作者: Giulia Valerio , Marco Pilotti , Stefano Barontini , Barbara Leoni
DOI: 10.1002/HYP.10183
关键词: Watershed 、 Glacier 、 Interflow 、 Environmental science 、 Period (geology) 、 Effects of global warming 、 Water column 、 Climate change scenario 、 Climate change 、 Hydrology
摘要: The study of the multiannual thermal dynamics Lake Iseo, a deep lake in Italian pre-alpine area, is presented. Interflow was found to be dominant river entrance mode, suggesting future susceptibility structure overall effects climate change expected upstream alpine watershed. A model employed results long-term hydrologic simulate scenario on lake's evolution for period 2012–2050. predicts an average increase water temperature 0.012 °C/year and reinforced Schmidt stability column winter up 800 J/m2. Both these may further hinder circulation process, which vital oxygenation water. Copyright © 2014 John Wiley & Sons, Ltd.