rainfall distribution

Figure 3.3.2 Rainfall distribution on 10-12 September 2002 ( isohyets are in millimetres ).

图3.3.2二零零二年九月十至十二日的雨量分布 ( 等雨量线单位为毫米 ).

Interannual and Interdecadal Varieties of Summer Rain-belt s Propagation and Corresponding Characters of Height and Sea Temperature; ACTIVITY CHARACTERISTICS OF EAST ASIA SUMMER MONSOON AND RAINFALL DISTRIBUTION OVER EASTERN CHINA IN 2006

中国夏季雨带推进过程的年际年代际变化及其相关海气背景分析2006年东亚夏季风活动特征与我国东部雨带分布

Moreover, in a small area, due to changes in altitude, rainfall distribution was not uniform.

不仅如此, 在小范围内, 由于海拔高度的变化, 降水的分布也不均匀.

Figure 3.1.2 Rainfall distribution on 15-18 May 2006 ( isohyets are in millimetres ).

图3.1.2二零零六年五月十五日至十八日的雨量分布 ( 等雨量线单位为毫米 ).

The annual rainfall distribution is balanced, the summer autumn is frequent , mean annual precipitation 619 millimeters.

全年降雨分布均衡, 夏秋季稍多,年平均降雨量619毫米.

The changes in land utilization and deforestation of primary rain forests may bring regional climatic changes especially temporal pattern of rainfall, which may in turn change the reproductive phenology of tropical plants even the distribution and species composition of the tropical forests.

土地利用方式的改变和原始热带雨林面积的减少，可能会带来区域气候特别是降雨格局的改变，从而影响到热带雨林植物的繁殖物候，甚至可能引起热带雨林植被分布和物种组成的改变。

The pulse fluctuation of terrestrial heat flow may affect the background thermal pattern of the underlying surface of the atmospheric system and the movement of airflow, so as to affect the spatial distribution of rainfall and humidity of the regional climate.

大地热流的脉动影响区域大气系统下垫面的热力背景和气流运动，从而影响降水的分布和区域气候的干湿程度；

Figure 3.2.2 Rainfall distribution on 14-17 July 2004 ( isohyets are in millimetres ).

图3.2.2二零零四年七月十四至十七日的雨量分布 ( 等雨量线单位为毫米 ).

Figure 3.2.2 Rainfall distribution on 17-18 September 2005 ( isohyets are in millimetres ).

图3.2.2二零零五年九月十七日至十八日的雨量分布 ( 等雨量线单位为毫米 ).

The splash region disperses over time and space, reflecting the form of the water jets entry and the influence of the splashing process on rainfall distribution.

该模型对溅水区进行时空离散，可反映水舌入水形态与喷溅过程对溅水分布的影响。

Most areas of the world frequently experience severe water deficit due and uneven rainfall distribution patterns.

由于雨量不均,目前全球多数地方正面临着严峻的干旱问题.

The climate difference between the early middle Miocene Shanwang palaeoclimate and the present day climate of the Shanwang region are mainly associated with significantly reduced levels of precipitation ( mean annual precipitation and rainfall distribution) and much colder mean temperatures in the coldest month.

与现代山旺地区气候上的区别主要在于年平均降雨量、降雨量的分配，以及最冷月份的平均温度。

Figure Rainfall distribution on 8-11 August 2007 ( isohyets are in millimetres ).

图3.1.2二零零七年八月八日至十一日的雨量分布 ( 等雨量线单位为毫米 ).