School of Oceanography, University of Washington, P.O. Box 357940, Seattle, Washington 98195, USA.
J Acoust Soc Am. 2013 Mar;133(3):1751-61. doi: 10.1121/1.4774275.
Fin whale calls recorded from 2003 to 2004 by a seafloor seismic network on the Endeavour segment of the Juan de Fuca Ridge were analyzed to determine tracks and calling patterns. Over 150 tracks were obtained with a total duration of ~800 h and swimming speeds from 1 to 12 km/h. The dominant inter-pulse interval (IPI) is 24 s and the IPI patterns define 4 categories: a 25 s single IPI and 24/30 s dual IPI produced by single calling whales, a 24/13 s dual IPI interpreted as two calling whales, and an irregular IPI interpreted as groups of calling whales. There are also tracks in which the IPI switches between categories. Call rates vary seasonally with all the tracks between August and April. From August to October tracks are dominated by the irregular IPI and are predominantly headed to the northwest, suggesting that a portion of the fin whale population does not migrate south in the fall. The other IPI categories occur primarily from November to March. These tracks have slower swimming speeds, tend to meander, and are predominantly to the south. The distribution of fin whales around the network is non-random with more calls near the network and to the east and north.
对 2003 年至 2004 年期间在胡安·德富卡海脊奋进段海底地震网络记录的长须鲸叫声进行了分析,以确定其活动轨迹和发声模式。共获得超过 150 条轨迹,总时长约 800 小时,游泳速度为 1 至 12 公里/小时。主要的脉冲间隔(IPI)为 24 秒,IPI 模式定义了 4 个类别:由单个发声鲸鱼产生的 25 秒单 IPI 和 24/30 秒双 IPI、解释为两个发声鲸鱼的 24/13 秒双 IPI 以及解释为鲸鱼群的不规则 IPI。还有一些轨迹的 IPI 在类别之间切换。叫声频率随季节变化,所有轨迹都在 8 月至 4 月之间。8 月至 10 月,不规则 IPI 主导了轨迹,并且主要向西北方向移动,这表明一部分长须鲸在秋季不会向南迁徙。其他 IPI 类别主要发生在 11 月至 3 月。这些轨迹的游泳速度较慢,倾向于蜿蜒曲折,并且主要向南移动。网络周围长须鲸的分布是非随机的,网络附近以及东部和北部有更多的叫声。