氣候變暖對呼和浩特地區自然物候的影響
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Impact of Climate Warming on Phenophases in Huhhot
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    摘要:

    分析了1982—2007年氣候變暖對內蒙古呼和浩特、武川自然物候的影響,結果表明:①春季,土壤表層解凍呼和浩特晚于武川,其余物候呼和浩特早于武川;秋季物候均為武川早于呼和浩特。且兩地物候間距均為“豆雁始(絕)見>氣象水文物候期>植物始花(落葉)”;兩地植物物候間呈顯著的正相關,豆雁始(絕)見呈顯著負相關,氣象水文物候期間相關不顯著;②兩地年、春、秋季平均氣溫呈增加趨勢,植物物候春季提前,秋季延遲趨勢顯著,與氣溫有很強的響應關系;豆雁在呼和浩特始見提前,絕見延遲,武川與此相反,豆雁與氣溫有一定的響應關系;氣象水文物候期也具有春季提前,秋季延遲的趨勢,與氣溫相關不顯著。

    Abstract:

    Based on the data from 1982 to 2007 of air temperature and phenophases in Huhhot and Wuchuan, an analysis is made of the variation trends of plants, animals and the related hydrometeorological phenophases in spring and autumn, and their relations to climate warming. The results show: (1) The spring soil thaw was later in Huhhot than in Wuchuan, and other phenophase was earlier in Huhhot than in Wuchuan; but in autumn, the phenophases in Wuchuan were earlier than in Huhhot. The phenophase difference between Huhhot and Wuchuan was: Douyan appearance (disappearance) >hydrometeorological factors>florescence (defoliation); the relationship between florescence (defoliation) dates in Huhhot and Wuchuan was positive significantly, and that of Douyan appearance (disappearance) was negative significantly, while that of hydrometeorological phenophases was not significant. (2) From 1982 to 2007, air temperature increased, the first flowering dates of plants advanced and the defoliating dates postponed, which have a strong relationship with temperature; the first appearance dates of Douyan in Huhhot advanced and the last appearance dates postponed, On the contrary in Wuchuan, there was a certain extent relationship with temperature; hydrometeorological phenophases also advanced in Spring and postponed in Autumn; and the relationship with temperature was not significant.

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呂景華,白靜,蘇利軍,劉旭,趙翠珍,田泓.氣候變暖對呼和浩特地區自然物候的影響[J].氣象科技,2012,40(2):299~303

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  • 收稿日期:2010-08-25
  • 定稿日期:2011-03-01
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  • 在線發布日期: 2012-04-23
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