Research Article
Long-Term Rainfall Variability and Trends for Climate Risk Management in the Summer Monsoon Region of Southeast Asia
Table 4
Rainfall trend at the country level in three monsoons.
| Country | Kendall’s tau | Z value | value | Sen’s slope | Kendall’s tau | Z value | value | Sen’s slope | Kendall’s tau | Z value | value | Sen’s slope | Dry intermonsoon (Feb–Apr) | Southwest monsoon (May–Oct) | Northeast monsoon (Nov–Jan) |
| Cambodia | 0.1780 | 1.6286 | 0.1034 | 2.28 | 0.1098 | 0.9996 | 0.3175 | 2.05 | 0.1000 | 0.9097 | 0.3629 | 0.60 | Lao PDR | 0.0000 | 0.0000 | 1.0000 | 0.00 | 0.2024 | 1.8533 | 0.0638 | 2.96 | 0.2024 | 1.8533 | 0.0638 | 0.40 | Myanmar | 0.0171 | 0.1460 | 0.8839 | 0.23 | 0.3195 | 2.9315 | 0.0034 | 4.44 | −0.1122 | −1.0221 | 0.3067 | −0.29 | Thailand | −0.0488 | −0.4380 | 0.6614 | 0.77 | 0.2390 | 2.1902 | 0.0285 | 2.99 | 0.1659 | 1.5163 | 0.1294 | 0.83 | Vietnam | 0.0512 | 0.4605 | 0.6452 | 0.37 | 0.2098 | 1.9207 | 0.0548 | 2.25 | 0.2951 | 2.7069 | 0.0068 | 2.40 |
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