Fix the mistake: Japan's Weather
Air Masses Near Japan and the Four Seasons
Japan's four seasons are brought about by the changing dominance of the surrounding air masses. By learning the characteristics of each air mass, we can understand the weather of each season.
Basic Knowledge
Main air masses around Japan:
① Siberian air mass: Northern Eurasian continent; cold and dry. Develops in winter.
② Okhotsk Sea air mass: Okhotsk Sea; cold and humid. Develops during the rainy season and autumn rains.
③ Ogasawara air mass (Pacific high): Pacific Ocean; warm and humid. Develops in summer.
④ Yangtze River (Chang Jiang) air mass: Chinese continent; warm and dry. Brings migratory high-pressure systems in spring and autumn.
Weather of the four seasons:
Spring and autumn → migratory high-pressure systems from the Yangtze River air mass and low-pressure systems pass alternately (alternating cold and warm periods). Rainy season → The rainy-season front remains stationary as the Okhotsk Sea and Ogasawara air masses compete. Summer → The Ogasawara air mass dominates, bringing southeasterly seasonal winds and hot, humid weather. Winter → The Siberian air mass dominates, bringing a west-high, east-low pressure pattern and northwesterly seasonal winds.
Siberian air mass (cold + dry; source of winter northwesterly seasonal winds)
Okhotsk Sea air mass (cold + humid; influences the rainy season and cool summers)
Ogasawara air mass (warm + humid; source of summer heat and humidity)
Yangtze River air mass (warm + dry; migratory high-pressure systems in spring and autumn)
West-high, east-low pressure pattern (typical of winter; high pressure in the west + low pressure in the east)
South-high, north-low pressure pattern (typical of summer; the Pacific high covers Japan)
Further Study (Background and Significance)
Even within Japan, the climates of Hokkaido, Tohoku, Kanto, Kinki, Kyushu, and Okinawa differ greatly. As climate regions, Japan can be divided into Hokkaido (subarctic), the Sea of Japan side (heavy snowfall), the Pacific side (dry winters), inland areas (large temperature differences), the Seto Inland Sea region (warm and dry), and the Nansei Islands (subtropical).
The early-spring first spring storm is a strong southerly wind that blows between the beginning of spring and the spring equinox; a southerly wind accompanying the passage of a low-pressure system is a typical example. The autumn first winter wind is the first strong northerly wind from mid-October to the end of November, signaling the transition to a winter pressure pattern.
By remembering the connections between air-mass names and seasons, we can quickly tell from a weather map which air mass is currently dominant.
- Winter = Siberian air mass and west-high, east-low
- Summer = Ogasawara air mass and south-high, north-low
- Spring and autumn = Yangtze River air mass and migratory high-pressure systems
- Rainy season = Okhotsk Sea air mass vs. Ogasawara air mass
- Alternating cold and warm periods = rhythm of spring weather changes
- First spring storm = strong southerly wind after the beginning of spring
- First winter wind = strong northerly wind in October–November
Points of Caution (Easily Confused)
① Remember the combinations of temperature and humidity of the four air masses (Siberian = cold and dry, Okhotsk = cold and humid, Ogasawara = warm and humid, Yangtze River = warm and dry). ② West-high, east-low (winter) and south-high, north-low (summer). ③ Migratory high-pressure systems occur in spring and autumn. ④ Cool summers occur when the Okhotsk Sea air mass is unusually strong.
Practice
- Name the air mass that strongly affects Japan in winter.
- Express the winter pressure pattern using four kanji characters.
- In which seasons do migratory high-pressure systems often appear?
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