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Impact of Sea Surface Temperature Anomalies in the Equatorial and North Pacific on the Arctic Stratosphere According to the INMCM5 Climate Model Simulations

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Abstract

Five 50-year simulations with version 5 of the INM RAS coupled climate model revealed that the winters with El Niño are characterized by higher Arctic stratospheric temperature as compared to the seasons with La Niña. Lower stratospheric temperature in the Arctic regions as compared to the seasons with negative sea surface temperature (SST) anomalies corresponds to the winter seasons with positive SST anomalies in the North Pacific.

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Funding

The research was supported by the Russian Foundation for Basic Research (project number 19-05-00370).

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Authors and Affiliations

  1. Central Aerological Observatory, 141700, Dolgoprudny, Moscow oblast, Russia

    P. N. Vargin

  2. Lomonosov Moscow State University, 119991, Moscow, Russia

    M. A. Kolennikova

  3. Marchuk Institute of Numerical Mathematics, Russian Academy of Sciences, 119333, Moscow, Russia

    S. V. Kostrykin & E. M. Volodin

Authors
  1. P. N. Vargin
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  2. M. A. Kolennikova
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  3. S. V. Kostrykin
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  4. E. M. Volodin
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Corresponding author

Correspondence to P. N. Vargin.

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Russian Text ©The Author(s), 2021, published in Meteorologiya i Gidrologiya, 2021, No. 1, pp. 5-16.

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Vargin, P.N., Kolennikova, M.A., Kostrykin, S.V. et al. Impact of Sea Surface Temperature Anomalies in the Equatorial and North Pacific on the Arctic Stratosphere According to the INMCM5 Climate Model Simulations. Russ. Meteorol. Hydrol. 46, 1–9 (2021). https://doi.org/10.3103/S1068373921010015

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  • DOI: https://doi.org/10.3103/S1068373921010015

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