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Pedersen Lagoon, Aialik Bay
Pedersen Lagoon receives freshwater from proglacial lakes of the Addison and Pedersen glaciers that descend from the Harding Icefield in Kenai Fjords National Park on the western shore of Aialik Bay, about 64 miles (103 km) east-northeast of Homer and 19 miles (31 km) south-southwest of Seward, Alaska.
Bodfish Island, Simpson Lagoon
Bodfish Island is part of the Jones Island barrier chain between Cottle Island to the east and Bertoncini Island to the west, separating Simpson Lagoon from the Beaufort Sea, about 178 miles (286 km) southeast of Utqiagvik and 30 miles (48 km) northwest of Deadhorse, Alaska.
Kasilof River, Kenai Peninsula
Kasilof River starts at the outlet of Tustumena Lake on the Kenai Peninsula and flows generally northwest for 17 miles (27 km) through the Kenai Lowland to Cook Inlet, draining a watershed of 93,275 acres (37,747 ha), about 51 miles (82 km) north-northeast of Homer and 13 miles (21 km) south-southwest of Kenai, Alaska.
Gilman Glacier, Johns Hopkins Inlet
Gilman Glacier starts at an elevation of roughly 6,000 feet (1,828 m)in the Fairweather Range of the Saint Elias Mountains and flows generally northwest for 7.5 miles (12 km) to Johns Hopkins Inlet in Glacier Bay National Park and Preserve, about 105 miles (169 km) southeast of Yakutat and 58 miles (93 km) northwest of Gustavus, Alaska.
Shoup Glacier, Port Valdez
Shoup Glacier starts at an elevation of roughly 6,800 feet (2,073 m) in the Chugach Mountains between Mount Shouplina to the west and Mount Logan to the east, and flows 16 miles (26 km) generally south-southwest to Shoup Bay on the northwest shore of Port Valdez in Prince William Sound, about 74 miles (119 km) east-northeast of Whittier and 9 miles (15 km) west of Valdez, Alaska.
Leffingwell Camp, Flaxman Island
Leffingwell Camp is situated on Flaxman Island, a shape-shifting barrier island separating the Beaufort Sea to the north and Lion Bay to the south, about 58 miles (94 km) east of Deadhorse and 58 miles (94 km) west of Kaktovik, Alaska.
Makarius Bay, Amchitka Island
Makarius Bay is on the southeastern coast of Amchitka Island, the southernmost of the Rat Islands group in the Aleutian Islands of Southwest Alaska, bounded by the Bering Sea to the north and the Pacific Ocean to the south, about 2500 miles (4024 km) north-northwest of Honolulu and 182 miles (293 km) west-southwest of Adak, Alaska.
Dinglestadt Glacier, Kenai Fjords National Park
Dinglestadt Glacier has two land terminating lobes that straddle a watershed divide in the Kenai Mountains, with a minor lobe descending southeast for 4 miles (6 km) from an elevation of roughly 3300 feet (1006 m) to a tidal delta on the western shore of McCarty Glacier in Kenai Fjords National Park, about 44 miles (71 km) south-southwest of Seward and 42 miles (68 km) east of Homer, Alaska.
Boot Bay, Adak Island
Boot Bay is 3 miles (5 km) west of Kagalaska Strait on the south coast of Adak Island, the site of intensive military activity from 1942 to 1997, near the western extent of the Andreanof Islands group of the Aleutian Islands, about 443 miles (713 km) southwest of Unalaska and 11 miles (18 km) southeast of the community of Adak, Alaska.
Alokut Point, Cape Lisburne
Alokut Point is a steep promontory with a summit elevation of 1015 feet (310 m) that represents an abrupt change in direction of the Cape Lisburne coastline and forms the northwest terminus of the Lisburne Hills, about 100 miles (160 km) southwest of Point Lay and 39 miles (63 km) north-northeast of Point Hope, Alaska.
About the background graphic
This ‘warming stripe’ graphic is a visual representation of the change in global temperature from 1850 (top) to 2019 (bottom). Each stripe represents the average global temperature for one year. The average temperature from 1971-2000 is set as the boundary between blue and red. The colour scale goes from -0.7°C to +0.7°C. The data are from the UK Met Office HadCRUT4.6 dataset.
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