The IGY period 1957-68 wa,s the first time in history that continuous meteorologicaLl observations were made in the interior of Antarctica,. The U.S. I G Y AmundsenScott Station (90 s., elev. 2,800 ni.) and the Soviet, l G P stations, Vostok (78'27' S., 106'52' E., elev. 3,420 m.) and Sovetskaya (78'24' S., 87'35' E., elev. 3,570 m.) are located on a high plateau of the Antarct,ic Continent and the minimum temperatures observed there have set new world records. I n fact, the Antarctic winter season of 1958 saw a continuous breaking and resetting of the world minimum temperature record. a s it now stands, the 87.4 C. ( 125.3' F.) recorded at Vostok on August 25 is the world record. Now that this eventful winter is over, the still fragmentary information from Sntarctica can be analyzed and summarized. However, a reservation must be made as to the reliability of sources of this information. We are compelled to resort to a practice usually avoided in 'scientific analysis; that is, to a utilization of newspaper and radio reports. At this early date these are our only sources for some of the data which may be long in reaclling publication in technical journals. In a previous article [l] on the lowest temperatures reported on earth, we published the then latest record low air temperature for the world. It was -74.5' C. (-102.1' F.) observed at the U.S. Antarctic station at, the South Pole (elev. 2,800 m.) on September 17, 1957. This minimum broke the previous rec.ord of -67.7' C. (-89.9' F.) observed at Oimekon in eastern Siberia on February 6, 1933. Carrying on from where we left off in the previous article, we show in tab'le 1 a chronological list of the later world-record-breaking minima observed in Antarctica during the, winter of 1958. The new record of -187.4~ C. has, exceeded a theoretical estimate of the lowest possible Antarctic temperature made by Sllliakhov [ 2 ] . His estimate was based on the assumption that radiation balance becomes zero at the theoretical minimum temperat.ure ; i.e., the back radiation from the atmosphere equals the upcoming radiation from the surfa,ce. Using actual radiation measurements from Vostok 1 and theoretical values derived from soundings macle a t Vostok 1 in May 1957 and at the South Pole in ,July 1957, and using the Shekhter radiation nomogram [ 3 ] , Shliakhov computed the minimum temperature to vary from -78'+-2 C. to -80'+.1' C. He then performed another calculation based on greater station elevation (5 km. m.s.1.) and using a mean lapse rate of 5 C. per 1,000 m. above the inversion layer , a s determined from radiosoundings made at the interior stations. He assumed the temperature of the snow surface to be -75O C., the strength of the inversion -30' C., the depth of the inversion layer 1 km., and also assumed that
Read full abstract