Haru Matsumoto – firstname.lastname@example.org
Robert P. Dziak – email@example.com
Joe Haxel – Joe.Haxel@oregonstate.edu
T-K Lau – firstname.lastname@example.org
Matt Fowler – email@example.com
Cooperative Institute for Marine Resources Studies
Oregon State University (OSU)
DelWayne R. Bohnenstiehl – firstname.lastname@example.org
Department of Marine, Earth, and Atmospheric Sciences
North Carolina State University
Minkyu Park – email@example.com
Won-Sang Lee – firstname.lastname@example.org
Korea Polar Research Institute
Popular version of paper 1aAO7
Presented Monday morning, December 2, 2013
166th ASA Meeting, San Francisco
In May of 2002, an iceberg about the size of Delaware (5,500 km2) calved off from the Ross Ice Shelf. This iceberg (C19), the second largest ever recorded, was trapped in sea ice for almost six years. It then broke into two pieces. The larger section (~5,100 km2), dubbed iceberg C19a, was released from the grip of the sea ice and started drifting slowly eastward into the open Pacific Ocean. As it sailed into warmer waters, currents and thermal and wind stresses caused the iceberg to crack and break apart. In January of 2008, OSU/NOAA's (Oregon State University/National Oceanic Atmospheric Administration) equatorial hydrophone (EEP-NW) began picking up underwater noise generated during its breakup. The sounds also were observed at the International Monitoring Station (IMS) hydrophone station near Juan Fernandez Island (H03N), off the coast of Chile (Fig. 1). Watch: C19a
Fig. 1: Red line is the satellite track of C19a. White triangles are the iceberg locations estimated using the EEP array and IMS Juan Fernandez acoustic records for 2008. Sea ice extent max (yellow) and min (green) of 2008 were based on the data from National Snow & Ice Data Center (NSICD)
Throughout 2008, as C19a disintegrated slowly, it generated frequent "icequakes," wide-band low-frequency sounds (Talendier et al., 2006), which were projected into the water column (Fig 2b). These ice-generated sounds can be a major contributor to the ocean ambient-sound environment. In the oceans, sound waves travel very efficiently through a deep sound channel. For example in the S. Atlantic a smaller iceberg (~1,000 km2), A53a, generated noise that averaged 220 dB rms re ?Pa @ 1m (Dziak et al., 2013) and had influence on the acoustic environment of the S. Atlantic. As a reference, a 500 kJ hydraulic pile driver generates ~230 dB rms re ?Pa @ 1m (Hildebrand, 2009) which indicates these icebergs are a significant source of sound in the ocean. Much larger icebergs, such as C19a, can therefore affect the sound environment of a large area. From January to December 2008, C19a was approximately 3,300 km to 6,400 km from the IMS hydrophone station H03N (33.44S-78.91W). Although the hydrophone station is on the north side of the Juan Fernandez Island, C19a was in the line of sight for much of 2008. At this time, distant iceberg sounds propagating across the southern Pacific raised the noise level at H03N by as much as ~220% (7 dB) in the 11-14 Hz range (Fig. 2a). C19a continued to influence the noise environment within the island's waters until early 2009, when it disintegrated into smaller-sized icebergs in the eastern south Pacific. (Listen: Iceberg calving sound)
Fig. 2: (a) Rise and fall of ocean noise observed at IMS Juan Fernandez station in 2008 as a result of C19a iceberg break up. The 11-14 Hz and 30-36 Hz frequency ranges were chosen to minimize the influence of blue and fin whale calls (S?irovic? et al., 2007). (b) Spectrogram of calving event on day 169, 2008.
The same icequake signals from C19a also were observed by the OSU/NOAA's portable hydrophone array in the eastern equatorial Pacific. EEP-NW was approximately 7,600 km - 8,400 km from the iceberg in 2008, which was about twice the distance of Juan Fernandez Island. Sound travels in the water at ~1,500 m/s; therefore it took ~1.5 hours for the iceberg sound to reach the EEP hydrophone. Fig 3(a) is the 13-year record at EEP-NW (with a 3-year gap) and shows that the noise level in 2008 is approximately 40% (~3 dB) higher than a normal year in the 11-14 Hz range. Fig 3(c) shows the 30-36 Hz noise level averaged over 10 years, which shows March-high and September-low seasonality. This noise level increase partially disrupted the annual cycle of seasonal variability that is observed in ambient noise level within the equatorial Pacific. The 34-year averaged sea ice extent off Antarctica (Fig 3(b) exhibits the exact opposite of the noise level seasonality.
Fig. 3: (a) Noise levels at NOAA's equatorial hydrophone. 2008 anomaly coincides with C19a break up. (b) Monthly sea ice extent off Antarctica from 1978 to 2012. (c) 10-year average of monthly 30-36 Hz noise level at EEP.
Elevated noise level anomalies at these two locations in 2008 can be explained by the presence of a large iceberg C19a in the open ocean of the south Pacific. Annual mean tonnage of icebergs in the sea ice-free southern ocean north of 67 degrees S is about 400 Gt. This represents ~35% of the mean annual mass calving from Antarctica (Tournadre et al., 2012). Typically less than 50 tabular icebergs, with size larger than 5 km, are tracked by satellite at any one time (Long et al., 2006). Most icebergs are smaller than 5 km but large in total volume. Therefore, they may play an important role not only in climate, fresh water flux and ocean circulation, but also in modulating the soundscape of the Southern Ocean. The release of icebergs trapped in sea ice starts at the beginning of the austral summer (Kunz, et al., 2007) when sea ice extent is at a minimum (~17% of maximum on average) (Cavalieri et al., 2003). Once in warm open water icebergs start disintegrating by thermal, wind, and current stress and collisions with other icebergs and the seafloor, and it starts getting noisy. Disintegration slows down as the sea ice advances and restricts the movement of the icebergs in the austral winter, and the Southern Ocean becomes a quieter place.
The study suggests that a single unusually large iceberg from Antarctica altered the low-frequency sound environment across much of the southern hemisphere. Moreover, the austral-summer-high and winter-low noise seasonality observed at mid-to-low southern latitudes may in part be controlled by the seasonal sea ice extent off Antarctica, the presence of drifting icebergs in open water and their breakdown during the austral summer.
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