1994
DOI: 10.1175/1520-0493(1994)122<1726:ctglau>2.0.co;2
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Cloud-to-Ground Lightning and Upper-Air Patterns during Bursts and Breaks in the Southwest Monsoon

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Cited by 33 publications
(37 citation statements)
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“…Intraseasonal variability in lightning activity associated with the MJO is manifested as a northwardpropagating mode akin to northward surges in monsoon activity (e.g., Watson et al 1994). Intraseasonal variability in lightning activity associated with the MJO is manifested as a northwardpropagating mode akin to northward surges in monsoon activity (e.g., Watson et al 1994).…”
Section: Resultsmentioning
confidence: 99%
See 1 more Smart Citation
“…Intraseasonal variability in lightning activity associated with the MJO is manifested as a northwardpropagating mode akin to northward surges in monsoon activity (e.g., Watson et al 1994). Intraseasonal variability in lightning activity associated with the MJO is manifested as a northwardpropagating mode akin to northward surges in monsoon activity (e.g., Watson et al 1994).…”
Section: Resultsmentioning
confidence: 99%
“…Although synoptic conditions conducive to lightning activity vary widely across the continental United States, the fundamental atmospheric ingredients necessary for enhanced lightning activity include a convectively unstable midtroposphere (e.g., Burrows et al 2005). Watson et al (1994) found that lightning activity over the desert Southwest is enhanced coincident with synoptic conditions associated with surges in the North American monsoon. Watson et al (1994) found that lightning activity over the desert Southwest is enhanced coincident with synoptic conditions associated with surges in the North American monsoon.…”
Section: Introductionmentioning
confidence: 99%
“…Watson et al (1994) used lightning data as an indicator of the convective activity to study the southwestern U.S. monsoon as related to upper-air characteristics. Lericos et al (2002) used NLDN data to study the cloud-to-ground lightning over the entire Florida peninsula and the surrounding seas during the warm season when synoptic forcing is relatively weak.…”
Section: Introductionmentioning
confidence: 99%
“…De maneira geral, observa-se no histograma a predominância de descargas negativas durante todo o período de acompanhamento do sistema, com exceção de alguns períodos na fase da dissipação. Segundo Watson et al (1994) e Macgorman & Burges (1994, as descargas negativas superam as positivas quando as precipitações são predominantemente de água líquida e, quando existe muita precipitação na forma de granizo, as descargas positivas tendem a ocorrer em maior quantidade. Nas cinco horas finais do sistema foi detectada uma descarga por imagem de satélite.…”
Section: Resultsunclassified