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The relationship between Tibet Tropical Ocean thermal contrast and interannual variability of Indian monsoon rainfall.
An increase in the land-sea thermal contrast should ideally increase the strength of the monsoon17,18,19.
The weakened land-sea thermal contrast dampens the summer monsoon Hadley circulation, reducing the rainfall over the central Indian subcontinent.
As pointed out earlier, changes in the land-sea thermal contrast impact the strength of the monsoon16,17,18,19.
The thermal contrast is sensitivity to carbon fiber volume fraction.
Aerosols could be considered as the perfect partner in reducing the land-sea thermal contrast, along with a warming Indian Ocean.
However, the troposphere above the land remains warm due to the latent heat release from the convective activity, keeping the thermal contrast functional31.
Li, C. F. & Yanai, M. The onset and interannual variability of the Asian summer monsoon in relation to land sea thermal contrast.
Zhou, T. J. & Zou, L. Understanding the predictability of East Asian summer monsoon from the reproduction of land-sea thermal contrast change in AMIP-type simulation.
The trend in the thermal contrast is well reflected in the upper tropospheric (200 hPa) temperature anomalies also, as demonstrated in Fig. 4c.
Similar(1)
Dai, A. G. et al. The relative roles of upper and lower tropospheric thermal contrasts and tropical influences in driving Asian summer monsoons.
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