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. 2015 Aug 18;96(6):1184–1193. doi: 10.1093/jmammal/gyv126

Table 1.

Hydrophone deployments used for a) geographical presence and b) interannual differences analysis across the southeast Indian Ocean (SEIO) and the southwest Pacific Ocean (SWPO). Days = number of days data were available. Detector rates = missed call rate, false detection rate, for AUSB and NZB.

Ocean basin Site name Location Instrument depth (m) Recording dates Days Detector rates AUSB (%) Detector rates NZB (%)
(a) Geographical presence
SEIO Perth Canyon −31°54′8.34″S, 115°1′36.42″E 465 February 2010– September 2010 256 7.9, 18.7
SEIO Bass Strait −38°33′1.86″S, 141°15′13.92″E 168 February 2010– September 2010 236 8.7, 36.6 0, 99.9
SWPO Tasman Sea −32°19′21.72″S, 152°56′40.32″E 147 February 2010– September 2010 233 0, 99.5 4.6, 75.4
SWPO Tonga −20°25′44.64″S, 176°47′39.06″W 1,042 February 2009– September 2009 242 0.3, 80.5
SWPO Samoa −15°8′30.12″S, 173°44′18.72″W 1,031 February 2010– September 2010 242 0, 100
(b) Interannual differences
SEIO Perth Canyon −31°54′8.34″S, 115°1′36.42″E 465 February 2009– June 2012 953 6.7a, 17.6a
SEIO Bass Strait −38°33′1.86″S, 141°15′13.92″E 168 May 2009– November 2012 860 9.4a, 21.1a 0, 100
SWPO Tasman Sea −32°19′21.72″S, 152°56′40.32″E 147 February 2010–December 2011 506 0, 99.7a 5.8a, 87a
SWPO Samoa −15°8′30.12″S, 173°44′18.72″W 1,031 January 2010– August 2011 575 0, 100

aAverage value for time period.