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Modeling deep ocean shipping noise in varying acidity conditions
Ilya A Udovydchenkov1, Timothy F Duda, Scott C Doney
1Applied Ocean Physics and Engineering, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts 02543, USA. ilya@whoi.edu, tduda@whoi.edu
Future ocean acidification may slightly increase shipping noise in the North Pacific. Decreasing pH reduces sound absorption, potentially raising noise levels by a few decibels in quiet, remote areas over the next century.
Area of Science:
- Oceanography
- Acoustics
- Environmental Science
Background:
- Seawater chemistry is changing, with probable decreases in pH.
- Shipping noise is a significant anthropogenic sound source in the ocean.
- Sound propagation in the ocean is influenced by absorption and environmental conditions.
Purpose of the Study:
- To analyze potential future changes in ambient shipping noise in the North Pacific.
- To investigate the impact of changing seawater chemistry, specifically pH, on underwater sound propagation.
- To quantify the effects of reduced sound absorption on noise levels.
Main Methods:
- Utilized a simplified acoustic propagation model for the North Pacific.
- Focused on low-frequency sound (0.1-1 kHz) relevant to shipping noise.
- Employed ray physics to compare sound energy attenuation from volume absorption and seafloor interaction.
Main Results:
- Decreasing pH is predicted to reduce the sound absorption coefficient in near-surface waters.
- A potential increase of a few decibels in ambient shipping noise over 100 years is projected.
- These noise increases are most pronounced in very quiet areas distant from noise sources.
- Effects are smaller in regions closer to shipping lanes.
Conclusions:
- Ocean acidification may lead to a measurable, albeit small, increase in underwater shipping noise in specific regions.
- The findings highlight the complex interplay between ocean chemistry and acoustic environments.
- Further research with more sophisticated models may refine these predictions for different ocean basins.
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