Climate change in terms of modes of atmospheric variability and circulation regimes over southern South America
The simulated low-frequency variability patterns of the atmospheric circulation, ranging from interannual to interdecadal timescales, are studied in an area encompassing southern South America. The experiment is a transient simulation performed with the IPSL CCM2 coupled global model, in which the g...
Guardado en:
| Publicado: |
2006
|
|---|---|
| Materias: | |
| Acceso en línea: | https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_09307575_v26_n7-8_p835_Solman http://hdl.handle.net/20.500.12110/paper_09307575_v26_n7-8_p835_Solman |
| Aporte de: |
| id |
paper:paper_09307575_v26_n7-8_p835_Solman |
|---|---|
| record_format |
dspace |
| spelling |
paper:paper_09307575_v26_n7-8_p835_Solman2023-06-08T15:52:36Z Climate change in terms of modes of atmospheric variability and circulation regimes over southern South America annual variation atmospheric circulation climate change decadal variation South America The simulated low-frequency variability patterns of the atmospheric circulation, ranging from interannual to interdecadal timescales, are studied in an area encompassing southern South America. The experiment is a transient simulation performed with the IPSL CCM2 coupled global model, in which the greenhouse forcing is continuously increasing. The main modes of low-frequency variability are found to remain stationary throughout the simulation, suggesting they depend more on the internal dynamics of the atmospheric flow than on its external forcing. Inspection of the circulation regimes that represent the more recurrent patterns at interannual and interdecadal timescales showed that climate change manifests itself as a change in regime population, suggesting that the negative phase of the Antarctic Oscillation-like pattern becomes more frequented in a climate change scenario. Changes of regime occurrence are superimposed to a positive trend whose spatial pattern is reminiscent of the structure of the Antarctic Oscillation-mode of variability. Moreover, it resembles the spatial patterns of those regimes that show a significant change in population. The change in regime frequencies of the circulation patterns of low-frequency variability are in opposite phase with respect to the trend, thus, the behaviour of these patterns of variability, superimposed to a changing mean state, modulates the climate change signal. The analysis of the high frequencies, in terms of recurrent patterns representing intraseasonal and synoptic-scale of variability, shows no significant changes in regime characteristics, concerning both spatial and temporal behaviour. © Springer-Verlag 2006. 2006 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_09307575_v26_n7-8_p835_Solman http://hdl.handle.net/20.500.12110/paper_09307575_v26_n7-8_p835_Solman |
| institution |
Universidad de Buenos Aires |
| institution_str |
I-28 |
| repository_str |
R-134 |
| collection |
Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) |
| topic |
annual variation atmospheric circulation climate change decadal variation South America |
| spellingShingle |
annual variation atmospheric circulation climate change decadal variation South America Climate change in terms of modes of atmospheric variability and circulation regimes over southern South America |
| topic_facet |
annual variation atmospheric circulation climate change decadal variation South America |
| description |
The simulated low-frequency variability patterns of the atmospheric circulation, ranging from interannual to interdecadal timescales, are studied in an area encompassing southern South America. The experiment is a transient simulation performed with the IPSL CCM2 coupled global model, in which the greenhouse forcing is continuously increasing. The main modes of low-frequency variability are found to remain stationary throughout the simulation, suggesting they depend more on the internal dynamics of the atmospheric flow than on its external forcing. Inspection of the circulation regimes that represent the more recurrent patterns at interannual and interdecadal timescales showed that climate change manifests itself as a change in regime population, suggesting that the negative phase of the Antarctic Oscillation-like pattern becomes more frequented in a climate change scenario. Changes of regime occurrence are superimposed to a positive trend whose spatial pattern is reminiscent of the structure of the Antarctic Oscillation-mode of variability. Moreover, it resembles the spatial patterns of those regimes that show a significant change in population. The change in regime frequencies of the circulation patterns of low-frequency variability are in opposite phase with respect to the trend, thus, the behaviour of these patterns of variability, superimposed to a changing mean state, modulates the climate change signal. The analysis of the high frequencies, in terms of recurrent patterns representing intraseasonal and synoptic-scale of variability, shows no significant changes in regime characteristics, concerning both spatial and temporal behaviour. © Springer-Verlag 2006. |
| title |
Climate change in terms of modes of atmospheric variability and circulation regimes over southern South America |
| title_short |
Climate change in terms of modes of atmospheric variability and circulation regimes over southern South America |
| title_full |
Climate change in terms of modes of atmospheric variability and circulation regimes over southern South America |
| title_fullStr |
Climate change in terms of modes of atmospheric variability and circulation regimes over southern South America |
| title_full_unstemmed |
Climate change in terms of modes of atmospheric variability and circulation regimes over southern South America |
| title_sort |
climate change in terms of modes of atmospheric variability and circulation regimes over southern south america |
| publishDate |
2006 |
| url |
https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_09307575_v26_n7-8_p835_Solman http://hdl.handle.net/20.500.12110/paper_09307575_v26_n7-8_p835_Solman |
| _version_ |
1768545745638522880 |