The influence of diabatic heating in the South Pacific Convergence Zone on Rossby wave propagation and the mean flow
The South Pacific Convergence Zone (SPCZ) is a northwest‐southeast oriented precipitation band over the South Pacific Ocean. Latent heat release from condensation leads to substantial diabatic heating, which has potentially large impacts on local and global climate. The influence of this diabatic he...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
van der Wiel, Karin [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2016 |
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| Rechteinformationen: |
Nutzungsrecht: © 2015 Royal Meteorological Society |
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| Systematik: |
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| Übergeordnetes Werk: |
Enthalten in: Quarterly journal of the Royal Meteorological Society - Reading : Soc., 1873, 142(2016), 695, Seite 901-910 |
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| Übergeordnetes Werk: |
volume:142 ; year:2016 ; number:695 ; pages:901-910 |
| Links: |
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| DOI / URN: |
10.1002/qj.2692 |
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| 245 | 1 | 4 | |a The influence of diabatic heating in the South Pacific Convergence Zone on Rossby wave propagation and the mean flow |
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| 520 | |a The South Pacific Convergence Zone (SPCZ) is a northwest‐southeast oriented precipitation band over the South Pacific Ocean. Latent heat release from condensation leads to substantial diabatic heating, which has potentially large impacts on local and global climate. The influence of this diabatic heating within the SPCZ is investigated using the Intermediate General Circulation Model (IGCM4). Precipitation in the SPCZ has been shown to be triggered by transient Rossby waves that originate in the Australian subtropical jet and are refracted towards the equatorial eastern Pacific. A Rossby wave triggers a SPCZ ‘convective event’, with associated diabatic heat release and vortex stretching. Consequently, the Rossby wave is dissipated in the SPCZ region. These features are simulated well in a control integration of IGCM4. In an experiment, convective heating is prescribed to its ‘climatological’ value in the SPCZ region during the Rossby wave ‘events’ and dynamic forcing from Rossby waves is decoupled from the usual thermodynamic response. In this experiment Rossby waves over the SPCZ region are not dissipated, confirming the vortex stretching mechanism from previous studies. Furthermore, the change in Rossby wave propagation has an impact on momentum transport. Overall, the effect of the Rossby wave‐induced convection in the SPCZ is to decrease the strength of the Pacific subtropical jet and the equatorial eastern Pacific upper‐tropospheric westerlies, by about 2–6 m s −1 . Following these changes to the basic state, two potential feedbacks in the SPCZ and larger Pacific climate system are suggested: increased SPCZ convection due to the enhancement of negative zonal stretching deformation in the SPCZ region and decreased equatorward refraction of Rossby waves into the westerly duct leading to less SPCZ ‘events’. As the convective events in the SPCZ have a significant impact on Pacific mean climate, it is crucial that the SPCZ is represented correctly in climate models. | ||
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| 650 | 4 | |a Rossby waves | |
| 650 | 4 | |a diabatic heating | |
| 650 | 4 | |a tropical‐extratropical interaction | |
| 650 | 4 | |a SPCZ | |
| 650 | 4 | |a Ocean currents | |
| 650 | 4 | |a Meteorology | |
| 650 | 4 | |a Heating | |
| 650 | 4 | |a Convergence | |
| 650 | 4 | |a Propagation | |
| 650 | 4 | |a Climate | |
| 700 | 1 | |a Matthews, Adrian J |4 oth | |
| 700 | 1 | |a Joshi, Manoj M |4 oth | |
| 700 | 1 | |a Stevens, David P |4 oth | |
