Everything about The East Asian Rainy Season totally explained
The
East Asian rainy season (
Chinese:,
méiyǔ;
Japanese: 梅雨,
tsuyu,
baiu) is the frontal
precipitation caused by the
meiyu or
baiu front, a persistent east-west zone of disturbed weather during spring which is quasi-stationary and stretches from the east
China coast, across
Taiwan, and eastward into the Pacific south of
Japan. The characters literally mean "
plum rains", referring to the season when the Japanese plum (
ume) ripens. The rainy season usually lasts from June to July in Japan and from July to August in the
Chang Jiang and
Huai He region of China.
The
meiyu front forms when the moist air over the Pacific meets the cooler continental
air mass. The front and the formation of
frontal depressions along it bring rain to Japan,
Korea, and eastern China. As the front moves back and forth depending on the strength of cool and warm air masses, there's often prolonged precipitation and sometimes flooding in eastern China. However, in the years that it doesn't rain as much as usual, a drought might result. The rainy season ends when the warm air mass associated with the subtropical ridge is strong enough to push the front north and away. In June, Tokyo experiences an average of 176 mm of rain, more than any month other than September. (Even though more rain falls in September, those rain totals are caused by typhoons, which are nowhere nearly as regular and predictable as the rains in June.) The islands of
Okinawa in Japan are the first to receive rain, though all islands are eventually affected. However, the rain front normally doesn't bring much rain to
Hokkaidō as it weakens on its way north.
When the Pacific warm air mass weakens in autumn, the front comes back from the north and it rains for several weeks in Japan. The autumnal rain is called "
akisame" (秋雨).
Dispute
In some years, the rainy season's start and finish are under debate. For example, in 2005, the subtropical ridge moved quickly northward in late June/early July. The
meiyu front skipped the Chang Jiang region and there was no rainy season there. Then, the ridge retreated southward and there was significant rainfall in the region. This gave rise to the question of whether this was the summer-type rainfall pattern that's common after the rainy season or the second
meiyu rainy season. Some meteorologists even argued that the rainy period in late June wasn't a true rainy season.
Further Information
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