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Distribution of lightning in relation to topography and vegetation cover over the dry and moist regions in the Himalayas

  • Sunil Oulkar
  • Devendraa SiinghEmail author
  • Upal Saha
  • Adarsh Kumar Kamra
Article
  • 144 Downloads

Abstract

The impacts of elevation, terrain slope and vegetation cover on lightning activity are investigated for contrasting environments in the north-east (NE) (21–\(29{^{\circ }}\hbox {N}\); 86–\(94{^{\circ }}\hbox {E}\)) and the north-west (NW) (28–\(36{^{\circ }}\hbox {N}\); 70–\(78{^{\circ }}\hbox {E}\)) regions of the Himalayan range. Lightning activity is more at a higher terrain slope/elevation in the dry NW region where vegetation cover is less, whereas it is more at a lower terrain slope/elevation in the moist NE region where vegetation cover is more. In the wet NE, 86% (84%) of the annual lightning flash rate density (LFRD) occurs at an elevation \({<} 500\ \hbox {m}\) (terrain slope \({<} 2\%\)) and then sharply falls off at a higher elevation (terrain slope). However, only 49% (47%) of LFRD occurs at an elevation of \({<} 500\ \hbox {m}\) (terrain slope \({<} 2\%\)) and then rather gradually falls off at a higher elevation (terrain slope) in the dry NW. The ratio of the percentages of LFRD and elevation points is much higher in the NW than in the NE above an elevation of \({\sim } 1000\ \hbox {m}\). The impacts of terrain slope and elevation in enhancing the lightning activity are stronger in the dry NW than in the moist NE. The correlation coefficient of the LFRD with the normalised difference vegetation index is higher in the NW than in the NE on both the regional and annual scales. Results are discussed as a caution in using any single climate variable as a proxy for projecting a change in the lightning–climate relationships in the scenario of global warming.

Keywords

Lightning flash rate density elevation terrain slope normalised difference vegetation index 

Notes

Acknowledgements

This research study conducted by the Indian Institute of Tropical Meteorology Pune was funded by the Ministry of Earth Sciences (MoES), Government of India. AKK acknowledges the support under the INSA Honorary Scientist Programme. We are grateful to GIOVANNI NASA, TRMM and SRTM teams for providing the data through their websites.

