2011
DOI: 10.22499/2.6103.001
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A severe thunderstorm climatology for Australia and associated thunderstorm environments

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Cited by 78 publications
(87 citation statements)
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References 23 publications
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“…MUCAPE is the index determining the instability energy computed for an air parcel at the most unstable isobaric level (the level at which the CAPE index has the highest value in the analyzed profile). It is used in thunderstorm detection as an index that is less sensitive to fluctuations in surface moisture and the boundary layer environment than CAPE, which considers buoyancy over the depth of the atmosphere (Lombardo and Colle 2010;Allen et al 2011).…”
Section: Mucape As a Predictor For Thunderstorm Occurrencementioning
confidence: 99%
See 1 more Smart Citation
“…MUCAPE is the index determining the instability energy computed for an air parcel at the most unstable isobaric level (the level at which the CAPE index has the highest value in the analyzed profile). It is used in thunderstorm detection as an index that is less sensitive to fluctuations in surface moisture and the boundary layer environment than CAPE, which considers buoyancy over the depth of the atmosphere (Lombardo and Colle 2010;Allen et al 2011).…”
Section: Mucape As a Predictor For Thunderstorm Occurrencementioning
confidence: 99%
“…Data derived from a model does not contain information on a specific thunderstorm occurrence; it may however be used for determining conditions that favor thunderstorm occurrences over a given area, which has been confirmed by numerous works in this field (e.g., Marsh et al 2007Marsh et al , 2009Trapp et al 2007Trapp et al , 2010Lombardo and Colle 2010;Allen et al 2011;Gensini et al 2014a). Of course, one needs to approach results with a certain dose of criticism towards analytical errors resulting from errors in observational data and errors that follow the implemented method of modeling (Thorne and Vose 2010).…”
Section: Introductionmentioning
confidence: 99%
“…A combination of indices is usually used to identify favourable conditions for severe convective storm environments, for example Convective Available Potential Energy (CAPE), Convective Inhibition (CIN) and 0-6 km Bulk Wind Difference (BWD)/deep-layer wind shear (e.g. Rasmussen and Blanchard 1998;Craven et al 2002;Brooks et al 2003;Allen et al 2011;Gensini and Ashley 2011). However, as cautioned by Doswell III and Schultz (2006), there are no specific thresholds that discriminate perfectly between severe and non-severe environments.…”
Section: Introductionmentioning
confidence: 99%
“…Brooks et al 2003), Australia (e.g. Allen et al 2011) and in some cases, such analysis has been extended onto a global scale (e.g. Brooks et al 2003).…”
Section: Introductionmentioning
confidence: 99%
“…Hail events likely produce dissimilar categories of damages to the natural environment and often disastrous consequences upon people in the region Allen et al, 2011). Severe hailstorms are localized events which could affect smaller areas and are responsible for everlasting damages (Alford, 1994;Johnson et al, 1995).…”
Section: Introductionmentioning
confidence: 99%