Matches in SemOpenAlex for { <https://semopenalex.org/work/W4211205404> ?p ?o ?g. }
- W4211205404 abstract "Abstract. Water resources are essential to the ecosystem and social economy in the desert and oasis of the arid Tarim River Basin, Northwest China, and expected to be vulnerable to climate change. Regional Climate Models (RCM) have been proved to provide more reliable results for regional impact study of climate change (e.g. on water resources) than GCM models. However, it is still necessary to apply bias correction before they are used for water resources research due to often considerable biases. In this paper, after a sensitivity analysis on input meteorological variables based on Sobol' method, we compared five precipitation correction methods and three temperature correction methods to the output of a RCM model with its application to the Kaidu River Basin, one of the headwaters of the Tarim River Basin. Precipitation correction methods include Linear Scaling (LS), LOCal Intensity scaling (LOCI), Power Transformation (PT), Distribution Mapping (DM) and Quantile Mapping (QM); and temperature correction methods include LS, VARIance scaling (VARI) and DM. These corrected precipitation and temperature were compared to the observed meteorological data, and then their impacts on streamflow were also compared by driving a distributed hydrologic model. The results show: (1) precipitation, temperature, solar radiation are sensitivity to streamflow while relative humidity and wind speed are not, (2) raw RCM simulations are heavily biased from observed meteorological data, which results in biases in the simulated streamflows, and all bias correction methods effectively improved theses simulations, (3) for precipitation, PT and QM methods performed equally best in correcting the frequency-based indices (e.g. SD, percentile values) while LOCI method performed best in terms of the time series based indices (e.g. Nash–Sutcliffe coefficient, R2), (4) for temperature, all bias correction methods performed equally well in correcting raw temperature. (5) For simulated streamflow, precipitation correction methods have more significant influence than temperature correction methods and the performances of streamflow simulations are consistent with these of corrected precipitation, i.e. PT and QM methods performed equally best in correcting flow duration curve and peak flow while LOCI method performed best in terms of the time series based indices. The case study is for an arid area in China based on a specific RCM and hydrologic model, but the methodology and some results can be applied to other area and other models." @default.
- W4211205404 created "2022-02-13" @default.
- W4211205404 creator A5008257477 @default.
- W4211205404 creator A5011089420 @default.
- W4211205404 creator A5036834753 @default.
- W4211205404 creator A5047918738 @default.
- W4211205404 date "2014-11-13" @default.
- W4211205404 modified "2023-10-18" @default.
- W4211205404 title "Comparing bias correction methods in downscaling meteorological variables for hydrologic impact study in an arid area in China" @default.
- W4211205404 cites W1602738779 @default.
- W4211205404 cites W1885115366 @default.
- W4211205404 cites W1917061602 @default.
- W4211205404 cites W1983724666 @default.
- W4211205404 cites W1988890060 @default.
- W4211205404 cites W1989959107 @default.
- W4211205404 cites W1990373075 @default.
- W4211205404 cites W1993389451 @default.
- W4211205404 cites W1998264544 @default.
- W4211205404 cites W1998360908 @default.
- W4211205404 cites W2000383402 @default.
- W4211205404 cites W2002340384 @default.
- W4211205404 cites W2011382719 @default.
- W4211205404 cites W2012402158 @default.
- W4211205404 cites W2014953946 @default.
- W4211205404 cites W2017559255 @default.
- W4211205404 cites W2027508270 @default.
- W4211205404 cites W2030504740 @default.
- W4211205404 cites W2033904036 @default.
- W4211205404 cites W2034174587 @default.
- W4211205404 cites W2038294068 @default.
- W4211205404 cites W2050320017 @default.
- W4211205404 cites W2050874362 @default.
- W4211205404 cites W2052138108 @default.
- W4211205404 cites W2061857023 @default.
- W4211205404 cites W2064908124 @default.
- W4211205404 cites W2073491504 @default.
- W4211205404 cites W2074380044 @default.
- W4211205404 cites W2080431423 @default.
- W4211205404 cites W2081580680 @default.
- W4211205404 cites W2082065802 @default.
- W4211205404 cites W2082276242 @default.
- W4211205404 cites W2084557503 @default.
- W4211205404 cites W2091918738 @default.
- W4211205404 cites W2101589741 @default.
- W4211205404 cites W2110630269 @default.
- W4211205404 cites W2117355623 @default.
- W4211205404 cites W2130408869 @default.
- W4211205404 cites W2130997496 @default.
- W4211205404 cites W2179874655 @default.
- W4211205404 cites W2352554431 @default.
- W4211205404 cites W3147714055 @default.
- W4211205404 doi "https://doi.org/10.5194/hessd-11-12659-2014" @default.
- W4211205404 hasPublicationYear "2014" @default.
- W4211205404 type Work @default.
- W4211205404 citedByCount "8" @default.
- W4211205404 countsByYear W42112054042015 @default.
- W4211205404 countsByYear W42112054042017 @default.
- W4211205404 countsByYear W42112054042018 @default.
- W4211205404 countsByYear W42112054042019 @default.
- W4211205404 countsByYear W42112054042022 @default.
- W4211205404 countsByYear W42112054042023 @default.
- W4211205404 crossrefType "posted-content" @default.
- W4211205404 hasAuthorship W4211205404A5008257477 @default.
- W4211205404 hasAuthorship W4211205404A5011089420 @default.
- W4211205404 hasAuthorship W4211205404A5036834753 @default.
- W4211205404 hasAuthorship W4211205404A5047918738 @default.
- W4211205404 hasBestOaLocation W42112054041 @default.
- W4211205404 hasConcept C105795698 @default.
- W4211205404 hasConcept C107054158 @default.
- W4211205404 hasConcept C111368507 @default.
- W4211205404 hasConcept C118671147 @default.
- W4211205404 hasConcept C126645576 @default.
- W4211205404 hasConcept C127313418 @default.
- W4211205404 hasConcept C127413603 @default.
- W4211205404 hasConcept C132651083 @default.
- W4211205404 hasConcept C150772632 @default.
- W4211205404 hasConcept C151730666 @default.
- W4211205404 hasConcept C153294291 @default.
- W4211205404 hasConcept C153823671 @default.
- W4211205404 hasConcept C161067210 @default.
- W4211205404 hasConcept C168754636 @default.
- W4211205404 hasConcept C18903297 @default.
- W4211205404 hasConcept C205649164 @default.
- W4211205404 hasConcept C21200559 @default.
- W4211205404 hasConcept C24326235 @default.
- W4211205404 hasConcept C33923547 @default.
- W4211205404 hasConcept C39432304 @default.
- W4211205404 hasConcept C41156917 @default.
- W4211205404 hasConcept C49204034 @default.
- W4211205404 hasConcept C49740808 @default.
- W4211205404 hasConcept C53739315 @default.
- W4211205404 hasConcept C58640448 @default.
- W4211205404 hasConcept C86803240 @default.
- W4211205404 hasConceptScore W4211205404C105795698 @default.
- W4211205404 hasConceptScore W4211205404C107054158 @default.
- W4211205404 hasConceptScore W4211205404C111368507 @default.
- W4211205404 hasConceptScore W4211205404C118671147 @default.
- W4211205404 hasConceptScore W4211205404C126645576 @default.
- W4211205404 hasConceptScore W4211205404C127313418 @default.
- W4211205404 hasConceptScore W4211205404C127413603 @default.