Dynamical mechanisms linking Indian monsoon precipitation and the circumglobal teleconnection
The circumglobal teleconnection (CGT) is an important mode of circulation variability, with an influence across many parts of the northern hemisphere. Here, we examine the excitation mechanisms of the CGT in the ECMWF seasonal forecast model, and the relationship between the Indian summer monsoon (I...
| Main Authors: | , , , , , |
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| Format: | Journal article |
| Language: | English |
| Published: |
Springer
2021
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| _version_ | 1797064395187027968 |
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| author | Beverley, JD Woolnough, SJ Baker, LH Johnson, SJ Weisheimer, A O'Reilly, CH |
| author_facet | Beverley, JD Woolnough, SJ Baker, LH Johnson, SJ Weisheimer, A O'Reilly, CH |
| author_sort | Beverley, JD |
| collection | OXFORD |
| description | The circumglobal teleconnection (CGT) is an important mode of circulation variability, with an influence across many parts of the northern hemisphere. Here, we examine the excitation mechanisms of the CGT in the ECMWF seasonal forecast model, and the relationship between the Indian summer monsoon (ISM), the CGT and the extratropical northern hemisphere circulation. Results from relaxation experiments, in which the model is corrected to reanalysis in specific regions, suggest that errors over northwest Europe are more important in inhibiting the model skill at representing the CGT, in addition to northern hemisphere skill more widely, than west-central Asia and the ISM region, although the link between ISM precipitation and the extratropical circulation is weak in all experiments. Thermal forcing experiments in the ECMWF model, in which a heating is applied over India, suggest that the ISM does force an extratropical Rossby wave train, with upper tropospheric anticyclonic anomalies over east Asia, the North Pacific and North America associated with increased ISM heating. However, this eastward-propagating branch of the wave train does not project into Europe, and the response there occurs largely through westward-propagating Rossby waves. Results from barotropic model experiments show a response that is highly consistent with the seasonal forecast model, with similar eastward- and westward-propagating Rossby waves. This westward-propagating response is shown to be important in the downstream reinforcement of the wave train between Asia and North America. |
| first_indexed | 2024-03-06T21:13:40Z |
| format | Journal article |
| id | oxford-uuid:3f092a39-e069-4555-ad22-312a68557938 |
| institution | University of Oxford |
| language | English |
| last_indexed | 2024-03-06T21:13:40Z |
| publishDate | 2021 |
| publisher | Springer |
| record_format | dspace |
| spelling | oxford-uuid:3f092a39-e069-4555-ad22-312a685579382022-03-26T14:29:26ZDynamical mechanisms linking Indian monsoon precipitation and the circumglobal teleconnectionJournal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:3f092a39-e069-4555-ad22-312a68557938EnglishSymplectic ElementsSpringer2021Beverley, JDWoolnough, SJBaker, LHJohnson, SJWeisheimer, AO'Reilly, CHThe circumglobal teleconnection (CGT) is an important mode of circulation variability, with an influence across many parts of the northern hemisphere. Here, we examine the excitation mechanisms of the CGT in the ECMWF seasonal forecast model, and the relationship between the Indian summer monsoon (ISM), the CGT and the extratropical northern hemisphere circulation. Results from relaxation experiments, in which the model is corrected to reanalysis in specific regions, suggest that errors over northwest Europe are more important in inhibiting the model skill at representing the CGT, in addition to northern hemisphere skill more widely, than west-central Asia and the ISM region, although the link between ISM precipitation and the extratropical circulation is weak in all experiments. Thermal forcing experiments in the ECMWF model, in which a heating is applied over India, suggest that the ISM does force an extratropical Rossby wave train, with upper tropospheric anticyclonic anomalies over east Asia, the North Pacific and North America associated with increased ISM heating. However, this eastward-propagating branch of the wave train does not project into Europe, and the response there occurs largely through westward-propagating Rossby waves. Results from barotropic model experiments show a response that is highly consistent with the seasonal forecast model, with similar eastward- and westward-propagating Rossby waves. This westward-propagating response is shown to be important in the downstream reinforcement of the wave train between Asia and North America. |
| spellingShingle | Beverley, JD Woolnough, SJ Baker, LH Johnson, SJ Weisheimer, A O'Reilly, CH Dynamical mechanisms linking Indian monsoon precipitation and the circumglobal teleconnection |
| title | Dynamical mechanisms linking Indian monsoon precipitation and the circumglobal teleconnection |
| title_full | Dynamical mechanisms linking Indian monsoon precipitation and the circumglobal teleconnection |
| title_fullStr | Dynamical mechanisms linking Indian monsoon precipitation and the circumglobal teleconnection |
| title_full_unstemmed | Dynamical mechanisms linking Indian monsoon precipitation and the circumglobal teleconnection |
| title_short | Dynamical mechanisms linking Indian monsoon precipitation and the circumglobal teleconnection |
| title_sort | dynamical mechanisms linking indian monsoon precipitation and the circumglobal teleconnection |
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