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10.1002/qj.2692 doi PQ20160430 (DE-627)OLC1973548232 (DE-599)GBVOLC1973548232 (PRQ)p1172-fa90cf971300c9fafdf281a9ee0e3b3c3a9a5caba088a5f9f1f4ea29cb6c6623 (KEY)0013343420160000142069500901influenceofdiabaticheatinginthesouthpacificconverg DE-627 ger DE-627 rakwb eng 550 DNB UA 7650 AVZ rvk van der Wiel, Karin verfasserin aut The influence of diabatic heating in the South Pacific Convergence Zone on Rossby wave propagation and the mean flow 2016 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier The South Pacific Convergence Zone (SPCZ) is a northwest‐southeast oriented precipitation band over the South Pacific Ocean. Latent heat release from condensation leads to substantial diabatic heating, which has potentially large impacts on local and global climate. The influence of this diabatic heating within the SPCZ is investigated using the Intermediate General Circulation Model (IGCM4). Precipitation in the SPCZ has been shown to be triggered by transient Rossby waves that originate in the Australian subtropical jet and are refracted towards the equatorial eastern Pacific. A Rossby wave triggers a SPCZ ‘convective event’, with associated diabatic heat release and vortex stretching. Consequently, the Rossby wave is dissipated in the SPCZ region. These features are simulated well in a control integration of IGCM4. In an experiment, convective heating is prescribed to its ‘climatological’ value in the SPCZ region during the Rossby wave ‘events’ and dynamic forcing from Rossby waves is decoupled from the usual thermodynamic response. In this experiment Rossby waves over the SPCZ region are not dissipated, confirming the vortex stretching mechanism from previous studies. Furthermore, the change in Rossby wave propagation has an impact on momentum transport. Overall, the effect of the Rossby wave‐induced convection in the SPCZ is to decrease the strength of the Pacific subtropical jet and the equatorial eastern Pacific upper‐tropospheric westerlies, by about 2–6 m s −1 . Following these changes to the basic state, two potential feedbacks in the SPCZ and larger Pacific climate system are suggested: increased SPCZ convection due to the enhancement of negative zonal stretching deformation in the SPCZ region and decreased equatorward refraction of Rossby waves into the westerly duct leading to less SPCZ ‘events’. As the convective events in the SPCZ have a significant impact on Pacific mean climate, it is crucial that the SPCZ is represented correctly in climate models. Nutzungsrecht: © 2015 Royal Meteorological Society Rossby waves diabatic heating tropical‐extratropical interaction SPCZ Ocean currents Meteorology Heating Convergence Propagation Climate Matthews, Adrian J oth Joshi, Manoj M oth Stevens, David P oth Enthalten in Quarterly journal of the Royal Meteorological Society Reading : Soc., 1873 142(2016), 695, Seite 901-910 (DE-627)129079324 (DE-600)3142-2 (DE-576)014411946 0035-9009 nnns volume:142 year:2016 number:695 pages:901-910 http://dx.doi.org/10.1002/qj.2692 Volltext http://onlinelibrary.wiley.com/doi/10.1002/qj.2692/abstract http://search.proquest.com/docview/1774535765 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_62 GBV_ILN_154 GBV_ILN_601 GBV_ILN_4012 GBV_ILN_4311 UA 7650 AR 142 2016 695 901-910 |
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10.1002/qj.2692 doi PQ20160430 (DE-627)OLC1973548232 (DE-599)GBVOLC1973548232 (PRQ)p1172-fa90cf971300c9fafdf281a9ee0e3b3c3a9a5caba088a5f9f1f4ea29cb6c6623 (KEY)0013343420160000142069500901influenceofdiabaticheatinginthesouthpacificconverg DE-627 ger DE-627 rakwb eng 550 DNB UA 7650 AVZ rvk van der Wiel, Karin verfasserin aut The influence of diabatic heating in the South Pacific Convergence Zone on Rossby wave propagation and the mean flow 2016 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier The South Pacific Convergence Zone (SPCZ) is a northwest‐southeast oriented precipitation band over the South Pacific Ocean. Latent heat release from condensation leads to substantial diabatic heating, which has potentially large impacts on local and global climate. The influence of this diabatic heating within the SPCZ is investigated using the Intermediate General Circulation Model (IGCM4). Precipitation in the SPCZ has been shown to be triggered by transient Rossby waves that originate in the Australian subtropical jet and are refracted towards the equatorial eastern Pacific. A Rossby wave triggers a SPCZ ‘convective event’, with associated diabatic heat release and vortex stretching. Consequently, the Rossby wave is dissipated in the SPCZ region. These features are simulated well in a control integration of IGCM4. In an experiment, convective heating is prescribed to its ‘climatological’ value in the SPCZ region during the Rossby wave ‘events’ and dynamic forcing from Rossby waves is decoupled from the usual thermodynamic response. In this experiment Rossby waves over the SPCZ region are not dissipated, confirming the vortex stretching mechanism from previous studies. Furthermore, the change in Rossby wave propagation