Long-term changes in the hydrological regime of high mountain Lake Morskie Oko (Tatra Mountains, Central Europe)

被引：30
|
作者：
Ptak, Mariusz [1 ]
Wrzesinski, Dariusz [1 ]
Choinski, Adam [1 ]
机构：
[1] Adam Mickiewicz Univ, Inst Phys Geog & Environm Planning, Dziegielowa 27, PL-61680 Poznan, Poland
来源：
JOURNAL OF HYDROLOGY AND HYDROMECHANICS | 2017年 / 65卷 / 02期
关键词：
Water temperature; Ice phenology; Water level; Climate change; Tatra Mountains; ICE COVER; CLIMATE-CHANGE; WATER TEMPERATURE; AIR-TEMPERATURE; POLAND; TRENDS; PHENOLOGY; IMPACT; ACIDIFICATION; SLOVAKIA;
D O I：
10.1515/johh-2017-0005
中图分类号：
TV21 [水资源调查与水利规划];
学科分类号：
081501 ;
摘要：
The paper discusses changes in the hydrological regime of high mountain Lake Morskie Oko located in the Tatra Mountains, in the Tatra Mountains National Park, a UNESCO biosphere reserve (MaB). According to the research conducted in the years 1971-2015, its water stages decreased by 3.5 cm.dec(-1), mean annual water temperature increased by 0.3 degrees C.dec(-1) and the duration of ice phenomena and ice cover was reduced by 10 day.dec(-1). No considerable changes in maximum values of ice cover thickness were recorded. Such tendencies are primarily caused by long-term changes in climatic conditions - air temperature and atmospheric precipitation. The hydrological regime of the lake was also determined by changes in land use in the lake's catchment and its location in high mountains.
引用
收藏
页码：146 / 153
页数：8
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