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Attributing the Evapotranspiration Trend in the Upper and Middle Reaches of Yellow River Basin Using Global Evapotranspiration Products

Wang, Zhihui, Cui, Zepeng, He, Tian, Tang, Qiuhong, Xiao, Peiqing, Zhang, Pan, and Wang, Lingling, 2021. Attributing the Evapotranspiration Trend in the Upper and Middle Reaches of Yellow River Basin Using Global Evapotranspiration Products. Remote Sensing, 14(1):175, doi:10.3390/rs14010175.

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@ARTICLE{2021RemS...14..175W,
       author = {{Wang}, Zhihui and {Cui}, Zepeng and {He}, Tian and {Tang}, Qiuhong and {Xiao}, Peiqing and {Zhang}, Pan and {Wang}, Lingling},
        title = "{Attributing the Evapotranspiration Trend in the Upper and Middle Reaches of Yellow River Basin Using Global Evapotranspiration Products}",
      journal = {Remote Sensing},
     keywords = {evapotranspiration trend, linear weighting method, ``two-step'' sensitivity analysis, quantitative attribution, upper and middle reaches of the Yellow River},
         year = 2021,
        month = dec,
       volume = {14},
       number = {1},
          eid = {175},
        pages = {175},
     abstract = "{Climate variation and underlying surface dynamics have caused a
        significant change in the trend of evapotranspiration (ET) in
        the Yellow River Basin (YRB) over the last two decades. Combined
        with the measured rainfall, runoff and gravity recovery and
        climate experiment (GRACE) product, five global ET products were
        firstly merged using a linear weighting method. Linear slope,
        ``two-step'' multiple regression, partial differential, and
        residual methods were then employed to explore the quantitative
        impacts of precipitation (PCPN), temperature (Temp), sunshine
        duration (SD), vapor pressure deficit (VPD), wind speed (WS),
        leaf area index (LAI), and the residual factors (e.g.,
        microtopography changes, irrigation, etc.) on the ET trend in
        the YRB. The results show that: (1) The ET estimates were
        improved by merging five global ET products using the linear
        weighting method. The sensitivities of climatic factors and LAI
        on the ET trend can be separately calculated using proposed
        ``two-step'' statistical regression method; (2) the overall ET
        trend in the entire study area during 2000-2018 was 3.82 mm/yr,
        and the highest ET trend was observed in the Toudaoguai-Longmen
        subregion. ET trend was dominantly driven by vegetation
        greening, with an impact of 2.47 mm/yr and a relative impact
        rate of 51.16\%. The results indicated that the relative impact
        rate of the residual factors (e.g., microtopography, irrigation,
        etc.) on the ET trend is up to 28.17\%. The PCPN and VPD had
        increasing roles on the ET trend, with impacts of 0.45 mm/yr and
        0.05 mm/yr, respectively, whereas the Temp, SD, and WS had
        decreasing impacts of -0.19 mm/yr, -0.15 mm/yr, and -0.17 mm/yr,
        respectively. (3) The spatial pattern of impact of specific
        influencing factor on the ET trend was determined by the spatial
        pattern of change trend slope of this factor and sensitivity of
        ET to this factor. ET trends of the source area and the
        Qingtongxia-Toudaoguai were dominated by the climatic factors,
        while the residual factors dominated the ET trend in the
        Tangnaihai-Qingtongxia area. The vegetation restoration was the
        dominant factor causing the increase in the ET in the middle
        reaches of the YRB, and the impact rates of the LAI were ranked
        as follows: Yanhe Rive > Wudinghe River > Fenhe River > Jinghe
        River > Beiluohe River > Qinhe River > Kuyehe River > Yiluohe
        River.}",
          doi = {10.3390/rs14010175},
       adsurl = {https://ui.adsabs.harvard.edu/abs/2021RemS...14..175W},
      adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}

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