Surface air temperature (t2m) data are essential for understanding climate dynamics and assessing the impacts of climate change. Reanalysis products, which combine observations with retrospective short-range weather forecasts, can provide consistent and comprehensive datasets. ERA5 represents the state-of-the-art in global reanalyses and supplies initial and boundary conditions for higher-resolution regional reanalyses designed to capture finer-scale atmospheric processes. However, these products require validation, especially in complex terrains like Italy. This study analyzes the capability of different reanalysis products to reproduce t2m fields over Italy during the 1991-2020 period. The analyses encompass ERA5, ERA5-Land, the MEteorological Reanalysis Italian DAtaset (MERIDA), the Copernicus European Regional ReAnalysis (CERRA), and the Very High-Resolution dynamical downscaling of ERA5 REAnalysis over ITaly (VHR-REA_IT). The validation we conduct pertains to both the spatial distribution of 30-year seasonal and annual normal values and the daily anomaly records. Each reanalysis is compared with observations projected onto its respective grid positions and elevations, overcoming any model bias resulting from an inaccurate representation of the real topography. Key findings reveal that normal values in reanalyses closely match observational values, with deviations typically below 1°C. However, in the Alps, winter cold biases sometimes exceed 3°C and show a relation with the elevation. Similar deviations occur in the Apennines, Sicily, Sardinia. VHR-REA_IT, on the contrary, presents a warm summer bias of about +3 °C on average over the Po valley. Daily anomalies generally exhibit lower errors, with MERIDA showing the highest accuracy. Moreover, when aggregating daily anomalies to annual time scales, the errors in the anomaly records rapidly decrease to less than 0.5 °C. The results of this study empower reanalysis users across multiple sectors to gain a more profound insight into the capabilities and constraints of different reanalysis products. This knowledge, in turn, enables them to make well-informed choices when incorporating these products into their research and practical applications.

Inter-comparison and validation of high-resolution surface air temperature reanalysis fields over Italy / F. Cavalleri, F. Viterbo, M. Brunetti, R. Bonanno, V. Manara, C. Lussana, M. Lacavalla, M. Maugeri. ((Intervento presentato al 25. convegno Annual Meeting of the European Meteorological Society tenutosi a Barcelona nel 2024.

Inter-comparison and validation of high-resolution surface air temperature reanalysis fields over Italy

F. Cavalleri;V. Manara;M. Maugeri
2024

Abstract

Surface air temperature (t2m) data are essential for understanding climate dynamics and assessing the impacts of climate change. Reanalysis products, which combine observations with retrospective short-range weather forecasts, can provide consistent and comprehensive datasets. ERA5 represents the state-of-the-art in global reanalyses and supplies initial and boundary conditions for higher-resolution regional reanalyses designed to capture finer-scale atmospheric processes. However, these products require validation, especially in complex terrains like Italy. This study analyzes the capability of different reanalysis products to reproduce t2m fields over Italy during the 1991-2020 period. The analyses encompass ERA5, ERA5-Land, the MEteorological Reanalysis Italian DAtaset (MERIDA), the Copernicus European Regional ReAnalysis (CERRA), and the Very High-Resolution dynamical downscaling of ERA5 REAnalysis over ITaly (VHR-REA_IT). The validation we conduct pertains to both the spatial distribution of 30-year seasonal and annual normal values and the daily anomaly records. Each reanalysis is compared with observations projected onto its respective grid positions and elevations, overcoming any model bias resulting from an inaccurate representation of the real topography. Key findings reveal that normal values in reanalyses closely match observational values, with deviations typically below 1°C. However, in the Alps, winter cold biases sometimes exceed 3°C and show a relation with the elevation. Similar deviations occur in the Apennines, Sicily, Sardinia. VHR-REA_IT, on the contrary, presents a warm summer bias of about +3 °C on average over the Po valley. Daily anomalies generally exhibit lower errors, with MERIDA showing the highest accuracy. Moreover, when aggregating daily anomalies to annual time scales, the errors in the anomaly records rapidly decrease to less than 0.5 °C. The results of this study empower reanalysis users across multiple sectors to gain a more profound insight into the capabilities and constraints of different reanalysis products. This knowledge, in turn, enables them to make well-informed choices when incorporating these products into their research and practical applications.
6-set-2024
Reanalysis; surface air temperature; ERA5; validation; complex orography
Settore PHYS-05/B - Fisica del sistema Terra, dei pianeti, dello spazio e del clima
European Meteorological Society
https://doi.org/10.5194/ems2024-67
Inter-comparison and validation of high-resolution surface air temperature reanalysis fields over Italy / F. Cavalleri, F. Viterbo, M. Brunetti, R. Bonanno, V. Manara, C. Lussana, M. Lacavalla, M. Maugeri. ((Intervento presentato al 25. convegno Annual Meeting of the European Meteorological Society tenutosi a Barcelona nel 2024.
Conference Object
File in questo prodotto:
File Dimensione Formato  
EMS_2024-67_OSA33_Cavalleri.pdf

accesso aperto

Descrizione: slideshow
Tipologia: Altro
Dimensione 15.11 MB
Formato Adobe PDF
15.11 MB Adobe PDF Visualizza/Apri
Pubblicazioni consigliate

I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.

Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/2434/1105110
Citazioni
  • ???jsp.display-item.citation.pmc??? ND
  • Scopus ND
  • ???jsp.display-item.citation.isi??? ND
social impact