首页> 外国专利> GRID BASED LONG TERM RAINFALL RUNOFF MODEL FOR LARGE SCALE WATERSHEDS

GRID BASED LONG TERM RAINFALL RUNOFF MODEL FOR LARGE SCALE WATERSHEDS

机译:大型流域基于网格的长期降雨径流模型

摘要

PURPOSE: A lattice-based large basin rainfall-runoff model is provided to resolve a problem caused by trial and error by applying an automatic correction method for setting an initial soil moisture condition. CONSTITUTION: A lattice-based large basin rainfall-runoff model includes a parallel processing method for quickly calculating the amount of large basin rainfall-runoff, a method for automatically correcting an initial soil moisture ratio, and an evapotranspiration rate calculating method. The lattice-based large basin rainfall-runoff model uses space sluice data as a parameter and tracks the amount of basin based on momentum theory. [Reference numerals] (AA) Building of input data; (BB) Initial setting; (C1) Rainfall data; (C2) Radar rainfall; (C3) Point-observation rainfall; (D1) Geographic information data; (D2) Thiessen map; (D3) Flow direction diagram; (D4) Land usage diagram; (D5) Soil diagram; (D6) Precise digital elevation; (E1) Parameter setting; (E2) Illuminance coefficient; (E3) Permeability coefficient; (E4) Infiltration rate; (E5) Soil depth; (E6) Porosity; (F1) Initial variable setting; (F2) Initialization of a variable; (F3) Input of data; (F4) Determination of a calculation order; (F5) Setting of an initial variable; (G1) Soil moisture estimation; (G2,H3) Calculation for an A layer; (G3,H4) Calculation for a B layer; (G4,H5) Calculation for a C layer; (G5,H6) Calculation for river; (G6) Determination of convergence; (H1) Rainfall-runoff analysis; (H2) Rainfall distribution; (II) MPI parallel calculation; (J1) Calculation result output; (J2) Surface runoff amount; (J3) River runoff amount; (J4) Soil moisture; (J5) Rainfall distribution diagram; (J6) Input parameter value; (J7) Flow accumulation diagram; (J8) River resistance value;
机译:目的:提供一种基于网格的大流域降雨径流模型,通过应用自动校正方法设置初始土壤湿度条件来解决由反复试验引起的问题。结论:基于格的大流域降雨径流模型包括一种用于快速计算大流域降雨径流量的并行处理方法,一种自动校正初始土壤水分比的方法以及一种蒸散速率计算方法。基于网格的大流域降雨径流模型以空间水闸数据为参数,并基于动量理论跟踪流域流量。 [参考数字](AA)建立输入数据; (BB)初始设定; (C1)降雨数据; (C2)雷达降雨; (C3)点观测降雨; (D1)地理信息数据; (D2)蒂森地图; (D3)流向图; (D4)土地利用图; (D5)土壤图; (D6)精确的数字高程; (E1)参数设定; (E2)照度系数; (E3)渗透系数; (E4)渗透率; (E5)土壤深度; (E6)孔隙率; (F1)初始变量设置; (F2)变量的初始化; (F3)数据输入; (F4)确定计算顺序; (F5)设置初始变量; (G1)土壤水分估算; (G2,H3)A层的计算; (G3,H4)B层的计算; (G4,H5)计算C层; (G5,H6)河流计算; (G6)确定收敛; (H1)降雨径流分析; (H2)降雨分布; (二)MPI并行计算; (J1)计算结果输出; (J2)地表径流量; (J3)河流径流量; (J4)土壤湿度; (J5)降雨分布图; (J6)输入参数值; (J7)流量累积图; (J8)河流阻力值;

著录项

  • 公开/公告号KR101319477B1

    专利类型

  • 公开/公告日2013-10-17

    原文格式PDF

  • 申请/专利权人

    申请/专利号KR20110103696

  • 发明设计人 허영택;김현식;황필선;

    申请日2011-10-11

  • 分类号G06F19;G06F17/10;

  • 国家 KR

  • 入库时间 2022-08-21 16:24:18

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