Evaluación de diferentes estrategias para la generación de sistemas de predicción por conjuntos regionales de escala convectiva en un caso de precipitación intensa

Autores/as

  • Cynthia Matsudo Servicio Meteorol´ogico Nacional
  • Yanina Garc´ıa Skabar Servicio Meteorol´ogico Nacional, Consejo Nacional de Investigaciones Científicas y Técnicas
  • Juan Jos´e Ruiz Universidad de Buenos Aires, Consejo Nacional de Investigaciones Científicas y Técnicas

DOI:

https://doi.org/10.24215/1850468Xe022

Palabras clave:

conjunto, alta resoluci´on, precipitaci´on

Resumen

El pronóstico por conjuntos constituye una metodología consolidada para incorporar la incertidumbre asociada a los pronósticos en diversas escalas espaciales y temporales. En particular, en la mesoescala, no es claro aún cuáles son las técnicas más efectivas para representar la incertidumbre asociada a las condiciones iniciales y a los errores de modelo. En este trabajo se evalúan tres alternativas diferentes para la generación de pronósticos por conjuntos en alta resolución, y se realiza una comparación con un sistema de predicción por conjuntos global de baja resolución. Cada conjunto se construyó con 20 miembros utilizando el modelo WRF-ARW y 4 km de resolución horizontal sobre un dominio que abarca el centro noreste de Argentina. Se explora el desempeño de los conjuntos para un caso de estudio de precipitación intensa entre el 22 y 24 de diciembre de 2015. Los resultados se centran en el análisis del desempeño del pronóstico de precipitación y muestran que los conjuntos en alta resolución tienen mejor desempeño que el sistema global de menor resolución tanto en términos de la precisión del pronóstico como en términos de la cuantificación de su incertidumbre. En este trabajo, los conjuntos donde solo se perturban las condiciones iniciales y de borde tienden a mostrar una menor dispersión que aquellos en donde se combinan diferentes parametrizaciones de los procesos de escala sub-reticular para la representación de los errores de modelo. Estos ´últimos presentan además un menor sesgo para umbrales mayores a 10 mm. Asimismo, aumentar la resolución de las condiciones iniciales y de borde de la media del ensamble aumenta levemente la dispersión y mejora la representación espacial de los patrones de precipitación para todos los umbrales considerados.

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Biografía del autor/a

Cynthia Matsudo, Servicio Meteorol´ogico Nacional

Servicio Meteorol´ogico Nacional, Buenos Aires, Argentina.

Yanina Garc´ıa Skabar, Servicio Meteorol´ogico Nacional, Consejo Nacional de Investigaciones Científicas y Técnicas

Servicio Meteorol´ogico Nacional, Buenos Aires, Argentina. CONICET, Buenos Aires, Argentina.

Juan Jos´e Ruiz, Universidad de Buenos Aires, Consejo Nacional de Investigaciones Científicas y Técnicas

Departamento de Ciencias de la Atm´osfera y los Oc´eanos, FCEyN, UBA. Centro de Investigaciones del Mar y la Atm´osfera, CONICET/FCEN-UBA.

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