Analysis of Precipitation Resource and Weather Modification Potential in Anyang

Using ground water vapor pressure and precipitation data at four times of one day during 1985- 2014 in each county（ city） of Anyang,precipitable water at each station was calculated,and temporal-spatial distribution of atmospheric maximum precipitable water and its change trend over the years in the city were analyzed. Results showed that atmospheric maximum precipitable water in Anyang City had the characteristics of summer far more than winter,autumn slightly higher than spring,west and south more,and east and north less,and presented the increasing trend year by year. We further analyzed the characteristic of monthly rainfall enhancement potential in each county,and mean in whole year was 80%. In spring and winter,rainfall enhancement potential in the west was bigger than east,while rainfall enhancement potential in the east was bigger than west in summer and autumn. The research provides reference basis for rationally carrying out artificial rainfall work,which could effectively ease uneven temporal-spatial distribution problem of water resource in Anyang City.

A Parameterization Scheme for Regional Average Runoff over Heterogeneous Land Surface Under Climatic Rainfall Forcing

The mean instantaneous runoff rate over a mesoscale region is considered to be the residue between the areal mean precipitation and the amount of water infiltrated into surface soil layer.A rainfall probability density function（PDF） derived from rainfall data in 1996 is used,in conjunction with the mathematic description and empirical expression of rain water infiltration physics,in order to accurately estimate the soil infiltration rate and distribution.A statistical-dynamic scheme of regional mean surface runoff is constructed.The runoff rate can be viewed as the difference between mean precipitation and infiltration on a regional basis,and the averaged infiltration can be treated independently over saturated and unsaturated areas.For the physics of land surface water cycle,infiltration is caused by a source of water supply associated with the properties of underlying surface.After rainfall,with part of the water transported into the soil surface layer,runoff occurs just due to the surplus from the water trapped by vegetation cover and soil infiltration.Hence,the key in calculating surface runoff lies dominantly in the estimation of water amount required for surface-layer soil.Thus,the expression for soil water flux is utilized to derive a formula for the infiltration.Similarly,from the PDF for soil moisture and precipitation,a formula of sub-grid regional mean runoff rate is obtained by considering heterogeneous soil water content and climatic rainfall forcing in 1996 as well as precipitation and soil data over the Yangtze delta region.Sensitivity experiments are also done to indentify affecting factors.Evidence suggests that the proposed scheme gives the runoff rates highly close to those from the Mosaic method,thereby demonstrating the high reliability and feasibility of the statistical-dynamic parameterization scheme.