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Variability of Thermohaline Characteristics at 26.5° N in Reanalyses and Oceanographic Section Data

机译:再分析和海洋剖面数据中26.5°N的热盐特性的变异性

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摘要

The most common methods for studying the variability of ocean parameters are field measurements and numerical modeling. Due to the insufficient availability of ocean measurement data, it is not always possible to verify the reliability of modeling results. Changes in temperature and salinity of the Atlantic Ocean water masses at 26.5 degrees N in the recent 30 and 70 years are estimated. The estimation is based on the data of SODA, ORAS4, ECCO, GECCO reanalyses, EN4 and WOA13 objective analyses, and six regular oceanographic sections. In 1992 to 2016, all reanalyses simulate an increase in temperature and salinity of surface water for the entire section, which is consistent with field data. On average, the reanalyses overestimate temperature by 0.1-0.3 degrees C and salinity by 0.02-0.05 psu. The closest values to field data are reproduced by the ORAS4 reanalysis and EN4 objective analysis. Trends in temperature and salinity coincide best with the EN4 results.
机译:研究海洋参数变化性的最常用方法是现场测量和数值模拟。由于海洋测量数据的可用性不足,因此无法始终验证建模结果的可靠性。估计在最近30年和70年中,大西洋水体在26.5度N处的温度和盐度变化。估算基于SODA,ORAS4,ECCO,GECCO再分析,EN4和WOA13客观分析以及六个常规海洋剖面的数据。从1992年到2016年,所有重新分析都模拟了整个断面的地表水温度和盐度升高,这与现场数据一致。平均而言,重新分析的温度高估了0.1-0.3摄氏度,盐度重估了0.02-0.05 psu。通过ORAS4重新分析和EN4客观分析可以再现与现场数据最接近的值。温度和盐度趋势与EN4结果最吻合。

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