Next Article in Journal
Investigations of Atmospheric Waves in the Earth Lower Ionosphere by Means of the Method of the Creation of the Artificial Periodic Irregularities of the Ionospheric Plasma
Next Article in Special Issue
Subseasonal Influences of Teleconnection Patterns on the Boreal Wintertime Surface Air Temperature over Southern China as Revealed from Three Reanalysis Datasets
Previous Article in Journal
Environmental Strategies for Selecting Eco-Routing in a Small City
Previous Article in Special Issue
Does the IOD Independently Influence Seasonal Monsoon Patterns in Northern Ethiopia?
Open AccessArticle

Analysis of Severe Elevated Thunderstorms over Frontal Surfaces Using DCIN and DCAPE

1
Atmospheric Science Program, School of Natural Resources, University of Missouri, Columbia, MO 65211, USA
2
Cooperative Institute for Mesoscale Meteorological Studies, University of Oklahoma, Norman, OK 73019, USA
*
Author to whom correspondence should be addressed.
Atmosphere 2019, 10(8), 449; https://doi.org/10.3390/atmos10080449
Received: 28 June 2019 / Revised: 31 July 2019 / Accepted: 2 August 2019 / Published: 5 August 2019
(This article belongs to the Special Issue 10th Anniversary of Atmosphere: Climatology and Meteorology)
A 10-year study of elevated severe thunderstorms was performed using The National Centers for Environmental Information Storm Events Database. A total of 80 elevated thunderstorm cases were identified, verified, and divided into “Prolific” and “Marginal” classes. These severe cases occurred at least 80 km away from, and on the cold side of, a surface boundary. The downdraft convective available potential energy (DCAPE), downdraft convective inhibition (DCIN), and their ratio are tools to help estimate the potential for a downdraft to penetrate through the depth of a stable surface layer. The hypothesis is that as the DCIN/DCAPE ratio decreases, there exists enhanced possibility of severe surface winds. Using the initial fields from the Rapid Refresh numerical weather prediction model, datasets of DCIN, DCAPE, and their ratio were created. Mann-Whitney U tests on the Prolific versus Marginal case sets were undertaken to determine if the DCAPE and DCIN values come from different populations for the two different case sets. Results show that the Prolific cases have values of DCIN closer to zero, suggesting the downdraft is able to penetrate to the surface causing severe winds. Thus, comparing DCIN and DCAPE is a viable tool in determining if downdrafts will reach the surface from elevated thunderstorms. View Full-Text
Keywords: elevated thunderstorm; downdraft convective inhibition; DCIN elevated thunderstorm; downdraft convective inhibition; DCIN
Show Figures

Figure 1

MDPI and ACS Style

Market, P.; Grempler, K.; Sumrall, P.; Henson, C. Analysis of Severe Elevated Thunderstorms over Frontal Surfaces Using DCIN and DCAPE. Atmosphere 2019, 10, 449.

Show more citation formats Show less citations formats
Note that from the first issue of 2016, MDPI journals use article numbers instead of page numbers. See further details here.

Article Access Map by Country/Region

1
Back to TopTop