GRACE and GRACE-FO Related Publications (no abstracts)

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Analysis of Ocean Bottom Pressure Anomalies and Seismic Activities in the MedRidge Zone

Kutoglu, Hakan S. and Becek, Kazimierz, 2021. Analysis of Ocean Bottom Pressure Anomalies and Seismic Activities in the MedRidge Zone. Remote Sensing, 13(7):1242, doi:10.3390/rs13071242.

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@ARTICLE{2021RemS...13.1242K,
       author = {{Kutoglu}, Hakan S. and {Becek}, Kazimierz},
        title = "{Analysis of Ocean Bottom Pressure Anomalies and Seismic Activities in the MedRidge Zone}",
      journal = {Remote Sensing},
     keywords = {GRACE, ocean bottom pressure, earthquakes, Mediterranean Ridge accretionary complex, FFT, earthquake energy time series},
         year = 2021,
        month = mar,
       volume = {13},
       number = {7},
          eid = {1242},
        pages = {1242},
     abstract = "{The Mediterranean Ridge accretionary complex (MAC) is a product of the
        convergence of Africa-Europe-Aegean plates. As a result, the
        region exhibits a continuous mass change (horizontal/vertical
        movements) that generates earthquakes. Over the last 50 years,
        approximately 430 earthquakes with M {\ensuremath{\geq}} 5,
        including 36 M {\ensuremath{\geq}} 6 earthquakes, have been
        recorded in the region. This study aims to link the ocean bottom
        deformations manifested through ocean bottom pressure variations
        with the earthquakes' time series. To this end, we investigated
        the time series of the ocean bottom pressure (OBP) anomalies
        derived from the Gravity Recovery and Climate Experiment (GRACE)
        and GRACE Follow-On (GRACE-FO) satellite missions. The OBP time
        series comprises a decreasing trend in addition to 1.02, 1.52,
        4.27, and 10.66-year periodic components, which can be explained
        by atmosphere, oceans, and hydrosphere (AOH) processes, the
        Earth's pole movement, solar activity, and core-mantle coupling.
        It can be inferred from the results that the OBP anomalies time
        series/mass change is linked to a rising trend and periods in
        the earthquakes' energy time series. Based on this preliminary
        work, ocean-bottom pressure variation appears to be a promising
        lead for further research.}",
          doi = {10.3390/rs13071242},
       adsurl = {https://ui.adsabs.harvard.edu/abs/2021RemS...13.1242K},
      adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}

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