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Enhanced hydrological cycle increases ocean heat uptake and moderates transient climate change

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Listed:
  • Maofeng Liu

    (University of Miami)

  • Gabriel Vecchi

    (Princeton University
    Princeton University)

  • Brian Soden

    (University of Miami)

  • Wenchang Yang

    (Princeton University)

  • Bosong Zhang

    (University of Miami)

Abstract

The large-scale moistening of the atmosphere in response to increasing greenhouse gases amplifies the existing patterns of precipitation minus evaporation (P − E), which, in turn, amplifies the spatial contrast in sea surface salinity. Here, by performing a series of transient CO2 doubling experiments, we demonstrate that surface salinification driven by the amplified dry conditions (P − E

Suggested Citation

  • Maofeng Liu & Gabriel Vecchi & Brian Soden & Wenchang Yang & Bosong Zhang, 2021. "Enhanced hydrological cycle increases ocean heat uptake and moderates transient climate change," Nature Climate Change, Nature, vol. 11(10), pages 848-853, October.
    • Handle: RePEc:nat:natcli:v:11:y:2021:i:10:d:10.1038_s41558-021-01152-0
    DOI: 10.1038/s41558-021-01152-0
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