| 祁连山林区大气降水特征与森林对降水的截留作用 |
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| 引用本文： | 常学向,赵爱芬,王金叶,常宗强,金博文.祁连山林区大气降水特征与森林对降水的截留作用[J].高原气象,2002,21(3):274-280. |
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| 作者姓名： | 常学向 赵爱芬 王金叶 常宗强 金博文 |
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| 作者单位： | 1. 中国科学院,寒区旱区环境与工程研究所,甘肃,兰州,730000
2. 甘肃省张掖祁连山水源林研究所,甘肃,张掖,734000 |
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| 基金项目： | 国家 973项目 (G2 0 0 0 0 4 870 5)，中国科学院知识创新工程项目“黑河流域水—生态—经济系统综合管理试验示范”(KZCX1 0 9)，国家林业局“九五”重点项目共同资助 |
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| 摘 要： | 通过对连山寺大隆林区定位站1975－2000年的降水特征与森林对降水的再分配分析，建立了祁连山大隆林区降水与温度，降水与湿度，林冠截留的关系式。该区多年平均降水量为433.5mm，年变幅在326.4-539.7mm;降水量最大出现在夏季，占全年降水量的65．70％；海拔高度每升高100m，年了量平均递增4．55％，林区温度和湿度均与降水有较好的拟合关系。青海云杉林与祁连圆柏林林冠对大气降水的平均截留率分别为37．5％，31．7％，灌木林的截留率平均高达66．5％。青海云杉林林冠层平均截留率随着降雨量的增大逐渐减小，当降雨量为18.67mm时，林冠截留量达到最大，为14.72mm；青海云杉树干径流量占降水量的0．51％，当降雨量超过12.0mm时，才开始产生树干径流。青海云杉林枯枝落叶层对降雨的截留量随降雨量级增加而增大，截留率则随降雨量减小而增大，枯枝落叶层所具有的截留降雨和调蓄降雨作用使祁连山林区基本不发生地表径流。分析结果表明，祁连山林区对水源涵养和水流出山的时间调控有重要意义。
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| 关 键 词： | 祁连山 降水特征 拟合方程 树冠 森林 温度 湿度 |
| 文章编号： | 1000-0534(2002)03-0274-07 |
| 修稿时间： | 2002年3月12日 |
Precipitation Characteristic and Interception of Forest in Qilian Mountain |
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| CHANG Xue xiang ,ZHAO Ai fen ,WANG Jin ye ,CHANG Zong qiang ,JIN Bo wen.Precipitation Characteristic and Interception of Forest in Qilian Mountain[J].Plateau Meteorology,2002,21(3):274-280. |
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| Authors: | CHANG Xue xiang ZHAO Ai fen WANG Jin ye CHANG Zong qiang JIN Bo wen |
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| Institution: | CHANG Xue xiang 1,ZHAO Ai fen 1,WANG Jin ye 2,CHANG Zong qiang 2,JIN Bo wen 2 |
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| Abstract: | The long term precipitation characteristic and forest entrapment were studied at Sidalong station,Qilian Mountains. The annual average precipitation is 433.6 mm(from 1972 to 2000), and varied from 326.4 mm to 539.7 mm, annual precipitation falls in summer is 65.70%. Precipitation is altered in different altitudes, its tendency increase 4.45% of the amount with altitude arising per 100 m.The average entrapmentrates are 37.5%, 31.7% on canopy entrapping precipitation of Picea crassifolia forest and Sabina Przewalsskii forest,the average entrapmentrate of brush forest even is as high as 66.5%. When the rainfall is intensive, its average entrapmentrate gradually diminished in Picea Crassifolia forest. When the amount of precipitation is 18.67 mm, the amount of canopy entrapment of Picea Crassifolia forest is 14.72 mm. The trunk runoff of Picea crassifolia is 0.51% of the amount of precipitation and its trunk runoff began when the amount of precipitation is over 12.0 mm. The litter entrapment precipitation gradually increased when amount of rainfall increased, the entrapment rate increased when the amount of rainfall diminished. |
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| Keywords: | Forest area in Qilian Mountains Precipitation characteristic Entrapment Relation equation |
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