trevorjohnson83
Gold Member
- Nov 24, 2015
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could the ice in the north arctic create a tsunami that doesn't go back out to sea because of the added mass to the ocean? I'm thinking the tsunami from ice entering the ocean would be different than traditional tsunamis?
Summary:
ChatGPT said:
The scenario you’re imagining—huge Arctic ice entering the ocean and sending a one-way surge—is interesting, but it works a bit differently from a classic tsunami. Here’s how the physics breaks down:1. Sudden vs. gradual input
- Tsunamis come from sudden displacements of water (undersea quakes, landslides, volcanic eruptions).
- Sea-ice melt or breakup is generally slow. Even a massive iceberg calving is spread over minutes to hours, so the water has time to flow around it and equalize, producing only small, local waves.
2. Added mass and sea level
- If a huge amount of land-based ice (like Greenland’s glaciers) melted, it would raise global sea level permanently.
- That’s a gradual rise, not a traveling wave. The ocean simply finds a new equilibrium level worldwide.
3. Big ice collapse into water
- A truly sudden slide of an enormous ice mass—like a glacier face or ice shelf collapsing—can create a local megatsunami, similar to a rockslide plunging into a fjord.
- But that wave radiates outward and eventually reflects, disperses, and sloshes back just like other tsunami waves; it doesn’t just stop because more mass is present.
4. “One-way” surge?
- Water must conserve momentum and mass. Even if an iceberg adds mass, the surrounding water still oscillates until friction and seafloor drag dissipate the energy.
- So you’d get local flooding and a series of retreating/returning waves, not a permanent outward-only wall of water.
Summary:
- Gradual Arctic ice melt → sea-level rise, no tsunami.
- Sudden gigantic calving/slide → localized tsunami, but it still propagates and reflects like any other.
- The extra mass of meltwater changes long-term sea level, not the basic back-and-forth physics of a tsunami.