The environment associated with significant tornadoes in Bangladesh
被引:22
|
作者:
Bikos, Dan
论文数: 0引用数: 0
h-index: 0
机构:
Colorado State Univ, Cooperat Inst Res Atmosphere, Ft Collins, CO 80523 USAColorado State Univ, Cooperat Inst Res Atmosphere, Ft Collins, CO 80523 USA
Bikos, Dan
[1
]
Finch, Jonathan
论文数: 0引用数: 0
h-index: 0
机构:
NOAA, Natl Weather Serv Forecast Off, Dodge City, KS USAColorado State Univ, Cooperat Inst Res Atmosphere, Ft Collins, CO 80523 USA
Finch, Jonathan
[2
]
Case, Jonathan L.
论文数: 0引用数: 0
h-index: 0
机构:
ENSCO Inc, Huntsville, AL USAColorado State Univ, Cooperat Inst Res Atmosphere, Ft Collins, CO 80523 USA
Case, Jonathan L.
[3
]
机构:
[1] Colorado State Univ, Cooperat Inst Res Atmosphere, Ft Collins, CO 80523 USA
[2] NOAA, Natl Weather Serv Forecast Off, Dodge City, KS USA
Tornado;
Bangladesh;
Thunderstorms;
Severe local storms;
Simulation;
Dryline;
CLIMATOLOGY;
SUPERCELL;
PARAMETERS;
MOTION;
D O I:
10.1016/j.atmosres.2015.08.002
中图分类号:
P4 [大气科学(气象学)];
学科分类号:
0706 ;
070601 ;
摘要:
This paper investigates the environmental parameters favoring significant tornadoes in Bangladesh through a simulation of ten high-impact events. A climatological perspective is first presented on classifying significant tornadoes in Bangladesh, noting the challenges since reports of tornadoes are not documented in a formal manner. The statistical relationship between United States and Bangladesh tornado-related deaths suggests that significant tornadoes do occur in Bangladesh so this paper identifies the most significant tornadic events and analyzes the environmental conditions associated with these events. Given the scarcity of observational data to assess the near-storm environment in this region, high-resolution (3-km horizontal grid spacing) numerical weather prediction simulations are performed for events identified to be associated with a significant tornado. In comparison to similar events over the United States, significant tornado environments in Bangladesh are characterized by relatively high convective available potential energy, sufficient deep-layer vertical shear, and a propensity for deviant (i.e., well to the right of the mean flow) storm motion along a low-level convergence boundary. (C) 2015 Elsevier B.V. All rights reserved.