Distinguishing changes in the Hadley circulation edge
Abstract The studies on poleward expansion of the Hadley circulation have mainly concentrated on linear trends with global warming. There is no consensus on how the edge of the Hadley circulation has been affected by the dynamical linkage to causes of change. Here, this study strives to make a robus...
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| Autor*in: |
Moon, Hyejin [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2019 |
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| Schlagwörter: |
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| Systematik: |
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| Anmerkung: |
© Springer-Verlag GmbH Austria, part of Springer Nature 2019 |
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| Übergeordnetes Werk: |
Enthalten in: Theoretical and applied climatology - Springer Vienna, 1986, 139(2019), 3-4 vom: 15. Nov., Seite 1007-1017 |
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| Übergeordnetes Werk: |
volume:139 ; year:2019 ; number:3-4 ; day:15 ; month:11 ; pages:1007-1017 |
| Links: |
|---|
| DOI / URN: |
10.1007/s00704-019-03017-1 |
|---|
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OLC2048472222 |
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| 520 | |a Abstract The studies on poleward expansion of the Hadley circulation have mainly concentrated on linear trends with global warming. There is no consensus on how the edge of the Hadley circulation has been affected by the dynamical linkage to causes of change. Here, this study strives to make a robust assessment of the changes in the edge latitude of the Hadley circulation by comparing two reanalysis datasets and two theoretical models, namely the Held and Hou. J Atmos Res 37: 515-533; (1980) model (HH80) and Held (2000) model (He00). A poleward shift in both hemispheres emerged after the mid-1990s in the two reanalysis datasets, except for the Northern Hemisphere from ERA-Interim. Comparing the edge latitudes of the two reanalysis datasets, HH80 (He00) is seen to be out of phase (in-phase) in the Hadley circulation edge. He00 only shows interdecadal change regarding the poleward expansion of the Hadley circulation. We found that the dominant factors affecting change in the edge latitude of the Hadley circulation were the subtropical static stability and subtropical tropopause height. The changes in the Hadley circulation in the Northern Hemisphere (Southern Hemisphere) are associated with negative ENSO and positive AO (positive SAM). | ||
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10.1007/s00704-019-03017-1 doi (DE-627)OLC2048472222 (DE-He213)s00704-019-03017-1-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk Moon, Hyejin verfasserin aut Distinguishing changes in the Hadley circulation edge 2019 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag GmbH Austria, part of Springer Nature 2019 Abstract The studies on poleward expansion of the Hadley circulation have mainly concentrated on linear trends with global warming. There is no consensus on how the edge of the Hadley circulation has been affected by the dynamical linkage to causes of change. Here, this study strives to make a robust assessment of the changes in the edge latitude of the Hadley circulation by comparing two reanalysis datasets and two theoretical models, namely the Held and Hou. J Atmos Res 37: 515-533; (1980) model (HH80) and Held (2000) model (He00). A poleward shift in both hemispheres emerged after the mid-1990s in the two reanalysis datasets, except for the Northern Hemisphere from ERA-Interim. Comparing the edge latitudes of the two reanalysis datasets, HH80 (He00) is seen to be out of phase (in-phase) in the Hadley circulation edge. He00 only shows interdecadal change regarding the poleward expansion of the Hadley circulation. We found that the dominant factors affecting change in the edge latitude of the Hadley circulation were the subtropical static stability and subtropical tropopause height. The changes in the Hadley circulation in the Northern Hemisphere (Southern Hemisphere) are associated with negative ENSO and positive AO (positive SAM). Hadley circulation Hadley circulation edge Tropopause height Static stability Held model Ha, Kyung-Ja (orcid)0000-0003-1753-9304 aut Enthalten in Theoretical and applied climatology Springer Vienna, 1986 139(2019), 3-4 vom: 15. Nov., Seite 1007-1017 (DE-627)129958808 (DE-600)405799-5 (DE-576)01552857X 0177-798X nnns volume:139 year:2019 number:3-4 day:15 month:11 pages:1007-1017 https://doi.org/10.1007/s00704-019-03017-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_4313 RA 1000 AR 139 2019 3-4 15 11 1007-1017 |
