiaopei Li
  • Fonction : Auteur
Marta Martín-Rey
Yun Yang
  • Fonction : Auteur
Jun-Young Choi
  • Fonction : Auteur
Bolan Gan
  • Fonction : Auteur
Geon-Il Kim
Chang-Eun Kim
  • Fonction : Auteur
Ping Chang
  • Fonction : Auteur

Résumé

The El Nino-Southern Oscillation (ENSO), which originates in the Pacific, is the strongest and most well-known mode of tropical climate variability. Its reach is global, and it can force climate variations of the tropical Atlantic and Indian Oceans by perturbing the global atmospheric circulation. Less appreciated is how the tropical Atlantic and Indian Oceans affect the Pacific. Especially noteworthy is the multidecadal Atlantic warming that began in the late 1990s, because recent research suggests that it has influenced Indo-Pacific climate, the character of the ENSO cycle, and the hiatus in global surface warming. Discovery of these pantropical interactions provides a pathway forward for improving predictions of climate variability in the current climate and for refining projections of future climate under different anthropogenic forcing scenarios.

Dates et versions

hal-02193169 , version 1 (24-07-2019)

Identifiants

Citer

Wenju Cai, Lixin Wu, Matthieu Lengaigne, Tim Li, Shayne Mcgregor, et al.. Pantropical climate interactions. Science, 2019, 363 (6430), pp.eaav4236. ⟨10.1126/science.aav4236⟩. ⟨hal-02193169⟩
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