长白山阔叶红松林生长季热量平衡变化特征

应用生态学报 ›› 2004, Vol. ›› Issue (10): 1828-1832.

长白山阔叶红松林生长季热量平衡变化特征

关德新, 吴家兵, 王安志, 赵晓松, 金明淑, 徐浩, 戴冠华, 何秀

中国科学院沈阳应用生态研究所, 沈阳 110016

收稿日期:2003-06-25 修回日期:2004-01-07 出版日期:2004-10-15
通讯作者: 关德新,男,1962年生,博士,研究员,主要从事生态气象、森林生态效应方面的研究,发表论文30余篇.E-mail:guandexin@hotmail.com,dxguan@iae.ac.cn
基金资助:
国家自然科学基金项目(30370293);中国科学院知识创新工程项目(KZCX2406);中国科学院沈阳应用生态研究所知识创新工程资助项目(SCXZD01010301)

Dynamics of heat balance during growing season of broadleaved Korean pine forest in Changbai Mountains

GUAN Dexin, WU Jiabing, WANG Anzhi, ZHAO Xiaosong, JIN Mingshu, XU Hao, DAI Guanhua, HE Xiu

Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110016, China

Received:2003-06-25 Revised:2004-01-07 Online:2004-10-15

摘要/Abstract

摘要： 根据长白山阔叶红松林2001年5月下旬至10月上旬微气象梯度观测资料和辐射、土壤热通量资料,用波文比-能量平衡方法(BREB方法)计算了森林的显热通量和感热通量,并计算了森林大气和植被体的储热量,分析了阔叶红松林热量平衡各项的日变化和季节变化,结果发现,热量平衡(净辐射)与太阳总辐射呈线性关系;热量平衡各项都与净辐射有相同的日变化特征,为昼正夜负的曲线.各项的绝对值一般表现为净辐射>潜热通量>感热通量>储热变化.受日照时间的影响,6～10月各分量正值的日持续时间逐渐缩短.月平均结果,白天净辐射6月份最大,10月上旬最小,变化于0～527 W·m^-2,夜间的净辐射在0～-121 W·m^-2.潜热通量白天和夜间分别在0～441、0～-81 W·m^-2,感热通量昼夜分别在0～80、0～-26 W·m^-2.储热变化则为0～44、0～-26 W·m^-2.白天潜热通量占净辐射的比例8～10月逐渐下降,而感热通量和储热变化的比例9～10月明显上升,特别在严霜后2～3d,出现潜热通量比例突减、感热通量比例突增的现象.文中还对通量观测仪器、方法进行了简要分析.

关键词: 热量平衡, 潜热, 感热, 储热量, 日变化, 生长季变化

Abstract: Based on the gradient measurement of microclimate factors,radiation and soil heat flux from late May to early October,2001 and by the method of Bowen ratio-energy balance (BREB),this paper estimated the latent heat and sensible heat above the broadleaved Korean pine forest in Changbai Mountains.The energy storage of forest air and vegetative was calculated,and the seasonal variations of heat balance components of the forest were analyzed.The results showed that the net radiation of the forest and the solar radiation were linearly correlated.All the heat balance components had the similar characteristics of diurnal variation to the net radiation,showing curves positive at daytime and negative at night,and the terms ranged as net radiation>latent heat>sensible heat>storage.The time of keeping positive terms in a day became shorter from June to October as influenced by shinning time.The highest net radiation was in June and the lowest in October.The monthly averaged net radiation was 0～527 and 0～-121 W·m^-2,and the latent heat was 0～441 and 0～-81 W·m^-2 for day and night,respectively.Sensible heat was 0～80 and 0～-26 W·m^-2,and energy storage was 0～44 and 0～-26 W·m^-2 for day and night,respectively.The ratio of latent heat to net radiation at daytime decreased gradually from August to October,and the ratio of sensible heat and energy storage increased correspondingly.Especially 2～3 days after the first sever frost,a sudden drop of latent heat and a sudden bounce of sensible heat were appeared.The instruments and measurement methods of heat flux were also concisely discussed in this paper.

Key words: Heat balance, Latent heat, Sensible heat, Energy storage, Diurnal variation, Seasonal variation

中图分类号:

S716

关德新, 吴家兵, 王安志, 赵晓松, 金明淑, 徐浩, 戴冠华, 何秀. 长白山阔叶红松林生长季热量平衡变化特征[J]. 应用生态学报, 2004, (10): 1828-1832.

GUAN Dexin, WU Jiabing, WANG Anzhi, ZHAO Xiaosong, JIN Mingshu, XU Hao, DAI Guanhua, HE Xiu. Dynamics of heat balance during growing season of broadleaved Korean pine forest in Changbai Mountains[J]. Chinese Journal of Applied Ecology, 2004, (10): 1828-1832.

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