ANALYSIS ON THE PULSE STORM EVENT IN THE SOUTH BANDUNG WEST JAVA BASED ON THE TRANSPORTABLE X-BAND DOPLLER RADAR CAMPAIGN, (CASE STUDY : MARCH 16, 2017)

Ginaldi Ari Nugroho, Tiin Sinatra, Trismidianto Trismidianto

Abstract

Pulse storm is a term to mention the occurrence of storms that have a short duration with the nature of its weak updraft. The results of the Transportable X-band radar campaign were able to capture a pulse storm at a location 25 km southwest from a radar position. Convective core with echo value > 50 dbz is detected at 4 km altitude but has a weak updraft so that it dissipated in the next 40 minutes. This convective activity is also showed by convective index value as well as Tbb value from Himawari Satellite data in those area. The microburst effect showed from the surface wind shear that expand along + 6.6 km with the edge of the area experiencing high wind with maximum speed from combine shear showed up to 14.5 m/s. The microburst category is dry microburst based on the increase in precipitation value from AWS surface data

Keywords

Pulse storm, Microburst, Transportable X-Band radar, wind shear.

Full Text:

PDF_Ginaldi

References

Cerniglia, C. S., and W. R. Snyder, 2002: Development of warning criteria for severe pulse thunderstorms in the Northeastern United States using the WSR-88D. National Weather Service. Eastern Region Technical Attachment No. 2002-391 03, 14 pp. [Available online at http://docs.lib.noaa.gov/noaa_documents/NWS/NWS_ER/Eastern_Region_Tech_Attacment/TA2002-03.pdf.

Miller, D., and A. Petrolito, 2008: Anticipating pulse severe thunderstorms 428 using the WSR-88D all-tilts display. National Weather Service. Eastern Region Technical Attachment No. 2008- 02,11pp.Availableonlineathttp://docs.lib.noaa.gov/noaa_documents/NWS/NWS_ER/Eastern_Region_Tech_Attachment/TA_2008-02.pdf.]

Miller, P., and T. Mote, 2016: Standardizing the definition of a "pulse"thunderstorm. Bull. Amer. Meteor. Soc. doi:10.1175/BAMS-D-16-0064.1

Fukao S dan Hamazu K, Radar for Meteorological and Atmospheric Observation, Springer, pp 410-411

Byers, H. R., and R. R. Braham, 1949: The Thunderstorm: Report of the Thunderstorm Project. US Government Printing Office, 287 pp

Fujita, T.T. 1985. The downburst: Microburst and macroburst, SMRP Res. Rep. 210, 122pp. Chicago: University of Chicago.

Rodi, A.R., K.L. Elmore, and W.P. Mahoney. 1983. Aircraft and Doppler air motion omparisons in a JAWS microburst. 21st Conference on Radar Meteorology (preprints), Edmonton, 624–629.Boston: American Meteorological Society.

Wolfson, M. M. 1983. Doppler radar observations of an Oklahoma downburst. In 21st Conference on radar meteorology (preprints), 590–595. Edmonton: American Meteorological Society

Wakimoto, R.M. 1985. Forecasting dry microburst activity over the high plains. Monthly Weather Review 113: 1131–1143.

Caracena, F., R.L. Holle, and C.A. Doswell. “Microbursts-A handbook for visual identification.†[Available 19 Jan. 2007 online at http://www.cimms.ou.edu/~doswell/microbursts/Handbook.html.]

Sinatra T, Noersomadi, Nugroho G A and Trilaksono N J 2014 Characterizing the diurnal cycle of convective activity over the south of west java using doppler x-band radar observation The 4th international symposium for sustainable humanosphere (ISSH)-a forum of the humanosphere science school (HSS) 2014ISSN:2088-91

P. Herald and K. Drozd, “ Use of combined shear and spectrum width in tornado detection,†National Weather Service, CRARP-24-06, https://www.weather.gov/media/crh/publications/ARP/arp24-06.pd

Refbacks

  • There are currently no refbacks.