The influence of rotational frontogenesis and its associated shearwise vertical motions on the development of an upper‐level front
The influence of rotational frontogenesis and its associated shearwise vertical motions on the development of an upper‐level front
复制标题
旋转锋生及其相关的剪切垂直运动对高层锋发展的影响
DOI:
10.1002/qj.551
复制
发表时间:
2010
影响因子:
8.9
通讯作者:
Jonathan E. Martin
中科院分区:
文献类型:
--
作者:
Andrea A. Lang;Jonathan E. Martin
The total quasi‐geostrophic (QG) vertical motion is partitioned into transverse and shearwise couplets oriented parallel to, and along, the geostrophic vertical shear, respectively, in order to examine the role of rotational frontogenesis, and its associated shearwise circulation, in the life cycle of an upper‐front/jet system in northwesterly flow. In particular the analysis emphasizes two aspects of that role: (1) the influence of shearwise ω on scalar frontogenesis, and (2) the effect of rotational frontogenesis, and its associated vertical circulation, on the initiation of along‐flow cold air advection during upper frontogenesis.