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reference : The seasonal footprinting mechanism in the Pacific: Implications for ENSO
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/report/climate-science-special-report/chapter/circulation-variability/reference/004ee9da-c802-4c6a-a315-3a128dd7cf37
/report/climate-science-special-report/chapter/circulation-variability/reference/004ee9da-c802-4c6a-a315-3a128dd7cf37
Referencing Publications:
Reference URIs:
Reference URIs:
- /reference/004ee9da-c802-4c6a-a315-3a128dd7cf37
- /report/climate-science-special-report/reference/004ee9da-c802-4c6a-a315-3a128dd7cf37
- /report/climate-science-special-report/chapter/circulation-variability/reference/004ee9da-c802-4c6a-a315-3a128dd7cf37
Referenced Publication:
article
reftype | Journal Article |
Abstract | Midlatitude atmospheric variability is identified as a particularly effective component of the stochastic forcing of ENSO. This forcing is realized via a seasonal footprinting mechanism (SFM), in which the tropical atmosphere is forced during the spring and summer by SST anomalies generated by midlatitude atmospheric variability during the previous winter. The strong relationship between the SFM and ENSO may serve to enhance ENSO predictability and supports the view that ENSO is linearly stable in nature. |
Author | Daniel J. Vimont; John M. Wallace; David S. Battisti |
DOI | 10.1175/1520-0442(2003)016<2668:tsfmit>2.0.co;2 |
Issue | 16 |
Journal | Journal of Climate |
Pages | 2668-2675 |
Title | The seasonal footprinting mechanism in the Pacific: Implications for ENSO |
Volume | 16 |
Year | 2003 |
.reference_type | 0 |
_record_number | 20905 |
_uuid | 004ee9da-c802-4c6a-a315-3a128dd7cf37 |