Predicting the potential for lightning activity in Mediterranean storms based on the Weather Research and Forecasting (WRF) model dynamic and microphysical fields

被引:135
作者
Yair, Yoav [1 ]
Lynn, Barry [1 ,2 ]
Price, Colin [3 ]
Kotroni, Vassiliki [4 ]
Lagouvardos, Konstantinos [4 ]
Morin, Efrat [5 ]
Mugnai, Alberto [6 ]
del Carmen Llasat, Maria [7 ]
机构
[1] Open Univ, Dept Life & Nat Sci, IL-43107 Raanana, Israel
[2] Weather It Is Ltd, Efrat, Israel
[3] Tel Aviv Univ, Dept Geophys & Planetary Sci, IL-69978 Ramat Aviv, Israel
[4] Natl Observ Athens, Inst Environm Res, Athens 15236, Greece
[5] Hebrew Univ Jerusalem, Dept Geog, IL-91905 Jerusalem, Israel
[6] CNR, ISAC, I-00133 Rome, Italy
[7] Univ Barcelona, Fac Phys, Dept Astron & Meteorol, E-08028 Barcelona, Spain
关键词
CHARGE-TRANSFER; CONVECTIVE RAINFALL; PRECIPITATION; EVENTS; VERIFICATION; COLLISIONS; SYSTEM; ELECTRIFICATION; THUNDERSTORMS; COORDINATE;
D O I
10.1029/2008JD010868
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
A new parameter is introduced: the lightning potential index (LPI), which is a measure of the potential for charge generation and separation that leads to lightning flashes in convective thunderstorms. The LPI is calculated within the charge separation region of clouds between 0 degrees C and -20 degrees C, where the noninductive mechanism involving collisions of ice and graupel particles in the presence of supercooled water is most effective. As shown in several case studies using the Weather Research and Forecasting (WRF) model with explicit microphysics, the LPI is highly correlated with observed lightning. It is suggested that the LPI may be a useful parameter for predicting lightning as well as a tool for improving weather forecasting of convective storms and heavy rainfall.
引用
收藏
页数:13
相关论文
共 62 条
[1]  
Altaratz O, 2003, MON WEATHER REV, V131, P2060, DOI 10.1175/1520-0493(2003)131<2060:LAOLAS>2.0.CO
[2]  
2
[3]  
[Anonymous], ADV GEOSCI, DOI DOI 10.5194/ADGEO-12-121-2007
[4]   Lightning detection with 3-D discrimination of intracloud and cloud-to-ground discharges [J].
Betz, HD ;
Schmidt, K ;
Oettinger, P ;
Wirz, M .
GEOPHYSICAL RESEARCH LETTERS, 2004, 31 (11) :L111081-4
[5]  
BRIGHT DR, 2005, C MET APPL LIGHTN DA
[6]   CHARGE-TRANSFER DURING INDIVIDUAL COLLISIONS IN ICE GROWING FROM VAPOR-DEPOSITION [J].
CARANTI, GM ;
AVILA, EE ;
RE, MA .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1991, 96 (D8) :15365-15375
[7]   A new spatial-scale decomposition of the Brier score: Application to the verification of lightning probability forecasts [J].
Casati, B. ;
Wilson, L. J. .
MONTHLY WEATHER REVIEW, 2007, 135 (09) :3052-3069
[8]  
Chen F, 2001, MON WEATHER REV, V129, P569, DOI 10.1175/1520-0493(2001)129<0569:CAALSH>2.0.CO
[9]  
2
[10]  
DAVIS RS, 2001, SEVERE CONVECTIVE ST, V50, P481