|
1000
|
Abstract/Summary
|
-
<jats:p>Abstract. Floods and landslides caused by extreme weather events, such as localized excessive rainfall in Japan, cause enormous devastation. Multicell clouds, on the other hand, have a common duration of over an hour and greater aerial coverage than single-cell clouds. For flood warning systems to function properly, the hazardous cloud must be detected quickly. Using pseudo and dual-Doppler vorticity approaches, the vertical vorticity estimate was extended from single-cell to multicell transitions case. According to the research, the single cells attained the peak of maximum vorticity of 0.08 and 0.01 s−1 for pseudo-vorticity and dual-Doppler vorticity, respectively. The maximum column of specific differential phase (Kdp) column above the melting layer indicated that the transition with 1 km depth as compared to differential reflectivity (Zdr) column was not observed after the cell merging. However, it was identified 5 min after the cell merged. In contrast, the Kdp column was always identified after the cell merging, and the column showed an increase in intensity 5 min after the cells merged. Vertical vorticity and multi-parameter radar analysis provided an insight into the transition from single-cell to multicell formation.
</jats:p>
|
|
1000
|
Hinweis
|
-
DeepGreen-ID: 5131fb80e9e24e7aa067a09336cff0bd ; metadata provieded by: DeepGreen (https://www.oa-deepgreen.de/api/v1/), LIVIVO search scope life sciences (http://z3950.zbmed.de:6210/livivo), Crossref Unified Resource API (https://api.crossref.org/swagger-ui/index.html), to.science.api (https://frl.publisso.de/), ZDB JSON-API (beta) (https://zeitschriftendatenbank.de/api/), lobid - Dateninfrastruktur für Bibliotheken (https://lobid.org/resources/search)
|