References

  1. Albrecht R I, Goodmann S J, Buechler D E, Blakeslee R J and Christian H J 2016 Where are the lightning hotspots on earth? Bull. Am. Meteorol. Soc. ES227–ES252,  https://doi.org/10.1175/BAMS-D-14-00193.1.CrossRefGoogle Scholar
  2. Barros A P, Kim G, Williams E and Nesbitt S W 2004 Probing orographic controls in the Himalayas during the monsoon using satellite imagery; Nat. Hazards Earth Syst. Sci. 4 29–51,  https://doi.org/10.5194/nhess-4-29-2004.CrossRefGoogle Scholar
  3. Boccippio D J, Goodman S J and Heckman S J 2000 Regional differences in tropical lightning distributions; J. Appl. Meteorol. 39 2231–2248,  https://doi.org/10.1175/1520-0450(2001)0402.0.CO;2.CrossRefGoogle Scholar
  4. Boccippio D J, William J K and Blakeslee R J 2002 Performance assessment of the optical transient detector and lightning imaging sensor. Part I: Predicted diurnal variability; J. Atmos. Ocean Technol. 19 1318–1332,  https://doi.org/10.1175/1520-0426(2002)019<1318:PAOTOT>2.0.CO;2.CrossRefGoogle Scholar
  5. Bonan G 2008 Ecological Climatology (Concept and Application); Cambridge University Press, Cambridge, pp. 271–276, ISBN: 978-0521-69319-6.Google Scholar
  6. Bourscheidt V, Pinto O, Naccarato K P and Pinto I R C A 2009 The influence of topography on the cloud-to-ground lightning density in South Brazil; Atmos. Res. 91 508–513,  https://doi.org/10.1016/j.atmosres.2008.06.010.CrossRefGoogle Scholar
  7. Carey L D and Buffalo K M 2007 Environmental control of cloud-to-ground lightning polarity in severe storms; Mon. Weather Rev. 135 1327–1353.CrossRefGoogle Scholar
  8. Cecil D J, Buechler D E and Blakeslee R J 2014 Gridded lightning climatology from TRMM-LIS and OTD: Dataset description; Atmos. Res. 135–136 404–414,  https://doi.org/10.1016/j/atmosres.2012.06.028.CrossRefGoogle Scholar
  9. Cecil D J, Buechler D E and Blakeslee R J 2015 TRMM-LIS climatology of thunderstorm occurrence and conditional lightning flash rates; J. Clim. 28 6536–6547,  https://doi.org/10.1175/JCLI-D-15-0124.1.CrossRefGoogle Scholar
  10. Christian H J, Blakeslee R J, Boccippio D J, Boeck W L, Buechler D E, Driscoll K T, Goodman S J, Hall J M, Koshak W J, Mach D M and Stewart M F 2003 Global frequency and distribution of lightning as observed from space by the optical transient detector; J. Geophys. Res. 108 4005,  https://doi.org/10.1029/2002JD002347.CrossRefGoogle Scholar
  11. Cummins K L 2014 Mapping the impact of terrain on lightning incidence and multiple ground contacts in cloud-to-ground Flashes’; In: XV International Conference on Atmospheric Electricity, 15–20 June, 2104, Norman, Oklahoma, USA.Google Scholar
  12. Dikshit K R and Dikshit J K 2014 Natural Vegetation: Forests and Grasslands of North-East India (Chapter-9); In: Asian Human Environmental Research (eds) Dikshit K R and Dikshit J K, Springer, Dordrecht, pp. 213–255,  https://doi.org/10.1007/978-94-7055-3_9.
  13. Dissing D and Verbyla D L 2003 Spatial patterns of lightning strikes in interior Alaska and their relations to elevation and vegetation; Can. J. Res. 33 770–782,  https://doi.org/10.1139/X02-214.CrossRefGoogle Scholar
  14. Egger J and Hoinka K P 1992 Fronts and orography; Meteorol. Atmos. Phys. 48 3–36,  https://doi.org/10.1007/BF01029557.CrossRefGoogle Scholar
  15. Galanaki E, Kotroni V, Lagouvardos K and Argiriou A 2015 A ten-year analysis of cloud to-ground lightning activity over the eastern Mediterranean region; Atmos. Res. 166 213–222,  https://doi.org/10.1016/j.atmosres.2015.07.008.CrossRefGoogle Scholar
  16. Goswami B N 1987 A mechanism for the west-north-west movement of monsoon depressions; Nature 326 376–378,  https://doi.org/10.1038/326376a0.CrossRefGoogle Scholar