has an impact on momentum transport. Overall, the effect of the Rossby wave‐induced convection in the SPCZ is to decrease the strength of the Pacific subtropical jet and the equatorial eastern Pacific upper‐tropospheric westerlies, by about 2–6 m s −1 . Following these changes to the basic state, two potential feedbacks in the SPCZ and larger Pacific climate system are suggested: increased SPCZ convection due to the enhancement of negative zonal stretching deformation in the SPCZ region and decreased equatorward refraction of Rossby waves into the westerly duct leading to less SPCZ ‘events’. As the convective events in the SPCZ have a significant impact on Pacific mean climate, it is crucial that the SPCZ is represented correctly in climate models. Nutzungsrecht: © 2015 Royal Meteorological Society Rossby waves diabatic heating tropical‐extratropical interaction SPCZ Ocean currents Meteorology Heating Convergence Propagation Climate Matthews, Adrian J oth Joshi, Manoj M oth Stevens, David P oth Enthalten in Quarterly journal of the Royal Meteorological Society Reading : Soc., 1873 142(2016), 695, Seite 901-910 (DE-627)129079324 (DE-600)3142-2 (DE-576)014411946 0035-9009 nnns volume:142 year:2016 number:695 pages:901-910 http://dx.doi.org/10.1002/qj.2692 Volltext http://onlinelibrary.wiley.com/doi/10.1002/qj.2692/abstract http://search.proquest.com/docview/1774535765 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_62 GBV_ILN_154 GBV_ILN_601 GBV_ILN_4012 GBV_ILN_4311 UA 7650 AR 142 2016 695 901-910 |
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10.1002/qj.2692 doi PQ20160430 (DE-627)OLC1973548232 (DE-599)GBVOLC1973548232 (PRQ)p1172-fa90cf971300c9fafdf281a9ee0e3b3c3a9a5caba088a5f9f1f4ea29cb6c6623 (KEY)0013343420160000142069500901influenceofdiabaticheatinginthesouthpacificconverg DE-627 ger DE-627 rakwb eng 550 DNB UA 7650 AVZ rvk van der Wiel, Karin verfasserin aut The influence of diabatic heating in the South Pacific Convergence Zone on Rossby wave propagation and the mean flow 2016 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier The South Pacific Convergence Zone (SPCZ) is a northwest‐southeast oriented precipitation band over the South Pacific Ocean. Latent heat release from condensation leads to substantial diabatic heating, which has potentially large impacts on local and global climate. The influence of this diabatic heating within the SPCZ is investigated using the Intermediate General Circulation Model (IGCM4). Precipitation in the SPCZ has been shown to be triggered by transient Rossby waves that originate in the Australian subtropical jet and are refracted towards the equatorial eastern Pacific. A Rossby wave triggers a SPCZ ‘convective event’, with associated diabatic heat release and vortex stretching. Consequently, the Rossby wave is dissipated in the SPCZ region. These features are simulated well in a control integration of IGCM4. In an experiment, convective heating is prescribed to its ‘climatological’ value in the SPCZ region during the Rossby wave ‘events’ and dynamic forcing from Rossby waves is decoupled from the usual thermodynamic response. In this experiment Rossby waves over the SPCZ region are not dissipated, confirming the vortex stretching mechanism from previous studies. Furthermore, the change in Rossby wave propagation has an impact on momentum transport. Overall, the effect of the Rossby wave‐induced convection in the SPCZ is to decrease the strength of the Pacific subtropical jet and the equatorial eastern Pacific upper‐tropospheric westerlies, by about 2–6 m s −1 . Following these changes to the basic state, two potential feedbacks in the SPCZ and larger Pacific climate system are suggested: increased SPCZ convection due to the enhancement of negative zonal stretching deformation in the SPCZ region and decreased equatorward refraction of Rossby waves into the westerly duct leading to less SPCZ ‘events’. As the convective events in the SPCZ have a significant impact on Pacific mean climate, it is crucial that the SPCZ is represented correctly in climate models. Nutzungsrecht: © 2015 Royal Meteorological Society Rossby waves diabatic heating tropical‐extratropical interaction SPCZ Ocean currents Meteorology Heating Convergence Propagation Climate Matthews, Adrian J oth Joshi, Manoj M oth Stevens, David P oth Enthalten in Quarterly journal of the Royal Meteorological Society Reading : Soc., 1873 142(2016), 695, Seite 901-910 (DE-627)129079324 (DE-600)3142-2 (DE-576)014411946 0035-9009 nnns volume:142 year:2016 number:695 pages:901-910 http://dx.doi.org/10.1002/qj.2692 Volltext http://onlinelibrary.wiley.com/doi/10.1002/qj.2692/abstract http://search.proquest.com/docview/1774535765 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_62 GBV_ILN_154 GBV_ILN_601 GBV_ILN_4012 GBV_ILN_4311 UA 7650 AR 142 2016 695 901-910 |
