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Perturbing the Surface Energy Balance to Emulate the Historical Pattern of Tropical Pacific Sea Surface Temperature Trends



Public Access Version Available on: May 01, 2026, 12:00 AM
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Details

  • Journal Title:
    Journal of Climate
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  • Description:
    The strengthening of the zonal sea surface temperature (SST) gradient observed in the tropical Pacific in recent decades is a regional climate change signal that may be outside the range of historical simulations with comprehensive climate models. Given the important role that this change has on other aspects of climate, a series of idealized surface energy balance calculations with imposed parameters are performed to build a baseline understanding of the sensitivities that govern these changes. I quantify the requisite magnitudes of five perturbations that reach a new equilibrium with a mean SST warming of about 0.5 K and about 0.4 K more west Pacific warming than east Pacific warming, based approximately on the observed trends. A characteristic magnitude of zonal asymmetry in a surface energy tendency that can bring changes in line with observed trends is ≈3 W m−2. Strengthened zonal SST gradients can arise from a more zonally asymmetric ocean heat flux that increases by ≈20% K−1 using that implied by ERA5’s surface fluxes, a spatially varying radiative forcing with a west–east contrast of ≈3.3 W m−2, a more amplifying surface radiative feedback in the west than in the east with a contrast of ≈4 W m−2 K−1, a surface-air relative humidity (RH) contrast that increases RH in the west and decreases it in the east by ≈0.5% K−1, or a more zonally asymmetric wind speed that increases by ≈16% K−1. The “storylines” of forced surface energy budget change identified here are valuable in determining the plausibility of mechanisms that may be absent or underestimated in coupled climate model simulations.
  • Keywords:
  • Source:
    J. Climate, 38, 6193–6206
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    Other
  • Compliance:
    Submitted
  • Main Document Checksum:
    urn:sha-512:5b02c1112bb054ab19a2334c7b7b5376ef3fced4964fcf01b8a8e4784a4b8101b410d09bb8ca853fa3c108ca48909a1ac574447498b950793f7a9521ba52f6c7
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