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Influence of Oceanic Features around Inlet on the Thermohaline Variability in the Cochin Estuary during 2011 and 2012

机译:Inlet海洋特征对2011年和2012年Cochin河口热卤素变异性的影响

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Thermohaline variability in the Cochin estuary primarily depends on the mixing of fresh water downstream and sea water intrusion upstream. Knowledge of sea water intrusion into the estuary is important for functioning of ecological systems. Therefore this study explored the possibility of monitoring sea water intrusion into the estuary using open ocean thermohaline properties obtained from satellite data. Recently, an extensive observational program has been carried out during 2011 and 2012 in the Cochin estuary to collect temperature and salinity profiles on a fortnightly interval with a station spacing of approximately 100m. Notable temporal variability in salinity is observed in the depth time plots constructed using profiles collected during high tide.Salinity intrusion into Harbor Mouth, during summer and winter monsoon period, exhibits considerable year to year variability. The retreat of summer monsoon rainfall and reduction in the freshwater water discharge resulted in a gradual increase in the salinity both in the surface and bottom. Earlier studies reported that the thermohaline variability on semi-diurnal and diurnal scales is solely due to tidal inflow and out flow.The present study looked into the influence of open ocean thermohaline properties around inlet as observed in the Sea Surface Salinity and Sea Surface Temperature derived from satellite data on the salinity variability in the estuary.
机译:科钦河口的热卤素变异主要取决于淡水下游和海水侵入上游的混合。对海水侵入到河口的知识对于生态系统的运作至关重要。因此,本研究探讨了使用从卫星数据获得的开阔的海洋热卤素特性监测海水侵入河口的可能性。最近,在2011年和2012年在科钦河口中进行了广泛的观察计划,以在每两周间隔内收集温度和盐度曲线,其中站间距约为100米。在使用在高潮中收集的曲线构建的曲线构建的深度时间图中观察到盐度的显着的时间变异性。在夏季和冬季季风期间,在夏季和冬季季风期间,迄今为止变异相当一年。夏季季风降雨和淡水放电减少的撤退导致表面和底部逐渐增加。早期的研究报道说,半昼夜和昼夜鳞片的热卤素变异仅是由于潮气流入和流动。目前的研究看着海洋表面盐度和海表面温度衍生的入口周围的开放海洋热卤素特性的影响从卫星数据到河口中的盐度变异性。

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