公开(公告)号：KR1020120101949A

公开(公告)日：2012-09-17

申请号：KR1020110020099

申请日：2011-03-07

Applicant: 부경대학교 산학협력단

Inventor： 권병혁 ,  강동환 ,  김광호 ,  김박사 ,  김민성 ,  진광호

IPC: G01W1/00

CPC classification number: G01W1/06 ,  G01P5/00 ,  G01P13/02 ,  G06F19/00 ,  G06T2207/30192

Abstract: PURPOSE: A system and a method for generating the wind field of a weather diagnostic model and a diffusion model are provided to express a wind vector field according to levels and color bars set by a user. CONSTITUTION: A method for generating the wind field of a weather diagnostic model includes the following: a three dimensional wind field is generated based on the result of modeling an MM5/CALMET model(S1); the topography of the wind field is generated based on the three dimensional wind field(S2); and a wind vector field is generated(S3). The three dimensional wind field generating process based on MM5 model-based and CALMET model-based modeling processes. [Reference numerals] (S1) Generating three dimensional wind field; (S1-1) Modeling MM5 model; (S1-2) Generating three dimensional wind filed using CALMET model; (S2) Generating the topography of the wind field; (S2-1) Converting coordinate; (S2-2) Generating topography data; (S3) Generating wind vector field; (S3-1) Calculating maximum/minimum wind speeds; (S3-2) Calculating wind components; (S3-3) Extracting wind components

Abstract translation: 目的：提供一种用于产生天气诊断模型和扩散模型的风场的系统和方法，以根据用户设置的水平和颜色条来表达风矢量场。 构成：用于产生天气诊断模型的风场的方法包括：基于MM5 / CALMET模型建模的结果生成三维风场（S1）; 基于三维风场产生风场的地形（S2）; 并产生风矢量场（S3）。 基于MM5模型和基于CALMET模型的建模过程的三维风场生成过程。 [参考数字]（S1）产生三维风场; （S1-1）建模MM5模型; （S1-2）使用CALMET模型生成三维风场; （S2）产生风场的地形; （S2-1）转换坐标; （S2-2）生成地形数据; （S3）生成风矢量场; （S3-1）计算最大/最小风速; （S3-2）计算风力分量; （S3-3）提取风力部件

公开(公告)号：KR1020120019312A

公开(公告)日：2012-03-06

申请号：KR1020100082656

申请日：2010-08-25

Applicant: 부경대학교 산학협력단

Inventor： 권병혁 ,  강동환 ,  김박사 ,  유훈선 ,  소윤환 ,  김광호 ,  김민성 ,  노영수

IPC: G01V9/00 ,  G01N33/24 ,  G01N1/22

Abstract: PURPOSE: A method for monitoring a carbon dioxide respiration rate in soil is provided to analogize a soil respiratory rate with soil temperature, a carbon oxide variation amount, a soil moisture percentage, soil pH, and a soil organic carbon amount. CONSTITUTION: The temperature of atmosphere and soil is measured(S1). The carbon oxide variation amount of the soil is analyzed(S2). The soil moisture percentage of the soil is analyzed(S3). The pH of the soil is analyzed(S4). The organic carbon amount of the soil is analyzed(S5). The soil respiratory rate function of the soil is obtained(S6).

Abstract translation: 目的：提供一种监测土壤二氧化碳呼吸速率的方法，以土壤呼吸速率与土壤温度，碳氧化物变化量，土壤水分百分比，土壤pH值和土壤有机碳含量进行类比。 规定：测量大气和土壤的温度（S1）。 分析土壤的碳氧化物变化量（S2）。 分析土壤土壤水分百分比（S3）。 分析土壤pH值（S4）。 分析土壤有机碳含量（S5）。 获得土壤土壤呼吸功能（S6）。

公开(公告)号：KR101035062B1

公开(公告)日：2011-05-19

申请号：KR1020090007613

申请日：2009-01-30

Applicant: 부경대학교 산학협력단

Inventor： 권병혁 ,  김동수 ,  이동현 ,  김박사 ,  김민성

IPC: G06F17/40 ,  G06F17/50 ,  G06F19/00

Abstract: 본 발명은 느낌열플럭스를 산출하는 방법에 관한 것으로, 더욱 자세하게는 종래의 경도법을 개선하여 느낌열플럭스를 산출하는 방법에 관한 것이다. 본 발명에 의한 느낌열플럭스 산출을 위해 개선된 경도법은, 자동기상관측장비를 이용하여 서로 다른 높이( , )의 두 지점에서 측정된 풍속( , )과 온도( , ) 자료를 수집하는 1단계; 중립인 조건을 가정하여 마찰속도( )와 느낌열플럭스( )를 산출하는 제2단계; 마찰속도( )와 느낌열플럭스( )를 이용하여 오브코프길이( )를 산출하는 제3단계; n-1번째로 산출된 오브코프길이( ) 값과 n번째로 산출된 오브코프길이( ) 값을 비교하여 다음 단계로 진행여부를 판단하는 제4단계; 및 앞서 구한 값들에 안정도 보정함수를 적용하여 마찰속도( )와 느낌열플럭스( )를 산출하고 제3단계로 되돌아가는 제5단계를 포함하는 것을 특징으로 한다.
느낌열플럭스, 현열플럭스, 경도법, 개선된 경도법

公开(公告)号：KR1020100088411A

公开(公告)日：2010-08-09

申请号：KR1020090007613

申请日：2009-01-30

Applicant: 부경대학교 산학협력단

Inventor： 권병혁 ,  김동수 ,  이동현 ,  김박사 ,  김민성

IPC: G06F17/40 ,  G06F17/50 ,  G06F19/00

CPC classification number: G06Q90/00 ,  G01W1/10 ,  G01W2201/00

Abstract: PURPOSE: An improved gradient method for estimating sensible heat flux is provided to implement the calculation of sensible heat flux of an automatic weather measurement device based on collected data of the automatic weather measurement device. CONSTITUTION: The speed of wind and temperature measured at two points of different heights are collected by an auto weather measurement device. Friction speed and sensible heat flux are produced. If temperature difference is bigger than 0.8 at the measurement point, obukhov length is produced by the sensible heat flux. End of sensible heat flux production procedure is determined by comparison between obukhov length values. The friction speed and the sensible heat flux are produced by appliance of stability compensation function about the acquired values.

Abstract translation: 目的：提供一种用于估计显热通量的改进的梯度法，用于根据自动天气测量装置的收集数据实现自动天气测量装置的显热通量计算。 构成：在不同高度的两个点测量的风速和温度的速度由自动天气测量装置收集。 产生摩擦速度和显热通量。 如果在测量点温度差大于0.8，则显热长度由显热通量产生。 通过比较无效长度值来确定显热通量生产程序的结束。 摩擦速度和显热通量由对所获得的值的稳定性补偿函数的器具产生。