...
首页> 外文期刊>Journal of Geophysical Research. Biogeosciences >NUMERICAL MODELING OF SHIP TRACKS PRODUCED BY INJECTIONS OF CLOUD CONDENSATION NUCLEI INTO MARINE STRATIFORM CLOUDS
【24h】

NUMERICAL MODELING OF SHIP TRACKS PRODUCED BY INJECTIONS OF CLOUD CONDENSATION NUCLEI INTO MARINE STRATIFORM CLOUDS

机译:将云状凝结核注入海洋层状云中产生的航迹的数值模拟

获取原文
获取原文并翻译 | 示例
   

获取外文期刊封面封底 >>

       

摘要

Ship tracks are long-lived, lineal regions of enhanced reflectivity in low-lying marine clouds that appear in satellite imagery downwind of ships. Ship tracks were first observed as cloud lines in visible satellite imagery (type 1), A second (and more common) type of ship track (type 2), which is masked at visible wavelengths by natural variability in cloud reflectivity, is seen at near-infrared wavelengths in satellite imagery. A one-dimensional numerical model is used to simulate measurements of both types of ship tracks and to investigate interactions between aerosol and cloud microphysics, radiative transfer, and turbulent mixing in the cloud-topped marine boundary layer that lead to the formation and provide for the persistence of ship tracks. We find that cloud condensation nuclei (CCN) injections can account for many of the observed properties of ship tracks. Higher CCN concentrations produce increased droplet concentrations, which enhance cloud reflectivity by reducing droplet radius and increasing droplet cross-sectional area. The smaller droplets also reduce the drizzle rate, which can allow cloud water to increase under some conditions, thereby leading to higher cloud reflectivity. However, smaller droplets also evaporate more readily below cloud base. Increased evaporation reduces mixing between the cloud and the subcloud layers during daytime, which causes a decrease in cloud water. The distinction between the two types of ship tracks is suggested to be due to differences in ambient concentrations of CCN that cause variations in turbulent mixing in the boundary layer, through the effect of cloud droplet concentrations on cloud-top longwave radiative cooling. The model predicts lifetimes of > 1 day and > 2 days for the simulated type 1 and type 2 ship tracks, respectively. In the atmosphere, processes not treated in the model, such as horizontal dispersion and changes in large-scale atmospheric conditions, may limit ship track lifetimes. [References: 29]
机译:船舶航迹是低层海洋云中反射率增强的长寿命线性区域,出现在船舶顺风的卫星图像中。首先在可见的卫星图像(类型1)中观察到云线时观察到了航迹,在附近看到了第二种(也是更常见的)类型的船迹(类型2)在可见波长处被云反射率的自然变化所掩盖。卫星图像中的红外波长。一维数值模型用于模拟两种类型的船舶航迹的测量,并研究气溶胶和云的微观物理学之间的相互作用,辐射传递以及云顶海洋边界层中的湍流混合,这些相互作用导致形成并为航迹的持久性。我们发现云凝结核(CCN)注入可以解释许多航迹的观测特性。较高的CCN浓度会产生增加的液滴浓度,从而通过减小液滴半径和增大液滴横截面积来提高云的反射率。较小的水滴还会降低毛毛雨率,这会使云水在某些条件下增加,从而导致更高的云反射率。但是,较小的液滴在云层下方也更容易蒸发。蒸发量的增加减少了白天云层和亚云层之间的混合,从而减少了云层中的水分。两种类型的航迹之间的区别被认为是由于CCN周围环境浓度的差异,通过云滴浓度对云顶长波辐射冷却的影响,边界层中湍流混合会发生变化。该模型分别针对模拟的1型和2型船舶航迹预测寿命> 1天和> 2天。在大气层中,模型中未处理的过程(例如水平分散和大规模大气条件的变化)可能会限制船舶航迹的寿命。 [参考:29]

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