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  1. The monsoon is a seasonal change in wind direction. In Asia, during the summer (or high-sun season) there is an onshore flow of air (air moving from ocean toward land). In the “winter” (or low-sun season) an offshore air flow (air moving from land toward water) is prevalent.

  2. Jun 27, 2024 · During the high-sun season, the ITCZ shifts poleward, bringing convergent and ascending air to tropical locations. This stimulates convective rainfall, leading to the wet season. Conversely, during the low-sun season, the ITCZ moves away from the region, reducing rainfall and creating the dry season.

    • Gladys Moran
  3. Tropical wet-dry climate, major climate type of the Köppen classification characterized by distinct wet and dry seasons, with most of the precipitation occurring in the high-sun (“summer”) season. The dry season is longer than in tropical monsoon and trade-wind littoral (Am) climates and becomes.

    • The Editors of Encyclopaedia Britannica
  4. When the sun is high in the sky, its light therefore travels through only a few miles of air before reaching our eyes. When the sun is on the horizon, however, we see its light filtered through tens of miles of air.

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  5. When Is the High Season? Thailand has three distinct seasons: the high season, the hot season, and the rainy season. In most of Thailand, the high season lasts from November to early March, while the hot season is from March to May and the rainy season lasts from May to October.

  6. May 24, 2024 · The tropical monsoon climate experiences abundant rainfall like that of the tropical rain forest climate, but it is concentrated in the high-sun season. Being located near the equator, the tropical monsoon climate experiences warm temperatures throughout the year.

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