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• W4304811929 endingPage "128512" @default.
• W4304811929 startingPage "128512" @default.
• W4304811929 abstract "• A structured trend and multiple change point framework was developed, suitable for Mediterranean regions. • Monthly/annual hydrological and climatic metrics assessed concurrently. • The extent of climatic change and drying trend revealed across an extensive regional network. • Main drivers of changes and their implication to the regional management were discussed. Many regions of the world have experienced rapid hydro-climatic changes in recent decades. Mediterranean areas have especially experienced prolonged droughts, changes to runoff, and low-flow periods. Many methods and assumptions for assessing trends in rainfall and runoff are available, however, a comprehensive framework is required that can consider variations at large temporal and spatial scales, long-term persistence (LTP), seasonal patterns, and multiple change points. An analysis framework has been developed in R and applied to a network of 107 rainfall gauges (with about 100 yrs data) and 90 streamflow-water quality gauges (30 – 50 yrs data) across South-west Western Australia, a region with a typical Mediterranean climate. Trends were estimated using the Original Mann–Kendall (OMK) family of tests including using the Mann-Kendall Test under the Scaling Hypothesis (MKLTP) and Seasonal Mann–Kendall (SMK). Single and multiple change points were calculated by the non-parametric Lanzante’s test (LAT), E-Agglomerative algorithm (ECP), and Energy Divisive (EDP). Trend tests show annual rainfall has decreased by 2.6 mm/yr in the Western areas and increased by 0.9 mm/yr in the Eastern areas with corresponding change points in the 1940 s-1960 s and from 1995 to 2000 although 30 % of the annual rainfall and 100 % of the standardized precipitation index (SPI) time series were found to be under LTP. A regional flow trend analysis shows catchments are yielding much less runoff in more than 90 % of gauged stations. The runoff in perennial and ephemeral streams has shown a decline with the rate of 6 (54 %) and 2 (50 %) mm/yr, respectively. Runoff and baseflow decline occurred as step changes lagged after rainfall, and the rate of decline in baseflow was more than for runoff, suggesting that groundwater connectivity with stream inverts has fallen substantially. Stream salinities increased by 64 mg/L/yr (or 15 %) overall which was highly significant. The framework provides a structured approach to analyse changes in rainfall, runoff and stream salinity for a Mediterranean climate that is projected to become even warmer and drier." @default.
• W4304811929 created "2022-10-13" @default.
• W4304811929 creator A5046401501 @default.
• W4304811929 creator A5057227298 @default.
• W4304811929 creator A5061991943 @default.
• W4304811929 creator A5063580497 @default.
• W4304811929 date "2022-11-01" @default.
• W4304811929 modified "2023-10-16" @default.
• W4304811929 title "A structured framework to interpret hydro-climatic and water quality trends in Mediterranean climate zones" @default.
• W4304811929 cites W116463698 @default.
• W4304811929 cites W1496051636 @default.
• W4304811929 cites W1603139408 @default.
• W4304811929 cites W1705299882 @default.
• W4304811929 cites W1733387413 @default.
• W4304811929 cites W1754676864 @default.
• W4304811929 cites W1971370460 @default.
• W4304811929 cites W1982683972 @default.
• W4304811929 cites W1987159447 @default.
• W4304811929 cites W1990061420 @default.
• W4304811929 cites W1990151882 @default.
• W4304811929 cites W1995896014 @default.
• W4304811929 cites W1996466328 @default.
• W4304811929 cites W2000149317 @default.
• W4304811929 cites W2000827109 @default.
• W4304811929 cites W2005751867 @default.
• W4304811929 cites W2018764772 @default.
• W4304811929 cites W2021851216 @default.
• W4304811929 cites W2022416564 @default.
• W4304811929 cites W2024369567 @default.
• W4304811929 cites W2028267147 @default.
• W4304811929 cites W2029364683 @default.
• W4304811929 cites W2031030742 @default.
• W4304811929 cites W2035008438 @default.
• W4304811929 cites W2036614267 @default.
• W4304811929 cites W2049162511 @default.
• W4304811929 cites W2052478647 @default.
• W4304811929 cites W2054356773 @default.
• W4304811929 cites W2069127101 @default.
• W4304811929 cites W2073583135 @default.
• W4304811929 cites W2077690389 @default.
• W4304811929 cites W2077968790 @default.
• W4304811929 cites W2078327278 @default.
• W4304811929 cites W2078762868 @default.
• W4304811929 cites W2080030486 @default.
• W4304811929 cites W2085767691 @default.
• W4304811929 cites W2086680745 @default.
• W4304811929 cites W2094695411 @default.
• W4304811929 cites W2100799918 @default.
• W4304811929 cites W2101108516 @default.
• W4304811929 cites W2101734430 @default.
• W4304811929 cites W2113318639 @default.
• W4304811929 cites W2115786653 @default.
• W4304811929 cites W2117180236 @default.
• W4304811929 cites W2123898918 @default.
• W4304811929 cites W2125106296 @default.
• W4304811929 cites W2127655344 @default.
• W4304811929 cites W2137595065 @default.
• W4304811929 cites W2141403554 @default.
• W4304811929 cites W2142873921 @default.
• W4304811929 cites W2148743119 @default.
• W4304811929 cites W2150427470 @default.
• W4304811929 cites W2154074878 @default.
• W4304811929 cites W2158825943 @default.
• W4304811929 cites W2203418528 @default.
• W4304811929 cites W2281490200 @default.
• W4304811929 cites W2318680928 @default.
• W4304811929 cites W2341760625 @default.
• W4304811929 cites W2564065799 @default.
• W4304811929 cites W2581646934 @default.
• W4304811929 cites W2587891669 @default.
• W4304811929 cites W2653910225 @default.
• W4304811929 cites W2678684796 @default.
• W4304811929 cites W2771261083 @default.
• W4304811929 cites W2773087541 @default.
• W4304811929 cites W2797259982 @default.
• W4304811929 cites W2887869531 @default.
• W4304811929 cites W2889092077 @default.
• W4304811929 cites W2896714603 @default.
• W4304811929 cites W2898708002 @default.
• W4304811929 cites W2900222225 @default.
• W4304811929 cites W2900679048 @default.
• W4304811929 cites W2914852528 @default.
• W4304811929 cites W2938253322 @default.
• W4304811929 cites W2945184802 @default.
• W4304811929 cites W2950174762 @default.
• W4304811929 cites W2977861049 @default.
• W4304811929 cites W2980769700 @default.
• W4304811929 cites W2986779729 @default.
• W4304811929 cites W2989176969 @default.
• W4304811929 cites W3025083537 @default.
• W4304811929 cites W3027408461 @default.
• W4304811929 cites W3042786529 @default.
• W4304811929 cites W3048389915 @default.
• W4304811929 cites W3090525197 @default.
• W4304811929 cites W3098561233 @default.
• W4304811929 cites W3118148064 @default.
• W4304811929 doi "https://doi.org/10.1016/j.jhydrol.2022.128512" @default.
• W4304811929 hasPublicationYear "2022" @default.

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