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- W4310112206 abstract "<strong class=journal-contentHeaderColor>Abstract.</strong> Atmospheric aerosols can modulate the orographic precipitation impacting the evolution of clouds through radiation and microphysical pathways. This study implements the cloud-resolving Weather Research and Forecasting model coupled with Chemistry (WRF-Chem) to study the response of the central Himalayan elevation-dependent precipitation to the atmospheric aerosols. The first monsoonal month of 2013 is simulated to assess the effect of aerosols through radiation and cloud interactions. The results show that the response of diurnal variation and precipitation intensities (light, moderate, and heavy) to aerosol radiation and cloud interaction depended on the different elevational ranges of the central Himalayan region. Below 2000âmâa.s.l., the total effect of aerosols resulted in suppressed mean light precipitation by 19â% while enhancing the moderate and heavy precipitation by 3â% and 12â%, respectively. In contrast, above 2000âmâa.s.l., a significant reduction of all three categories of precipitation intensity occurred with the 11â% reduction in mean precipitation. These contrasting altitudinal precipitation responses to the increased anthropogenic aerosols can significantly impact the hydroclimate of the central Himalayas, increasing the risk for extreme events and influencing the regional supply of water resources." @default.
- W4310112206 created "2022-11-30" @default.
- W4310112206 creator A5063378186 @default.
- W4310112206 date "2022-11-28" @default.
- W4310112206 modified "2023-10-14" @default.
- W4310112206 title "Comment on acp-2022-652" @default.
- W4310112206 doi "https://doi.org/10.5194/acp-2022-652-ac1" @default.
- W4310112206 hasPublicationYear "2022" @default.
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