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10.1002/qj.2692 doi PQ20160430 (DE-627)OLC1973548232 (DE-599)GBVOLC1973548232 (PRQ)p1172-fa90cf971300c9fafdf281a9ee0e3b3c3a9a5caba088a5f9f1f4ea29cb6c6623 (KEY)0013343420160000142069500901influenceofdiabaticheatinginthesouthpacificconverg DE-627 ger DE-627 rakwb eng 550 DNB UA 7650 AVZ rvk van der Wiel, Karin verfasserin aut The influence of diabatic heating in the South Pacific Convergence Zone on Rossby wave propagation and the mean flow 2016 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier The South Pacific Convergence Zone (SPCZ) is a northwest‐southeast oriented precipitation band over the South Pacific Ocean. Latent heat release from condensation leads to substantial diabatic heating, which has potentially large impacts on local and global climate. The influence of this diabatic heating within the SPCZ is investigated using the Intermediate General Circulation Model (IGCM4). Precipitation in the SPCZ has been shown to be triggered by transient Rossby waves that originate in the Australian subtropical jet and are refracted towards the equatorial eastern Pacific. A Rossby wave triggers a SPCZ ‘convective event’, with associated diabatic heat release and vortex stretching. Consequently, the Rossby wave is dissipated in the SPCZ region. These features are simulated well in a control integration of IGCM4. In an experiment, convective heating is prescribed to its ‘climatological’ value in the SPCZ region during the Rossby wave ‘events’ and dynamic forcing from Rossby waves is decoupled from the usual thermodynamic response. In this experiment Rossby waves over the SPCZ region are not dissipated, confirming the vortex stretching mechanism from previous studies. Furthermore, the change in Rossby wave propagation has an impact on momentum transport. Overall, the effect of the Rossby wave‐induced convection in the SPCZ is to decrease the strength of the Pacific subtropical jet and the equatorial eastern Pacific upper‐tropospheric westerlies, by about 2–6 m s −1 . Following these changes to the basic state, two potential feedbacks in the SPCZ and larger Pacific climate system are suggested: increased SPCZ convection due to the enhancement of negative zonal stretching deformation in the SPCZ region and decreased equatorward refraction of Rossby waves into the westerly duct leading to less SPCZ ‘events’. As the convective events in the SPCZ have a significant impact on Pacific mean climate, it is crucial that the SPCZ is represented correctly in climate models. Nutzungsrecht: © 2015 Royal Meteorological Society Rossby waves diabatic heating tropical‐extratropical interaction SPCZ Ocean currents Meteorology Heating Convergence Propagation Climate Matthews, Adrian J oth Joshi, Manoj M oth Stevens, David P oth Enthalten in Quarterly journal of the Royal Meteorological Society Reading : Soc., 1873 142(2016), 695, Seite 901-910 (DE-627)129079324 (DE-600)3142-2 (DE-576)014411946 0035-9009 nnns volume:142 year:2016 number:695 pages:901-910 http://dx.doi.org/10.1002/qj.2692 Volltext http://onlinelibrary.wiley.com/doi/10.1002/qj.2692/abstract http://search.proquest.com/docview/1774535765 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_62 GBV_ILN_154 GBV_ILN_601 GBV_ILN_4012 GBV_ILN_4311 UA 7650 AR 142 2016 695 901-910 |
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10.1002/qj.2692 doi PQ20160430 (DE-627)OLC1973548232 (DE-599)GBVOLC1973548232 (PRQ)p1172-fa90cf971300c9fafdf281a9ee0e3b3c3a9a5caba088a5f9f1f4ea29cb6c6623 (KEY)0013343420160000142069500901influenceofdiabaticheatinginthesouthpacificconverg DE-627 ger DE-627 rakwb eng 550 DNB UA 7650 AVZ rvk van der Wiel, Karin verfasserin aut The influence of diabatic heating in the South Pacific Convergence Zone on Rossby wave propagation and the mean flow 2016 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier The South Pacific Convergence Zone (SPCZ) is a northwest‐southeast oriented precipitation band over the South Pacific Ocean. Latent heat release from condensation leads to substantial diabatic heating, which has potentially large impacts on local and global climate. The influence of this diabatic heating within the SPCZ is