IMOS - ANMN Queensland and Northern Australia, Kimberley 400m (KIM400) Mooring Platform

金伯利400米系泊（IMOS平台代码KIM 400）是金伯利阵列的一部分。它最初于2012年2月3日在（15.93 S，123.55 E）部署。现场水深396米。该系泊阵列已停止使用，该系泊装置于2014年8月拆除。<br /> <br /> 系泊设计在可能的情况下复制了与货架ITF系泊类似的仪器。在整个阵列中收集海流、温度和盐度的观测结果，沿海系泊也观测荧光和浊度等光学水质参数。<br /> <br /> 金伯利阵列与皮尔巴拉阵列和ITF阵列相结合，将有助于确定印度尼西亚洋流对沿着西北大陆架海流的影响，以及处理过的驱动跨大陆架交换。<br /> <br /> 金伯利线将有助于记录向南流动的季节性霍洛威大陆架流（被认为与印度尼西亚洋流相连）。金伯利海岸的特点是高淡水输入，导致跨大陆架密度梯度。 交叉大陆架阵列将允许密度梯度的变化和由此产生的重力流被确定。

The Kimberley 400m mooring (IMOS platform code KIM400) is part of the Kimberley array. It was initially deployed on the 03/02/2012 at (15.93 S, 123.55 E). The site depth is 396m. This mooring array was discontinued, and this mooring removed in August 2014.<br /> <br /> Mooring Designs replicate where possible similar instrumentation to the Shelf ITF moorings. Observations of currents, temperature and salinity are collected throughout the array with the coastal mooring also observing optical water quality parameters of fluorescence and turbidity. <br /> <br /> The Kimberley array, in combination with the Pilbara array and the ITF Array will help determine the influence of the Indonesian Throughflow on the currents along the Northwest shelf and as well as processed driving cross shelf exchange. <br /> <br /> The Kimberly line will help document the southward flowing seasonal Holloway shelf current (thought to be connected to the Indonesian Throughflow). The Kimberly coast is characterised by high freshwater inputs, leading to a cross shelf density gradient. The cross shelf arrays will allow variability in the gradient of density and the resultant gravitational currents to be determined.