parame meaning in English
帕拉梅
Examples
- The quality of life was assessed in terms the following five parame - ters : activity , family support , psychological well - being , physical well - being , and economic function
参与复健医疗计画的病人其生活品质中的活动性与经济功能较未参与者佳。 - Finally , this paper establishes a grey method of assessing indoor air quality based on the abundant information provided by grey incidence matrix and illuminates the application of grey cluster in predigesting the evaluation parame ters
最后本文着重研究了室内空气品质现状评价的灰色方法，根据灰色关联矩阵提供的丰富信息对室内空气品质进行综合评判，同时分析了灰色聚类在室内空气品质评价参数简化中的应用。 - Since the deadbeat control property is effect by the operating system parameters , the deadbeat control parameters are corrected using the scheme , called " on line least mean square method with moving range " , in real time by stages . so the controller is adaptable to the change of operating system parame
研究中针对无差拍控制性能受系统参数变化的影响，提出了应用“在线限定记忆最小二乘”的参数辨识方法，分期实时地修正其控制参数，使之对系统的参数变化具有自适应性。 - Traditionally , the saturated zone is modeled as a simple lumped continuity equation : , dsitqsdt where t is time , s is the total storage in the reservoir , i is the spatially integrated volume of incoming wa - ter , and q is the discharge subsurface runoff which only depends on the total storage s . this kind of subsurface runoff model has many different parame - terizations 10 12 , however it has a very common char - acteristic that the subsurface runoff is just a sin - gle - valued storage - discharge function
对于大尺度水文模型而言,目前常常采用的是集总式的地下径流机制,其连续性方程一般可表示为d , dsitqst ? 1这里t是时间, s表示整个流域潜水面土壤层的饱和区域总的水分储存量, i t表示t时刻土壤的非饱和区域向整个潜水面的水分补充量, q s表示仅依赖于水分储存量s的地下径流量量 - Subsurface runoff is obviously closely related with soil water movement in the unsaturated soil zone and dynamic change of the groundwater table . there - fore , it is necessary to develop the subsurface runoff model with a physical base associated with recharge on the aquifer and total storage in the reservoir . also a soil model with a dynamic representation of the groundwater table makes it possible and reasonable to represent a more logical subsurface runoff parame - terization
地下径流显然与非饱和土壤层中的水分运动以及地下水位的动态变化密切相关,因而有必要发展考虑土壤含水量与潜水面science in china ser . d earth sciences 376中国科学d辑地球科学第36卷水分通量以及地下水位动态变化的土壤水模型相适应且具有物理意义的地下径流模型;同时地下水位动态表示的土壤水模型也为发展更为合理的地下径流模型创造了很好的条件