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      氣候變化研究進(jìn)展 ?? 2007, Vol. 03 ?? Issue (05): 282-286.

      ? 研究短論 ? 上一篇    下一篇

      武漢市城市熱島強(qiáng)度非對(duì)稱(chēng)性變化

      陳正洪 王海軍 任國(guó)玉   

      1. 武漢區(qū)域氣候中心 中國(guó)氣象局國(guó)家氣候中心
      • 收稿日期:2007-03-05 修回日期:2007-05-27 出版日期:2007-09-30 發(fā)布日期:2007-09-30
      • 通訊作者: 陳正洪

      Asymmetrical Change of Urban Heat Island Intensity in Wuhan, China

        

      • Received:2007-03-05 Revised:2007-05-27 Online:2007-09-30 Published:2007-09-30

      摘要: 利用武漢市區(qū)氣象站及其周邊4個(gè)縣氣象站1960-2005年的氣溫資料,計(jì)算了46 a及分時(shí)段的季節(jié)和年平均氣溫、平均最高和最低氣溫傾向率,城市熱島強(qiáng)度傾向率及其貢獻(xiàn)率。結(jié)果表明:46 a來(lái),城區(qū)和郊區(qū)的平均氣溫均以上升趨勢(shì)為主,最低氣溫增幅最大,最高氣溫增幅最小,甚至下降;冬季增幅最快,夏季增幅最慢,甚至下降,這是第一類(lèi)非對(duì)稱(chēng)性。 城市熱島效應(yīng)也存在增強(qiáng)趨勢(shì),以年平均、最低和最高氣溫表示的城市熱島強(qiáng)度傾向率分別為0.235℃/10 a、0.425℃/10 a和0.034℃/10 a,熱島效應(yīng)貢獻(xiàn)率分別達(dá)到60.4%、67.7%和21.8%,這是第二類(lèi)非對(duì)稱(chēng)性。 46 a來(lái)的增溫和城市熱島強(qiáng)度加強(qiáng)主要是最近23 a快速增溫所致,進(jìn)入本世紀(jì)增溫進(jìn)一步加劇。 摘要 計(jì)算了武漢市氣象站、周邊4縣氣象站平均的1960~2005年間以及前后兩半時(shí)段四季和年平均、最高、最低氣溫傾向率,城市熱島強(qiáng)度傾向率和貢獻(xiàn)率。結(jié)果表明:1)46年來(lái),城區(qū)和郊區(qū)的平均氣溫均以增趨勢(shì)為主,平均氣溫傾向率為正,最低氣溫增幅最大,最高氣溫增幅最小甚至下降,冬季增幅最快,夏季增幅最慢甚至下降,這是第一類(lèi)非對(duì)稱(chēng)性;2)城市熱島效應(yīng)也存在增趨勢(shì),以年平均、最低、最高氣溫表示的城市熱島強(qiáng)度傾向率分別為0.235、0.425、0.034 ℃/10a,熱島效應(yīng)貢獻(xiàn)率分別達(dá)到60.4%、67.7%、21.8%,這是第二類(lèi)非對(duì)稱(chēng)性,3)46年來(lái)的增溫和城市熱島強(qiáng)度加強(qiáng)主要是后23年快速增溫所致,前23年氣溫變化不明顯。武漢市氣象站氣溫資料嚴(yán)重地保留著城市化影響,建議盡快遷站。 關(guān)鍵詞 城市熱島強(qiáng)度 最高氣溫 最低氣溫 非對(duì)稱(chēng)性變化

      關(guān)鍵詞: 城市熱島強(qiáng)度, 最高氣溫, 最低氣溫, 非對(duì)稱(chēng)性變化

      Abstract: Seasonal and annual trends of mean, minimum and maximum temperature series in Wuhan meteorological station and four rural stations averaged from 1960 to 2005, from 1960 to 1982 and from 1983 to 2005, respectively, together with the trends of urban heat island intensity and its contribution rate were calculated. The main results are: 1) most of the temperature trends are positive, the warming rate of minimum temperature is higher than that of maximum temperature, the warming rate is high in winter than in summer, there is an apparent asymmetrical change; 2) the urban heat island effect has intensified during the last 46 years in Wuhan, the warming rates of mean, minimum and maximum temperatures are 0.235, 0.425 and 0.034℃/10a, and the contribution rates to the series are 60.4%, 67.7% and 21.8%, respectively; 3) the increases of the temperature and heat island intensity are mainly contributed by the rapid warming in the latest two decades. Abstract: Seasonal and annual bias rates of mean,minimum and maximum temperature series in Wuhan meteorological station and 4 suburb stations averaged from 1960 to 2005, form 1960 to 1982, from 1983-2005, together with the bias rates of urban heat island intensity and its contribution rate are calculated. The main results are: 1)most of the temperature bias rates are positive, the warming rate of minimum temperature is higher than that of maximum temperature, the warming rate is high in winter than in summer, there is apparent asymmetric change; 2)the urban heat island effect has intensified in last 46 years, in Wuhan, the warming rate of mean, minimum and maximum temperature is 0.235, 0.425 and 0.034℃/10a, and the contribution rates to the series get 60.4%, 67.7% and 21.8% respectively; 3)the increasing of the temperature and heat island intensity in last 46 years is mainly contributed by the latest 23 years. The urban heat island effect is seriously included in the temperature series in Wuhan, moving the station is strongly suggested. Key words: urban heat island intensity, maximum temperature, minimum temperature, asymmetric change

      Key words: urban heat island intensity, maximum temperature, minimum temperature, asymmetrical change

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