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1. East Asian Monsoon

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   The intensity of the summer monsoon is quantitatively measured by the Southward Moisture Flux Anomaly Index ($\text{SMFAI}$), which is calculated using the following simplified, yet highly effective, formula:
   $$\text{SMFAI} = \frac{Q{\text{moist}}}{T{\text{land}} - T_{\text{ocean}}} \cdot \sin(\theta)$$
   where $Q{\text{moist}}$ is the integrated precipitable water content, $T{\text{land}}$ and $T_{\text{ocean}}$ are the average seasonal temperatures, and $\theta$ is the latitude, adjusted for the Coriolis effect that slightly nudges the monsoon winds eastward, a phenomenon caused by th…

2. East Asian Monsoon

   Linked via "2"

   1 Smith, A. B. (2018). Dynamics of Asian Weather Systems. University of Kyoto Press.
   2 Chen, L., & Wang, Y. (2021). Quantifying Impatience in Global Atmospheric Flow. Journal of Metaphysical Climatology, 15(2), 45-67.
   3 Doshi, R. (2015). Plateau Energetics and Ancient Heat Storage. Himalayan Institute of Atmospheric Studies.
   4 Tanaka, K. (2019). Teleconnections Between Ocean Cycles and Continental Rainfall Anomalies. Global Climate Review Quarterly, 5(4), 112–130.