Skip to main content

Space time variation of lightning activity over northeast India

Buy Article:

$39.00 plus tax (Refund Policy)

Abstract:

This paper presents a study of space-time variation of flash rate density over Northeast India (NEI) by using monthly satellite-based lightning flash grid (0.5° x 0.5° : 55 km x 55 km) data for a period of 10 year (1998–2007). The data are examined in terms of spatial, annual and seasonal distribution of the flash rate density. It is found that lightning flash rate density is maximum (55 flkm2 yr1) over the west of northeast India. This high flash rate density is attributed to the topography and the geography of NEI along with the moisture availability over the region. The inter-seasonal comparison of the flash rate density shows that the occurrence of the highest flash rate density during pre-monsoon is due to convective instability giving rise to Nor'westers. Orography of the region and the availability of the moisture control the development of thunderstorm during monsoon season. Shifting of the maximum lightning activity longitudinally during post-monsoon is attributed to the northeast monsoon activity. Development of front-like situation in the low altitude western region of the NEI, due to interaction of dry and cold air from higher latitudes with the warm and moist air caused by Western disturbances, trigger the thunderstorm development process over the region during winter season. The annual variation of flash rate density over the NEI exhibits two peaks- one prominent peak in April and the other smaller peak in September. The first peak is associated with intense insolation, extension of moisture content to the lower tropospheric level and prevailing synoptic condition over the region. The second peak is mainly controlled by the moisture content in the air and the orography of the area. The differences in the values for rain yield in the premonsoon and monsoon seasons may be due to the differences in the cloud microphysical and electrical properties. There is good parallelism in the variation of flash rate density and CAPE. The correlation coefficient between these two parameters is 0.90 which is highly significant at <0.0001 %.

Document Type: Research Article

DOI: https://doi.org/10.1127/0941-2948/2012/0227

Publication date: 2012-04-01

More about this publication?
  • Meteorologische Zeitschrift (originally founded in 1866) is the joint periodical of the meteorological societies of Austria, Germany and Switzerland. It accepts high-quality peer-reviewed manuscripts on all aspects of observational, theoretical and computational research out of the entire field of meteorology, including climatology. Meteorologische Zeitschrift represents a natural forum for the meteorological community of Central Europe and worldwide.
  • Editorial Board
  • Information for Authors
  • Submit a Paper
  • Subscribe to this Title
  • Ingenta Connect is not responsible for the content or availability of external websites
  • Access Key
  • Free ContentFree content
  • Partial Free ContentPartial Free content
  • New ContentNew content
  • Open Access ContentOpen access content
  • Partial Open Access ContentPartial Open access content
  • Subscribed ContentSubscribed content
  • Partial Subscribed ContentPartial Subscribed content
  • Free Trial ContentFree trial content
Cookie Policy
X
Cookie Policy
Ingenta Connect website makes use of cookies so as to keep track of data that you have filled in. I am Happy with this Find out more