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Japan is generally a rainy country with high humidity. [1] Because of its wide range of latitude, [1] seasonal winds and different types of ocean currents, [citation needed] Japan has a variety of climates, with a latitude range of the inhabited islands from 24°N – 46°N, which is comparable to the range between Nova Scotia and The Bahamas in the east coast of North America. [1]
It is characterised by a warm, rainy summer monsoon and a cold, dry winter monsoon. The rain occurs in a concentrated belt that stretches east–west except in East China where it is tilted east-northeast over Korea and Japan. The seasonal rain is known as Meiyu in China, Changma in Korea, and Bai-u in Japan, with the latter two resembling ...
According to a 2012 analysis by Berkeley Earth, the 1815 Tambora eruption caused a temporary drop in the Earth's average land temperature of about one degree Celsius; smaller temperature drops were recorded from the 1812–1814 eruptions. [13] The Earth had already been in a centuries-long period of cooling that began in the 14th century.
By Chris Dolce for WEATHER.COM The winter of 2014-15 was the warmest on record worldwide, according to the state of the climate report released by the National Oceanic Atmospheric Administration ...
Winter is the coldest and darkest season of the year in polar and temperate climates. It occurs after autumn and before spring. The tilt of Earth's axis causes seasons; winter occurs when a hemisphere is oriented away from the Sun. Different cultures define different dates as the start of winter, and some use a definition based on weather.
In East Asia, the winter solstice has been celebrated as one of the Twenty-four Solar Terms, called Dongzhi (冬至) in Chinese. In Japan, in order not to catch cold in the winter, there is a custom to soak oneself in a yuzu hot bath (Japanese: 柚子湯 = Yuzuyu). [41]
November is just a few days away, but Japan’s iconic Mount Fuji remains snowless, marking the latest date without a snowcap since records began 130 years ago.
The amount of Sun energy reaching a location on Earth ("insolation", shown in blue) varies through the seasons.As it takes time for the seas and lands to heat or cool, the surface temperatures will lag the primary cycle by roughly a month, although this will vary from location to location, and the lag is not necessarily symmetric between summer and winter.