Thermodynamic and dynamic controls on changes in the zonally anomalous hydrological cycle

The wet gets wetter, dry gets drier paradigm explains the expected moistening of the extratropics and drying of the subtropics as the atmospheric moisture content increases with global warming. Here we show, using precipitation minus evaporation (P − E) data from climate models, that it cannot be ex...

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Main Authors: Wills, R, Byrne, M, Schneider, T
Format: Journal article
Published: American Geophysical Union 2016
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author Wills, R
Byrne, M
Schneider, T
author_facet Wills, R
Byrne, M
Schneider, T
author_sort Wills, R
collection OXFORD
description The wet gets wetter, dry gets drier paradigm explains the expected moistening of the extratropics and drying of the subtropics as the atmospheric moisture content increases with global warming. Here we show, using precipitation minus evaporation (P − E) data from climate models, that it cannot be extended to apply regionally to deviations from the zonal mean. Wet and dry zones shift substantially in response to shifts in the stationary‐eddy circulations that cause them. Additionally, atmospheric circulation changes lead to a smaller increase in the zonal variance of P − E than would be expected from atmospheric moistening alone. The P − E variance change can be split into dynamic and thermodynamic components through an analysis of the atmospheric moisture budget. This reveals that a weakening of stationary‐eddy circulations and changes in the zonal variation of transient‐eddy moisture fluxes moderate the strengthening of the zonally anomalous hydrological cycle with global warming.
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spelling oxford-uuid:2e008a6d-ec10-4af5-a209-53b8260bff222022-03-26T12:46:26ZThermodynamic and dynamic controls on changes in the zonally anomalous hydrological cycleJournal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:2e008a6d-ec10-4af5-a209-53b8260bff22Symplectic Elements at OxfordAmerican Geophysical Union2016Wills, RByrne, MSchneider, TThe wet gets wetter, dry gets drier paradigm explains the expected moistening of the extratropics and drying of the subtropics as the atmospheric moisture content increases with global warming. Here we show, using precipitation minus evaporation (P − E) data from climate models, that it cannot be extended to apply regionally to deviations from the zonal mean. Wet and dry zones shift substantially in response to shifts in the stationary‐eddy circulations that cause them. Additionally, atmospheric circulation changes lead to a smaller increase in the zonal variance of P − E than would be expected from atmospheric moistening alone. The P − E variance change can be split into dynamic and thermodynamic components through an analysis of the atmospheric moisture budget. This reveals that a weakening of stationary‐eddy circulations and changes in the zonal variation of transient‐eddy moisture fluxes moderate the strengthening of the zonally anomalous hydrological cycle with global warming.
spellingShingle Wills, R
Byrne, M
Schneider, T
Thermodynamic and dynamic controls on changes in the zonally anomalous hydrological cycle
title Thermodynamic and dynamic controls on changes in the zonally anomalous hydrological cycle
title_full Thermodynamic and dynamic controls on changes in the zonally anomalous hydrological cycle
title_fullStr Thermodynamic and dynamic controls on changes in the zonally anomalous hydrological cycle
title_full_unstemmed Thermodynamic and dynamic controls on changes in the zonally anomalous hydrological cycle
title_short Thermodynamic and dynamic controls on changes in the zonally anomalous hydrological cycle
title_sort thermodynamic and dynamic controls on changes in the zonally anomalous hydrological cycle
work_keys_str_mv AT willsr thermodynamicanddynamiccontrolsonchangesinthezonallyanomaloushydrologicalcycle
AT byrnem thermodynamicanddynamiccontrolsonchangesinthezonallyanomaloushydrologicalcycle
AT schneidert thermodynamicanddynamiccontrolsonchangesinthezonallyanomaloushydrologicalcycle