Results 131 to 140 of about 534 (178)
Climatology of severe hail potential in Europe based on a convection-permitting simulation. [PDF]
Kahraman A, Kendon EJ, Fowler HJ.
europepmc +1 more source
Projections of winter polynyas and their biophysical impacts in the Ross Sea Antarctica. [PDF]
DuVivier AK +6 more
europepmc +1 more source
A Mesocyclone Detection Algorithm (MDA) and a near-storm environment (NSE) algorithm have been developed at the National Severe Storms Laboratory.
Gregory J. Stumpf +2 more
core
Weather and environmental hazards at mass gatherings.
Soomaroo L, Murray V.
europepmc +1 more source
A comprehensive characterization of mesocyclonic and nonmesocyclonic tornadoes in Italy
Roberto Ingrosso +9 more
openaire +1 more source
This study investigated the occurrence conditions of polar mesocyclones over the Sea of Japan in winter using the Japanese 55-year Reanalysis (JRA-55) data, the Meso-Scale Model (MSM) data, surface and upper weather charts provid-ed by the Japan ...
山川, 修治, 齋藤, 優弥
core
The idealized supercell simulations in a previous study by Roberts et al. are further analyzed to clarify the physical mechanisms leading to differences in mesocyclone intensification between an experiment with surface friction applied to the full wind ...
Brett Roberts, Ming Xue
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Mesocyclonic and non-mesocyclonic convective storms in Germany: Storm characteristics and life-cycle
Atmospheric Research, 2021Abstract A multi-year analysis of mesocyclonic (approximately 4300) and non-mesocyclonic convective storms (more than 100,000) is presented. A comprehensive data set is generated which includes measurements from a lightning location system, a precipitation radar network, as well as information from automated cell detection algorithms based on radar ...
openaire +1 more source
Nature, 2009
A strong volcanic plume consists of a vertical column of hot gases and dust topped with a horizontal 'umbrella'. The column rises, buoyed by entrained and heated ambient air, reaches the neutral-buoyancy level, then spreads radially to form the umbrella.
Pinaki, Chakraborty +2 more
openaire +2 more sources
A strong volcanic plume consists of a vertical column of hot gases and dust topped with a horizontal 'umbrella'. The column rises, buoyed by entrained and heated ambient air, reaches the neutral-buoyancy level, then spreads radially to form the umbrella.
Pinaki, Chakraborty +2 more
openaire +2 more sources

