GSTDTAP  > 气候变化
DOI10.1002/2017JD027639
Optimizing Precipitation Thresholds for Best Correlation Between Dry Lightning and Wildfires
Vant-Hull, Brian1; Thompson, Tollisha2; Koshak, William3
2018-03-16
发表期刊JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
ISSN2169-897X
EISSN2169-8996
出版年2018
卷号123期号:5页码:2628-2639
文章类型Article
语种英语
国家USA
英文摘要

This work examines how to adjust the definition of dry lightning in order to optimize the correlation between dry lightning flash count and the climatology of large (>400km(2)) lightning-ignited wildfires over the contiguous United States (CONUS). The National Lightning Detection Network and National Centers for Environmental Prediction Stage IV radar-based, gauge-adjusted precipitation data are used to form climatic data sets. For a 13year analysis period over CONUS, a correlation of 0.88 is found between annual totals of wildfires and dry lightning. This optimal correlation is found by defining dry lightning as follows: on a 0.1 degrees hourly grid, a precipitation threshold of no more than 0.3mm may accumulate during any hour over a period of 3-4days preceding the flash. Regional optimized definitions vary. When annual totals are analyzed as done here, no clear advantage is found by weighting positive polarity cloud-to-ground (+CG) lightning differently than -CG lightning. The high variability of dry lightning relative to the precipitation and lightning from which it is derived suggests it would be an independent and useful climate indicator.


Plain Language Summary Many wildfires are started by dry lightning, which are flashes that occur with low or no precipitation. There is no uniformly accepted definition for dry lightning, which must include an upper threshold on precipitation, the length of the dry period preceding the precipitation, and the spatial resolution over which lightning and precipitation are colocated. This work attempts to find a definition of dry lightning over the continental United States using lightning, precipitation, and wildfire data sets. The lightning and precipitation are located in space and time to the hour and on a 0.1 degrees grid. The location and timing of wildfire initiation is much harder to identify, and so is left as annual/national totals to be targeted by the best definition of dry lightning. We found an upper precipitation threshold of 0.2 mm/h and a dry duration of 30 h defines dry lightning that best matches the wildfire data set.


领域气候变化
收录类别SCI-E
WOS记录号WOS:000428437100015
WOS关键词WILDLAND FIRE ; FOREST-FIRES ; IGNITION
WOS类目Meteorology & Atmospheric Sciences
WOS研究方向Meteorology & Atmospheric Sciences
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文献类型期刊论文
条目标识符http://119.78.100.173/C666/handle/2XK7JSWQ/33606
专题气候变化
作者单位1.CUNY, CREST Inst, New York, NY 10021 USA;
2.New York City Coll Technol, Brooklyn, NY USA;
3.NASA, Marshall Space Flight Ctr, Huntsville, AL USA
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Vant-Hull, Brian,Thompson, Tollisha,Koshak, William. Optimizing Precipitation Thresholds for Best Correlation Between Dry Lightning and Wildfires[J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES,2018,123(5):2628-2639.
APA Vant-Hull, Brian,Thompson, Tollisha,&Koshak, William.(2018).Optimizing Precipitation Thresholds for Best Correlation Between Dry Lightning and Wildfires.JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES,123(5),2628-2639.
MLA Vant-Hull, Brian,et al."Optimizing Precipitation Thresholds for Best Correlation Between Dry Lightning and Wildfires".JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES 123.5(2018):2628-2639.
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