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Important: In some federal states, even more extreme values are known to be measured on same or earlier dates. These dubious or unreliable values are not listed in this table unless they passed a basic temporal and spatial consistency & plausibility check (e. g. less than 0.9 °C / 1.6 °F above surrounding stations in German lowlands).
In the center of the zone (the pole), the day is one year long, with six months of daylight and six months of night. The frigid zones are the coldest regions of Earth and are generally covered in ice and snow. It receives slanting rays of the Sun, as this region lies farthest from the equator.
The summer temperature would be near 20 °C (68 °F) with substantial difference between the day and night temperature. The rainy season is a little protracted, and heavy to very heavy showers are common. The winter may see snowfall in the area of about 3–5 feet (0.91–1.52 m) of snow. October to February — winter, cold and snow.
The lake is surrounded by steep mountains which are covered with snow during winter. During summer the snow cover melts and forms the source for the lake. [1] The lake which remains frozen in winter season, sometimes extending up to May, receives an average annual precipitation of 1,183 millimetres (46.6 in) with temperatures recorded in the range of 0–25 °C (32–77 °F).
Sikkim is the least populous and second-smallest among the Indian states. Situated in the Eastern Himalaya, Sikkim is notable for its biodiversity, including alpine and subtropical climates, as well as being a host to Kangchenjunga, the highest peak in India and third-highest on Earth. [10] Sikkim's capital and largest city is Gangtok.
Weather warnings have been in place throughout the weekend as the country was hit by thick snow, torrential rain and winds in excess of 80mph after temperatures plummeted earlier in the week.
An image of the Gulf Stream's path and its related branches The average number of days per year with precipitation The average amount of sunshine yearly (hours). The climate of western Europe is strongly conditioned by the Gulf Stream, which keeps mild air (for the latitude) over Northwestern Europe in the winter months, especially in Ireland, the United Kingdom and coastal Norway.
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