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[科尔沁草地能量平衡的日变化和季节变化]

[Diurnal and seasonal variations of energy balance over Horqin meadow].

作者信息

Li Hui-dong, Guan De-Xin, Yuan Feng-Hui, Ren Yan, Wang An-Zhi, Jin Chang-Jie, Wu Jia-Bing

出版信息

Ying Yong Sheng Tai Xue Bao. 2014 Jan;25(1):69-76.

Abstract

Based on the measurements of eddy flux and micrometeorological factors, this paper analyzed the diurnal and seasonal variations of energy balance over Horqin meadow. The results showed that annual energy balance ratio (EBR) of the eddy covariance system was 0.77, and EBR was biggest in growing season, middle in bare soil period and smallest in snow-covered period. Diurnal variations of energy components all presented bell-shaped curves. The peak of net radiation appeared around 12:00 and peaks of other components slightly lagged. Seasonal variation of net radiation presented a single-peak curve, and the annual average was 5.71 MJ x m(-2) x d(-1). Seasonal variation of latent heat flux was similar to that of net radiation, and the annual average was 2.84 MJ x m(-2) x d(-1). Seasonal variation of sensible heat flux presented a double-peak curve, and the peaks appeared in April and September, respectively. Annual averaged sensible heat flux was 1.87 MJ x m(-2) x d(-1). Maximum soil heat flux (3.47 MJ x m(-2) x d(-1)) appeared in April, and the soil heat flux became negative after September. Annual budget ratios of energy components presented a decreasing order of latent heat flux, sensible heat flux and soil heat flux, which accounted for 49.8%, 35.8% and 3.1% of net radiation, respectively. Seasonal variation of Bowen ratio (beta) presented a 'U' shape, and the annual average was 1.61. beta was small (0.18) and relatively stable in growing season, while it was large (2.39) and fluctuated severely in non-growing season.

摘要

基于涡动通量和微气象因子的观测数据,分析了科尔沁草甸能量平衡的日变化和季节变化特征。结果表明,涡度相关系统的年能量平衡比率(EBR)为0.77,其中生长季EBR最大,裸土期次之,积雪期最小。各能量分量的日变化均呈钟形曲线,净辐射峰值出现在12:00左右,其他分量峰值稍有滞后。净辐射的季节变化呈单峰曲线,年平均值为5.71 MJ·m-2·d-1。潜热通量的季节变化与净辐射相似,年平均值为2.84 MJ·m-2·d-1。感热通量的季节变化呈双峰曲线,峰值分别出现在4月和9月,年平均感热通量为1.87 MJ·m-2·d-1。土壤热通量最大值(3.47 MJ·m-2·d-1)出现在4月,9月后土壤热通量转为负值。各能量分量的年收支比率由大到小依次为潜热通量、感热通量和土壤热通量,分别占净辐射的49.8%、35.8%和3.1%。 Bowen比(β)的季节变化呈“U”形,年平均值为1.61。β在生长季较小(0.1

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