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A comparison between energy transfer and atmospheric turbulent exchanges over alpine meadow and banana plantation

机译:高寒草甸和香蕉人工林能量传递与大气湍流交换的比较

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摘要

Banana plantation and alpine meadow ecosystems in southern China and the Tibetan Plateau (TP) are unique in the underlying surfaces they exhibit. In this study, we used eddy covariance and a micrometeorological tower to examine the characteristics of land surface energy exchanges over a banana plantation in southern China and an alpine meadow in the Tibetan Plateau from May 2010 to August 2012. The results showed that the diurnal and seasonal variations in upward shortwave radiation flux and surface soil heat flux were larger over the alpine meadow than over the banana plantation surface. Dominant energy partitioning varied with season. Latent heat flux was the main consumer of net radiation flux in the growing season, whereas sensible heat flux was the main consumer during other periods. The Monin-Obukhov similarity theory was employed for comparative purposes, using sonic anemometer observations of flow over the surfaces of banana plantations in the humid southern China monsoon region and the semi-arid areas of the TP, and was found to be applicable. Over banana plantation and alpine meadow areas, the average surface albedo and surface aerodynamic roughness lengths under neutral atmospheric conditions were similar to 0.128 and 0.47 m, and similar to 0.223 and 0.01 m, respectively. During the measuring period, the mean annual bulk transfer coefficients for momentum and sensible heat were 1.47 x 10(-2) and 7.13 x 10(-3), and 2.91 x 10(-3) and 1.96 x 10(-3), for banana plantation and alpine meadow areas, respectively.
机译:中国南方和青藏高原(TP)的香蕉种植园和高山草甸生态系统在它们展现的下伏表面中是独特的。在这项研究中,我们使用涡度协方差和微气象塔研究了中国南部香蕉种植园和青藏高原高寒草甸从2010年5月至2012年8月的土地表面能量交换的特征。高山草甸上短波向上辐射通量和地表土壤热通量的季节性变化大于香蕉种植园表面的季节性变化。主要的能量分配随季节而变化。潜热通量是生长季节净辐射通量的主要消耗者,而感热通量则是其他时期的主要消耗者。 Monin-Obukhov相似性理论用于比较目的,利用声速风速计观测湿润的中国南方季风区和TP半干旱区的香蕉种植园表面上的水流,并发现是适用的。在香蕉种植园和高寒草甸地区,中性大气条件下的平均表面反照率和表面空气动力学粗糙度长度分别约为0.128和0.47 m,分别约为0.223和0.01 m。在测量期间,动量和显热的年平均体传系数为1.47 x 10(-2)和7.13 x 10(-3),以及2.91 x 10(-3)和1.96 x 10(-3),分别用于香蕉种植园和高山草甸地区。

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  • 来源
    《Theoretical and applied climatology》 |2017年第2期|59-76|共18页
  • 作者单位

    Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Tibetan Environm Changes & Land Surface P, Beijing, Peoples R China|CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing, Peoples R China;

    Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Tibetan Environm Changes & Land Surface P, Beijing, Peoples R China|CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing, Peoples R China;

    Sun Yat Sen Univ, Ctr Monsoon & Environm Res, Guangzhou, Guangdong, Peoples R China|Sun Yat Sen Univ, Coll Atmospher Sci, Guangzhou, Guangdong, Peoples R China;

    Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Tibetan Environm Changes & Land Surface P, Beijing, Peoples R China|CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing, Peoples R China;

    Chongqing Meteorol Serv Ctr, Chongqing, Peoples R China;

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