On the existence of the logarithmic surface layer in the inner core of hurricanes

被引:24
作者
Smith, Roger K. [1 ]
Montgomery, Michael T. [2 ]
机构
[1] Univ Munich, Inst Meteorol, D-80333 Munich, Germany
[2] Naval Postgrad Sch, Dept Meteorol, Monterey, CA USA
关键词
hurricanes; tropical cyclones; typhoons; surface layer; logarithmic layer; spin-up; HIGH-RESOLUTION SIMULATIONS; PLANETARY BOUNDARY-LAYER; IN-SITU OBSERVATIONS; PART I; TROPICAL CYCLONES; WIND STRUCTURE; SIMPLE-MODEL; INTENSITY; PARAMETERIZATIONS; INTENSIFICATION;
D O I
10.1002/qj.2121
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
We question recent studies invoking the existence of a traditional `logarithmic surface layer', or log layer, in the boundary layer of the rapidly rotating core of a hurricane. One such study argues that boundary-layer parametrization schemes that do not include a log layer are `badly flawed'. Another study assumes the existence of a log layer to infer drag coefficients at hurricane wind speeds. We provide theoretical reasoning supported by observational evidence as to why significant departures from the normally assumed logarithmic layer might be expected, questioning its use in the inference of the drag coefficient at high wind speeds and laying bare suggestions that hurricane models using boundary-layer schemes that do not represent the log layer should not be used. The ramifications of these findings for hurricane modelling are discussed. Finally, we draw attention to a study examining a range of boundary-layer schemes demonstrating that a recently articulated boundary-layer spin-up mechanism transcends the presence of a log layer.
引用
收藏
页码:72 / 81
页数:10
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