Sea ice & icebergs

Seaice

A few hundred meters out of the coastline, Lofoten, Norway.

Year: 2018


Photographer: Benjamin Behre (edited by Frameworks)


Interventions

Sea ice covered Coast in July, Sterlegova, Taymyr, Russia

Sea ice is simply frozen ocean water. It forms, grows, and melts in the ocean. In contrast, icebergs, glaciers, ice sheets, and ice shelves all originate on land.

Year: 1991


Photographer: Peter Prokosch

Sea ice thickening is an idea to slow or reverse the decline of Arctic sea ice by artificially thickening it.

Inuit hunter traveling by snow scooter on melting sea ice, Pond Inlet, Canada

Seal hunting (mainly on abundant ring seals) is an important part of life for the Inuit of Pond Inlet (Inuktitut: Mittimatalik).

Year: 2013


Photographer: Peter Prokosch

Apart from thickening sea ice by directly adding mass to it (see sea ice thickening), it has been suggested that the ice could also be protected by increasing its albedo and thereby reducing the amount of absorbed energy (Field et al. 2018).

Sea ice, North-West Spitsbergen National Park, Svalbard

Sea ice is frozen seawater that floats on the ocean surface. It forms in both the Arctic and the Antarctic in each hemisphere’s winter, and it retreats, but does not completely disappear, in the summer.

Year: 2015


Photographer: Peter Prokosch

In 2010, Veli Albert Kallio suggested the use of ‘floating cables or levees, even platforms’, to act as ‘seeding points to fasten the seasonal growth of the Arctic Ocean's sea ice’ (Geoengineering Google Groups n.d.)

Sea ice melting, North of Dickson, Taymyr, Russia

Sea ice is simply frozen ocean water. It forms, grows, and melts in the ocean. In contrast, icebergs, glaciers, ice sheets, and ice shelves all originate on land.

Year: 1991


Photographer: Peter Prokosch

Pykrete is a 6:1 mix of ice and sawdust that has the property of melting slower than regular ice. Several references have been made online to the use of pykrete as an artificial barrier, as artificial sea ice, or as blockers of moulins.

Blue Iceberg, Rødefjord, Northeast Greenland National Park

The ice in glaciers has been under enormous pressure for eons. The compression eliminates air and reflective surfaces within the ice.

Year: 2014


Photographer: Peter Prokosch

In 2019, an Indonesian design team came up with the idea of a submersible device that could take in sea water, desalinate it, and then have it freeze into a solid block they called a “new ice baby” (Griffiths, 2019).

Shelf-Ice pieces, Antarctic Peninsula

An ice shelf is a thick platform of ice that forms at the grounding line of a glacier, where the glacier meets the coastline.

Year: 2016


Photographer: Peter Prokosch

With rising Arctic temperatures, there have been major changes in iceberg production rates from marine terminating glaciers. These icebergs drift into warmer sea waters where they will slowly melt.

Antarctic Peninsula 1

Unlike the Arctic, which at its center is an ocean, Antarctica is a landmass that is surrounded by the Southern Ocean.

Year: 2016


Photographer: Peter Prokosch

Similar to other ideas to pump water on sea ice (see Sea ice thickening), engineer Sev Clarke (Planetary Restoration n.d.) and engineering student Katy Cartlidge (University of Cambridge 2022) both came up with designs to artificially produce sea ice.

Nuclear icebreaker "Taymyr" operating in sea ice North of Dickson, Taymyr, Russia

Sea ice is simply frozen ocean water. It forms, grows, and melts in the ocean. In contrast, icebergs, glaciers, ice sheets, and ice shelves all originate on land.

Year: 1991


Photographer: Peter Prokosch

Sea ice can be an effective insulator between colder winter air and the warmer ocean below, thereby reducing the potential dissipation of heat into space.