eCite Digital Repository

A linear inverse model of tropical and South Pacific climate variability: optimal structure and stochastic forcing

Citation

Lou, J and O'Kane, TJ and Holbrook, NJ, A linear inverse model of tropical and South Pacific climate variability: optimal structure and stochastic forcing, Journal of Climate, 34, (1) pp. 143-155. ISSN 0894-8755 (2021) [Refereed Article]


Preview
PDF
Pending copyright assessment - Request a copy
2Mb

Preview
PDF (author version - OA)
Pending copyright assessment - Request a copy
2Mb

DOI: doi:10.1175/JCLI-D-19-0964.1

Abstract

A stochastically forced linear inverse model (LIM) of the combined modes of variability from the tropical and South Pacific Oceans is used to investigate the linear growth of optimal initial perturbations and to identify the spatiotemporal features of the stochastic forcing associated with the atmospheric Pacific–South American patterns 1 and 2 (PSA1 and PSA2). Optimal initial perturbations are shown to project onto El Niño–Southern Oscillation (ENSO) and South Pacific decadal oscillation (SPDO), where the inclusion of subsurface South Pacific Ocean temperature variability significantly increases the multiyear linear predictability of the deterministic system. We show that the optimal extratropical sea surface temperature (SST) precursor is associated with the South Pacific meridional mode, which takes from 7 to 9 months to linearly evolve into the final ENSO and SPDO peaks in both the observations and as simulated in an atmosphere-forced ocean model. The optimal subsurface precursor resembles its peak phase, but with a weak amplitude, representing oceanic Rossby waves in the extratropical South Pacific. The stochastic forcing is estimated as the residual by removing the deterministic dynamics from the actual tendency under a centered difference approximation. The resulting stochastic forcing time series satisfies the Gaussian white noise assumption of the LIM. We show that the PSA-like variability is strongly associated with stochastic SST forcing in the tropical and South Pacific Oceans and contributes not only to excite the optimal initial perturbations associated with ENSO and the SPDO but in general to activate the entire stochastic SST forcing, especially in austral summer.

Item Details

Item Type:Refereed Article
Keywords:climate variability, inverse methods, forecasting, ENSO, oscillations, Pacific decadal oscillation
Research Division:Earth Sciences
Research Group:Oceanography
Research Field:Physical oceanography
Objective Division:Environmental Policy, Climate Change and Natural Hazards
Objective Group:Natural hazards
Objective Field:Climatological hazards (e.g. extreme temperatures, drought and wildfires)
UTAS Author:Lou, J (Mr Jiale LOU)
UTAS Author:O'Kane, TJ (Dr Terry O'Kane)
UTAS Author:Holbrook, NJ (Professor Neil Holbrook)
ID Code:142885
Year Published:2021
Deposited By:Oceans and Cryosphere
Deposited On:2021-02-15
Last Modified:2021-02-15
Downloads:0

Repository Staff Only: item control page