Arid
DOI10.3390/w11010150
The Po River Water Isotopes during the Drought Condition of the Year 2017
Marchina, Chiara1; Natali, Claudio2; Bianchini, Gianluca2
通讯作者Bianchini, Gianluca
来源期刊WATER
ISSN2073-4441
出版年2019
卷号11期号:1
英文摘要The year 2017 was anomalously warm and dry across the whole Italian Peninsula, and the paucity of precipitation was emphasized during the extreme summer drought of the main Italian river, i.e., the Po river, which was characterized by a discharge persistently below 600 m(3)/s (in spite of the average discharge of 1500 m(3)/s). During these extreme conditions, the Po river oxygen and hydrogen stable isotopes (D, O-18) displayed a relation (D = 6.1*O-18 - 6.6) significantly different from that recorded in the previous investigation of the years 2012-2014 (D = 7.5*O-18 + 6.5). The lowering of the slope and the negative intercept clearly reflect the transition toward arid conditions that characterized the investigated period. The difference is expressed by the derivative parameter Line-Conditioned excess (LC-exc), which better describes the compositional difference of Po river water in the year 2017 with respect to that of the period 2012-2014, when the system was less affected by warm or dry conditions and the river discharge was more similar to the historical trends. The isotopic anomaly observed in 2017 throughout the river is even greater in the terminal part of the river, where in the meanders of the deltaic branches, the river flow progressively slows down, suffering significant evaporation. The isotopic signature of the water appears, therefore, an appropriate tool to monitor the watershed response to evolving environmental conditions. These sensitive isotopic parameters could be interpreted as essential climate variables (ECV) that are physical, chemical, or biological geo-referenced parameters that critically contribute to the characterization of Earth's climate. Future research needs to find relationships between ECV (including the water stable isotopes) and the evolution of ecosystems, which especially in the Mediterranean area, appear to be fragile and severely affected by natural and anthropogenic processes.
英文关键词Po river Large-scale catchment drought hydro-archive water stable isotopes
类型Article
语种英语
国家Italy
开放获取类型Green Published, gold, Green Submitted
收录类别SCI-E
WOS记录号WOS:000459735100148
WOS关键词STABLE-ISOTOPES ; CLIMATE-CHANGE ; INSIGHTS ; IMPACTS ; NETWORK ; PRECIPITATION ; EVAPORATION ; HYDROLOGY ; DEUTERIUM ; DISCHARGE
WOS类目Environmental Sciences ; Water Resources
WOS研究方向Environmental Sciences & Ecology ; Water Resources
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/219169
作者单位1.Univ Padua, Dept Land Environm Agr & Forestry, I-35020 Padua, Italy;
2.Univ Ferrara, Dept Phys & Earth Sci, I-44122 Ferrara, Italy
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GB/T 7714
Marchina, Chiara,Natali, Claudio,Bianchini, Gianluca. The Po River Water Isotopes during the Drought Condition of the Year 2017[J],2019,11(1).
APA Marchina, Chiara,Natali, Claudio,&Bianchini, Gianluca.(2019).The Po River Water Isotopes during the Drought Condition of the Year 2017.WATER,11(1).
MLA Marchina, Chiara,et al."The Po River Water Isotopes during the Drought Condition of the Year 2017".WATER 11.1(2019).
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