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气候变化对小麦生产影响的数值模型研究 总被引:12,自引:0,他引:12
在未来气候变化对作物影响的研究基础上,分析未来不同气候情景对南京地区小麦生长发育、产量形成的影响,并考虑了紫外辐射变化的影响。采用数值模拟方法具体估算了温度升高、降水变化、CO2 浓度上升及紫外辐射增强对南京地区小麦产量的影响。计算结果表明:未来CO2 增加可提高小麦产量,气温升高、降水变化及紫外辐射增强均使得小麦产量有所降低。 相似文献
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The favourable synoptic situation and climate background for a sandstorm process,which occurred in theperiod 9—16 April 1988,have been studied through analyzing weather maps,meteorological elements,satellitecloud pictures and sandstorm trajectories.The sand dust origin area,the directions and the paths of sanddust transport,and the extent the sand dust reached are also investigated.The results of measurments andanalysis indicate that the concentration of sand dust particles is 10 times greater than the normal.It is also shownthat the elements in the sand dust are lithophylic and come from natural source through the chemical composi-tion analysis of the sand dust,so that the sand dust has not been polluted by human activities. 相似文献
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The favourable synoptic situation and climate background for a sandstorm process,which occurred in the period 9-16 April 1988,have been studied through analyzing weather maps,meteorological elements,satellite cloud pictures and sandstorm trajectories.The sand dust origin area,the directions and the paths of sand dust transport,and the extent the sand dust reached are also investigated.The results of measurments and analysis indicate that the concentration of sand dust particles is 10 times greater than the normal.It is also shown that the elements in the sand dust are lithophylic and come from natural source through the chemical composition analysis of the sand dust,so that the sand dust has not been polluted by human activities. 相似文献
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确立以日蒸发量来作为描述可晾晒程度的物理量。根据日蒸发量与日最高温度、日平均相对湿度等诸多因子的相关性,进行回归计算,建立其预报方程。通过数轴凝聚,对1998、1999年常州市气象站的逐日蒸发量的变化范围并结合天空状况等因素进行分类,以此作为晾晒指数等级的标准。将方程结果与标准相对照,即可得到次日的晾晒指数等级和相应决策。 相似文献
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地形对降水影响的数值试验 总被引:10,自引:8,他引:10
用MM5v3模式研究地形高度对江淮流域降水的影响,通过在模式中提高和降低大别山和黄山的地形高度来模拟降水的变化,个例是1998年6月28日和1991年6月12日的暴雨过程,进行了24 h模拟,并分析了垂直速度、涡散度、湿位涡、水汽通量等的变化,结果表明,上述各因子都在地形高度变化后有了明显变化,并因此影响了降水变化。各因子都有影响,综合各因子的影响是预测地形降水的途径之一。总的说,地形引起的降水变化主要在地形变化的附近,特别是在山的迎风面,降水有明显增加。决定降水落区和强度的主要仍是大中尺度环流,但地形起了改变落区和强度的作用。 相似文献