淮河中游雨季前后大氣邊界層綜合觀測分析
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淮河流域氣象開放研究基金項目(HRM200708)、安徽省氣象局科研項目(KM0608)資助


Comprehensive Observation Analysis of Atmospheric Boundary Layer in Huaihe River Basin
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    摘要:

    利用安徽省壽縣站邊界層綜合觀測試驗資料,對近地面層風、氣溫、濕度等微氣象要素及感熱通量、潛熱通量、摩擦速度進行綜合分析,總結2005年淮河中游雨季開始前后大氣邊界層的微氣象學基本特征及其異同。結果表明:雨季前,氣溫、相對濕度有明顯的日變化,呈單峰單谷型分布;伴隨雨季的開始,近地面層氣溫下降、相對濕度加大,風速波動增大,且各要素日變化減小。6—7月淮河中游的潛熱通量遠大于感熱通量。邊界層要素的變化對淮河雨季的開始和結束具有一定的指示意義。

    Abstract:

    The data from the SinoJapanese cooperational experiment on atmosphereland interaction processes at Shouxian in the Huaihe River Basin are used to analysis the variations of wind speed, air temperature, relative humidity, and radiation before and during rainy season. Some micrometeorological properties in the nearsurface layer are studied. The results show that there was obvious diurnal variation in both air temperature and relative humidity with one peak pattern in dry season. With the onset of rainy season, the air temperature decreased, relative humidity increased, wind speed fluctuated significantly, and the diurnal variation of meteorological elements became less obvious. It is clearly shown that the latent heat flux was far larger than the sensible heat flux over the middle of the Huaihe River basin. The clear variation trends of micrometeorological elements in dry and rainy season have certain indicative significance for forecasting the beginning and ending of rainy season.

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張曉紅,胡雯,劉遠永,葉金印,劉靜.淮河中游雨季前后大氣邊界層綜合觀測分析[J].氣象科技,2012,40(2):280~284

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歷史
  • 收稿日期:2010-08-03
  • 定稿日期:2011-08-25
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  • 在線發布日期: 2012-04-23
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