investigated using the Intermediate General Circulation Model (IGCM4). Precipitation in the SPCZ has been shown to be triggered by transient Rossby waves that originate in the Australian subtropical jet and are refracted towards the equatorial eastern Pacific. A Rossby wave triggers a SPCZ ‘convective event’, with associated diabatic heat release and vortex stretching. Consequently, the Rossby wave is dissipated in the SPCZ region. These features are simulated well in a control integration of IGCM4. In an experiment, convective heating is prescribed to its ‘climatological’ value in the SPCZ region during the Rossby wave ‘events’ and dynamic forcing from Rossby waves is decoupled from the usual thermodynamic response. In this experiment Rossby waves over the SPCZ region are not dissipated, confirming the vortex stretching mechanism from previous studies. Furthermore, the change in Rossby wave propagation has an impact on momentum transport. Overall, the effect of the Rossby wave‐induced convection in the SPCZ is to decrease the strength of the Pacific subtropical jet and the equatorial eastern Pacific upper‐tropospheric westerlies, by about 2–6 m s −1 . Following these changes to the basic state, two potential feedbacks in the SPCZ and larger Pacific climate system are suggested: increased SPCZ convection due to the enhancement of negative zonal stretching deformation in the SPCZ region and decreased equatorward refraction of Rossby waves into the westerly duct leading to less SPCZ ‘events’. As the convective events in the SPCZ have a significant impact on Pacific mean climate, it is crucial that the SPCZ is represented correctly in climate models. Nutzungsrecht: © 2015 Royal Meteorological Society Rossby waves diabatic heating tropical‐extratropical interaction SPCZ Ocean currents Meteorology Heating Convergence Propagation Climate Matthews, Adrian J oth Joshi, Manoj M oth Stevens, David P oth Enthalten in Quarterly journal of the Royal Meteorological Society Reading : Soc., 1873 142(2016), 695, Seite 901-910 (DE-627)129079324 (DE-600)3142-2 (DE-576)014411946 0035-9009 nnns volume:142 year:2016 number:695 pages:901-910 http://dx.doi.org/10.1002/qj.2692 Volltext http://onlinelibrary.wiley.com/doi/10.1002/qj.2692/abstract http://search.proquest.com/docview/1774535765 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_62 GBV_ILN_154 GBV_ILN_601 GBV_ILN_4012 GBV_ILN_4311 UA 7650 AR 142 2016 695 901-910 |
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influence of diabatic heating in the south pacific convergence zone on rossby wave propagation and the mean flow |
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The influence of diabatic heating in the South Pacific Convergence Zone on Rossby wave propagation and the mean flow |
| abstract |
The South Pacific Convergence Zone (SPCZ) is a northwest‐southeast oriented precipitation band over the South Pacific Ocean. Latent heat release from condensation leads to substantial diabatic heating, which has potentially large impacts on local and global climate. The influence of this diabatic heating within the SPCZ is investigated using the Intermediate General Circulation Model (IGCM4). Precipitation in the SPCZ has been shown to be triggered by transient Rossby waves that originate in the Australian subtropical jet and are refracted towards the equatorial eastern Pacific. A Rossby wave triggers a SPCZ ‘convective event’, with associated diabatic heat release and vortex stretching. Consequently, the Rossby wave is dissipated in the SPCZ region. These features are simulated well in a control integration of IGCM4. In an experiment, convective heating is prescribed to its ‘climatological’ value in the SPCZ region during the Rossby wave ‘events’ and dynamic forcing from Rossby waves is decoupled from the usual thermodynamic response. In this experiment Rossby waves over the SPCZ region are not dissipated, confirming the vortex stretching mechanism from previous studies. Furthermore, the change in Rossby wave propagation has an impact on momentum transport. Overall, the effect of the Rossby wave‐induced convection in the SPCZ is to decrease the strength of the Pacific subtropical jet and the equatorial eastern Pacific upper‐tropospheric westerlies, by about 2–6 m s −1 . Following these changes to the basic state, two potential feedbacks in the SPCZ and larger Pacific climate system are suggested: increased SPCZ convection due to the enhancement of negative zonal stretching deformation in the SPCZ region and decreased equatorward refraction of Rossby waves into the westerly duct leading to less SPCZ ‘events’. As the convective events in the SPCZ have a significant impact on Pacific mean climate, it is crucial that the SPCZ is represented correctly in climate models. |
