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A Twenty-Year Dynamical Oceanic Climatology: 1994-2013. Part 1: Active Scalar Fields: Temperature, Salinity, Dynamic Topography, Mixed-Layer Depth, Bottom Pressure.

机译:二十年动态海洋气候学:1994-2013。第1部分:活动标量场:温度,盐度,动态地形,混合层深度,底部压力。

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摘要

The World Ocean Circulation Experiment (WOCE) was created to produce the first climatologically useful picture of the ocean circulation and its low-frequency variability. This goal is addressed here from the state estimate of the Estimating the Circulation and Climate of the Ocean (ECCO) consortium, which uses almost all of the data obtained during WOCE and its aftermath along with the much improved general circulation modeling capabilities. A dynamically and data-consistent, time-evolving, state estimate is available depicting the ocean and its ice-cover over a 23-year time-span, globally, from the sea surface to the sea floor. The resulting time-dependent 20-year long climatology includes temperature, salinity, surface elevation, bottom pressure, sea-ice, and three components of velocity. Accompanying the state estimate are modified estimates of meteorological forcing-fields, ocean interior mixing coefficients, and initial conditions. Much spatial structure persists through the two decade averaging. Results here are primarily pictorial in nature, intended to give the wider community a sense of what is now available and useful and where more detailed analysis would be fruitful. An extended reference list is included.
机译:创建世界海洋环流实验(WOCE)的目的是产生第一份对海洋环流及其低频变化具有气候学意义的图像。这个目标是通过估算海洋环流和气候联盟(ECCO)的状态估算来解决的,该估算使用了WOCE及其后果中获得的几乎所有数据,以及大大改善的总体环流建模能力。提供了一个动态且与数据一致的,随时间变化的状态估计值,该估计值描述了从海表到海底的全球23年时间跨度的海洋及其冰盖。由此产生的随时间变化的长达20年的气候包括温度,盐度,表面海拔,底部压力,海冰和速度的三个分量。伴随状态估计的是气象强迫场,海洋内部混合系数和初始条件的修正估计。在过去的十年中,大部分空间结构都持续存在。这里的结果本质上主要是图形化的,旨在使更广泛的社区了解现在可用和有用的内容,以及在哪些地方进行更详细的分析将富有成果。包括扩展参考列表。

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    The ECCO Consortium;

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