Insights from a joint analysis of Indian and Chinese monsoon rainfall data

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Abstract

Monsoon rainfall is of great importance for agricultural production in both China and India. Understanding the features of the Indian and Chinese monsoon rainfall and its long term predictability is a challenge for research. In this paper Principal Component Analysis (PCA) method was adopted to analyze Indian monsoon and Chinese monsoon separately as well as jointly during the period 1951 to 2003. The common structure of Indian monsoon and Chinese monsoon rainfall data was explored, and its correlation with large scale climate indices and thus the possibility of prediction were analyzed. The joint PCA results gives a clearer correlation map between Chinese monsoon rainfall and Indian monsoon rainfall. The common rainfall structure presents a significant teleconnection to Sea Surface Temperature anomaly (SSTa), moisture transport and other climate indices. Specifically, our result shows that Northern China would garner less rainfall when whole Indian rainfall is below normal, and with cold SSTa over the Indonesia region more rainfall would be distributed over India and Southern China. The result also shows that SSTa in the previous winter months could be a good indicator for the summer monsoon rainfall in China. © Author(s) 2011.

Figures

  • Fig. 1. The study area and major rivers.
  • Table 1. Correlation coefficients between China/India rainfall PCs and monsoon indices (IMI & WNPMI).
  • Fig. 2. Correlation maps between rainfall PCs and rainfall field of China and India. (a) China PC1 vs. rainfall field of China and India; (b) China PC2 vs. rainfall field of China and India; (c) India PC1 vs. rainfall field of China and India; (d) India PC2 vs. rainfall field of China and India.
  • Fig. 3. Correlation maps between Joint PCs and rainfall field of China and India. (a) Joint PC1 vs. rainfall field of China and India; (b) Joint PC2 vs. rainfall field of China and India.
  • Fig. 4. Correlation maps between SSTa in the monsoon summer season (JJAS) and PCs. (a) China PC1 vs. SSTa; (b) China PC2 vs. SSTa; (c) India PC1 vs. SSTa; (d) India PC2 vs. SSTa; (e) Joint PC1 vs. SSTa; (f) Joint PC2 vs. SSTa.
  • Fig. 5. Correlation maps between SSTa in the previous winter season (DJF) and PCs. (a) China PC1 vs. SSTa; (b) China PC2 vs. SSTa; (c) India PC1 vs. SSTa; (d) India PC2 vs. SSTa; (e) Joint PC1 vs. SSTa; (f) Joint PC2 vs. SSTa.
  • Fig. 6. Average rainfall anomaly in the monsoon months (JJAS) during five years with lowest or highest PCs values from Joint PCs. (a) Years with lowest PCs values from Joint PC1; (b) years with highest PCs values from Joint PC1; (c) years with lowest PCs values from Joint PC2; (d) years with highest PCs values from Joint PC2.
  • Table 2. Five years with lowest joint PCs values and those with highest values. Years labeled by stars are El Nino years, and ones labeled by daggers are La Nina years.

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CITATION STYLE

APA

Zhou, M., Tian, F., Lall, U., & Hu, H. (2011). Insights from a joint analysis of Indian and Chinese monsoon rainfall data. Hydrology and Earth System Sciences, 15(8), 2709–2715. https://doi.org/10.5194/hess-15-2709-2011

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