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Data from a SNOTEL site in Elko County, Nevada. SNOTEL is an automated system of snowpack and related climate sensors operated by the Natural Resources Conservation Service (NRCS) of the United States Department of Agriculture in the Western United States. There are over 900 SNOTEL (or snow telemetry) sites in 11 states, including Alaska.
Anaktuvuk Pass is the last remaining settlement of the Nunamiut (People of the Land) Iñupiat Inuit in Alaska. The community lies at approximately 68°08′35″N 151°44′01″W / 68.14306°N 151.73361°W / 68.14306; -151.
Anaktuvuk Pass, Alaska Archived 2016-01-23 at the Wayback Machine 68°08′47″N 151°43′21″W / 68.14639°N 151.72250°W / 68.14639; -151 This article about a location in the North Slope Borough, Alaska is a stub .
The Upper Tsaina River SNOTEL weather station is located close to the summit of Thompson Pass at a height of 1750 feet (533 metres). Climate data for Upper Tsaina River, Alaska, 2004–2020 normals, 1991-2020 precipitation: 1750ft (533m)
Nightmute is located on Nelson Island near Toksook Bay.The two villages connect by snowmachine trail in winter. According to the United States Census Bureau, the city has a total area of 101.5 square miles (263 km 2), of which 97.0 square miles (251 km 2) is land and 4.6 square miles (12 km 2) (4.50%) is water.
Map of the Pribilof Islands. The Pribilof Islands (formerly the Northern Fur Seal Islands; Aleut: Amiq, [1] Russian: Острова Прибылова, romanized: Ostrova Pribylova) are a group of four volcanic islands off the coast of mainland Alaska, in the Bering Sea, about 200 miles (320 km) north of Unalaska and 200 miles (320 km) southwest of Cape Newenham.
Snowbird Glacier is located near the southwestern corner of the Talkeetna Mountains of Alaska. It sits in a high alpine bowl surrounded by largely unnamed rugged granite peaks, glaciers, and canyons. Snowbird Glacier is located in a high alpine zone characterized by rock, ice, and minimal vegetation.
Exit Glacier is a glacier derived from the Harding Icefield in the Kenai Mountains of Alaska [1] and one of Kenai Fjords National Park's major attractions. It is one of the most accessible valley glaciers in Alaska and is a visible indicator of glacial recession due to climate change.