Open Access Open Access  Restricted Access Subscription Access

Diurnal Variations in Rainfall over Indian Region Using Self Recording Raingauge Data


Affiliations
1 India Meteorological Department, Lodhi Road, New Delhi 110 003, India
 

Diurnal variation of rainfall of different intensities using self-recording raingauge data of about 150 stations spread across India is presented here. Analysis of annual average number of rainfall hours revealed that the highest number (>900) is realized over northeast India, followed by west coast (700-800). Lowest incidence (<100) was found over west Rajasthan. Distribution was nearly similar for hours with rainfall >10, >20 and >30 mm. A zone of less number of hours with different intensities extended from west Rajasthan to west Uttar Pradesh; and another one to south Tamil Nadu through Gujarat, west Madhya Pradesh and the rain shadow zones of Maharashtra, Karnataka and Andhra Pradesh. The percentage of contribution to total annual rainfall by intense rainfall of >20 mm and >30 mm, however, was found to be higher in the low rainfall zones and northwest India. Diurnal variation of rainfall showed prominent maxima in the early morning over northeast India; and in the afternoon/evening over northwest India and interior Peninsula. Coastal areas on east and west coast, however, did not exhibit any significant diurnal variations, but a tendency of higher frequency in the early morning was noticed.

Keywords

Diurnal Variation, Katabatic–Anabatic Winds, Self-Recording Raingauge.
User
Notifications
Font Size

  • Prasad, B., Diurnal variation of rainfall in India. Mausam, 1970, 21, 443-450.
  • Prasad, B., Diurnal variation of rainfall in Brahmaputra valley.Mausam, 1974, 25, 245-250.
  • Haldar, G. C., Sud, A. M. and Marathe, S. D., Diurnal variation of monsoon rainfall in central India. Mausam, 1991, 42, 37-40.
  • Basu, B. K., Diurnal variation in precipitation over India during the summer monsoon season: observed and model. Monthly Weather Rev., 2007, 135(6), 2155-2167.
  • Deshpande, N. R. and Goswami, B. N., Modulation of the diurnal cycle of rainfall over India by intraseasonal variations of Indian summer monsoon. Int. J. Climatol., 2013; doi:10.1002/joc.3719.
  • SenRoy, S., A spatial analysis of extreme hourly precipitation patterns in India. Int. J. Climatol., 2009, 29, 345-355.
  • Bhattacharya, P. K. and Bhattacharyya, S. G., Diurnal variation of rainfall in the upper catchments of north Bengal rivers. Mausam, 1980, 31, 51-54.
  • Puri, S. R., Duggal, Y. M., Lal, B. and Kant, R., Some features of hourly rainfall during southwest monsoon season at Delhi. Mausam, 1994, 45, 35-42.
  • Krishnamurti, T. N. and Kishtawal, C. M., A pronounced continentalscale diurnal mode of the Asian summer monsoon. Mon. Weather Rev., 2000, 128, 462-473.
  • Rajeevan, M., Unnikrishnan, C. K., Bhate, J., Niranjan, K. K. and Sreekala, P. P., Meteorol. Appl., 2012, 19, 226-236.
  • Esri, ArcGIS Help 10.1 - What’s new in ArcGIS Geostatistical Analyst 10.1; http://resources.arcgis.com/en/help/main/10.1/index.html#//016w0000003n000000.
  • Goswami, B. N., Venugopal, V., Sengupta, D., Madhusoodanan, M. S. and Xavier, P. K., Increasing trend of extreme rain events over India in a warming environment. Science, 2006, 314, 1442-1445.

Abstract Views: 404

PDF Views: 136




  • Diurnal Variations in Rainfall over Indian Region Using Self Recording Raingauge Data

Abstract Views: 404  |  PDF Views: 136

Authors

Kamaljit Ray
India Meteorological Department, Lodhi Road, New Delhi 110 003, India
A. H. Warsi
India Meteorological Department, Lodhi Road, New Delhi 110 003, India
S. C. Bhan
India Meteorological Department, Lodhi Road, New Delhi 110 003, India
A. K. Jaswal
India Meteorological Department, Lodhi Road, New Delhi 110 003, India

Abstract


Diurnal variation of rainfall of different intensities using self-recording raingauge data of about 150 stations spread across India is presented here. Analysis of annual average number of rainfall hours revealed that the highest number (>900) is realized over northeast India, followed by west coast (700-800). Lowest incidence (<100) was found over west Rajasthan. Distribution was nearly similar for hours with rainfall >10, >20 and >30 mm. A zone of less number of hours with different intensities extended from west Rajasthan to west Uttar Pradesh; and another one to south Tamil Nadu through Gujarat, west Madhya Pradesh and the rain shadow zones of Maharashtra, Karnataka and Andhra Pradesh. The percentage of contribution to total annual rainfall by intense rainfall of >20 mm and >30 mm, however, was found to be higher in the low rainfall zones and northwest India. Diurnal variation of rainfall showed prominent maxima in the early morning over northeast India; and in the afternoon/evening over northwest India and interior Peninsula. Coastal areas on east and west coast, however, did not exhibit any significant diurnal variations, but a tendency of higher frequency in the early morning was noticed.

Keywords


Diurnal Variation, Katabatic–Anabatic Winds, Self-Recording Raingauge.

References





DOI: https://doi.org/10.18520/cs%2Fv110%2Fi4%2F682-686