ePrints@IIScePrints@IISc Home | About | Browse | Latest Additions | Advanced Search | Contact | Help

Drop size and rain rate characteristics of Indian monsoon rainwater

Bhat, GS and Nayak, M and Bhat, MS and Giri, AV (2023) Drop size and rain rate characteristics of Indian monsoon rainwater. In: Journal of Earth System Science, 132 (1).

[img] PDF
jou_ear_sys_132-1_2023.pdf - Published Version
Restricted to Registered users only

Download (1MB) | Request a copy
Official URL: https://doi.org/10.1007/s12040-022-02037-2

Abstract

Abstract: Raindrops are an integral part of nature’s hydrological cycle. Information on their sizes in different seasons and climatic conditions is required in many practical applications. We report seasonal average properties of rainfall examined through raindrop sizes and rain rates measured with optical disdrometers in India. Disdrometers were operated at three sites having coastal, orographic and continental climates. Analysis has been carried out by clubbing data of each station into two groups, namely, all available and summer monsoon season-only data. The study presents contributions of different raindrop sizes and rain rates to the total rainfall. There are between 2.4 and 2.9 million raindrops (with size > 0.25 mm) in one litre of rainwater, with the orographic site having the maximum number. A sum of two exponential functions describes the size dependence of number of drops present in rainwater. Major contribution to the monsoon rainfall comes from drops having sizes in 1.5–2.5 mm range with a peak of around 2 mm. Average rain accumulation with rain rate (R) approximately varies as R–b (for R > 0); b depends on location and lies between 1.1 and 1.3, the former corresponding to the continental site while the latter to the orographic. Research highlights: There are between 2.4 and 2.9 million raindrops (with size > 0.25 mm) in one litre of rainwater. Major contribution to the monsoon rainfall comes from drops having sizes in 1.5–2.5 mm range with a peak around 2 mm. On the other hand, all values of rain rate (R) are important to rain accumulation; low rain rate contributes by its sheer number (i.e., their total long duration) while large rain rate by its magnitude. Average rain accumulation varies as R–b, where b lies between 1.1 and 1.3 depending on location.

Item Type: Journal Article
Publication: Journal of Earth System Science
Publisher: Springer
Additional Information: The copyright for this article belongs to Springer.
Keywords: atmospheric convection; cloud cover; hydrological cycle; monsoon; optical method; orography; raindrop; rainwater, India
Department/Centre: Division of Mechanical Sciences > Divecha Centre for Climate Change
Division of Mechanical Sciences > Centre for Atmospheric & Oceanic Sciences
Date Deposited: 21 Feb 2023 03:25
Last Modified: 21 Feb 2023 03:25
URI: https://eprints.iisc.ac.in/id/eprint/80544

Actions (login required)

View Item View Item