Ocean Bottom Seismometer data captures the dynamic response of the Ross Ice Shelf to wave-induced vibrations. The instrument was deployed in front of the Ross Ice Shelf, Antarctica, by the organization AMD_KOPRI. Data collection concluded in December 2015.
Use Cases
- Analyze seismic vibration frequency and amplitude to assess ice shelf mechanical properties.
- Correlate wave activity timestamps with seismic signals to model energy transfer from the ocean.
- Map the spatial distribution of seismic events recorded by the ocean-bottom instrument near the ice front.
- Study temporal patterns in the seismic data to identify seasonal or tidal influences on ice shelf vibrations.
Strengths
- Data originates from a specific, targeted deployment in a critical polar region.
- Focuses on the dynamic response of a major ice shelf, a key topic in cryospheric research.
Limitations
- Dataset size, row count, and specific features are unspecified.
- Data is from a single year (2015), limiting analysis of long-term trends.
- Geographic coverage is limited to one location in the Ross Sea.
Provenance
- Source
- AMD_KOPRI via NASA Earthdata.
- Collection Method
- Deployment of an Ocean Bottom Seismometer on the seafloor.
- Time Range
- 2015
- Freshness
- null
- Geography
- Front of the Ross Ice Shelf, Ross Sea, Antarctica.