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The South Pacific Convergence Zone (SPCZ) is a northwest‐southeast oriented precipitation band over the South Pacific Ocean. Latent heat release from condensation leads to substantial diabatic heating, which has potentially large impacts on local and global climate. The influence of this diabatic heating within the SPCZ is investigated using the Intermediate General Circulation Model (IGCM4). Precipitation in the SPCZ has been shown to be triggered by transient Rossby waves that originate in the Australian subtropical jet and are refracted towards the equatorial eastern Pacific. A Rossby wave triggers a SPCZ ‘convective event’, with associated diabatic heat release and vortex stretching. Consequently, the Rossby wave is dissipated in the SPCZ region. These features are simulated well in a control integration of IGCM4. In an experiment, convective heating is prescribed to its ‘climatological’ value in the SPCZ region during the Rossby wave ‘events’ and dynamic forcing from Rossby waves is decoupled from the usual thermodynamic response. In this experiment Rossby waves over the SPCZ region are not dissipated, confirming the vortex stretching mechanism from previous studies. Furthermore, the change in Rossby wave propagation has an impact on momentum transport. Overall, the effect of the Rossby wave‐induced convection in the SPCZ is to decrease the strength of the Pacific subtropical jet and the equatorial eastern Pacific upper‐tropospheric westerlies, by about 2–6 m s −1 . Following these changes to the basic state, two potential feedbacks in the SPCZ and larger Pacific climate system are suggested: increased SPCZ convection due to the enhancement of negative zonal stretching deformation in the SPCZ region and decreased equatorward refraction of Rossby waves into the westerly duct leading to less SPCZ ‘events’. As the convective events in the SPCZ have a significant impact on Pacific mean climate, it is crucial that the SPCZ is represented correctly in climate models. |
| abstract_unstemmed |
The South Pacific Convergence Zone (SPCZ) is a northwest‐southeast oriented precipitation band over the South Pacific Ocean. Latent heat release from condensation leads to substantial diabatic heating, which has potentially large impacts on local and global climate. The influence of this diabatic heating within the SPCZ is investigated using the Intermediate General Circulation Model (IGCM4). Precipitation in the SPCZ has been shown to be triggered by transient Rossby waves that originate in the Australian subtropical jet and are refracted towards the equatorial eastern Pacific. A Rossby wave triggers a SPCZ ‘convective event’, with associated diabatic heat release and vortex stretching. Consequently, the Rossby wave is dissipated in the SPCZ region. These features are simulated well in a control integration of IGCM4. In an experiment, convective heating is prescribed to its ‘climatological’ value in the SPCZ region during the Rossby wave ‘events’ and dynamic forcing from Rossby waves is decoupled from the usual thermodynamic response. In this experiment Rossby waves over the SPCZ region are not dissipated, confirming the vortex stretching mechanism from previous studies. Furthermore, the change in Rossby wave propagation has an impact on momentum transport. Overall, the effect of the Rossby wave‐induced convection in the SPCZ is to decrease the strength of the Pacific subtropical jet and the equatorial eastern Pacific upper‐tropospheric westerlies, by about 2–6 m s −1 . Following these changes to the basic state, two potential feedbacks in the SPCZ and larger Pacific climate system are suggested: increased SPCZ convection due to the enhancement of negative zonal stretching deformation in the SPCZ region and decreased equatorward refraction of Rossby waves into the westerly duct leading to less SPCZ ‘events’. As the convective events in the SPCZ have a significant impact on Pacific mean climate, it is crucial that the SPCZ is represented correctly in climate models. |
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The influence of diabatic heating in the South Pacific Convergence Zone on Rossby wave propagation and the mean flow |
