Translation Characteristics of Orographic Precipitation by using the animation of Radar observed Rainfall and Digital Terrain Model.

利用雷达观测降雨动画和数字地形模型转换地形降水特征。

• 批准号: 08650594
• 负责人: TAKEUCHI Kuniyoshi
• 金额: $ 1.28万
• 依托单位: Yamanashi University
• 依托单位国家: 日本
• 项目类别: Grant-in-Aid for Scientific Research (C)
• 财政年份: 1996
• 资助国家: 日本
• 起止时间: 1996 至 1997
• 项目状态: 已结题
• 来源: https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-08650594/
• 关键词: Digital Terrain Model; Radar Observed Precipitation; Rainfall Prediction; Animation

The purpose of this study is to understand the effect of orography on translation of storm area or temporal and spatial distribution of rainfall intensity. The 5 min interval radar data observed at 3 sites (Mt Yae, Mt Akagi and Mt Yakushi) and 5km grid Digital Terrain Model are used in this study. The translation characteristics of rainfall area is identified from the animation of radar observed rainfall which is overlaid on the 3-D displayd topography. Based on this analysis, translation pattern of storm area is classified into several cases. In each cases (or each rainfall type), the relationship between the topographic parameters and rainfall intensity is investigated by using the digital terrain model and radar observed rainfall. Elevation, inclination and aspect of a slope, angle between slope aspect and direction of rainfall cloud movement and distance from coastal line are selected as the topographic parameters and correlation between these parameters and time-averaged rainfall intensity, maximum rainfall intensity and total rainfall are examined at each radar cells. The results of this analysis shows that1) angle between slope aspect and direction of rainfall cloud movement and distance from coastal line shows the reasonable correlation between rainfall intensity or time-space distribution.2) orographic effect on translation of storm area or temporal and spatial distribution of rainfall intensity is different in each rainfall type, such as typhoon type, low pressure type, frontal type or thunder storm type.

本研究的目的是了解地形对风暴区平移或降雨强度时空分布的影响。本研究使用了在 3 个站点（八重山、赤城山和药师山）观测到的 5 分钟间隔雷达数据和 5 公里网格数字地形模型。降雨区域的平移特征是通过叠加在 3D 显示地形上的雷达观测降雨动画来识别的。在此基础上，将风暴区的平移模式分为几种情况。在每种情况（或每种降雨类型）中，利用数字地形模型和雷达观测降雨量来研究地形参数与降雨强度之间的关系。选取坡度、坡度、坡向、坡向与降雨云运动方向的夹角以及距海岸线的距离作为地形参数，考察这些参数与时均降雨强度、最大降雨强度和总降雨量的相关性。在每个雷达单元。分析结果表明：1）坡向与降雨云运动方向的夹角以及距海岸线的距离显示了降雨强度或时空分布之间的合理相关性；2）地形对风暴区平移或时空分布的影响每种降雨类型的降雨强度不同，如台风型、低压型、锋面型或雷暴型。

项目成果

中林,竹内: "雨域の移動に及ぼす地形影響の評価" 土木学会第51回年次学術講演会講演概要集. 766-767 (1996)

Nakabayashi、Takeuchi：“地形对雨区运动影响的评估”日本土木工程师学会第 51 届年度学术会议摘要 766-767（1996 年）。

竹内,中林,岸: "Relation between GMS-Visible ray reflectivity and solar radiation on the ground in Japan" Proc.Int.Workshop on Macro-Scale Hydrological Modeling. 41-49 (1996)

Takeuchi、Nakabayashi、Kishi：“GMS-可见光反射率与日本地面太阳辐射之间的关系”Proc.Int.宏观尺度水文模拟研讨会 41-49 (1996)。

竹内・中林・岸: "Relation between GMS-Visible ray reflectivity and solan ratiation on the ground in Japan" Proc.Int.Workshop on Macro-Hydrological Modelling,Nanjing,China,May. 41-49 (1996)

Takeuchi、Nakabayashi 和 Kishi：“GMS-可见光反射率与日本地面 solan 批准之间的关系”Proc.Int.Workshop on Macro-Hydrological Modelling，南京，中国，5 月 41-49 (1996)。

Nakabayashi, T and Takeuchi, K.: "Evaluation of the Effect of Topography on movement of storm area" Proc.of the 52th annual conference of the JSCE. 766-767 (1996)

Nakabayashi, T 和 Takeuchi, K.：“评估地形对风暴区运动的影响”，JSCE 第 52 届年会论文集。

竹内, 中林, 岸: "Relation between GMS-Visible ray reflectivity and solar radiation on the ground in Japan" Proc.Int.Workshop on Macro-Scale Hydrological Modeling. 41-49 (1996)

Takeuchi、Nakabayashi、Kishi：“GMS-可见光反射率与日本地面太阳辐射之间的关系”Proc.Int.宏观尺度水文模拟研讨会 41-49 (1996)。