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How to better simulate the advection and distribution of water substance has an important significance for the improvement of the numerical weather prediction, especially for precipitation.

如何更好地模拟水物质的平流和分布,对于数值天气预报效果的改进,特别是对于更好地模拟降水过程,具有重要的意义。

The results showed that TPS was of the best accuracy of three methods for temperature, precipitation and relative humidity, significantly for air temperature and precipitation. The difference of the accuracy of three interpolation methods for the aestival relative humidity was not significant.

结果表明:薄盘光滑样条函数法的插值精度最优,特别是温度和降水的效果尤其明显;对于三种插值方法,相对湿度的插值精度在夏季差异不明显。

In the hydrology analysis chart fluent direction, the afflux cumulant as well as the fluent length, may reflect the precipitation the surface runoff flows and collects the region.

水文分析图中的水流方向、汇流累积量以及水流长度,可以反映出降水的地表径流的流向和汇集区域。

According to the relationship between the surface albedo and meteorological factors such as temperature, rainfall were analyzed, and we obtained the correlations between albedo and NDVI, temperature and precipitation.

对东北地区月均地表反照率与相关气象因子之间的关系进行了分析,给出了其与NDVI、温度和降水之间的统计关系。

By the budgetary estimate of the water and heat conditions at the glacial equilibrium line and the water balance of lakes in the area of the West Kunlun Mountains during the late stadial of the Last Glaciation. before the summer mean temperature decreased by 1.5 C, the annal mean precipitation was 10-20% more than that of the present. As the summer mean temperature lowering was over 1. 5 C, the precipitation was decreased and the negtive of the lake water balance appeared.

文中还根据对西昆仑山区冰川零平衡线处水热状况及湖泊水量平衡状况的推算,指出末次盛冰期中,在夏季温度降低1-1.5℃以前,其年降水量应大于现代值,增加量大约在10-20%左右;在夏季温度降低值大于1-1.5℃以后,其降水减少,湖泊水量平衡出现负值,这与冰川、湖泊变化的地质记录所反映的早期冷湿、中期冷干气候条件相符。

This might be one of the reasons that caused the rain belt anomalously southward for the summer of 1997 and 1999. In addition, the phase-locked west and south wind phases of the 30-60 day low-frequency oscillations happened together made obvious contributions to the heavy rainfall to the south of the Yangtze River Valley.

另外,在中国东部30°N及其以南地区,30~60天低频振荡的西风和南风位相锁相的叠加,对这两年夏季长江流域及其以南地区的降水做出了贡献。

It is found that in summer, the region between the southern edge of the westerlies and the northern margin in the subtropical anticyclone of the West Pacific is a favorable location for strong deep summer convection and MCS development.

夏季汛期降水主要受东亚夏季风的影响,非台风暴雨的出现与夏季风的进退一致。夏季在东亚西风带南缘和西太平洋副热带高压之间的地区,是夏季最有利于深对流和MCS发展的地区。

WT5BZ The operational numerical weather forecasting model T63 is employed to study the impacts of precipitation on the movement of the anticyclone over the Western Pacific.

利用国家气象中心的 T63业务数值模式,通过不同的对流潜热加热的敏感性试验,研究降水对西太平洋反气旋中、短期运动的影响。

The results show that:(1) the dynamical conditions for returnflow events are a little different from other rainfall events, with divergence and anticyclonic circulation at lower levels;(2) the air of the returnflow from Northeast China, through the Bohai Sea, then to North China, is relatively dry.

结果表明:涡度和散度的垂直分布与一般的降水过程不同,低层存在辐散和反气旋环流;自东北南下经渤海回流到华北平原的空气是比较干的。该文分析结果有助于预报业务人员了解回流天气,提高华北回流天气的预报准确率。

In addition, antiphase relationship in precipitation changes between the northern Tibetan Plateau (climatically controlled by westerlies) and southern Tibetan Plateau (mainly influenced by Indian monsoon circulation) exists on decadal to centennial timescale.

不仅如此,在分属西风和季风影响区的青藏高原北部和南部,年代际-百年尺度上降水变化也表现出反相位关系。

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