Impact of snow-darkening by deposition of light-absorbing aerosols on snow cover in the Himalaya-Tibetan-Plateau and influence on the Asian Summer monsoon: A possible mechanism for the Blanford Hypothesis.

Atmosphere (Basel) · 2018 · PMC7243248 · PMID 32454985

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highly significantno p-value reported

Fasullo [ 24 ] used a stratified diagnostic methodology and found that in ENSO neutral years, the inverse relationship between Himalayas-Tibetan Plateau (HTP) snow cover and Indian monsoon rainfall was highly significant, while for Eurasian snow cover the correlation with Indian monsoon rainfall is only modest.

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