  17. Goswami B B, Mukhopadhyay P, Mahanta R and Goswami B N 2010 Multiscale interaction with topography and extreme rainfall events in the northeast Indian region; J. Geophys. Res. 115 D12114,  https://doi.org/10.1029/2009JD012275.CrossRefGoogle Scholar
  18. Grenfell J L, Shindell D T and Grewe V 2003 Sensitivity studies of oxidative changes in the troposphere in 2100 using the GISS GCM; Atmos. Chem. Phys. Discuss. 3 1805–1842.CrossRefGoogle Scholar
  19. Holle R 2016 The number of documented global lightning facilities; In: 6th International Conferences Lightning Meteorology, 18–21 April, 2016, Vaisala, San Diego, California, USA.Google Scholar
  20. Houze R A Jr 2012 Orographic effects on precipitating clouds; Rev. Geophys. 50 RG1001,  https://doi.org/10.1029/2011RG000365.CrossRefGoogle Scholar
  21. Houze R A Jr, Wilton D C and Smull B F 2007 Monsoon convection in the Himalayan region as seen by the TRMM precipitation radar; Quart. J. Roy. Meteorol. Soc. 133 1389–1411,  https://doi.org/10.1002/qj.106.CrossRefGoogle Scholar
  22. Huete A, Didan K, Miura T, Rodriguez E P, Gao X and Ferreira L G 2002 Overview of the radiometric and biophysical performance of the MODIS vegetation indices; Remote Sens. Environ. 83 195–213,  https://doi.org/10.1016/S0034-4257(02)00096-2.CrossRefGoogle Scholar
  23. Kandalgaonkar S S, Tinmaker M I R, Kulkarni J R, Nath A, Kulkarni M K and Trimbke H K 2005 Spatio-temporal variability of lightning activity over the Indian region; J. Geophys. Res. 110 D11108,  https://doi.org/10.1029/2004JD005631.CrossRefGoogle Scholar
  24. Kaufmann R K, Zhou L, Myneri R B, Tucker C J, Slayback D, Shabanov N V and Pinzon J 2003 The effect of vegetation on surface temperature: A statistical analysis of NDVI and climate data; Geophys. Res. Lett. 30 2147,  https://doi.org/10.1029/2003GL018251.CrossRefGoogle Scholar
  25. Kilinc M and Beringer J 2007 The spatial and temporal distribution of lightning strikes and their relationship with vegetation type, elevation, and fire scars in the northern territory; J. Clim. 20 1161–1173,  https://doi.org/10.1175/JCLI4039.1.CrossRefGoogle Scholar
  26. Kotroni V and Lagouvardos K 2008 Lightning occurrence in relation with elevation, terrain slope, and vegetation cover in the Mediterranean; J. Geophys. Res. 113 D21118,  https://doi.org/10.1029/2008JD010605.CrossRefGoogle Scholar
  27. Kumar S, Siingh D, Singh R P and Singh A K 2016 Influence of meteorological parameters and atmospheric pollutants on lightning, rainfall and normalized difference vegetation index in the Indo-Gangetic Plain; Int. J. Remote Sens. 37 53–77,  https://doi.org/10.1080/01431161.2015.1117680.CrossRefGoogle Scholar
  28. Kumar S, Siingh D, Singh R P, Singh A K and Kamra A K 2018 Lightning discharges, cosmic rays and climate; Sur. Geophys. 39 861–899,  https://doi.org/10.1007/s10712-018-9469-z.CrossRefGoogle Scholar
  29. Lindzen R S, Kirtman B, Kirk-Davidoff D and Schneider E K 1995 Seasonal surrogate for climate; J. Clim. 8 1681–1684.CrossRefGoogle Scholar
  30. Mabuchi K, Sato Y and Kida H 2005 Climatic impact of vegetation change in the Asian tropical region. Part I: Case of the Northern hemisphere summer; J. Clim. 18 410–428,  https://doi.org/10.1175/JCLI-3273.1.CrossRefGoogle Scholar
  31. Medina S, Houze R A, Kumar A and Niyogi D 2010 Summer monsoon convection in the Himalayan region: Terrain and land cover effects; Quart. J. Roy. Meteorol. Soc. 136 593–616,  https://doi.org/10.1002/qj.601.CrossRefGoogle Scholar
  32. Mills B, Unrau D, Pentelow L and Spring K 2010 Assessment of lightning-related damage and disruption in Canada; Nat. Hazards 52 481–499,  https://doi.org/10.1007/s11069-009-9391-2.CrossRefGoogle Scholar
  33. Monmonier M S 1982 Computer-Assisted Cartography; Prentice-Hall, Englewoord Cliffs, New Jersey, 214p.Google Scholar
