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Sensitivity of the reference evapotranspiration to key climatic variables in Shandong Province, China

机译:中国山东省重点气候变量的参考蒸散对关键气候变量的敏感性

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The aim of this work was to predict responses of reference evapotranspiration (ET_o) to perturbations of four climatic variables in Shandong province, China. For this purpose, ET_o was estimated based on the FAO-56 Penman-Monteith equation and the non-dimensional relative sensitivity coefficient was employed. Climatic variables (i.e., daily air temperature, sunshine duration, wind speed and daily relative humidity) at 12 meteorological stations covering whole area (1960 to 2013) were collected firstly and used for the analysis. Results showed that ET_o had positive sensitivities to air temperature, sunshine duration and wind speed, opposite to what were observed to relative humidity. The sensitivity of climatic parameters to ET_o showed a decreasing trend: relative humidity > sunshine duration > wind speed > air temperature. The sensitivity coefficients of different factors varied in time and space. From 1960 to 2013, the sensitivity coefficient of sunshine duration (S_n) showed a downward trend at a rate of (-4.3e-4) per annum. The sensitivity coefficient of wind speed (Sws) and relative humidity (S_(RH)) increased at a rate of (3.9e-4) per annum and (1.9e-3) per annum respectively, while the sensitivity coefficient of air temperature (S_T) waved with a tiny decrease trend. The values of S_T and S_n in southern were larger than in northern region. The values of S_(WS) in southern and northeast region were smaller than that in the northern area. Srh in the central region was lower than other area, opposite to what were observed in coastal areas.
机译:这项工作的目的是预测参考蒸散(ET_O)对中国山东四气候变量扰动的响应。为此目的,基于FAO-56 Penman-Monteith方程估计ET_O,并且采用非尺寸相对灵敏度系数。首先收集12个气象站(即2016年至2013年)的12个气象站(即2016年)的气候变量(即,日常空气温度,阳光持续时间,风速和日常相对湿度)并用于分析。结果表明,ET_O对空气温度,阳光持续时间和风速,与观察到相对湿度相反的敏感性。气候参数对ET_O的敏感性显示出趋势降低:相对湿度>阳光持续时间>风速>空气温度。不同因素的敏感度系数在时间和空间中变化。从1960年到2013年,阳光持续时间(S_N)的敏感性系数以每年(-4.3e-4)的速率显示下降趋势。风速(SWS)和相对湿度的灵敏度系数(S_(RH))以每年和每年(1.9E-3)(3.9E-4)的速度分别增加,而空气温度的灵敏度系数( s_t)挥手,减小趋势。南部的S_T和S_N的值大于北部地区。南部和东北地区的S_(WS)的价值小于北部地区的价值。中部地区的SRH低于其他地区,与在沿海地区观察到的其他地区。

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