Climate change over the extratropical Southern Hemisphere: The tale from an ensemble of reanalysis datasets
In this study, a set of five reanalysis datasets [ERA-Interim, NCEP-DOE AMIP-II reanalysis (R2), MERRA, the Twentieth Century Reanalysis (20CR), and the CFS Reanalysis (CFSR)] is used to provide a robust estimation of precipitation change in the middle-to-high latitudes of the Southern Hemisphere du...
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paper:paper_08948755_v29_n5_p1673_Solman2023-06-08T15:47:55Z Climate change over the extratropical Southern Hemisphere: The tale from an ensemble of reanalysis datasets Solman, Silvina Alicia Orlanski, Isidoro Atm/ocean structure/phenomena Circulation/dynamics Databases Extratropical cyclones Large-scale motions Models and modeling Observational techniques and algorithms Precipitation Reanalysis data Trends Variability Database systems Greenhouse gases Inverse problems Moisture Ozone layer Precipitation (chemical) Storms Extratropical cyclones Large scale motion Reanalysis Trends Variability Climate change algorithm atmospheric modeling climate change data set ensemble forecasting precipitation (climatology) Southern Hemisphere trend analysis tropical cyclone In this study, a set of five reanalysis datasets [ERA-Interim, NCEP-DOE AMIP-II reanalysis (R2), MERRA, the Twentieth Century Reanalysis (20CR), and the CFS Reanalysis (CFSR)] is used to provide a robust estimation of precipitation change in the middle-to-high latitudes of the Southern Hemisphere during the last three decades. Based on several metrics accounting for the eddy activity and moisture availability, an attempt is also made to identify the dynamical mechanisms triggering these changes during extended summer and winter seasons. To that aim, a weighted reanalysis ensemble is built using the inverse of the variance as weighting factors for each variable. Results showed that the weighted reanalysis ensemble reproduced the observed precipitation changes at high and middle latitudes during the two seasons, as depicted by the GPCP dataset. For the extended summer season, precipitation changes were dynamically consistent with changes in the eddy activity, attributed mostly to ozone depletion. For the extended winter season, the eddy activity and moisture availability both contributed to the precipitation changes, with the increased concentration of greenhouse gases being the main driver of the climate change signal. In addition, output from a five-member ensemble of the high-resolution GFDL CM2.5 for the period 1979-2010 was used in order to explore the capability of the model in reproducing both the observed precipitation change and the underlying dynamical mechanisms. The model was able to capture the rainfall change signal. However, the increased availability of moisture from the lower levels controls the precipitation change during both summer and winter. © 2016 American Meteorological Society. Fil:Solman, S.A. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Orlanski, I. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. 2016 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_08948755_v29_n5_p1673_Solman http://hdl.handle.net/20.500.12110/paper_08948755_v29_n5_p1673_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 |
Atm/ocean structure/phenomena Circulation/dynamics Databases Extratropical cyclones Large-scale motions Models and modeling Observational techniques and algorithms Precipitation Reanalysis data Trends Variability Database systems Greenhouse gases Inverse problems Moisture Ozone layer Precipitation (chemical) Storms Extratropical cyclones Large scale motion Reanalysis Trends Variability Climate change algorithm atmospheric modeling climate change data set ensemble forecasting precipitation (climatology) Southern Hemisphere trend analysis tropical cyclone |
spellingShingle |
Atm/ocean structure/phenomena Circulation/dynamics Databases Extratropical cyclones Large-scale motions Models and modeling Observational techniques and algorithms Precipitation Reanalysis data Trends Variability Database systems Greenhouse gases Inverse problems Moisture Ozone layer Precipitation (chemical) Storms Extratropical cyclones Large scale motion Reanalysis Trends Variability Climate change algorithm atmospheric modeling climate change data set ensemble forecasting precipitation (climatology) Southern Hemisphere trend analysis tropical cyclone Solman, Silvina Alicia Orlanski, Isidoro Climate change over the extratropical Southern Hemisphere: The tale from an ensemble of reanalysis datasets |
topic_facet |
Atm/ocean structure/phenomena Circulation/dynamics Databases Extratropical cyclones Large-scale motions Models and modeling Observational techniques and algorithms Precipitation Reanalysis data Trends Variability Database systems Greenhouse gases Inverse problems Moisture Ozone layer Precipitation (chemical) Storms Extratropical cyclones Large scale motion Reanalysis Trends Variability Climate change algorithm atmospheric modeling climate change data set ensemble forecasting precipitation (climatology) Southern Hemisphere trend analysis tropical cyclone |
description |
In this study, a set of five reanalysis datasets [ERA-Interim, NCEP-DOE AMIP-II reanalysis (R2), MERRA, the Twentieth Century Reanalysis (20CR), and the CFS Reanalysis (CFSR)] is used to provide a robust estimation of precipitation change in the middle-to-high latitudes of the Southern Hemisphere during the last three decades. Based on several metrics accounting for the eddy activity and moisture availability, an attempt is also made to identify the dynamical mechanisms triggering these changes during extended summer and winter seasons. To that aim, a weighted reanalysis ensemble is built using the inverse of the variance as weighting factors for each variable. Results showed that the weighted reanalysis ensemble reproduced the observed precipitation changes at high and middle latitudes during the two seasons, as depicted by the GPCP dataset. For the extended summer season, precipitation changes were dynamically consistent with changes in the eddy activity, attributed mostly to ozone depletion. For the extended winter season, the eddy activity and moisture availability both contributed to the precipitation changes, with the increased concentration of greenhouse gases being the main driver of the climate change signal. In addition, output from a five-member ensemble of the high-resolution GFDL CM2.5 for the period 1979-2010 was used in order to explore the capability of the model in reproducing both the observed precipitation change and the underlying dynamical mechanisms. The model was able to capture the rainfall change signal. However, the increased availability of moisture from the lower levels controls the precipitation change during both summer and winter. © 2016 American Meteorological Society. |
author |
Solman, Silvina Alicia Orlanski, Isidoro |
author_facet |
Solman, Silvina Alicia Orlanski, Isidoro |
author_sort |
Solman, Silvina Alicia |
title |
Climate change over the extratropical Southern Hemisphere: The tale from an ensemble of reanalysis datasets |
title_short |
Climate change over the extratropical Southern Hemisphere: The tale from an ensemble of reanalysis datasets |
title_full |
Climate change over the extratropical Southern Hemisphere: The tale from an ensemble of reanalysis datasets |
title_fullStr |
Climate change over the extratropical Southern Hemisphere: The tale from an ensemble of reanalysis datasets |
title_full_unstemmed |
Climate change over the extratropical Southern Hemisphere: The tale from an ensemble of reanalysis datasets |
title_sort |
climate change over the extratropical southern hemisphere: the tale from an ensemble of reanalysis datasets |
publishDate |
2016 |
url |
https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_08948755_v29_n5_p1673_Solman http://hdl.handle.net/20.500.12110/paper_08948755_v29_n5_p1673_Solman |
work_keys_str_mv |
AT solmansilvinaalicia climatechangeovertheextratropicalsouthernhemispherethetalefromanensembleofreanalysisdatasets AT orlanskiisidoro climatechangeovertheextratropicalsouthernhemispherethetalefromanensembleofreanalysisdatasets |
_version_ |
1768542132758380544 |