Streamflow trends during recent decades at some near-natural catchments in Iran
In this study, we assessed the impacts of climate variations on streamflow in 28 near-natural catchments in Iran. To this end, we analysed the trend of annual streamflow, precipitation, and temperatures using the Mann-Kendall test and Sen's slope between water years 1982 and 2011. We evaluated...
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Published in | Hydrological sciences journal Vol. 67; no. 1; pp. 107 - 116 |
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Main Authors | , , , |
Format | Journal Article |
Language | English |
Published |
Abingdon
Taylor & Francis
02.01.2022
Taylor & Francis Ltd |
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Online Access | Get full text |
ISSN | 0262-6667 2150-3435 2150-3435 |
DOI | 10.1080/02626667.2021.2011287 |
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Abstract | In this study, we assessed the impacts of climate variations on streamflow in 28 near-natural catchments in Iran. To this end, we analysed the trend of annual streamflow, precipitation, and temperatures using the Mann-Kendall test and Sen's slope between water years 1982 and 2011. We evaluated the frequency of precipitation in different classes, i.e. below 5, 5-10, 10-15, and above 15 mm/day. Our results indicate a decline in streamflow at 25 catchments, at a rate of −5.66 to −0.19 mm/year. The annual precipitation amount did not decrease significantly, while the frequency of light precipitation events (<5 mm/day) increased. About 60% of the upward trend was significant. Mean temperature increased at all studied catchments, at an average rate of 0.055°C/year. In short, our results indicate that increases in temperature and the frequency of light precipitation events are two leading factors in streamflow reduction across studied catchments. |
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AbstractList | In this study, we assessed the impacts of climate variations on streamflow in 28 near-natural catchments in Iran. To this end, we analysed the trend of annual streamflow, precipitation, and temperatures using the Mann-Kendall test and Sen’s slope between water years 1982 and 2011. We evaluated the frequency of precipitation in different classes, i.e. below 5, 5–10, 10–15, and above 15 mm/day. Our results indicate a decline in streamflow at 25 catchments, at a rate of −5.66 to −0.19 mm/year. The annual precipitation amount did not decrease significantly, while the frequency of light precipitation events (<5 mm/day) increased. About 60% of the upward trend was significant. Mean temperature increased at all studied catchments, at an average rate of 0.055°C/year. In short, our results indicate that increases in temperature and the frequency of light precipitation events are two leading factors in streamflow reduction across studied catchments. |
Author | Wang, Zhihui Zhang, Qinghuan Tang, Qiuhong Hosseini-Moghari, Seyed-Mohammad |
Author_xml | – sequence: 1 givenname: Qinghuan surname: Zhang fullname: Zhang, Qinghuan organization: Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences – sequence: 2 givenname: Seyed-Mohammad surname: Hosseini-Moghari fullname: Hosseini-Moghari, Seyed-Mohammad organization: Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences – sequence: 3 givenname: Qiuhong surname: Tang fullname: Tang, Qiuhong email: tangqh@igsnrr.ac.cn organization: University of Chinese Academy of Sciences – sequence: 4 givenname: Zhihui surname: Wang fullname: Wang, Zhihui organization: Yellow River Institute of Hydraulic Research, Yellow River Conservancy Commission, Ministry of Water Resources |
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SubjectTerms | Annual precipitation atmospheric precipitation Catchments Climate variations Iran light precipitation events Mann-Kendall test Mean temperatures Precipitation Sen's slope estimator Stream discharge Stream flow Streamflow trends Temperature Temperature rise Trends Watersheds |
Title | Streamflow trends during recent decades at some near-natural catchments in Iran |
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