Environment and Remote Sensing Laboratory, Department of Water Resources, Graduate School of Water Resources, Sungkyunkwan University, Suwon, 16419, Republic of Korea.
Center for Built Environment, Sungkyunkwan University, Suwon, 16419, Republic of Korea.
Sci Rep. 2020 Jul 15;10(1):11644. doi: 10.1038/s41598-020-68472-7.
Rising atmospheric CO, changing climate, and other environmental factors such as nitrogen deposition and aerosol concentration influence carbon and water fluxes significantly. Water-use efficiency (WUE) was used to analyze these factors over 3 decades (1981-2010) using the Community Land Model 5.0 (CLM5.0). The study analyzes the effects of climate and other environmental factors on multiple land cover types (forest, grassland, and cropland) with divided study periods (1981-2000 and 2001-2010). Ecosystem WUE (EWUE) and transpiration WUE (TWUE) increased at the forest site due to the CO fertilization effect but decreased at the grassland and cropland sites due to lower gross primary production and higher/lower (cropland/grassland) evapotranspiration as consequences of rising temperature and water availability. Inherent WUE confirmed that EWUE and TWUE trends were controlled by the rising temperature and CO-induced warming through an increase in vapor pressure deficit. In this way, forest and cropland sites showed warming patterns, while the grassland site showed a drier climate. The later period (2001-2010) showed steeper trends in WUE compared with the earlier period at all sites, implying a change in climate. The results showed implications for rising temperature due to increased CO concentration at multiple land cover types.
大气 CO 浓度升高、气候变化以及氮沉降和气溶胶浓度等其他环境因素显著影响碳和水通量。本研究利用 5.0 版陆面模式(CLM5.0),采用水分利用效率(WUE)分析了过去 30 年来(1981-2010 年)这些因素的影响。研究分析了气候和其他环境因素对多种土地覆盖类型(森林、草地和耕地)的影响,分为两个研究阶段(1981-2000 年和 2001-2010 年)。由于 CO 施肥效应,森林样地的生态系统水分利用效率(EWUE)和蒸腾水分利用效率(TWUE)增加,而草地和耕地样地的 EWUE 和 TWUE 由于温度升高导致总初级生产力降低,以及水分可利用性升高导致蒸散增加而降低。内在水分利用效率(inherent WUE)证实,EWUE 和 TWUE 趋势受温度升高和 CO 引起的变暖的控制,这是通过蒸气压亏缺的增加实现的。因此,森林和耕地样地呈现出变暖的模式,而草地样地则表现出更干燥的气候。与早期相比,所有样地在后期(2001-2010 年)的 WUE 趋势更为陡峭,表明气候发生了变化。结果表明,多种土地覆盖类型由于 CO 浓度升高,气温上升会带来一定影响。