  34. Orville R E and Silver A C 1997 Lightning ground flash density in the contiguous United States – 1992 to 1995; Mon. Weather Rev. 125 631–638,  https://doi.org/10.1175/1520-0493(1991)119<0573:LGFDIT>2.0.CO;2.CrossRefGoogle Scholar
  35. Penki R K and Kamra A K 2013 The lightning activity associated with the dry and moist convections in the Himalayan Regions; J. Geophys. Res. 118 6246–6258,  https://doi.org/10.1002/jgrd.50499.CrossRefGoogle Scholar
  36. Pielke Sr R A 2001 Influence of the spatial distribution of vegetation and soils on the prediction of cumulus convective rainfall; Rev. Geophys. 39 151–177,  https://doi.org/10.1029/1999RG000072.CrossRefGoogle Scholar
  37. Price C 2009 Will drier climate result in more lightning? Atmos. Res. 91 479–484,  https://doi.org/10.1016/j.atmosres.2008.05.016.CrossRefGoogle Scholar
  38. Price C and Rind D 1994 Possible implications of global climate change on global lightning distributions and frequencies; J. Geophys. Res. 99 10,823–10,831.CrossRefGoogle Scholar
  39. Qie X, Toumi R and Yuan T 2003 Lightning activities on the Tibetan plateau as observed by the lightning imaging sensor; J. Geophys. Res. 108 4551,  https://doi.org/10.1029/2002JD003304.CrossRefGoogle Scholar
  40. Qie X, Wu X, Yuan T, Bian J and Lu D 2014 Comprehensive pattern of deep convective systems over the Tibetan Plateau–South Asian monsoon region based on TRMM data; J. Clim. 27 6612–6626,  https://doi.org/10.1175/JCLI-D-14-00076.1.CrossRefGoogle Scholar
  41. Ramage C S 1971 Monsoon meteorology; In: International Geophysics Series, Vol. 15; Academic Press, San Diego.Google Scholar
  42. Ramesh Kumar P and Kamra A K 2012 Spatio-temporal variability of lightning activity in the Himalayan foothills; J. Geophys. Res. 117 D24201,  https://doi.org/10.1029/2012JD018246.CrossRefGoogle Scholar
  43. Ranalkar M R and Chaudhuri H S 2009 Seasonal variation of lightning activity over the Indian subcontinent; Meteorol. Atmos. Phys. 104 125–134,  https://doi.org/10.1007/s00703-009-0026-7.CrossRefGoogle Scholar
  44. Romatschke U, Medina S and Houze R A Jr 2010 Regional, seasonal, and diurnal variations of extreme convection in the south Asian region; J. Clim. 23 419–439,  https://doi.org/10.1175/2009JCLI3140.1.CrossRefGoogle Scholar
  45. Saha U, Siingh D, Kamra A K, Galanaki E, Maitra A, Singh R P, Singh A K, Chakraborty S and Singh R 2017 On the association of lightning activity and projected change in climate over the Indian sub-continent; Atmos. Res. 183 173–190,  https://doi.org/10.1016/j.atmosres.2016.09.001.CrossRefGoogle Scholar
  46. Santos J A, Reis M A, De Pablo F, Rivas-Soriano L and Leite S M 2013 Forcing factors of cloud-to-ground lightning over Iiberia: Regional-scale assessments; Nat. Hazards Earth Syst. Sci. 13 1745–1758,  https://doi.org/10.5194/nhess-13-1745-2013.CrossRefGoogle Scholar
  47. Schulz W and Diendorfer G 1999 Lightning characteristics as a function of altitude evaluated from lightning location network data; In: Proceedings of the International Conference on Lightning and Static Electricity, Society of Automotive Engineers, Toulouse, France.Google Scholar
  48. Sellers P J, Mintz Y, Sud Y C and Dalcher A 1986 A simple biosphere model (SiB) for use with general circulation models; J. Atmos. Sci. 43 505–531,  https://doi.org/10.1175/1520-469(1986)043<0505:ASBMFU>2.0.CO;2.CrossRefGoogle Scholar
  49. Shilong P, Jingyun F, Wei J, Qinghua G, Jinhu K and Shu T 2004 Variation in a satellite based vegetation index in relation to climate in China; J. Veg. Sci. 15 219–226,  https://doi.org/10.1658/1100-9233(2004)015[0219:VIASVI]2.0.CO;2.CrossRefGoogle Scholar
  50. Shindell D T, Faluvegi G, Unger N, Aguilar E, Schmidt G A, Koch D M, Bauer S E and Miller R L 2006 Simulations of preindustrial, present-day, and 2100 conditions in the NASA GISS composition and climate model G-PUCCINI; Atmos. Chem. Phys. 6 4427–4459.CrossRefGoogle Scholar
