Holocene hydroclimatic variability in the tropical Pacific explained by changing ENSO diversity
Multivariate ENSO index
DOI:
10.1038/s41467-022-34880-8
Publication Date:
2022-11-25T21:32:02Z
AUTHORS (2)
ABSTRACT
Abstract Understanding El Niño-Southern Oscillation (ENSO) response to past climate forcings is hindered by conflicting paleoclimate evidence. Records from the eastern Pacific show an intensification of ENSO variability early late Holocene, while records central highly variable throughout Holocene without obvious relation insolation forcing, which main driver during this interval. Here, we via model simulations that can be reconciled considering changes in relative frequency three preferred spatial patterns Niño events occur (Eastern Pacific, Central and Coastal) strength their hydroclimatic impacts. The relationship between diversity variance not only crucial for interpreting paleo-ENSO understanding external but also used across help evaluate realism projections a changing climate.
SUPPLEMENTAL MATERIAL
Coming soon ....
REFERENCES (41)
CITATIONS (11)
EXTERNAL LINKS
PlumX Metrics
RECOMMENDATIONS
FAIR ASSESSMENT
Coming soon ....
JUPYTER LAB
Coming soon ....