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Tide gauges can only measure relative sea level, whilst satellites can also measure absolute sea level changes. If that height changes a bit, this has large consequences for glaciers with a shallow slope. After an initial period of melting, the height of the ice sheet will have lowered. Still, mountain glaciers have contributed appreciably to historical sea level rise and are set to contribute a smaller, but still significant fraction of sea level rise in the 21st century. The Thwaites glacier itself will cause a rise of sea level by 65 centimetres if it will completely collapse, but this can also destabilize other glaciers in west Antarctica. The Thwaites Ice Shelf can collapse in three to five years which can destabilize the entire Thwaites glacier. The Thwaites and Pine Island glaciers have been identified to be potentially prone to these processes, since both glaciers bedrock topography gets deeper farther inland, exposing them to more warm water intrusion into the grounding zone. If you have an idea to share, please click the e-mail link at the bottom and send it along to share with others
Humans impact how much water is stored on land. Building dams prevents large masses of water from flowing into the sea and therefore increases the storage of water on land. Some of Greenland’s largest outlet glaciers, such as Jakobshavn Isbræ and Kangerlussuaq Glacier, are flowing faster into the ocean. Sea level changes can be driven either by variations in the amount of water in the oceans, the volume of the ocean or by changes of the land compared to the sea surface. 345 Many glaciers drain into the ocean and ice loss can therefore increase when ocean temperatures increase. The sea level rise due to Antarctica has been estimated to be 0.25 mm per year from 1993 to 2005, and 0.42 mm per year from 2005 to 2015. All datasets generally show an acceleration of mass loss from the Antarctic ice-sheet, but with year-to-year variations. Over a consistent time period, conducting assessments can source contributions to sea level rise and provide early indications of change in trajectory
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