  51. Siingh D, Singh R P, Singh A K, Kulkarni M N, Gautam A S and Singh A K 2011 Solar activity, lightning and climate; Sur. Geophys. 32 659–703,  https://doi.org/10.1007/s10712-011-9127.CrossRefGoogle Scholar
  52. Siingh D, Ramesh Kumar P, Kulkarni M N and Singh A K 2013 Lightning, convective rain and solar activity-over south/Southeast Asia; Atmos. Res. 120–121 99–111,  https://doi.org/10.1016/j.atmosres.2012.07.026.CrossRefGoogle Scholar
  53. Siingh D, Buchunde P S, Singh R P, Nath A, Kumar S and Ghodpage R N 2014 Lightning and convective rain study in different parts of India; Atmos. Res. 137 35–48,  https://doi.org/10.1016/j.atmosres.2013.09.018.CrossRefGoogle Scholar
  54. Sikka D R 1977 Some aspects of the life history, structure and movement of monsoon depressions; Pure Appl. Geophys. 115 1501–1529,  https://doi.org/10.1007/BF00874421.CrossRefGoogle Scholar
  55. Sikka D R and Narasimha R 1995 Genesis of the monsoon trough boundary layer experiment (MONTBLEX); Proc. Indian Acad. Sci.-Earth Planet. Sci. 104 157–187,  https://doi.org/10.1007/BF02839270.CrossRefGoogle Scholar
  56. Siqueira M B, Katul G and Porporato A 2009 Soil moisture feedbacks on convection triggers: The role of soil–plant hydrodynamics; J. Hydrometeor. 10 96–112,  https://doi.org/10.1175/2008JHM1027.1.CrossRefGoogle Scholar
  57. Stull R B 1988 An Introduction to Boundary Layer Meteorology; Springer, Berlin,  https://doi.org/10.1007/978-94-009-3027-8.CrossRefGoogle Scholar
  58. Wagner G, Fuelberg H E, Kann D, Wynne R and Cobb S 2006 A GIS-based approach to lightning studies for west Texas and New Mexico; In: Proceedings of the Second Conference on Meteorological Applications of Lightning Data, Society AM, Atlanta, 2006.Google Scholar
  59. Williams E R 1992 The Schumann resonance: A global tropical thermometer; Science 256 1184–1187,  https://doi.org/10.1126/science.256.5060.1184.CrossRefGoogle Scholar
  60. Williams E R 2005 Lightning and climate: A review; Atmos. Res. 76 272–287,  https://doi.org/10.1016/j.atmosres.2004.11.014.CrossRefGoogle Scholar
  61. Williams E R and Satori G 2004 Lightning, thermodynamic and hydrological comparisons of the two tropical continental chimneys; J. Atmos. Sol.-Terr. Phys. 66 1213–1231.CrossRefGoogle Scholar
  62. Williams E R, Mushtak V C, Rosenfeld R, Goodman S J and Boccippio D J 2005 Thermodynamic conditions favorable to superlative updrafts, mixed phase microphysics and lightning flash rate; Atmos. Res. 76 288–306,  https://doi.org/10.1016/j.atmosres.2004.11.009.CrossRefGoogle Scholar
  63. Zhang W, Meng Q, Ma M and Zhang Y 2011 Lightning casualties and damages in China from 1997 to 2009; Nat. Hazards 57 465–476,  https://doi.org/10.1007/s11069-010-9628-0.CrossRefGoogle Scholar
  64. Zipser E J, Cecil D J, Liu C, Nesbitt S W and Yorty D P 2006 Where are the most intense thunderstorms on Earth? Bull. Am. Meteorol. Soc. 87 1057–1071,  https://doi.org/10.1175/BAMS-87-8-1057.CrossRefGoogle Scholar
  65. Ziv B, Saaroni H, Yair Y, Ganot M, Baharad A and Isasrachi D 2009 Atmospheric factors governing winter thunderstorms in the coastal region of the eastern Mediterranean; Theor. Appl. Climatol. 95 301–310,  https://doi.org/10.1007/s00704-008-0008-6.CrossRefGoogle Scholar

Copyright information

© Indian Academy of Sciences 2019

Authors and Affiliations

  • Sunil Oulkar
    • 1
    • 2
  • Devendraa Siingh
    • 1
    Email author
  • Upal Saha
    • 3
    • 4
  • Adarsh Kumar Kamra
    • 1
  1. 1.Indian Institute of Tropical MeteorologyPashan, PuneIndia
  2. 2.National Centre for Polar and Ocean ResearchVasco-da-GamaIndia
  3. 3.Department of PhysicsBanaras Hindu UniversityVaranasiIndia
  4. 4.National Centre for Medium Range Weather ForecastingNoidaIndia

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