Towards a convection‐permitting regional reanalysis over the Italian domain
Abstract A new convection‐permitting regional reanalysis, SPHERA (High Resolution REAnalysis over Italy), has been developed over Italy and the surrounding seas using the COSMO model at 2.2 km horizontal resolution. The reanalysis system is nested in the global reanalysis ERA5; upper‐air and surface...
| Main Authors: | , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Wiley
2022-09-01
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| Series: | Meteorological Applications |
| Subjects: | |
| Online Access: | https://doi.org/10.1002/met.2092 |
| _version_ | 1811335888564649984 |
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| author | Ines Maria Luisa Cerenzia Antonio Giordani Tiziana Paccagnella Andrea Montani |
| author_facet | Ines Maria Luisa Cerenzia Antonio Giordani Tiziana Paccagnella Andrea Montani |
| author_sort | Ines Maria Luisa Cerenzia |
| collection | DOAJ |
| description | Abstract A new convection‐permitting regional reanalysis, SPHERA (High Resolution REAnalysis over Italy), has been developed over Italy and the surrounding seas using the COSMO model at 2.2 km horizontal resolution. The reanalysis system is nested in the global reanalysis ERA5; upper‐air and surface observations are assimilated at the convection‐permitting scale by the COSMO nudging scheme. Before the complete production of the hourly three‐dimensional fields and surface/soil parameters over the period 1995–2020, general issues regarding the reanalysis set‐up needed to be addressed over a shorter test period. These include the identification of the best approach to downscale the lateral boundary conditions from the global driver, and the definition of the bottom boundary condition related to deep soil temperature. With respect to the downscaling methodology, the results show a clear benefit in using lateral boundary conditions directly from the global ERA5, despite the large resolution difference between the two modes (1:15), instead of providing them from an intermediate resolution COSMO‐based reanalysis. Moreover, the soil bottom boundary condition for temperature is reconstructed from the shallower ERA5 soil, using a site‐dependent method based on a delayed running mean of the ERA5 temperature at the deepest soil level. Finally, an evaluation of SPHERA has been performed with respect to the skill in simulating daily precipitation over 2 years. Compared with ERA5, SPHERA shows a higher ability in simulating moderate and intense events, markedly during summer, in terms of skill scores, frequency of occurrence and bias. |
| first_indexed | 2024-04-13T17:30:35Z |
| format | Article |
| id | doaj.art-5f5ebc6fa8be44099157f00f5c95661c |
| institution | Directory Open Access Journal |
| issn | 1350-4827 1469-8080 |
| language | English |
| last_indexed | 2024-04-13T17:30:35Z |
| publishDate | 2022-09-01 |
| publisher | Wiley |
| record_format | Article |
| series | Meteorological Applications |
| spelling | doaj.art-5f5ebc6fa8be44099157f00f5c95661c2022-12-22T02:37:34ZengWileyMeteorological Applications1350-48271469-80802022-09-01295n/an/a10.1002/met.2092Towards a convection‐permitting regional reanalysis over the Italian domainInes Maria Luisa Cerenzia0Antonio Giordani1Tiziana Paccagnella2Andrea Montani3HydroMeteoClimate Service ARPAE‐Emilia Romagna Bologna ItalyHydroMeteoClimate Service ARPAE‐Emilia Romagna Bologna ItalyHydroMeteoClimate Service ARPAE‐Emilia Romagna Bologna ItalyHydroMeteoClimate Service ARPAE‐Emilia Romagna Bologna ItalyAbstract A new convection‐permitting regional reanalysis, SPHERA (High Resolution REAnalysis over Italy), has been developed over Italy and the surrounding seas using the COSMO model at 2.2 km horizontal resolution. The reanalysis system is nested in the global reanalysis ERA5; upper‐air and surface observations are assimilated at the convection‐permitting scale by the COSMO nudging scheme. Before the complete production of the hourly three‐dimensional fields and surface/soil parameters over the period 1995–2020, general issues regarding the reanalysis set‐up needed to be addressed over a shorter test period. These include the identification of the best approach to downscale the lateral boundary conditions from the global driver, and the definition of the bottom boundary condition related to deep soil temperature. With respect to the downscaling methodology, the results show a clear benefit in using lateral boundary conditions directly from the global ERA5, despite the large resolution difference between the two modes (1:15), instead of providing them from an intermediate resolution COSMO‐based reanalysis. Moreover, the soil bottom boundary condition for temperature is reconstructed from the shallower ERA5 soil, using a site‐dependent method based on a delayed running mean of the ERA5 temperature at the deepest soil level. Finally, an evaluation of SPHERA has been performed with respect to the skill in simulating daily precipitation over 2 years. Compared with ERA5, SPHERA shows a higher ability in simulating moderate and intense events, markedly during summer, in terms of skill scores, frequency of occurrence and bias.https://doi.org/10.1002/met.2092convection‐permittingcoupledheavy precipitation eventshydro‐meteorologylong‐rangeprecipitation |
| spellingShingle | Ines Maria Luisa Cerenzia Antonio Giordani Tiziana Paccagnella Andrea Montani Towards a convection‐permitting regional reanalysis over the Italian domain Meteorological Applications convection‐permitting coupled heavy precipitation events hydro‐meteorology long‐range precipitation |
| title | Towards a convection‐permitting regional reanalysis over the Italian domain |
| title_full | Towards a convection‐permitting regional reanalysis over the Italian domain |
| title_fullStr | Towards a convection‐permitting regional reanalysis over the Italian domain |
| title_full_unstemmed | Towards a convection‐permitting regional reanalysis over the Italian domain |
| title_short | Towards a convection‐permitting regional reanalysis over the Italian domain |
| title_sort | towards a convection permitting regional reanalysis over the italian domain |
| topic | convection‐permitting coupled heavy precipitation events hydro‐meteorology long‐range precipitation |
| url | https://doi.org/10.1002/met.2092 |
| work_keys_str_mv | AT inesmarialuisacerenzia towardsaconvectionpermittingregionalreanalysisovertheitaliandomain AT antoniogiordani towardsaconvectionpermittingregionalreanalysisovertheitaliandomain AT tizianapaccagnella towardsaconvectionpermittingregionalreanalysisovertheitaliandomain AT andreamontani towardsaconvectionpermittingregionalreanalysisovertheitaliandomain |