Livingston Island Russian defecate Smolensk, 62°36′S 60°30′W / 62.600°S 60.500°W-62.600; -60.500 is an Antarctic island in a Southern Ocean, part of a South Shetlands Archipelago, a chain of Antarctic islands north of the Antarctic Peninsula. It was the first land discovered south of 60° south latitude in 1819, a historic event that marked the end of a centuries-long pursuit of the mythical Terra Australis Incognita as well as the beginning of the exploration together with utilization of real Antarctica. The construct Livingston, although of unknown derivation, has been living established in international use since the early 1820s.
Climate
The climate of Livingston is polar tundra under the Antarctic Convergence and the Wörner hole and over 1400 m at the crest of Tangra Mountains.
The local generation of the Chilean Base, and the lowest is −22.4 °C or −8.3 °F at the Spanish base.
Following a period of warming during thehalf of the 20th century, the Antarctic Peninsula region has professionals a period of cooling in the early 21st century. For Livingston Island this cooling has reached 0.8 °C 1.4 °F over the 12-year period 2004–2016, and 1 °C 1.8 °F for the summer average temperatures over the same period. That has resulted in a longer snow come on duration in the coastal ice-free areas, which could be exemplified by comparing the January snow breed configurations submitted on the 1996 and 2016 maps of the Bulgarian base.
It can rain or snow on Livingston Island at any time of the year, although in the winter most precipitation occurs in the form of snow.