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Effect of the Indo-Pacific Warm Pool on Lower-Stratospheric Water Vapor and Comparison with the Effect of ENSO

https://doi.org/10.1175/jcli-d-17-0575.1
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Outgoing claims: the papers this work cites, builds on, or argues with.

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Recent variability of the tropical tropopause inversion layer
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inferredcites →https://doi.org/10.1088/1748-9326/11/12/124026openalex-snapshot
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inferredcites →https://doi.org/10.1126/science.1092703openalex-snapshot
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inferredcites →https://doi.org/10.1126/science.1222978openalex-snapshot
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Residual circulation trajectories and transit times into the extratropical lowermost stratosphere
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What points at this work

Incoming claims: where this work appears in other papers’ reference lists and arguments.

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Secular Changes in the Stratospheric Water Vapour Induced by the Indo-Pacific Warm Pool Warming
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Representation of the Stratospheric Circulation in CRA-40 Reanalysis: The Arctic Polar Vortex and the Quasi-Biennial Oscillation
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Extreme precipitation driven by the rapid tropical Atlantic warming and the second developing La Niña over the Yangtze–Huaihe River Basin in August 2021
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North Atlantic SSTA triggers persistent extreme precipitation over South China by modulating the 25–50-day intraseasonal oscillation
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Amplification of ENSO’s influence on the atmospheric circulation over Western Tibetan Plateau in autumn during 1948–2021
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An Estimate of the Relative Contributions of Sea Surface Temperature Variations in Various Regions to Stratospheric Change
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Reply on RC1
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Reply on RC2
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Comment on acp-2021-697
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Comment on acp-2021-697
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Comment on acp-2021-697
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A vertical transport window of water vapor in the troposphere over the Tibetan Plateau with implications for global climate change
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