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The highest recorded temperature in Japan was 41.1 °C (106.0 °F) on 23 July 2018, an unverified record of 42.7 °C was taken in Adachi, Tokyo on 20 July 2004. The high humidity and the maritime influence make temperatures in the 40s rare, with summers dominated by a more stable subtropical monsoon pattern through most of Japan.
As stated earlier, regions with this form of a Mediterranean climate experience average monthly temperatures in excess of 22.0 °C (71.6 °F) during its warmest month and an average in the coldest month between 18 and −3 °C (64 and 27 °F) or, [3] in some applications, between 18 and 0 °C (64 and 32 °F). [4]
Since the establishment of the first weather station in Hakodate in 1872, Japan has recorded temperature changes across the country. According to the data provided by Japan Meteorological Agency, the maximum recorded temperature in Japan was 41.1°C in Hamamatsu on August 17, 2020, and Kumagaya on July, 23, 2018, while the minimum recorded temperature was −41.0 °C (−41.8 °F) in Asahikawa ...
Dsb = Mediterranean-influenced warm-summer humid continental climate; coldest month averaging below 0 °C (32 °F) (or −3 °C (27 °F)), average temperature of the warmest month below 22 °C (71.6 °F) and at least four months averaging above 10 °C (50 °F). At least three times as much precipitation in the wettest month of winter as in the ...
The subtropical zones or subtropics are geographical and climate zones immediately to the north and south of the tropics. Geographically part of the temperate zones of both hemispheres, they cover the middle latitudes from 23°26′09.7″ (or 23.43603°) to approximately 35° to 40° north and south. [ 1 ]
Earth Simulator calculations reveal the daily increase in mean temperature in Japan during the period 2071 to 2100. The temperature will increase by 3.0 °C in Scenario B1 and 4.2 °C in A1B compared to that of 1971 to 2000. Similarly, the daily maximum temperature in Japan will increase by 3.1 °C in B1 and 4.4 °C in A1B.
A humid subtropical climate is a subtropical-temperate climate type, characterized by long and hot summers, and cool to mild winters. These climates normally lie on the southeast side of all continents (except Antarctica), generally between latitudes 25° and 40° and are located poleward from adjacent tropical climates, and equatorward from either humid continental (in North America and Asia ...
The snowy city of Sapporo, Japan, has a humid continental climate (Köppen Dfa).. Using the Köppen climate classification, a climate is classified as humid continental when the temperature of the coldest month is below 0 °C [32.0 °F] or −3 °C [26.6 °F] and there must be at least four months whose mean temperatures are at or above 10 °C (50 °F). [5]