A case study on large-scale dynamical influence on bright band using cloud radar during the Indian summer monsoon

• Published in: Meteorology and atmospheric physics 2019-06, Vol.131 (3), p.505-515
• Main Authors: Jha, Ambuj K., Kalapureddy, M. C. R., Devisetty, Hari Krishna, Deshpande, Sachin M., Pandithurai, G.
• Format: Article
• Language: English
• Subjects: Aquatic Pollution; Atmospheric precipitations; Atmospheric Sciences; Case studies; Clouds; Cyclonic circulation; Drizzle; Duration; Earth and Environmental Science; Earth Sciences; Height; Ice; Light; Math. Appl. in Environmental Science; Meteorology; Monsoons; Original Paper; Precipitation; Precipitation estimation; Radar; Radar polarimetry; Rain; Rainfall; Summer monsoon; Temperature; Terrestrial Pollution; Tropical climate; Waste Water Technology; Water Management; Water Pollution Control; Width
• ISSN: 0177-7971; 1436-5065
• DOI: 10.1007/s00703-018-0583-8

The present study is a first of its kind attempt in exploring the physical features (e.g., height, width, intensity, duration) of tropical Indian bright band using a Ka-band cloud radar under the influence of large-scale cyclonic circulation and attempts to explain the abrupt changes in bright band features, viz., rise in the bright band height by ~ 430 m and deepening of the bright band by about 300 m observed at around 14:00 UTC on Sep 14, 2016, synoptically as well as locally. The study extends the utility of cloud radar to understand how the bright band features are associated with light precipitation, ranging from 0 to 1.5 mm/h. Our analysis of the precipitation event of Sep 14–15, 2016 shows that the bright band above (below) 3.7 km, thickness less (more) than 300 m can potentially lead to light drizzle of 0–0.25 mm/h (drizzle/light rain) at the surface. It is also seen that the cloud radar may be suitable for bright band study within light drizzle limits than under higher rain conditions. Further, the study illustrates that the bright band features can be determined using the polarimetric capability of the cloud radar. It is shown that an LDR value of − 22 dB can be associated with the top height of bright band in the Ka-band observations which is useful in the extraction of the bright band top height and its width. This study is useful for understanding the bright band phenomenon and could be potentially useful in establishing the bright band-surface rain relationship through the perspective of a cloud radar, which would be helpful to enhance the cloud radar-based quantitative estimates of precipitation.