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• W2404740504 endingPage "2947" @default.
• W2404740504 startingPage "2930" @default.
• W2404740504 abstract "Few high‐elevation tropical catchments worldwide are gauged, and even fewer are studied using combined hydrometric and isotopic data. Consequently, we lack information needed to understand processes governing rainfall–runoff dynamics and to predict their influence on downstream ecosystem functioning. To address this need, we present a combination of hydrometric and water stable isotopic observations in the wet Andean paramo ecosystem of the Zhurucay Ecohydrological Observatory (7.53 km²). The catchment is located in the Andes of south Ecuador between 3400 and 3900 m a.s.l. Water samples for stable isotopic analysis were collected during 2 years (May 2011–May 2013), while rainfall and runoff measurements were continuously recorded since late 2010. The isotopic data reveal that andosol soils predominantly situated on hillslopes drain laterally to histosols (Andean paramo wetlands) mainly located at the valley bottom. Histosols, in turn, feed water to creeks and small rivers throughout the year, establishing hydrologic connectivity between wetlands and the drainage network. Runoff is primarily composed of pre‐event water stored in the histosols, which is replenished by rainfall that infiltrates through the andosols. Contributions from the mineral horizon and the top of the fractured bedrock are small and only seem to influence discharge in small catchments during low flow generation (non‐exceedance flows < Q₃₅). Variations in source contributions are controlled by antecedent soil moisture, rainfall intensity, and duration of rainy periods. Saturated hydraulic conductivity of the soils, higher than the year‐round low precipitation intensity, indicates that Hortonian overland flow rarely occurs during high‐intensity precipitation events. Deep groundwater contributions to discharge seem to be minimal. These results suggest that, in this high‐elevation tropical ecosystem, (1) subsurface flow is a dominant hydrological process and (2) (histosols) wetlands are the major source of stream runoff. Our study highlights that detailed isotopic characterization during short time periods provides valuable information about ecohydrological processes in regions where very few basins are gauged." @default.
• W2404740504 created "2016-06-24" @default.
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• W2404740504 date "2016-07-24" @default.
• W2404740504 modified "2023-10-05" @default.
• W2404740504 title "Combined use of isotopic and hydrometric data to conceptualize ecohydrological processes in a high-elevation tropical ecosystem" @default.
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• W2404740504 cites W1498704255 @default.
• W2404740504 cites W1503701864 @default.
• W2404740504 cites W1503982519 @default.
• W2404740504 cites W1511829535 @default.
• W2404740504 cites W1525969628 @default.
• W2404740504 cites W1538572330 @default.
• W2404740504 cites W1565092356 @default.
• W2404740504 cites W1572548019 @default.
• W2404740504 cites W1577178214 @default.
• W2404740504 cites W1671483852 @default.
• W2404740504 cites W1894335410 @default.
• W2404740504 cites W1920055338 @default.
• W2404740504 cites W1964769610 @default.
• W2404740504 cites W1969678236 @default.
• W2404740504 cites W1971950064 @default.
• W2404740504 cites W1974366588 @default.
• W2404740504 cites W1976329200 @default.
• W2404740504 cites W1984782542 @default.
• W2404740504 cites W1988378253 @default.
• W2404740504 cites W1988576677 @default.
• W2404740504 cites W1994144655 @default.
• W2404740504 cites W1995453954 @default.
• W2404740504 cites W1995646567 @default.
• W2404740504 cites W2001624316 @default.
• W2404740504 cites W2010117399 @default.
• W2404740504 cites W2016526631 @default.
• W2404740504 cites W2016544738 @default.
• W2404740504 cites W2019395141 @default.
• W2404740504 cites W2019395269 @default.
• W2404740504 cites W2019553362 @default.
• W2404740504 cites W2023833696 @default.
• W2404740504 cites W2028681688 @default.
• W2404740504 cites W2029962400 @default.
• W2404740504 cites W2034552250 @default.
• W2404740504 cites W2038500107 @default.
• W2404740504 cites W2041596733 @default.
• W2404740504 cites W2042615284 @default.
• W2404740504 cites W2044865858 @default.
• W2404740504 cites W2045469782 @default.
• W2404740504 cites W2048240973 @default.
• W2404740504 cites W2050971313 @default.
• W2404740504 cites W2052509795 @default.
• W2404740504 cites W2060636082 @default.
• W2404740504 cites W2063206655 @default.
• W2404740504 cites W2064124042 @default.
• W2404740504 cites W2065389015 @default.
• W2404740504 cites W2068001876 @default.
• W2404740504 cites W2082903678 @default.
• W2404740504 cites W2089020125 @default.
• W2404740504 cites W2089667468 @default.
• W2404740504 cites W2099088651 @default.
• W2404740504 cites W2107023230 @default.
• W2404740504 cites W2115786644 @default.
• W2404740504 cites W2116725059 @default.
• W2404740504 cites W2117415912 @default.
• W2404740504 cites W2122203956 @default.
• W2404740504 cites W2125623572 @default.
• W2404740504 cites W2125775218 @default.
• W2404740504 cites W2127226096 @default.
• W2404740504 cites W2130571159 @default.
• W2404740504 cites W2132360832 @default.
• W2404740504 cites W2132893462 @default.
• W2404740504 cites W2136690550 @default.
• W2404740504 cites W2138946635 @default.
• W2404740504 cites W2143932700 @default.
• W2404740504 cites W2144936475 @default.
• W2404740504 cites W2157551605 @default.
• W2404740504 cites W2160156450 @default.
• W2404740504 cites W2162719469 @default.
• W2404740504 cites W2166488439 @default.
• W2404740504 cites W2173842868 @default.
• W2404740504 cites W4233201992 @default.
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• W2404740504 doi "https://doi.org/10.1002/hyp.10927" @default.
• W2404740504 hasPublicationYear "2016" @default.
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