Carlos Pinto da Silva NetoHumberto Alves BarbosaCesar Augustus Assis BenetiAtmósferaNeto C. P. S., Barbosa H. A., Beneti C. A. A. A method for convective storm detection using satellite data. Atmosfera 2016:29(4):343-358. doi:10.20937/ATM.2016.29.04.05...
Evolution of the Total Lightning Activity in a Leading-Line and Trailing Stratiform Mesoscale Convective System over Beijing Data from the Beijing SAFIR 3000 lightning detection system and Doppler radar provided some insights into the three-dimensional lightning structure and evo... D Liu,X Qie,Y Xi...
A. Storm morphology and rainfall characteristics of TRMM precipitation features. Mon. Weather Rev. 134, 2702–2721 (2006). Article Google Scholar Haberlie, A. M. & Ashley, W. S. A radar-based climatology of mesoscale convective systems in the United States. J. Clim. 32, 1591–1606 (...
Validation of the Meteosat storm detection and nowcasting system Cb-TRAM with lightning network data – Europe and South Africa In this paper, recent changes to the Meteosat thunderstorm TRacking And Monitoring algorithm (Cb-TRAM) are presented as well as a validation of Cb-TRAM aga... T.,Zinn...
Lightning location relative to storm structure in a leading-line, trailing-stratiform mesoscale convective system [1] Horizontal and line-normal, vertical cross-sections and composite images of Dallas-Fort Worth Lightning Detection and Ranging (LDAR II) VHF radiation s... Carey,D Lawrence - 《Journ...
The morphological parameters of convective systems have been gridded on the same 1° × 1° daily grid as the precipitation estimates, so as to enable simultaneous analysis of storm characteristics and precipitation amount. In this Eulerian framework, the properties of systems are viewed from ...
Chen, M. X., F. Gao, R. Kong, et al., 2010: Introduction of auto-nowcasting system for convective storm and its performance in Beijing Olympics meteorological service.J. Appl. Meteor. Sci.,21, 395–404, doi:https://doi.org/10.9699/j.issn.100-7310.2010.44.002. (in Chinese) ...
5(b), this group of reflectivity has an outstanding vertical extend (doubling the average height of echo top in other parts of the storm) and is narrow and upright in the form of a tall tower. Such features may be explained with a violent up-draft that overshot the average cloud top ...
The SP+CGs are more scattered than CGs without sprites in the storm system and these strokes are quite far—as distant as 200 km—from the coldest part of the cloud top. View Download Figure 4 Location of CG strokes (color-coded according to time of occurrence) detected by the WWLLN. ...
Stevens, B. & Feingold, G. Untangling aerosol effects on clouds and precipitation in a buffered system.Nature461, 607–613 (2009). ArticleADSCASGoogle Scholar Gryspeerdt, E., Stier, P., White, B. A. & Kipling, Z. Wet scavenging limits the detection of aerosol effects on precipitation....