Verification of an algorithm (DWSR
Paraschivescu, M.; Stefan, S.; Bogdan, M.
Instituto de Ciencias de la Atmósfera y Cambio Climático, UNAM, publicado en Atmósfera, y cosechado de Revistas UNAM
dor_id: 10824
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650.#.4.x: Físico Matemáticas y Ciencias de la Tierra
336.#.#.b: article
336.#.#.3: Artículo de Investigación
336.#.#.a: Artículo
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351.#.#.b: Atmósfera
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856.4.0.u: https://www.revistascca.unam.mx/atm/index.php/atm/article/view/27742/26023
100.1.#.a: Paraschivescu, M.; Stefan, S.; Bogdan, M.
524.#.#.a: Paraschivescu, M., et al. (2011). Verification of an algorithm (DWSR. Atmósfera; Vol. 24 No. 4, 2011. Recuperado de https://repositorio.unam.mx/contenidos/10824
245.1.0.a: Verification of an algorithm (DWSR
502.#.#.c: Universidad Nacional Autónoma de México
561.1.#.a: Instituto de Ciencias de la Atmósfera y Cambio Climático, UNAM
264.#.0.c: 2011
264.#.1.c: 2011-09-30
653.#.#.a: hail; size of hail; radar products; C-band weather radar; Aladin model
506.1.#.a: La titularidad de los derechos patrimoniales de esta obra pertenece a las instituciones editoras. Su uso se rige por una licencia Creative Commons BY-NC 4.0 Internacional, https://creativecommons.org/licenses/by-nc/4.0/legalcode.es, para un uso diferente consultar al responsable jurídico del repositorio por medio del correo electrónico editora@atmosfera.unam.mx
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001.#.#.#: 022.oai:ojs.pkp.sfu.ca:article/27742
041.#.7.h: eng
520.3.#.a: The aim of this paper is to determine the real-time forecast and warning critera for hail events, using height of maximum reflectivity (Hmax), vertically integrated liquid water (VIL), hail occurrence probability (HailP) and reflectivity radar products (PPIZ). In addition, criteria were sought for use in estimating the size of hail stones. The study is based on data supplied by the Bucharest C-band weather radar along with observation data during the 2001-2008 period. The following radar products: HailP, Hmax, (PPIZ) and VIL, have been determined for each hail event reported by the weather station. A number of 320 cases have been analyzed when hail was determined for 20 weather stations in Muntenia area, Romania. One related result is that in situations when the 0 ºC isotherm is between 3000 and 4000 m, the frequency of hail events certified on the ground is 50%. Another conclusion is that if the maximum reflectivity appears at heights between 7000 and 8000 m, there is an approximately 20% chance of hail events. The HailP, Hmax, Reflectivity and VIL were computed both for the exact locations where hail was reported and for an area of 5 km around those locations. The performed analysis showed that both obtained data sets can be used with confidence. A comparison was performed regarding the year 2008 between the values of HailP from the Bucharest vertical sounding and those extracted from the Aladin model, using its requested parameters. The results show an overestimate of the hail occurrence probability (HailP) when the Aladin model was used.
773.1.#.t: Atmósfera; Vol. 24 No. 4 (2011)
773.1.#.o: https://www.revistascca.unam.mx/atm/index.php/atm/index
046.#.#.j: 2021-10-20 00:00:00.000000
022.#.#.a: ISSN electrónico: 2395-8812; ISSN impreso: 0187-6236
310.#.#.a: Trimestral
264.#.1.b: Instituto de Ciencias de la Atmósfera y Cambio Climático, UNAM
handle: 00e686d4553061f2
harvesting_date: 2023-06-20 16:00:00.0
856.#.0.q: application/pdf
last_modified: 2023-06-20 16:00:00
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license_type: by-nc
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Paraschivescu, M.; Stefan, S.; Bogdan, M.
Instituto de Ciencias de la Atmósfera y Cambio Climático, UNAM, publicado en Atmósfera, y cosechado de Revistas UNAM
Paraschivescu, M., et al. (2011). Verification of an algorithm (DWSR. Atmósfera; Vol. 24 No. 4, 2011. Recuperado de https://repositorio.unam.mx/contenidos/10824