NWS Tornado Warnings with Zero or Negative Lead Times

被引:31
作者
Brotzge, J. [1 ]
Erickson, S. [2 ]
机构
[1] Univ Oklahoma, Ctr Anal & Predict Storms, Norman, OK 73072 USA
[2] NOAA, Natl Severe Storms Lab, Norman, OK 73069 USA
基金
美国国家科学基金会;
关键词
DETECTION ALGORITHM; WSR-88D; RADAR;
D O I
10.1175/2008WAF2007076.1
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
During a 5-yr period of study from 2000 to 2004, slightly more than 10% of all National Weather Service (NWS) tornado warnings were issued either simultaneously as the tornado formed (i.e., with zero lead time) or minutes after initial tornado formation but prior to tornado dissipation (i.e., with "negative'' lead time). This study examines why these tornadoes were not warned in advance, and what climate, storm morphology, and sociological factors may have played a role in delaying the issuance of the warning. This dataset of zero and negative lead time warnings are sorted by their F-scale ratings, geographically by region and weather forecast office (WFO), hour of the day, month of the year, tornado-to-radar distance, county population density, and number of tornadoes by day, hour, and order of occurrence. Two key results from this study are (i) providing advance warning on the first tornado of the day remains a difficult challenge and (ii) the more isolated the tornado event, the less likelihood that an advance warning is provided. WFOs that experience many large-scale outbreaks have a lower proportion of warnings with negative lead time than WFOs that experience many more isolated, one-tornado or two-tornado warning days. Monthly and geographic trends in lead time are directly impacted by the number of multiple tornado events. Except for a few isolated cases, the impacts of tornado-to-radar distance, county population density, and storm morphology did not have a significant impact on negative lead-time warnings.
引用
收藏
页码:140 / 154
页数:15
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