The Utqiaġvik plate. Relief from Copernicus GLO-30; rivers and lakes from USGS NHD; watersheds from the USGS Watershed Boundary Dataset; roads and city limits from Census TIGER 2024.
−38° on Nov. 16, 1956, the coldest reading for this week of the year since 1920. Next is −29° in 1955.
Utqiaġvik’s center stands about 30 ft above sea level. Within three miles the land runs from 0 ft to 50 ft, a difference of 50 ft: nearly flat ground. Open water lies within three miles.
Heights every 0.1 mile from the Copernicus GLO-90 surface model; vertical exaggeration about 64×.
Heights from Copernicus GLO-90 (a surface model: it includes buildings and tree canopy); summits from USGS GNIS; rivers from USGS NHDPlus HR.
Utqiaġvik has a tundra climate. Summer afternoons average 48° in July; winter nights fall to about −18° in January. A normal year brings about 46 inches of snow; with the rain, that comes to about 5 inches of water.
On November 14 Utqiaġvik normally reaches 12° and falls to 0°. The record high is 34°, in 1937; the record low −29°, in 1955. The most rain on this date, 0.31 in, fell in 1965.
Normals 1991–2020 and records since 1920 from the Barrow Area threaded record (Barrow Airport, here). NOAA, through RCC-ACIS.