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10.1007/s00704-019-03017-1 doi (DE-627)OLC2048472222 (DE-He213)s00704-019-03017-1-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk Moon, Hyejin verfasserin aut Distinguishing changes in the Hadley circulation edge 2019 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag GmbH Austria, part of Springer Nature 2019 Abstract The studies on poleward expansion of the Hadley circulation have mainly concentrated on linear trends with global warming. There is no consensus on how the edge of the Hadley circulation has been affected by the dynamical linkage to causes of change. Here, this study strives to make a robust assessment of the changes in the edge latitude of the Hadley circulation by comparing two reanalysis datasets and two theoretical models, namely the Held and Hou. J Atmos Res 37: 515-533; (1980) model (HH80) and Held (2000) model (He00). A poleward shift in both hemispheres emerged after the mid-1990s in the two reanalysis datasets, except for the Northern Hemisphere from ERA-Interim. Comparing the edge latitudes of the two reanalysis datasets, HH80 (He00) is seen to be out of phase (in-phase) in the Hadley circulation edge. He00 only shows interdecadal change regarding the poleward expansion of the Hadley circulation. We found that the dominant factors affecting change in the edge latitude of the Hadley circulation were the subtropical static stability and subtropical tropopause height. The changes in the Hadley circulation in the Northern Hemisphere (Southern Hemisphere) are associated with negative ENSO and positive AO (positive SAM). Hadley circulation Hadley circulation edge Tropopause height Static stability Held model Ha, Kyung-Ja (orcid)0000-0003-1753-9304 aut Enthalten in Theoretical and applied climatology Springer Vienna, 1986 139(2019), 3-4 vom: 15. Nov., Seite 1007-1017 (DE-627)129958808 (DE-600)405799-5 (DE-576)01552857X 0177-798X nnns volume:139 year:2019 number:3-4 day:15 month:11 pages:1007-1017 https://doi.org/10.1007/s00704-019-03017-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_4313 RA 1000 AR 139 2019 3-4 15 11 1007-1017 |
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10.1007/s00704-019-03017-1 doi (DE-627)OLC2048472222 (DE-He213)s00704-019-03017-1-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk Moon, Hyejin verfasserin aut Distinguishing changes in the Hadley circulation edge 2019 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag GmbH Austria, part of Springer Nature 2019 Abstract The studies on poleward expansion of the Hadley circulation have mainly concentrated on linear trends with global warming. There is no consensus on how the edge of the Hadley circulation has been affected by the dynamical linkage to causes of change. Here, this study strives to make a robust assessment of the changes in the edge latitude of the Hadley circulation by comparing two reanalysis datasets and two theoretical models, namely the Held and Hou. J Atmos Res 37: 515-533; (1980) model (HH80) and Held (2000) model (He00). A poleward shift in both hemispheres emerged after the mid-1990s in the two reanalysis datasets, except for the Northern Hemisphere from ERA-Interim. Comparing the edge latitudes of the two reanalysis datasets, HH80 (He00) is seen to be out of phase (in-phase) in the Hadley circulation edge. He00 only shows interdecadal change regarding the poleward expansion of the Hadley circulation. We found that the dominant factors affecting change in the edge latitude of the Hadley circulation were the subtropical static stability and subtropical tropopause height. The changes in the Hadley circulation in the Northern Hemisphere (Southern Hemisphere) are associated with negative ENSO and positive AO (positive SAM). Hadley circulation Hadley circulation edge Tropopause height Static stability Held model Ha, Kyung-Ja (orcid)0000-0003-1753-9304 aut Enthalten in Theoretical and applied climatology Springer Vienna, 1986 139(2019), 3-4 vom: 15. Nov., Seite 1007-1017 (DE-627)129958808 (DE-600)405799-5 (DE-576)01552857X 0177-798X nnns volume:139 year:2019 number:3-4 day:15 month:11 pages:1007-1017 https://doi.org/10.1007/s00704-019-03017-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_4313 RA 1000 AR 139 2019 3-4 15 11 1007-1017 |
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Distinguishing changes in the Hadley circulation edge |
