| 盛夏流域面融雪量初步分析 |
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| 引用本文： | 毛炜峄.盛夏流域面融雪量初步分析[J].新疆气象,2007,1(6):24-28. |
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| 作者姓名： | 毛炜峄 |
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| 作者单位： | 新疆气候中心 新疆乌鲁木齐830002 |
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| 基金项目： | 中国沙漠气象科研项目;国家自然科学基金 |
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| 摘 要： | 盛夏主汛期我国西部地区流域的洪水类型较东部地区复杂,为了提高当地防洪气象服务水平和丰富全国汛期气象服务技术,分析了融雪洪水与暴雨洪水物理过程的差异,提出了描述流域融雪洪水过程的面融雪量等概念。指出了盛夏主汛期流域融雪洪水的气象服务关键技术。
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| 关 键 词： | 雪-洪过程 面融雪量 积雪遥感监测 高温过程预报 |
| 文章编号： | 1002-0799（2007）06-0024-05 |
| 收稿时间： | 2007-03-21 |
| 修稿时间： | 2007年3月21日 |
Analysis of the Area Melting-Snow Amounts in Midsummer |
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| MAO Wei-yi.Analysis of the Area Melting-Snow Amounts in Midsummer[J].Bimonthly of Xinjiang Meteorology,2007,1(6):24-28. |
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| Authors: | MAO Wei-yi |
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| Abstract: | In the midsummer,the flood types in the western China are more complex than in the eastern China.The difference between the rain-flood processes and the snowmelt-flood processes is analyzed to improve local meteorological service level and to be affluent for the technology of national meteorology service.The concept about area melting snow is brought forward to describe the physical processes of snowmelt flood in the valley.The key technologies of meteorological service to preventing snowmelt flood are showed. |
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| Keywords: | snowmelt flood area melting-snow amounts remote sensing monitoring on snow cover forecast of the rapid increasing temperature process |
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