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国家自然科学基金(91025014)

作品数:2 被引量:31H指数:2
相关作者:刘鹄何志斌唐振兴更多>>
相关机构:中国科学院更多>>
发文基金:国家自然科学基金中国科学院“百人计划”更多>>
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祁连山中段林草交错带土壤水热特征及其对气象要素的响应被引量:29
2012年
利用综合环境观测仪(ENVIS)的长期监测数据,分析了2002-06-01—2008-05-31期间祁连山阴坡林草交错带土壤水热特征及其与气象要素的统计关系,结果表明:1)土壤温度与空气温度年内变化格局相似,但存在滞后期,滞后时间随土壤深度增加而增加;土壤温度年际变化与气温一致,呈逐渐降低趋势。2)土壤水分表现为20—80 cm土壤水分易受外界降水过程影响,120 cm和160 cm深度土壤水分变化相对平缓;土壤水分季节性冻融过程中的主要控制因子为温度,但20—80 cm冻土的融化还受上层土壤水分融化和降雨下渗影响。3)月尺度上土壤水分和温度与气象要素的统计关系优于日尺度。利用气象要素在月尺度上建立的经验模型上对20—60 cm深度土壤温度的估算效果相对较好。
唐振兴何志斌刘鹄
关键词:气象要素
Response of tree-ring growth to climate at treeline ecotones in the Qilian Mountains,northwestern China被引量:2
2011年
Climate constitutes the main limiting factor for tree-ring growth in high-elevation forests, and the relationship between tree-ring growth and climate is complex. Based on tree-ring chronology and meteorological data, the influence of precipitation, mean temperature and mean minimum temperature at yearly, seasonal and monthly scales on the tree-ring growth of Picea crossifolia was studied at treeline ecotones in the Qilian Mountains, northwestern China. The results show that growing season temperatures of previous and current years are important limiting factors on tree-ring growth, particularly June mean temperature and mean minimum temperature of current year. The precipitations in the previous winter and current spring have a positive correlation, and in the current fall has a negative correlation with tree-ring growth, but these correlations are not significant. Our results suggest that temperature controls tree-ring growth more strongly than precipitation at treeline ecotones in the Qilian Mountains.
ZhiBin HeWenZhi ZhaoLiJie ZhangHU LiuZhenXing Tang
关键词:CLIMATE
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