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Latent heat release from condensation leads to substantial diabatic heating, which has potentially large impacts on local and global climate. The influence of this diabatic heating within the SPCZ is investigated using the Intermediate General Circulation Model (IGCM4). Precipitation in the SPCZ has been shown to be triggered by transient Rossby waves that originate in the Australian subtropical jet and are refracted towards the equatorial eastern Pacific. A Rossby wave triggers a SPCZ ‘convective event’, with associated diabatic heat release and vortex stretching. Consequently, the Rossby wave is dissipated in the SPCZ region. These features are simulated well in a control integration of IGCM4. In an experiment, convective heating is prescribed to its ‘climatological’ value in the SPCZ region during the Rossby wave ‘events’ and dynamic forcing from Rossby waves is decoupled from the usual thermodynamic response. In this experiment Rossby waves over the SPCZ region are not dissipated, confirming the vortex stretching mechanism from previous studies. Furthermore, the change in Rossby wave propagation has an impact on momentum transport. Overall, the effect of the Rossby wave‐induced convection in the SPCZ is to decrease the strength of the Pacific subtropical jet and the equatorial eastern Pacific upper‐tropospheric westerlies, by about 2–6 m s −1 . Following these changes to the basic state, two potential feedbacks in the SPCZ and larger Pacific climate system are suggested: increased SPCZ convection due to the enhancement of negative zonal stretching deformation in the SPCZ region and decreased equatorward refraction of Rossby waves into the westerly duct leading to less SPCZ ‘events’. As the convective events in the SPCZ have a significant impact on Pacific mean climate, it is crucial that the SPCZ is represented correctly in climate models.</subfield></datafield><datafield tag="540" ind1=" " ind2=" "><subfield code="a">Nutzungsrecht: © 2015 Royal Meteorological Society</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Rossby waves</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">diabatic heating</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">tropical‐extratropical interaction</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">SPCZ</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Ocean currents</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Meteorology</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Heating</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Convergence</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Propagation</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Climate</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Matthews, Adrian J</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Joshi, Manoj M</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Stevens, David P</subfield><subfield code="4">oth</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Quarterly journal of the Royal Meteorological Society</subfield><subfield code="d">Reading : Soc., 1873</subfield><subfield code="g">142(2016), 695, Seite 901-910</subfield><subfield code="w">(DE-627)129079324</subfield><subfield code="w">(DE-600)3142-2</subfield><subfield code="w">(DE-576)014411946</subfield><subfield code="x">0035-9009</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:142</subfield><subfield code="g">year:2016</subfield><subfield code="g">number:695</subfield><subfield code="g">pages:901-910</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">http://dx.doi.org/10.1002/qj.2692</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">http://onlinelibrary.wiley.com/doi/10.1002/qj.2692/abstract</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">http://search.proquest.com/docview/1774535765</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_OLC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_62</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_154</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_601</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4012</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4311</subfield></datafield><datafield tag="936" ind1="r" ind2="v"><subfield code="a">UA 7650</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">142</subfield><subfield code="j">2016</subfield><subfield code="e">695</subfield><subfield code="h">901-910</subfield></datafield></record></collection>
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