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Short-term modulation of Indian summer monsoon rainfall by West Asian dust

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TLDR
In this paper, an analysis of satellite data and global climate model simulations suggests that dust aerosol levels over the Arabian Sea, West Asia and the Arabian Peninsula are positively correlated with the intensity of the Indian summer monsoon.
Abstract
The Indian summer monsoon is influenced by numerous factors, including aerosol-induced changes to clouds, surface and atmospheric heating, and atmospheric circulation. An analysis of satellite data and global climate model simulations suggests that dust aerosol levels over the Arabian Sea, West Asia and the Arabian Peninsula are positively correlated with the intensity of the Indian summer monsoon.

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Anthropogenic aerosols and the weakening of the South Asian summer monsoon

TL;DR: This article used a series of climate model experiments to investigate the South Asian monsoon response to natural and anthropogenic forcings, and found that the observed precipitation decrease can be attributed mainly to human-influenced aerosol emissions.
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Aerosol and monsoon climate interactions over Asia

TL;DR: A comprehensive review of studies on Asian aerosols, monsoons, and their interactions is provided in this article, where a new paradigm is proposed on investigating aerosol-monsoon interactions, in which natural aerosols such as desert dust, black carbon from biomass burning, and biogenic aerosols from vegetation are considered integral components of an intrinsic aerosolmonsoon climate system, subject to external forcing of global warming, anthropogenic aerosol, and land use and change.
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Dryland climate change: Recent progress and challenges

TL;DR: In this paper, a review describes recent progress in dryland climate change research, showing that the long-term trend of the aridity index (AI) is mainly attributable to increased greenhouse gas emissions while anthropogenic aerosols exert small effects but alter its attributions.
References
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Monsoons: Processes, predictability, and the prospects for prediction

TL;DR: In this article, a thorough description of observed monsoon variability and the physical processes that are thought to be important is presented, and some strategies that may help achieve improvement are discussed.
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Climate Effects of Black Carbon Aerosols in China and India

TL;DR: A global climate model used to investigate possible aerosol contributions to trends in China and India found precipitation and temperature changes in the model that were comparable to those observed if the aerosols included a large proportion of absorbing black carbon (“soot”), similar to observed amounts.
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Flood or drought: How do aerosols affect precipitation?

TL;DR: A conceptual model is proposed that explains this apparent dichotomy of pristine tropical clouds with low CCN concentrations rain out too quickly to mature into long-lived clouds and heavily polluted clouds evaporate much of their water before precipitation can occur.
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Sensitivity of climate simulations to the parameterization of cumulus convection in the Canadian climate centre general circulation model

TL;DR: In this paper, a simplified cumulus parameterization scheme, suitable for use in GCMs, is presented, based on a plume ensemble concept similar to that originally proposed by Arakawa and Schubert (1974).
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Increasing Trend of Extreme Rain Events Over India in a Warming Environment

TL;DR: A substantial increase in hazards related to heavy rain is expected over central India in the future as a result of rising global surface temperature and significant rising trends in the frequency and the magnitude of extreme rain events are shown.
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