Work

The character of seafloor ambient noise recorded offshore New Zealand: Results from the MOANA ocean bottom seismic experiment

Year: 2012

Type: article

Abstract: We analyze the characteristics of ambient noise recorded on ocean‐bottom seismographs using data from the 2009–2010 MOANA (Marine Observations of Anisotropy Near Aotearoa) seismic experiment deployed west and east of South Island, New Zealand. Microseism and infragravity noise peaks are clear on data recorded on the vertical channel of the seismometer and on the pressure sensor. The noise levels in the infragravity band (<0.03 Hz) on the horizontal seismometer channels are too high to show the infragravity peak. There is a small difference (∼0.25 Hz versus ∼0.2 Hz) in microseism peak frequencies between the two sides of the South Island on all three seismic channels. Our results show clear depth dependence between the peak frequency of infragravity waves and the water depth. We find that the product of water depth and wave number at the peak frequency is a constant,koH = 1.5. This relationship can be used to determine the variation of phase and group velocity of infragravity waves with water depth, and the location of the infragravity peak and corresponding noise notch at any water depth. These estimates of spectral characteristics, particularly low noise bands, are useful for future OBS deployments.

Source: Geochemistry Geophysics Geosystems

DOI: 10.1029/2012gc004201

Authors: Zhaohui Yang, Anne F. Sheehan, John A. Collins, Gabi Laske

Institutions: Cooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Woods Hole Oceanographic Institution, University of California San Diego

Language: English

Topic: Seismic Waves and Analysis

Subfield: Geophysics

Field: Earth and Planetary Sciences

Domain: Physical Sciences

Open Access status: bronze

Funder: National Science Foundation

Awards: Collaborative Research: Constraining Mantle Rheology, Mantle Flow, and Crust/Mantle coupling Beneath New Zealand, Collaborative Research: Constraining Mantle Rheology, Mantle Flow, and Crust/Mantle Coupling Beneath New Zealand, Collaborative Research: Constraining mantle rheology, mantle flow, and crust/mantle coupling beneath New Zealand