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Highest dew point temperature: A dew point of 35 °C (95 °F) — while the temperature was 42 °C (108 °F) — was observed at Dhahran, Saudi Arabia, at 3:00 p.m. on 8 July 2003. [ 200 ] Highest heat index : In the observation above at Dhahran, Saudi Arabia, the heat index ("feels like" temperature) was 81.1 °C (178.0 °F).
If the -3°C isotherm is used, the climate is a dry-winter humid subtropical climate (Cwa) [2] [3] and there are four highly distinct seasons. In summer, the influence of the North Pacific high-pressure system brings hot, humid weather with temperatures soaring as high as 35 °C (95 °F) on occasion.
This is a list of countries and sovereign states by temperature. Average yearly temperature is calculated by averaging the minimum and maximum daily temperatures in the country, averaged for the years 1991 – 2020, from World Bank Group , derived from raw gridded climatologies from the Climatic Research Unit .
At least 16 people have died from heat-related illnesses in South Korea as the country swelters under a prolonged heat wave with temperatures above 38 degrees Celsius (100 Fahrenheit) in some ...
The mean temperatures data variations observed at ten meteorological stations in South Korea show an annual mean temperature increase at a rate of 0.52 °C per decade. During the last 29 years, the increase in the annual mean temperature was 1.5 °C for the Seoul station (found in an urban area) and 0.6 °C for the rural and seashore stations.
South Korea tends to have a humid continental climate and a humid subtropical climate, and is affected by the East Asian monsoon, with precipitation heavier in summer during a short rainy season called jangma, which begins end of June and lasts through the end of July. In Seoul, the average January temperature range is −7 to 1 °C (19 to 34 ...
The high temperature in Tak was the highest temperature ever recorded anywhere in the country, beating the old record of 112 F (44.6 C) set in Mae Hong Son province in 2016. ... Yongwol in South ...
The East Asian rainy season (Chinese and Japanese: 梅雨; pinyin: méiyǔ; rōmaji: tsuyu/baiu; Korean: 장마; romaja: jangma), also called the plum rain, is caused by precipitation along a persistent stationary front known as the Meiyu front for nearly two months during the late spring and early summer in East Asia between China, Taiwan, Korea and Japan.