METEOROLOGICAL OVERVIEW OF THE DEVASTATING 27 APRIL 2011 TORNADO OUTBREAK

被引:93
作者
Knupp, Kevin R. [1 ]
Murphy, Todd A. [1 ]
Coleman, Timothy A. [1 ]
Wade, Ryan A. [1 ]
Mullins, Stephanie A. [1 ]
Schultz, Christopher J. [1 ]
Schultz, Elise V. [1 ]
Carey, Lawrence [1 ]
Sherrer, Adam [1 ]
McCaul, Eugene W., Jr. [2 ]
Carcione, Brian
Latimer, Stephen [3 ]
Kula, Andy [3 ]
Laws, Kevin [4 ]
Marsh, Patrick T. [5 ]
Klockow, Kim [6 ]
机构
[1] Univ Alabama, Huntsville, AL 35805 USA
[2] Univ Space Res Assoc, Columbia, MD USA
[3] Natl Weather Serv, Huntsville, AL USA
[4] Natl Weather Serv, Birmingham, AL USA
[5] Natl Severe Storms Lab, Cooperat Inst Mesoscale Meteorol Studies, Norman, OK 73069 USA
[6] Univ Oklahoma, Norman, OK 73019 USA
基金
美国国家科学基金会;
关键词
MESOSCALE CONVECTIVE SYSTEM; DOPPLER RADAR OBSERVATIONS; LOW-LEVEL MESOVORTICES; LONG-LIVED SUPERCELLS; PART I; SQUALL LINES; BOW ECHOES; OBSERVATIONAL EXAMINATION; ENVIRONMENTAL-CONDITIONS; CASA RADAR;
D O I
10.1175/BAMS-D-11-00229.1
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
By many metrics, the tornado outbreak on 27 April 2011 was the most significant tornado outbreak since 1950, exceeding the super outbreak of 3-4 April 1974. The number of tornadoes over a 24-h period (midnight to midnight) was 199; the tornado fatalities and injuries were 316 and more than 2,700, respectively; and the insurable loss exceeded $4 billion (U.S. dollars). In this paper, we provide a meteorological overview of this outbreak and illustrate that the event was composed of three mesoscale events: a large early morning quasi-linear convective system (QLCS), a midday QLCS, and numerous afternoon supercell storms. The main data sources include NWS and research radars, profilers, surface measurements, and photos and videos of the tornadoes. The primary motivation for this preliminary research is to document the diverse characteristics (e.g., tornado characteristics and mesoscale organization of deep convection) of this outbreak and summarize preliminary analyses that are worthy of additional research on this case.
引用
收藏
页码:1041 / +
页数:23
相关论文
共 91 条
[1]  
Andra DL, 1997, 28TH CONFERENCE ON RADAR METEOROLOGY, P364
[2]  
[Anonymous], 2012, 2011 TORN INF
[3]   Bow Echo Mesovortices. Part II: Their Genesis [J].
Atkins, Nolan T. ;
Laurent, Michael St. .
MONTHLY WEATHER REVIEW, 2009, 137 (05) :1514-1532
[4]   Reconstruction of Near-Surface Tornado Wind Fields from Forest Damage [J].
Beck, Veronika ;
Dotzek, Nikolai .
JOURNAL OF APPLIED METEOROLOGY AND CLIMATOLOGY, 2010, 49 (07) :1517-1537
[5]   Interactions between a Supercell and a Quasi-Stationary Frontal Boundary [J].
Blanchard, David O. .
MONTHLY WEATHER REVIEW, 2008, 136 (12) :5199-5210
[6]  
Bluestein H. B., 2012, 26 C SEV LOC STORMS
[7]   The structure of tornadoes near Attica, Kansas, on 12 May 2004: High-resolution, mobile, Doppler radar observations [J].
Bluestein, Howard B. ;
Weiss, Christopher C. ;
French, Michael M. ;
Holthaus, Eric M. ;
Tanamachi, Robin L. ;
Frasier, Stephen ;
Pazmany, Andrew L. .
MONTHLY WEATHER REVIEW, 2007, 135 (02) :475-506
[8]   Tornado Damage Estimation Using Polarimetric Radar [J].
Bodine, David J. ;
Kumjian, Matthew R. ;
Palmer, Robert D. ;
Heinselman, Pamela L. ;
Ryzhkov, Alexander V. .
WEATHER AND FORECASTING, 2013, 28 (01) :139-158
[9]   Supercell tornadogenesis over complex terrain: The Great Barrington, Massachusetts, tornado on 29 May 1995 [J].
Bosart, Lance F. ;
Seimon, Anton ;
LaPenta, Kenneth D. ;
Dickinson, Michael J. .
WEATHER AND FORECASTING, 2006, 21 (06) :897-922
[10]  
Brooks HE, 2004, WEATHER FORECAST, V19, P310, DOI 10.1175/1520-0434(2004)019<0310:OTROTP>2.0.CO