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2000—2012年科爾沁沙地植被與氣候因子間的響應關系
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國家自然科學基金項目(50869005),、教育部半干旱地區(qū)影響水資源高效利用的水文過程及其調控技術創(chuàng)新人才團隊項目和內蒙古自治區(qū)自然科學基金項目(2014MS0407)


Response Relationship between Vegetation and Climate Factors in Horqin Sandy Land from 2000 to 2012
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    利用2000—2012年氣溫,、降水量、歸一化植被指數(NDVI)數據,,對科爾沁沙地氣候與植被變化特征及其定性與定量響應關系進行了分析。結果表明,,研究區(qū)植被長勢自東向西逐漸變差有28.56%的面積呈變差趨勢,,其余呈變好趨勢;多年植被長勢呈變好趨勢,,降水呈微弱增加趨勢,,氣溫變化趨勢不明顯。累積2~3個月降水量,、當月及平均2~3個月氣溫對植被影響較大,;降水量增多、年內4—11月份氣溫升高,、4—8月份單月年際變化中4月最低氣溫升高和6—8月份平均,、最高氣溫降低,均促進植被生長,;水熱同期比單獨因子變化對植被影響更大,。NDVI在0.03~0.33時受氣溫影響顯著;在0.33~0.43時受降水量影響顯著,;在0.43~0.62時受水熱共同影響顯著,;在0.53~0.62時氣溫升高會抑制生長。當降水,、氣溫分別在一定范圍內變化,,或在一定范圍內變化時的水熱共同作用下,NDVI響應于一定范圍,,且部分響應范圍間有共同的重疊響應區(qū)域,。

    Abstract:

    Making full use of the air temperature, precipitation, normalized difference vegetation index (NDVI) data during 2000 to 2012, the variation of climate and vegetation in Horqin sandy land, as well as the response relationship between vegetation and climate factors were analyzed by qualitative and quantitative methods. The results showed that the vegetation in the region deteriorated gradually from east to west, the area of vegetation growth deteriorated accounted for 28.56% of the research area, and the vegetation growth of the remained area showed ameliorated trend. Perennial vegetation grew well with NDVI, while the precipitation increased faintly and the temperature variation trend was not obvious. The vegetation growth was influenced greatly by 2~3 months accumulated precipitation, the temperature of the month and average temperature of 2~3 months. The vegetation growth was promoted by the following factors, including precipitation increment, temperature rising during April to November, the lowest temperature increment in April compared with inter-annual variation of April to August, as well as the highest or the average temperature decrease from June to August. When NDVI was 0.03~0.33, the vegetation growth was influenced obviously by temperature, when NDVI was 0.33~0.43, it was influenced obviously by precipitation, when NDVI was 0.43~0.62, it was influenced by both temperature and precipitation, however, when NDVI was 0.53~0.62, it was inhibited by the rising temperature. NDVI responded to the changes of precipitation or temperature or combined action of precipitation and temperature in different response ranges, which might overlap.

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馬龍,王靜茹,劉廷璽,黃星,劉丹輝,李虹雨.2000—2012年科爾沁沙地植被與氣候因子間的響應關系[J].農業(yè)機械學報,2016,47(4):162-172. Ma Long, Wang Jingru, Liu Tingxi, Huang Xing, Liu Danhui, Li Hongyu. Response Relationship between Vegetation and Climate Factors in Horqin Sandy Land from 2000 to 2012[J]. Transactions of the Chinese Society for Agricultural Machinery,2016,47(4):162-172.

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  • 收稿日期:2015-10-29
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  • 在線發(fā)布日期: 2016-04-10
  • 出版日期: 2016-04-10
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