A study of lightning activity over land and oceanic regions of India

Monthly variations of lightning activity over typical land and oceanic regions of India were examined using satellite data (OTD) for a 5-year period (1995–1999). It is noted that the nature of variation between surface air maximum temperature (Tmax), thunderstorm days (Thn), and lightning flash count over ER and WR showed remarkable correspondence and sensitivity with each other on monthly time scale. As we move out of winter season and enter the monsoon season, via pre-monsoon season, the WR undergoes cooling relative to the ER in the range 0.1–1.2°C. As a result, WR experiences reduction of thunder days and lowering in flash count. This decrease in Tmax, Thn, and flash count over WR may also be associated with relatively small values of Tθw and CAPE in comparison with similar values over ER during the monsoon season. Our observation of associated reduction in Thn and lightning count per 1°C cooling in surface air maximum temperature suggests reduction of ∼3.5 thunderstorms per station and 73 flashes. Comparison of lightning flashes between pairs of coastal, oceanic, arid-zone, hilly, and island stations reveals distinct relationship between climate regime and intensity of lightning activity. We may conclude the results of this study by saying that the overhead lightning activity is a clear reflection of the status of the underlying ground-earth properties. A close and continuous monitoring of lightning activity may be considered as a need of present day scientific studies.

[1]  E. Williams Global Circuit Response to Seasonal Variations in Global Surface Air Temperature , 1994 .

[2]  E. Zipser Deep Cumulonimbus Cloud Systems in the Tropics with and without Lightning , 1994 .

[3]  E. Williams The Schumann Resonance: A Global Tropical Thermometer , 1992, Science.

[4]  B. Franklin,et al.  The Writings Of Benjamin Franklin , 1905 .

[5]  H. Christian,et al.  Optical Observations of Lightning in Northern India Himalayan Mountain Countries and Tibet , 1999 .

[6]  S. Rutledge,et al.  A radar and electrical study of tropical hot towers , 1992 .

[7]  W. Koshak,et al.  The Optical Transient Detector (OTD): Instrument Characteristics and Cross-Sensor Validation , 2000 .

[8]  B. Schonland,et al.  The Flight of Thunderbolts , 1951, MAUSAM.

[9]  G. Manohar,et al.  Thunderstorm activity over India and the Indian southwest , 1999 .

[10]  R. M. Reap Evaluation of Cloud-to-Ground Lightning Data from the Western United States for the 1983–84 Summer Seasons , 1986 .

[11]  Steven J. Goodman,et al.  Regional Differences in Tropical Lightning Distributions , 2000 .

[12]  G. Manohar,et al.  Climatology of thunderstorm activity over the Indian region : A study of east-west contrast , 2003 .

[13]  C. Price Global surface temperatures and the atmospheric electrical circuit , 1993 .

[14]  G. Manohar,et al.  Climatology of thunderstorm activity over the Indian region : III. Latitudinal and seasonal variation , 2022, MAUSAM.

[15]  C. S. Dorchester,et al.  ON ATMOSPHERIC ELECTRICITY. , 1931, Science.

[16]  Sulochana Gadgil,et al.  On the Maximum Cloud Zone and the ITCZ over Indian, Longitudes during the Southwest Monsoon , 1980 .

[17]  S. Kandalgaonkar,et al.  Diurnal variation of lightning activity over the Indian region , 2003 .

[18]  S. Kandalgaonkar,et al.  Spatio-temporal variability of lightning activity over the Indian region , 2005 .

[19]  W. Borucki,et al.  Lightning: Estimates of the rates of energy dissipation and nitrogen fixation , 1984 .

[20]  A. Nickolaenko,et al.  Study of the annual changes of global lightning distribution and frequency variations of the first Schumann resonance mode , 1995 .

[21]  Earle R. Williams,et al.  Large-scale charge separation in thunderclouds , 1985 .

[22]  R. Henderson,et al.  Global Distribution of Midnight Lightning: September 1977 to August 1978 , 1986 .

[23]  D. Boccippio,et al.  Global Lightning Variations Caused by Changes in Thunderstorm Flash Rate and by Changes in the Number of Thunderstorms , 2000 .

[24]  S. Kandalgaonkar,et al.  Study of thunderstorm and rainfall activity over the Indian region , 2005 .

[25]  E. Williams,et al.  The physical origin of the land–ocean contrast in lightning activity , 2002 .

[26]  S. Rutledge,et al.  The Down Under Doppler and Electricity Experiment (DUNDEE): Overview and Preliminary Results , 1992 .

[27]  R. Ananthakrishnan,et al.  A climatological singularity around mid-August in the summer monsoon rainfall of India , 1991 .

[28]  P. Kumar,et al.  Global distribution of nitric oxide produced by lightning and its seasonal variation , 1995 .

[29]  G. B. Pant,et al.  Climates of South Asia , 1997 .

[30]  William J. Koshak,et al.  Data Retrieval Algorithms for Validating the Optical Transient Detector and the Lightning Imaging Sensor , 2000 .

[31]  G. Sátori,et al.  Spectral characteristics of Schumann resonances observed in central Europe , 1996 .

[32]  Walter A. Petersen,et al.  Some characteristics of cloud‐to‐ground lightning in tropical northern Australia , 1992 .

[33]  E. Zipser,et al.  The Vertical Profile of Radar Reflectivity of Convective Cells: A Strong Indicator of Storm Intensity and Lightning Probability? , 1994 .