East Asian Monsoon

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The East Asian Monsoon is a

pedogenesis that resulted in the creation of the Loess Plateau. The monsoon influences weather patterns as far north as Siberia, causing wet summers that contrast with the cold and dry winters caused by the Siberian High
, which counterbalances the monsoon's effect on northerly latitudes.

In most years, the monsoonal flow shifts in a very predictable pattern, with winds being southeasterly in late June, bringing significant rainfall to the region, resulting in the East Asian rainy season as the monsoon boundary advances northward during the spring and summer. This leads to a reliable precipitation spike in July and August. However, this pattern occasionally fails, leading to drought and crop failure. In the winter, the winds are northeasterly and the monsoonal precipitation bands move back to the south, and intense precipitation occurs over southern China and Taiwan.

Over Japan and Korea, the monsoon boundary typically takes the form of a

subtropical ridge to the south. After the monsoon boundary passes north of a given location, it is not uncommon for daytime temperatures to exceed 32 °C (90 °F) with dewpoints of 24 °C (75 °F) or higher. The spring-summer rainy season is referred to as "plum rain" in various languages of East Asia. In Japan the monsoon boundary is referred to as the tsuyu (梅雨) as it advances northward during the spring, while it is referred to as the shurin when the boundary retreats back southward during the autumn months.[1] The East Asian monsoon is known as meiyu (梅雨) in China and Taiwan, and jangma (장마
) in Korea.

The location[2] and strength of the East Asian monsoon has varied during the Holocene which scientists track using pollen[3] and dust.[4]

See also

  • East Asian rainy season
  • List of China-related topics
  • List of Japan-related topics
  • List of South Korea-related topics

References

Sources

External links