Results 1 to 10 of about 283 (160)
Shear‐Convection Interactions and Orientation of Tropical Squall Lines [PDF]
Abstract Squall lines are known to be the consequence of the interaction of low‐level shear with cold pools associated with convective downdrafts. Also, as the magnitude of the shear increases beyond a critical shear, squall lines tend to orient themselves.
Sophie Abramian +2 more
exaly +8 more sources
Extreme Precipitation in Tropical Squall Lines
Squall lines are substantially influenced by the interaction of low‐level shear with cold pools associated with convective downdrafts. Beyond an optimal shear amplitude, squall lines tend to orient themselves at an angle with respect to the low‐level ...
Sophie Abramian +2 more
doaj +4 more sources
Propagation of tropical squall line-induced storm coastal inundation episodes in Java-Bali, Indonesia [PDF]
The short-lived tropical squall lines could trigger weather-related hazards to the northern part of the Indonesia Maritime Continent (IMC), such as Sumatra and Kalimantan.
Erma Yulihastin +17 more
doaj +2 more sources
An improvement of wind gust estimate (WGE) method for squall lines
Severe wind gusts produced by squall lines are difficult to monitor and forecast. This paper assessed and improved the physics-based Brasseur WGE (wind gust estimate) method for diagnosing wind gust of squall lines by coupling the WGE methods with the ...
Zhengqi Lu +6 more
doaj +3 more sources
Mesoscale convective systems (MCS) contribute about half of the world's precipitation and create flash flooding as well as other extreme weather events. Despite steady progress in research of these systems in the last several decades, better theoretical ...
Minghua Zhang
doaj +2 more sources
Water isotopes are tracers of convective processes and are often used as proxies for past precipitation. These applications require a better understanding of the impact of convective processes on the isotopic composition of water vapor and precipitation.
Camille Risi +6 more
doaj +2 more sources
Divergent convective outflow in large-eddy simulations [PDF]
Upper-tropospheric outflow is analysed in cloud-resolving large-eddy simulations. Thereby, the role of convective organization, latent heating, and other factors in upper-tropospheric divergent-outflow variability from deep convection is diagnosed using ...
E. Groot, H. Tost
doaj +1 more source
Numerical simulation and study of a squall in the north of Jiangsu in midsummer
A squall line event in northern Jiangsu in midsummer is simulated and analyzed by adopting regional WRF model with triple nesting, and the conceptual model diagram in the radial section of squall line is given. The main results are as follows.
Juan ZHU, Lifeng ZHANG, Ming ZHANG
doaj +1 more source
Four typical double-moment cloud microphysical schemes (Milbrandt, Morrison, NSSL and WDM6) in WRF (Weather Research and Forecasting) are used to investigate the impact of the different schemes on the simulation of a straight squall line evolving into a ...
Qian Cao +3 more
doaj +1 more source
Evolution of squall line variability and error growth in an ensemble of large eddy simulations [PDF]
A chain of processes is identified that regulates much of the spread in an ensemble of squall lines in large eddy simulations with tight initial conditions.
E. Groot, H. Tost
doaj +1 more source

