Long-term variability of water temperature and salinity at the Polish coast

Pub Date : 2019-06-18 DOI:10.2478/bgeo-2019-0008
M. Świątek
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引用次数: 3

Abstract

Abstract The variability of surface water temperature and water salinity at the south coast of the Baltic in the years 1950–2015 was studied in the article. To that aim, monthly surface water temperature values in Świnoujście, Międzyzdroje, Kołobrzeg (from 1957), Władysławowo, Hel and Gdynia were used, as well as monthly water salinity values in Międzyzdroje, Władysławowo, Hel and Gdynia, all obtained from IMGW-PIB (Institute of Meteorology and Water Management – National Research Institute). Linear regression and Pearson’s simple correlation coefficient of individual monthly, seasonal and annual series of temperature and salinity values over time (in subsequent years) were used to analyse the temporal changes of the examined parameters. In the analysed period a rise in the annual water temperature was recorded in Międzyzdroje, Władysławowo, Hel and Gdynia, while the extent of the changes increased towards the east. There were also positive trends in temperature values in individual months. At the same time, there was a decrease in water salinity, which was also found to be most distinct in the eastern part of the coast. In Władysławowo, Hel and Gdynia, statistically significant drops occurred in nearly all months. During the months featuring statistically insignificant trends, the observed change trends were also negative. Concurrent water temperature increases and water salinity decreases consequently caused a decline in sea water surface density at the Polish Baltic coast.
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波兰海岸水温和盐度的长期变化
本文研究了1950—2015年波罗的海南海岸地表水温度和水盐度的变化。为此,我们使用了Świnoujście、Międzyzdroje、Kołobrzeg(1957年开始)、Władysławowo、Hel和Gdynia的月地表水温值,以及Międzyzdroje、Władysławowo、Hel和Gdynia的月水盐度值,这些数据均来自IMGW-PIB(国家气象和水管理研究所)。利用逐月、逐季和逐年温度和盐度序列的线性回归和Pearson简单相关系数分析了各参数的时间变化。在分析期间,Międzyzdroje, Władysławowo, Hel和Gdynia记录到年水温的上升,而变化的程度向东增加。个别月份的温度值亦有上升趋势。与此同时,海水的盐度也有所下降,这种下降在沿海东部地区最为明显。在Władysławowo、Hel和Gdynia,几乎所有月份都出现了统计上显著的下降。在统计趋势不显著的月份,观察到的变化趋势也是负的。水温升高和盐度降低同时发生,导致波兰波罗的海沿岸海水表面密度下降。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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