什切青海岸气候变化及其对河流流量的影响

Pub Date : 2017-12-21 DOI:10.2478/14607
M. Świątek
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引用次数: 0

摘要

本文分析了1955-2014年Szczecin、Świnoujście、Resko和Kolobrzeg站点的气温和降水变化,以及Goleniow、Resko和Trzebiatow地区的Ina和Rega河流流量。数据由IMGW-PIB提供。运用了相关分析和回归分析。研究表明,什切青海滨的年、春、夏平均气温均呈上升趋势。降水总量基本保持不变。它们在二月和三月长了一点。在研究的60年期间,河流流量没有发生显著变化。2月和9月,伊纳河的流量略有上升,10月,雷加河的流量减少。河流流量的长期变率受降水总量变率的影响比受气温变率的影响更大。3月、4月和11月的流量变异性与降水总量的相关性最强,而前一个月降水对河流流量的影响在春季和秋季最为明显。
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Climatic changes on Szczecin Seashore and their impact on river flow volumes
The analysis of variability of temperature and precipitation on following station: Szczecin, Świnoujście, Resko and Kolobrzeg, as well as the study of river flows in the Ina and Rega Rivers in Goleniow, Resko and Trzebiatow in 1955-2014 years has been made. Data was provided by IMGW-PIB. The correlation an regression analysis have been used. The conducted research demonstrated that the average year, spring and summer air temperature on Szczecin Seashore rises. Precipitation totals remain basically unchanged. They grow a little in February and in March. No significant changes of river flows occurred in the course of the examined sixty-year period. Flows in the Ina River rose slightly in February and in September and they diminished in the Rega River in October. Long-term variability of river flows is more strongly affected by the variability of precipitation totals rather than by the variability of air temperature. The variability of flows correlates the strongest with the variability of precipitation totals in March, April and in November, while the influence of precipitation in a preceding month on river flows is the most evident in spring and autumn.
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