| abstract |
Abstract The studies on poleward expansion of the Hadley circulation have mainly concentrated on linear trends with global warming. There is no consensus on how the edge of the Hadley circulation has been affected by the dynamical linkage to causes of change. Here, this study strives to make a robust assessment of the changes in the edge latitude of the Hadley circulation by comparing two reanalysis datasets and two theoretical models, namely the Held and Hou. J Atmos Res 37: 515-533; (1980) model (HH80) and Held (2000) model (He00). A poleward shift in both hemispheres emerged after the mid-1990s in the two reanalysis datasets, except for the Northern Hemisphere from ERA-Interim. Comparing the edge latitudes of the two reanalysis datasets, HH80 (He00) is seen to be out of phase (in-phase) in the Hadley circulation edge. He00 only shows interdecadal change regarding the poleward expansion of the Hadley circulation. We found that the dominant factors affecting change in the edge latitude of the Hadley circulation were the subtropical static stability and subtropical tropopause height. The changes in the Hadley circulation in the Northern Hemisphere (Southern Hemisphere) are associated with negative ENSO and positive AO (positive SAM). © Springer-Verlag GmbH Austria, part of Springer Nature 2019 |
| abstractGer |
Abstract The studies on poleward expansion of the Hadley circulation have mainly concentrated on linear trends with global warming. There is no consensus on how the edge of the Hadley circulation has been affected by the dynamical linkage to causes of change. Here, this study strives to make a robust assessment of the changes in the edge latitude of the Hadley circulation by comparing two reanalysis datasets and two theoretical models, namely the Held and Hou. J Atmos Res 37: 515-533; (1980) model (HH80) and Held (2000) model (He00). A poleward shift in both hemispheres emerged after the mid-1990s in the two reanalysis datasets, except for the Northern Hemisphere from ERA-Interim. Comparing the edge latitudes of the two reanalysis datasets, HH80 (He00) is seen to be out of phase (in-phase) in the Hadley circulation edge. He00 only shows interdecadal change regarding the poleward expansion of the Hadley circulation. We found that the dominant factors affecting change in the edge latitude of the Hadley circulation were the subtropical static stability and subtropical tropopause height. The changes in the Hadley circulation in the Northern Hemisphere (Southern Hemisphere) are associated with negative ENSO and positive AO (positive SAM). © Springer-Verlag GmbH Austria, part of Springer Nature 2019 |
| abstract_unstemmed |
Abstract The studies on poleward expansion of the Hadley circulation have mainly concentrated on linear trends with global warming. There is no consensus on how the edge of the Hadley circulation has been affected by the dynamical linkage to causes of change. Here, this study strives to make a robust assessment of the changes in the edge latitude of the Hadley circulation by comparing two reanalysis datasets and two theoretical models, namely the Held and Hou. J Atmos Res 37: 515-533; (1980) model (HH80) and Held (2000) model (He00). A poleward shift in both hemispheres emerged after the mid-1990s in the two reanalysis datasets, except for the Northern Hemisphere from ERA-Interim. Comparing the edge latitudes of the two reanalysis datasets, HH80 (He00) is seen to be out of phase (in-phase) in the Hadley circulation edge. He00 only shows interdecadal change regarding the poleward expansion of the Hadley circulation. We found that the dominant factors affecting change in the edge latitude of the Hadley circulation were the subtropical static stability and subtropical tropopause height. The changes in the Hadley circulation in the Northern Hemisphere (Southern Hemisphere) are associated with negative ENSO and positive AO (positive SAM). © Springer-Verlag GmbH Austria, part of Springer Nature 2019 |
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GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_4313 |
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3-4 |
| title_short |
Distinguishing changes in the Hadley circulation edge |
| url |
https://doi.org/10.1007/s00704-019-03017-1 |
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| author2 |
Ha, Kyung-Ja |
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| doi_str |
10.1007/s00704-019-03017-1 |
| up_date |
2024-07-03T18:53:08.261Z |
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