FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2799281272> ?p ?o ?g. }

• W2799281272 endingPage "2117" @default.
• W2799281272 startingPage "2096" @default.
• W2799281272 abstract "Abstract Understanding climate change impacts on hydrological regime and assessing future water supplies are essential to effective water resources management and planning, which is particularly true for the Tibetan Plateau (TP), one of the most vulnerable areas to climate change. In this study, future climate change in the TP was projected for 2041–2060 by a high‐resolution regional climate model, RegCM4, under 3 representative concentration pathways (RCPs): 2.6, 4.5, and 8.5. Response of all key hydrological elements, that is, evapotranspiration, surface run‐off, baseflow, and snowmelt, to future climate in 2 typical catchments, the source regions of Yellow and Yangtze rivers, was further investigated by the variable infiltration capacity microscale hydrological model incorporated with a 2‐layer energy balance snow model and a frozen soil/permafrost algorithm at a 0.25° × 0.25° spatial scale. The results reveal that (a) spatial patterns of precipitation and temperature from RegCM4 agree fairly well with the data from China Meteorological Forcing Dataset, indicating that RegCM4 well reproduces historical climatic information and thus is reliable to support future projection; (b) precipitation increase by 0–70% and temperature rise by 1–4 °C would occur in the TP under 3 RCPs. A clear south‐eastern–north‐western spatial increasing gradient in precipitation would be seen. Besides, under RCP8.5, the peak increase in temperature would approach to 4 °C in spring and autumn in the east of the TP; (c) evapotranspiration would increase by 10–60% in 2 source regions due to the temperature rise, surface run‐off and baseflow in higher elevation region would experience larger increase dominantly due to the precipitation increase, and streamflow would display general increases by more than 3% and 5% in the source regions of Yellow and Yangtze rivers, respectively; (d) snowmelt contributes 11.1% and 16.2% to total run‐off in the source regions of Yellow and Yangtze rivers, respectively, during the baseline period. In the source region of Yangtze River, snowmelt run‐off would become more important with increase of 17.5% and 18.3%, respectively, under RCP2.6 and RCP4.5 but decrease of 15.0% under RCP8.5." @default.
• W2799281272 created "2018-05-17" @default.
• W2799281272 creator A5005227620 @default.
• W2799281272 creator A5016155416 @default.
• W2799281272 creator A5035702797 @default.
• W2799281272 creator A5057198274 @default.
• W2799281272 creator A5067539443 @default.
• W2799281272 creator A5073794558 @default.
• W2799281272 creator A5073966541 @default.
• W2799281272 creator A5075496043 @default.
• W2799281272 date "2018-05-29" @default.
• W2799281272 modified "2023-10-17" @default.
• W2799281272 title "Hydrological projections of future climate change over the source region of Yellow River and Yangtze River in the Tibetan Plateau: A comprehensive assessment by coupling RegCM4 and VIC model" @default.
• W2799281272 cites W1526327218 @default.
• W2799281272 cites W1527805269 @default.
• W2799281272 cites W1535117618 @default.
• W2799281272 cites W1595609746 @default.
• W2799281272 cites W1756015726 @default.
• W2799281272 cites W1822086910 @default.
• W2799281272 cites W1823692044 @default.
• W2799281272 cites W1891315830 @default.
• W2799281272 cites W1901995175 @default.
• W2799281272 cites W1908569208 @default.
• W2799281272 cites W1912201981 @default.
• W2799281272 cites W1953693726 @default.
• W2799281272 cites W1966049345 @default.
• W2799281272 cites W1967988861 @default.
• W2799281272 cites W1967991775 @default.
• W2799281272 cites W1968215713 @default.
• W2799281272 cites W1988416196 @default.
• W2799281272 cites W1989959107 @default.
• W2799281272 cites W1990189505 @default.
• W2799281272 cites W1991137077 @default.
• W2799281272 cites W1991898844 @default.
• W2799281272 cites W1992719120 @default.
• W2799281272 cites W1994769111 @default.
• W2799281272 cites W1995622703 @default.
• W2799281272 cites W2005088832 @default.
• W2799281272 cites W2009618031 @default.
• W2799281272 cites W2016989768 @default.
• W2799281272 cites W2019888227 @default.
• W2799281272 cites W2020678807 @default.
• W2799281272 cites W2020858585 @default.
• W2799281272 cites W2020954320 @default.
• W2799281272 cites W2024941759 @default.
• W2799281272 cites W2025826259 @default.
• W2799281272 cites W2026631551 @default.
• W2799281272 cites W2027312777 @default.
• W2799281272 cites W2027920662 @default.
• W2799281272 cites W2030223774 @default.
• W2799281272 cites W2032668966 @default.
• W2799281272 cites W2034633661 @default.
• W2799281272 cites W2038653615 @default.
• W2799281272 cites W2042680364 @default.
• W2799281272 cites W2044165646 @default.
• W2799281272 cites W2044899848 @default.
• W2799281272 cites W2046216120 @default.
• W2799281272 cites W2047341983 @default.
• W2799281272 cites W2049885513 @default.
• W2799281272 cites W2054268874 @default.
• W2799281272 cites W2054345041 @default.
• W2799281272 cites W2054715181 @default.
• W2799281272 cites W2054938123 @default.
• W2799281272 cites W2059711881 @default.
• W2799281272 cites W2062909954 @default.
• W2799281272 cites W2062974753 @default.
• W2799281272 cites W2064488236 @default.
• W2799281272 cites W2065450689 @default.
• W2799281272 cites W2069384557 @default.
• W2799281272 cites W2070528371 @default.
• W2799281272 cites W2071276036 @default.
• W2799281272 cites W2075371124 @default.
• W2799281272 cites W2084170744 @default.
• W2799281272 cites W2085585287 @default.
• W2799281272 cites W2086872405 @default.
• W2799281272 cites W2087405923 @default.
• W2799281272 cites W2091684523 @default.
• W2799281272 cites W2091739189 @default.
• W2799281272 cites W2092128325 @default.
• W2799281272 cites W2094771455 @default.
• W2799281272 cites W2100386237 @default.
• W2799281272 cites W2103497845 @default.
• W2799281272 cites W2107680164 @default.
• W2799281272 cites W2111160730 @default.
• W2799281272 cites W2115223366 @default.
• W2799281272 cites W2119713927 @default.
• W2799281272 cites W2120496201 @default.
• W2799281272 cites W2120691864 @default.
• W2799281272 cites W2122389133 @default.
• W2799281272 cites W2123913292 @default.
• W2799281272 cites W2124549270 @default.
• W2799281272 cites W2142488084 @default.
• W2799281272 cites W2146029867 @default.
• W2799281272 cites W2148368858 @default.
• W2799281272 cites W2153301836 @default.
• W2799281272 cites W2167476440 @default.
• W2799281272 cites W2173844276 @default.
• W2799281272 cites W2187699728 @default.

• next