Page 18: Research news on sea-level change

Sea-level change refers to temporal variations in the height of the global or regional ocean surface relative to a reference datum, driven by combined effects of eustatic, isostatic, and steric processes. Eustatic change primarily arises from alterations in ocean mass, notably through glacial–interglacial ice-sheet dynamics and contemporary land ice melt. Isostatic and tectonic processes modify the vertical position of the solid Earth, producing relative sea-level change at specific locations. Steric contributions reflect temperature- and salinity-driven density changes that alter ocean volume. Quantifying sea-level change integrates tide-gauge records, satellite altimetry, gravimetry, and glacial isostatic adjustment models for reconstructing past variability and constraining projections.

High-res insights into NZ's sinking coastal sites

Coastal sites subsiding at rates of up to 10 mm/year, making them more vulnerable to sea-level rise, have been pinpointed in new high-resolution maps of five major urban centers.

Exploring the future of frozen water

As the world focuses on glacier preservation on UN World Water Day, researchers at the University of Waterloo are exploring the glaciers of the Yukon's St. Elias Mountains. These massive bodies of ice, part of the planet's ...

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