浙江省大氣混合層高度變化特征分析
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浙江省公益性技術應用研究項目(2015C33226)、寧波市科技計劃社發重點項目(2013C51013)資助


Variation Characteristics of Atmospheric Mixing Layer Height in Zhejiang
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    摘要:

    利用2000—2013年浙江4個站點(杭州、舟山、衢州和大陳)每日8個時次的氣象數據,采用羅氏法計算分析了混合層高度總體變化特征。結果表明,浙江大氣混合層總體呈現北部低、南部高,海島最高的空間分布特征,舟山最低954 m,其次杭州1073 m、衢州1181 m,大陳最高1631 m,具有混合層高度越低,起伏變化越小的特征。混合層高度具有較明顯時間特征,杭州、舟山、衢州表現為雙峰雙谷型,即春季(3—4月)和夏季(7—8月)較高、初夏(6月)和秋冬季(11月至次年2月)較低,大陳為單峰單谷型,即秋冬季較高(12月至次年1月)、春末夏初(5月)較低的季節(月)特征,以及白天高、夜間低的日變化特征。2002年杭州混合層高度明顯上升的主要與風速加大、1月和6月日照雨日減少、以及9月雨日偏少和2月日照時數偏多密切相關。風速和大氣穩定度是影響混合層高度主要因子,風速3 m/s以上時,大氣即呈不穩定狀態,有利混合層高度抬升。大風速決定大陳最高混合層高度,舟山氣溫較衢州明顯偏低導致其混合層高度偏低,杭州混合層高度高于舟山得益于較高的氣溫?;旌蠈痈叨仍降?,雨日、雨量越明顯,(輕)霧越多、能見度越低,反之亦然,另外,輕霧、霾共存頻率最高的杭州,混合層高度降低除利于出現霧外,更需警惕中度霾以上天氣。研究結果對于認知浙江大氣質量評估、污染物擴散能力分布現狀具有參考價值,為區域內污染源合理分布提供科學依據。

    Abstract:

    Based on the meteorological data of 8 times per day in 4 stations over Zhejiang (Hangzhou, Zhoushan, Quzhou and Dachen) from 2000 to 2013, an analysis is made of the atmospheric mixed layer height (MLH) and their overall regional variations by the Nozaki methodThe results show that MLH in Zhoushan is the lowest, 954 m; then that in Hangzhou, 1073 m and that in Quzhou, 1181 m. MLH in Dachen is the highest, 1631 m; the spatial distribution of MLH is low in the north, high in south, and the highest in the Dachen island in Zhejiang; and the lower the MLH, the more stable it isThe variation of seasonal and daily average of MLH is obviousThe MLH changes in Hangzhou, Zhoushan and Quzhou follow the double peaktotrough pattern, which is higher in spring (from March to April) and summer (from July to August) and lower in early summer (June), autumn, and winter (November to next February) But Dachen MLH follows the single peaktotrough pattern, which is higher in autumn and winter (December to next January), and lower in late spring and early summer (May), and higher in daytime and lower in nighttimeThe increased MLH in Hangzhou of 2002 was more closely related to stronger wind speed, less sunshine and more rainy days in January and June, less rainy days in September, more sunshine in February Wind and atmospheric stability are the main factors of influencing MLHThe atmosphere is unstable when wind speed is more than 3 m〖DK〗·s-1, which is favorable for MLH uplifting This is the reason why Dachen MLH is the highest Zhoushan MLH is lower than Quzhou MLH because of lower temperature, which is why Hangzhou MLH is higher The lower the MLH, more rainy days, greater precipitation, more fog days, and the poorer visibility there are, and vice versaThe frequencies of light fog and haze appearing during same period are the highest in Hangzhou, and there will be more moderate hazes and fogs during lower MLHThe results of study are of great significance for cognitive air quality assessment and distribution of pollutant diffusion capability in Zhejiang, and it also can provide scientific reference for the rational distribution of regional pollution sources

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俞科愛,陳磊,張晶晶,朱純陽,林陳爽,胡曉,陳迪輝.浙江省大氣混合層高度變化特征分析[J].氣象科技,2017,45(4):735~744

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  • 收稿日期:2016-07-27
  • 定稿日期:2017-02-07
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  • 在線發布日期: 2017-08-30
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