FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2034162040> ?p ?o ?g. }

• W2034162040 endingPage "232" @default.
• W2034162040 startingPage "219" @default.
• W2034162040 abstract "Trend of precipitation and runoff in major Chinese rivers was calculated and compared in order to better quantify the hydrological processes and evaluate the role of human activities in changing river discharge. Records from 160 meteorological stations in China show that from 1951 to 2000 precipitation has increased (2%) in the south but decreased (4 to 11%) in the north. Hydrological data from 22 stations in five major Chinese rivers reveal that over the same period in the south runoff of Pearl River (Zhujiang) increased by 10% but Yangtze (Changjiang) runoff had little change. In the north flows in the Yellow (Huanghe), Liao and Songhua rivers decreased by 80%, 54% and 14%, respectively, all statistically significant based on Mann–Kendall trend analysis. Annual runoff in the Pearl and Yangtze rivers is correlated with basin-wide precipitation (R2 of 0.72 and 0.81). Runoff from northern “deficit” rivers, however, was much lower than precipitation suggested, reflecting severe human impacts. Sub-basin analyses show that runoff in the “excess” southern Yangtze has increased more than precipitation would suggest, most likely indicating decreased water storage, decreased evapotranspiration, or both. In contrast, the marked decreases of runoff in northern sub-basins (including northern Yangtze and middle-lower Yellow) reflect drastically increased water consumption. The water crisis in northern China has been exacerbated by decreasing precipitation, doubling population and expanding water withdrawal, putting pressure on water management and economic development." @default.
• W2034162040 created "2016-06-24" @default.
• W2034162040 creator A5005793976 @default.
• W2034162040 creator A5042987873 @default.
• W2034162040 creator A5074404951 @default.
• W2034162040 date "2010-09-01" @default.
• W2034162040 modified "2023-10-16" @default.
• W2034162040 title "Temporal trend of precipitation and runoff in major Chinese Rivers since 1951" @default.
• W2034162040 cites W1521975376 @default.
• W2034162040 cites W1533743728 @default.
• W2034162040 cites W1912201981 @default.
• W2034162040 cites W1967314147 @default.
• W2034162040 cites W1972946703 @default.
• W2034162040 cites W1973693963 @default.
• W2034162040 cites W1984909502 @default.
• W2034162040 cites W1991170883 @default.
• W2034162040 cites W2003868148 @default.
• W2034162040 cites W2005751867 @default.
• W2034162040 cites W2005837741 @default.
• W2034162040 cites W2008023754 @default.
• W2034162040 cites W2008602827 @default.
• W2034162040 cites W2009535901 @default.
• W2034162040 cites W2015027435 @default.
• W2034162040 cites W2015420417 @default.
• W2034162040 cites W2018180914 @default.
• W2034162040 cites W2018680235 @default.
• W2034162040 cites W2030866283 @default.
• W2034162040 cites W2032923200 @default.
• W2034162040 cites W2038052013 @default.
• W2034162040 cites W2045839683 @default.
• W2034162040 cites W2050841105 @default.
• W2034162040 cites W2051648535 @default.
• W2034162040 cites W2059631400 @default.
• W2034162040 cites W2060680089 @default.
• W2034162040 cites W2062875618 @default.
• W2034162040 cites W2063259011 @default.
• W2034162040 cites W2065689397 @default.
• W2034162040 cites W2082608203 @default.
• W2034162040 cites W2091739189 @default.
• W2034162040 cites W2094406967 @default.
• W2034162040 cites W2099172830 @default.
• W2034162040 cites W2111611099 @default.
• W2034162040 cites W2114381891 @default.
• W2034162040 cites W2118685715 @default.
• W2034162040 cites W2129161539 @default.
• W2034162040 cites W2131517559 @default.
• W2034162040 cites W2166186402 @default.
• W2034162040 cites W2169733412 @default.
• W2034162040 cites W2176800120 @default.
• W2034162040 cites W2318680928 @default.
• W2034162040 doi "https://doi.org/10.1016/j.gloplacha.2010.07.002" @default.
• W2034162040 hasPublicationYear "2010" @default.
• W2034162040 type Work @default.
• W2034162040 sameAs 2034162040 @default.
• W2034162040 citedByCount "172" @default.
• W2034162040 countsByYear W20341620402012 @default.
• W2034162040 countsByYear W20341620402013 @default.
• W2034162040 countsByYear W20341620402014 @default.
• W2034162040 countsByYear W20341620402015 @default.
• W2034162040 countsByYear W20341620402016 @default.
• W2034162040 countsByYear W20341620402017 @default.
• W2034162040 countsByYear W20341620402018 @default.
• W2034162040 countsByYear W20341620402019 @default.
• W2034162040 countsByYear W20341620402020 @default.
• W2034162040 countsByYear W20341620402021 @default.
• W2034162040 countsByYear W20341620402022 @default.
• W2034162040 countsByYear W20341620402023 @default.
• W2034162040 crossrefType "journal-article" @default.
• W2034162040 hasAuthorship W2034162040A5005793976 @default.
• W2034162040 hasAuthorship W2034162040A5042987873 @default.
• W2034162040 hasAuthorship W2034162040A5074404951 @default.
• W2034162040 hasConcept C100970517 @default.
• W2034162040 hasConcept C107054158 @default.
• W2034162040 hasConcept C109007969 @default.
• W2034162040 hasConcept C126645576 @default.
• W2034162040 hasConcept C127313418 @default.
• W2034162040 hasConcept C144024400 @default.
• W2034162040 hasConcept C149923435 @default.
• W2034162040 hasConcept C151730666 @default.
• W2034162040 hasConcept C153294291 @default.
• W2034162040 hasConcept C153823671 @default.
• W2034162040 hasConcept C166957645 @default.
• W2034162040 hasConcept C176783924 @default.
• W2034162040 hasConcept C187320778 @default.
• W2034162040 hasConcept C18903297 @default.
• W2034162040 hasConcept C191935318 @default.
• W2034162040 hasConcept C205649164 @default.
• W2034162040 hasConcept C2908647359 @default.
• W2034162040 hasConcept C3018003528 @default.
• W2034162040 hasConcept C39432304 @default.
• W2034162040 hasConcept C50477045 @default.
• W2034162040 hasConcept C58640448 @default.
• W2034162040 hasConcept C66465714 @default.
• W2034162040 hasConcept C76886044 @default.
• W2034162040 hasConcept C86803240 @default.
• W2034162040 hasConceptScore W2034162040C100970517 @default.
• W2034162040 hasConceptScore W2034162040C107054158 @default.
• W2034162040 hasConceptScore W2034162040C109007969 @default.

• next