A seafloor cable located tsunamis from falling ice.

Glacier‑calving tsunamis — Eqalorutsit Kangilliit Sermiat (Qajuuttap Sermia), South Greenland

In August 2023, a team laid a 10‑kilometre fiber‑optic cable on the floor of a South Greenland fjord and listened with distributed acoustic sensing for 21 days. A Nature paper published 2025‑08‑13 reports that the array resolved and located several hundred tsunamis triggered by falling ice, while a nearby tide gauge recorded waves up to 1.6 meters (trough to crest). It offers a practical way to monitor hazardous calving from below the surface.

Why it’s interesting

Fig. 022 Surface rings from a calving face meet a seabed fiber; the black post marks the tide gauge that recorded up to 1.6 m.

Why it’s interesting

It turns a quiet line on the seabed into a locator for sudden waves that satellites miss. Reported on 2025‑08‑13, it shows calving can be heard and placed from the floor of a fjord.

The longer version

When slabs of ice break from a tidewater glacier, they can shove short, steep waves down a narrow fjord. These near‑field tsunamis start without warning and fade fast, so satellites and distant instruments rarely catch them. A fiber‑optic line on the seafloor can act like thousands of closely spaced ears, sensitive to passing waves.

In South Greenland, researchers self‑deployed a 10 km subsea fiber and ran distributed acoustic and temperature sensing continuously from August 9–29, 2023. A Nature paper published 2025‑08‑13 reports several hundred calving‑driven tsunamis resolved and located on the array using DAS hyperbola vertices, while a nearby tide gauge measured waves up to 1.6 m (trough to crest). The fiber was not an in‑service telecom cable, but a dedicated line for the experiment.

Edition
No. 022
Date
Wednesday 21 October 2026
Subject
Glacier‑calving tsunamis
Locality
Eqalorutsit Kangilliit Sermiat (Qajuuttap Sermia), South Greenland
Period
August 9–29, 2023
Field
ocean
Evidence
3 sources, 1 primary

See how we got here

Found after 21 research paths · Selected from 6 candidates

  1. 01 Glacier calving Blocks of ice fall from tidewater glacier fronts.
  2. 02 Fjord tsunamis Icefalls can launch short, steep waves.
  3. 03 Seafloor fiber One cable becomes thousands of sensors with DAS.
  4. 04 Greenland field study 10 km cable, 21 days in Aug 2023.
  5. 05 Wave localization DAS hyperbola vertices pinpointed sources.
  6. 06 Tide‑gauge height Up to 1.6 m recorded nearby.
  7. → A seafloor cable located tsunamis from falling ice.

Sources

Nothing publishes without independent sources. How we verify →

  1. 1
    Calving-driven fjord dynamics resolved by seafloor fibre sensing

    Nature · 2025 · peer reviewed Primary

    Primary evidence: reports several hundred calving‑generated tsunamis, wave heights up to 1.6 m at a local tide gauge, and that the DAS array resolved and located the tsunamis in a South Greenland fjord; confirms publication date.

    doi.org

  2. 2
    ‘Revolutionary’ seafloor fiber sensing reveals how falling ice drives glacial retreat in Greenland

    University of Washington · 2025 · university

    Independent institutional coverage corroborating that the team used a seafloor fiber with DAS in a South Greenland fjord to capture calving‑induced tsunamis and related wave processes; references the Nature paper and date.

    washington.edu

  3. 3
    Falling ice drives glacial retreat in Greenland

    ETH Zurich · 2025 · university

    Independent institutional coverage confirming seafloor fiber‑optic measurements of calving‑induced surface and internal waves in the same Greenland fjord study and linking to the Nature article and its date.

    ethz.ch

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