2016
DOI: 10.1016/j.atmosres.2015.10.017
|View full text |Cite
|
Sign up to set email alerts
|

A thunderstorm cell-lightning activity analysis: The new concept of air mass catchment

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1
1

Citation Types

0
7
0
5

Year Published

2016
2016
2023
2023

Publication Types

Select...
4
2
1
1

Relationship

0
8

Authors

Journals

citations
Cited by 10 publications
(12 citation statements)
references
References 46 publications
0
7
0
5
Order By: Relevance
“…Large ranges were observed in each characteristic as expected from the evolving nature of some storm clusters, while others remained isolated. Therefore, the larger CAPE associated with some anomalously electrified storms did not translate to higher flash rates unlike Mona et al (2016) or larger storms indicative of stronger updrafts (e.g., Fuchs et al, 2015;Lang & Rutledge, 2011).…”
Section: Analysis Of Storm Cell Propertiesmentioning
confidence: 99%
“…Large ranges were observed in each characteristic as expected from the evolving nature of some storm clusters, while others remained isolated. Therefore, the larger CAPE associated with some anomalously electrified storms did not translate to higher flash rates unlike Mona et al (2016) or larger storms indicative of stronger updrafts (e.g., Fuchs et al, 2015;Lang & Rutledge, 2011).…”
Section: Analysis Of Storm Cell Propertiesmentioning
confidence: 99%
“…They also serve as proxies for climatologies of the occurrence of thunderstorms (e.g. Gladich et al, 2011;Poelman, 2014;Mona et al, 2016) and thunderstorm intensity. The climatologies will be compiled for a region in the south-eastern Alps.…”
mentioning
confidence: 99%
“…Every year Italy is meanly stroked by about 600,000 lightning strokes (excluding seas), with an average ground lightning density of about 2 strokes per km 2 each year, even if the actual density of lightning depends largely on the geographical conformation [1][2][3]. Different ways of upward warm air masses with a sufficiently high humidity gives rise to dense masses of clouds (cumulus) having a height ranging from 5 to 12 km and a diameter ranging from 5 to 10 km [4,5].…”
Section: Introductionmentioning
confidence: 99%