首页> 外文期刊>Journal of Geophysical Research. Biogeosciences >Dynamic and thermodynamic structure of the lower troposphere above rain forest and wet savanna during the EXPRESSO campaign
【24h】

Dynamic and thermodynamic structure of the lower troposphere above rain forest and wet savanna during the EXPRESSO campaign

机译:EXPRESSO战役期间雨林和湿大草原上空对流层下部的动态和热力学结构

获取原文
获取原文并翻译 | 示例
获取外文期刊封面目录资料

摘要

This paper focuses on the energy budget of atmospheric surface and boundary layers over the wet savanna and the rain forest during the Experiment of Regional Sources and Sinks of Oxidants (EXPRESSO). It assesses dynamic features at the transition between savanna and forest at the beginning of the dry season. The experimental zone was still influenced by the monsoon flow with water vapor mixing ratio of about 16 g/kg. Thermodynamic characteristics of the savanna and forest ecosystems are similar. However, for an equivalent net radiation, evaporation is greater over the forest and leads to lower Bowen ratios (0.2 over the forest, 0.45 over the savanna). Low horizontal winds with no mean direction are observed, due to the proximity of the Intertropical Convergence Zone (ITCZ). However, in spite of low horizontal winds, the momentum flux is high, owing to high drag coefficients and roughness lengths. Some differences appear in the turbulent kinetic energy budget: dynamic and thermal production terms over the forest are nearly half those over the savanna. As a consequence, turbulent exchanges are more efficient over the savanna. Entrainment velocities are deduced from the latent heat flux values at the top of the atmospheric boundary layer (ABL) and from the jump in water vapor mixing ratio between the ABL and the free troposphere. Entrainment velocities are of the same order as subsidence velocities deduced from European Centre Medium-Range Weather Forecasts statistical analyses. High pollution levels are observed in the forest ABL (CO concentration is around 280 ppb), Pollutants, produced by savanna fires, are transported from the free troposphere into the forest ABL by entrainment. Furthermore, horizontal exchanges between the savanna and the forest, induced by large eddies, may occur, increasing the pollution of the forest ABL. Through this study, the ITCZ appears to be an exchange zone rather than a barrier to the transfer of pollutants. [References: 33]
机译:本文在区域性氧化剂源和汇实验(EXPRESSO)中,重点研究了湿大草原和雨林大气表面和边界层的能量收支。它评估了干旱季节开始时热带稀树草原和森林之间过渡时的动态特征。实验区仍受季风影响,水蒸气混合比约为16 g / kg。稀树草原和森林生态系统的热力学特征相似。但是,对于等效的净辐射,整个森林的蒸发量更大,并且导致较低的鲍恩比(整个森林为0.2,大草原为0.45)。由于靠近热带辐合带(ITCZ),观测到的低水平风没有平均方向。但是,尽管水平风较小,但由于较高的阻力系数和粗糙度长度,动量通量还是很高的。动荡的动能预算中出现了一些差异:森林的动态和热生产条件几乎是热带稀树草原的一半。结果,湍流交换在大草原上更加有效。从大气边界层(ABL)顶部的潜热通量值和ABL与自由对流层之间水蒸气混合比的跃迁推导出夹带速度。夹带速度与从欧洲中心中程天气预报统计分析得出的沉降速度的阶次相同。在森林ABL中观察到高污染水平(CO浓度约为280 ppb),稀树草原大火产生的污染物通过引流从对流层自由地转移到森林ABL中。此外,大涡旋可能引起热带稀树草原与森林之间的水平交换,增加了森林ABL的污染。通过这项研究,ITCZ似乎是一个交换区,而不是污染物转移的障碍。 [参考:33]

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号