Publications des scientifiques de l'IRD

Jebri B., Khodri Myriam, Echevin Vincent, Gastineau G., Thiria S., Vialard Jérôme, Lebas N. (2020). Contributions of internal variability and external forcing to the recent trends in the Southeastern Pacific and Peru-Chile upwelling system. Journal of Climate, 33 (24), p. 10555-10578. ISSN 0894-8755.

Titre du document
Contributions of internal variability and external forcing to the recent trends in the Southeastern Pacific and Peru-Chile upwelling system
Année de publication
2020
Type de document
Article référencé dans le Web of Science WOS:000615175200011
Auteurs
Jebri B., Khodri Myriam, Echevin Vincent, Gastineau G., Thiria S., Vialard Jérôme, Lebas N.
Source
Journal of Climate, 2020, 33 (24), p. 10555-10578 ISSN 0894-8755
In a warming world context, sea surface temperature (SST) off central-south Peru, northern Chile, and farther offshore increases at a slower rate than the global average since several decades (i.e., cools, relative to the global average). This tendency is synchronous with an interdecadal Pacific oscillation (IPO) negative trend since similar to 1980, which has a cooling signature in the southeastern Pacific. Here, we use a large ensemble of historical coupled model simulations to investigate the relative roles of internal variability (and in particular the IPO) and external forcing in driving this relative regional cooling, and the associated mechanisms. The ensemble mean reproduces the relative cooling, in response to an externally forced southerly wind anomaly, which strengthens the upwelling off Chile in recent decades. This southerly wind anomaly results from the poleward expansion of the Southern Hemisphere Hadley cell. Attribution experiments reveal that this poleward expansion and the resulting enhanced upwelling mostly occur in response to increasing greenhouse gases and stratospheric ozone depletion since similar to 1980. An oceanic heat budget confirms that the wind-forced upwelling enhancement dominates the relative cooling near the coast. In contrast, a wind-forced deepening of the mixed layer drives the offshore cooling. While internal variability contributes to the spread of tendencies, the ensemble-mean relative cooling in the southeastern Pacific is consistent with observations and occurs irrespectively of the IPO phase, hence, indicating the preeminent role of external forcing.
Plan de classement
Limnologie physique / Océanographie physique [032]
Description Géographique
PACIFIQUE ; PEROU ; CHILI
Localisation
Fonds IRD [F B010080977]
Identifiant IRD
fdi:010080977
Contact