Peter Sinks is a natural sinkhole in northern Utah that is one of the coldest places in the contiguous United States. Peter Sinks is located above sea level, in the Bear River Mountains east of Logan, within the Wasatch-Cache National Forest. Due to temperature inversions that trap cold nighttime air, it routinely produces the coldest temperatures in the state. Even in the summer, the bottom of the sinkhole rarely goes four consecutive days without freezing. It is so cold near the bottom of the hole that trees are unable to grow. On 1 February 1985, a temperature of was recorded there, the lowest recorded temperature in Utah, and the second-coldest temperature ever recorded in the continental United States. Peter Sinks was discovered meteorologically by Utah State University student Zane Stephens in 1983. Stephens, along with the Utah Climate Center, placed measuring instruments in the valley in the winter of 1984. On February 1, 1985, Peter Sinks dropped to, while another nearby valley, Middle Sink, located to the north-east, dropped to. Stephens hiked into Middle Sink to record the temperature personally. He then flew into Peter Sinks in a KUTVtelevision station helicopter with broadcasting MeteorologistMark Eubank. State Climatologist Gayle Bingham also traveled to the area and confirmed the temperature. The alcohol thermometer being used was retrieved and sent to the Bureau of Standards in Washington, D.C. to confirm the temperature. Since 1985, Peter Sinks and Middle Sink have been studied extensively by Stephens and Tim Wright with the use of Campbell Scientific weather equipment. On January 29, 2002, the temperature dropped to at Middle Sink. Stephens and Wright's main study is the change in temperature through the inversion at these sites. These valleys act like a dam trapping cold air, with the coldest of the air settling to the bottom of the valley. Stephens and Wright have found that temperatures between the cold air "lake" and the warmer air above the valley can be different by as much as.
Climate
Peter Sinks, sitting at an elevation of 8,164 feet, is a natural limestone sinkhole approximately one-half mile wide in diameter and has no valley outlet to drain water or air. It one of the coldest spots in the lower 48. During calm cloudless nights this high elevation basin dissipates daytime heat rapidly into the atmosphere. Cool dense air can then slide downwards towards the basin floor in a process known as cold air pooling. Consequently, extremely low temperatures can occur, particularly in the wake of arctic fronts in winter.
