Impact of Ensemble-Variational Data Assimilation in Heavy Rain Forecast over Brazilian Northeast
The Brazilian Northeast (BNE) is located in the tropical region of Brazil. It is bounded by the Atlantic Ocean, and its climate and vegetation are strongly affected by continental plateaus. The plateaus keep the humid air masses to the east and are responsible for the rain episodes, and at the west...
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| Format: | Article |
| Language: | English |
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MDPI AG
2021-09-01
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| Series: | Atmosphere |
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| Online Access: | https://www.mdpi.com/2073-4433/12/9/1201 |
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| author | João Pedro Gonçalves Nobre Éder Paulo Vendrasco Carlos Frederico Bastarz |
| author_facet | João Pedro Gonçalves Nobre Éder Paulo Vendrasco Carlos Frederico Bastarz |
| author_sort | João Pedro Gonçalves Nobre |
| collection | DOAJ |
| description | The Brazilian Northeast (BNE) is located in the tropical region of Brazil. It is bounded by the Atlantic Ocean, and its climate and vegetation are strongly affected by continental plateaus. The plateaus keep the humid air masses to the east and are responsible for the rain episodes, and at the west side the northeastern hinterland and dry air masses are observed. This work is a case study that aims to evaluate the impact of updating the model initial condition using the 3DEnVar (Three-Dimensional Ensemble Variational) system in heavy rain episodes associated with Mesoscale Convective Systems (MCS). The results were compared to 3DVar (Three-Dimensional Variational) and EnSRF (Ensemble Square Root Filter) systems and with no data assimilation. The study enclosed two MCS cases occurring on 14 and 24 January 2017. For that purpose, the RMS (Regional Modeling System) version 3.0.0, maintained by the Center for Weather Forecasting and Climate Studies (CPTEC), used two components: the Weather Research and Forecasting (WRF) mesoscale model and the GSI (Gridpoint Statistical Interpolation) data assimilation system. Currently, the RMS provides the WRF initial conditions by using 3DVar data assimilation methodology. The 3DVar uses a climatological covariance matrix to minimize model errors. In this work, the 3DEnVar updates the RMS climatological covariance matrix through the forecast members based on the errors of the day. This work evaluated the improvements in the detection and estimation of 24 h accumulated precipitation in MCS events. The statistic index RMSE (Root Mean Square Error) showed that the hybrid data assimilation system (3DEnVar) performed better in reproducing the precipitation in the MCS occurred on 14 January 2017. On 24 January 2017, the EnSRF was the best system for improving the WRF forecast. In general, the BIAS showed that the WRF initialized with different initial conditions overestimated the 24 h accumulated precipitation. Therefore, the viability of using a hybrid system may depend on the hybrid algorithm that can modify the weights attributed to the EnSRF and 3DVar matrix in the GSI over the assimilation cycles. |
| first_indexed | 2024-03-10T07:54:29Z |
| format | Article |
| id | doaj.art-ba1f3120a4104debacac89028f49e3e3 |
| institution | Directory Open Access Journal |
| issn | 2073-4433 |
| language | English |
| last_indexed | 2024-03-10T07:54:29Z |
| publishDate | 2021-09-01 |
| publisher | MDPI AG |
| record_format | Article |
| series | Atmosphere |
| spelling | doaj.art-ba1f3120a4104debacac89028f49e3e32023-11-22T12:00:46ZengMDPI AGAtmosphere2073-44332021-09-01129120110.3390/atmos12091201Impact of Ensemble-Variational Data Assimilation in Heavy Rain Forecast over Brazilian NortheastJoão Pedro Gonçalves Nobre0Éder Paulo Vendrasco1Carlos Frederico Bastarz2National Institute for Space Research (INPE), Cachoeira Paulista 12630-970, BrazilNational Institute for Space Research (INPE), Cachoeira Paulista 12630-970, BrazilNational Institute for Space Research (INPE), Cachoeira Paulista 12630-970, BrazilThe Brazilian Northeast (BNE) is located in the tropical region of Brazil. It is bounded by the Atlantic Ocean, and its climate and vegetation are strongly affected by continental plateaus. The plateaus keep the humid air masses to the east and are responsible for the rain episodes, and at the west side the northeastern hinterland and dry air masses are observed. This work is a case study that aims to evaluate the impact of updating the model initial condition using the 3DEnVar (Three-Dimensional Ensemble Variational) system in heavy rain episodes associated with Mesoscale Convective Systems (MCS). The results were compared to 3DVar (Three-Dimensional Variational) and EnSRF (Ensemble Square Root Filter) systems and with no data assimilation. The study enclosed two MCS cases occurring on 14 and 24 January 2017. For that purpose, the RMS (Regional Modeling System) version 3.0.0, maintained by the Center for Weather Forecasting and Climate Studies (CPTEC), used two components: the Weather Research and Forecasting (WRF) mesoscale model and the GSI (Gridpoint Statistical Interpolation) data assimilation system. Currently, the RMS provides the WRF initial conditions by using 3DVar data assimilation methodology. The 3DVar uses a climatological covariance matrix to minimize model errors. In this work, the 3DEnVar updates the RMS climatological covariance matrix through the forecast members based on the errors of the day. This work evaluated the improvements in the detection and estimation of 24 h accumulated precipitation in MCS events. The statistic index RMSE (Root Mean Square Error) showed that the hybrid data assimilation system (3DEnVar) performed better in reproducing the precipitation in the MCS occurred on 14 January 2017. On 24 January 2017, the EnSRF was the best system for improving the WRF forecast. In general, the BIAS showed that the WRF initialized with different initial conditions overestimated the 24 h accumulated precipitation. Therefore, the viability of using a hybrid system may depend on the hybrid algorithm that can modify the weights attributed to the EnSRF and 3DVar matrix in the GSI over the assimilation cycles.https://www.mdpi.com/2073-4433/12/9/12013DEnVarmesoscale convective systemsWRFGSI |
| spellingShingle | João Pedro Gonçalves Nobre Éder Paulo Vendrasco Carlos Frederico Bastarz Impact of Ensemble-Variational Data Assimilation in Heavy Rain Forecast over Brazilian Northeast Atmosphere 3DEnVar mesoscale convective systems WRF GSI |
| title | Impact of Ensemble-Variational Data Assimilation in Heavy Rain Forecast over Brazilian Northeast |
| title_full | Impact of Ensemble-Variational Data Assimilation in Heavy Rain Forecast over Brazilian Northeast |
| title_fullStr | Impact of Ensemble-Variational Data Assimilation in Heavy Rain Forecast over Brazilian Northeast |
| title_full_unstemmed | Impact of Ensemble-Variational Data Assimilation in Heavy Rain Forecast over Brazilian Northeast |
| title_short | Impact of Ensemble-Variational Data Assimilation in Heavy Rain Forecast over Brazilian Northeast |
| title_sort | impact of ensemble variational data assimilation in heavy rain forecast over brazilian northeast |
| topic | 3DEnVar mesoscale convective systems WRF GSI |
| url | https://www.mdpi.com/2073-4433/12/9/1201 |
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