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Geocentric Changes of the Mean Sea Level of the Baltic Sea from Altimeter and Tide Gauge Data

机译:从高度计和潮汐计资料看波罗的海平均海平面的地心变化

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The global mean sea level is one of the most important indicators of climate changes. Until recently, changes in ocean level were determined from tide gauge observations, currently from satellite altimetry. The main objective of this work is to analyse the available data from the satellite altimetry in order to determine the trend in the Baltic sea level changes. We used these data to investigate regional trend at selected eight tide gauge stations. In the first step sea level anomaly were extracted from the multi mission global product available at CMEMS and next analysed using Ferret and Hector software. Furthermore absolute mean sea level computed from tide gauge data and GNSS observations was taken from the SONEL web page. The results were compared and this comparison shows some differences in both method of the order of 1 mm/year and significant difference of the order 2.4 mm/year at station Helsinki.
机译:全球平均海平面是气候变化的最重要指标之一。直到最近,海平面的变化都是根据潮汐仪的观测结果确定的,而目前的观测结果来自卫星测高仪。这项工作的主要目的是分析来自卫星测高仪的可用数据,以确定波罗的海海平面变化的趋势。我们使用这些数据来调查选定的8个潮位仪站的区域趋势。第一步,从CMEMS的多任务全球产品中提取海平面异常,然后使用Ferret和Hector软件进行分析。此外,从潮汐仪数据和GNSS观测值计算得出的绝对平均海平面从SONEL网页获取。比较了结果,此比较显示了两种方法在赫尔辛基站的1 mm /年量级的一些差异和2.4 mm /年的量级的显着差异。

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