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Simulating the impacts of chronic ozone exposure on plant conductance and photosynthesis, and on the regional hydroclimate using WRF/Chem

机译:使用WRF / Chem模拟长期暴露于臭氧对植物电导和光合作用以及对区域水气候的影响

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The Noah-Multiparameterization land surface model in the Weather Research and Forecasting (WRF) with Chemistry (WRF/Chem) is modified to include the effects of chronic ozone exposure (COE) on plant conductance and photosynthesis (PCP) found from field experiments. Based on the modified WRF/Chem, the effects of COE on regional hydroclimate have been investigated over the continental United States. Our results indicate that the model with/without modification in its current configuration can reproduce the rainfall and temperature patterns of the observations and reanalysis data, although it underestimates rainfall in the central Great Plains and overestimates it in the eastern coast states. The experimental tests on the effects of COE include setting different thresholds of ambient ozone concentrations ([O3]) and using different linear regressions to quantify PCP against the COE. Compared with the WRF/Chem control run (i.e., without considering the effects of COE), the modified model at different experiment setups improves the simulated estimates of rainfall and temperatures in Texas and regions to the immediate north. The simulations in June, July and August of 2007–2012 show that surface [O3] decrease latent heat fluxes (LH) by 10–27 W m?2, increase surface air temperatures (T 2) by 0.6 °C–2.0 °C, decrease rainfall by 0.9–1.4 mm d?1, and decrease runoff by 0.1–0.17 mm d?1 in Texas and surrounding areas, all of which highly depends on the precise experiment setup, especially the [O3] threshold. The mechanism producing these results is that COE decreases the LH and increases sensible heat fluxes, which in turn increases the Bowen ratios and air temperatures. This lowering of the LH also results in the decrease of convective potential and finally decreases convective rainfall. Employing this modified WRF/Chem model in any high [O3] region can improve the understanding of the interactions of vegetation, meteorology, chemistry/emissions, and crop productivity.
机译:修改了《天气研究与天气预报》(WRF)和化学(WRF / Chem)中的诺亚多参数化陆地表面模型,以包括长期臭氧暴露(COE)对植物电导和光合作用(PCP)的影响。基于修改后的WRF / Chem,已经研究了美国大陆上COE对区域水气候的影响。我们的结果表明,尽管该模型低估了大平原中部地区的降雨,而高估了东部沿海地区的降雨,但其当前配置中有/无修改的模型可以重现观测和再分析数据的降雨和温度模式。对COE的影响的实验测试包括设置不同的环境臭氧浓度阈值([O3]),并使用不同的线性回归来量化针对COE的PCP。与WRF / Chem控制运行相比(即不考虑COE的影响),在不同的实验设置下修改后的模型可以改善德克萨斯州和紧邻北部地区的降雨和温度的模拟估算值。 2007–2012年6月,7月和8月的模拟显示,表面[O3]使潜热通量(LH)降低10–27 W m?2,使表面空气温度(T 2)升高0.6°C–2.0°C ,在得克萨斯州及周边地区将降雨量减少0.9-1.4 mm d?1,并将径流减少0.1-0.17 mm d?1,所有这些都高度取决于精确的实验设置,尤其是[O3]阈值。产生这些结果的机制是COE降低了LH并增加了显热通量,这反过来又增加了Bowen比和空气温度。 LH的降低还导致对流潜力的降低,并最终降低了对流降雨。在任何高[O3]区域采用这种改良的WRF / Chem模型可以增进对植被,气象,化学/排放和作物生产力之间相互作用的理解。

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