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Environmental Flow Impacts on Tropical Cyclone Structure Diagnosed from Airborne Doppler Radar Composites
被引:201
|作者:
Reasor, Paul D.
[1
]
Rogers, Robert
[1
]
Lorsolo, Sylvie
[1
,2
]
机构:
[1] NOAA, Atlantic Oceanog & Meteorol Lab, Hurricane Res Div, Miami, FL 33149 USA
[2] Univ Miami, Cooperat Inst Marine & Atmospher Studies, Miami, FL USA
关键词:
Hurricanes;
typhoons;
Tropical cyclones;
Aircraft observations;
Radars;
Radar observations;
VERTICAL WIND SHEAR;
HIGH-RESOLUTION SIMULATION;
HURRICANE BONNIE 1998;
BOUNDARY-LAYER JETS;
INNER-CORE;
PART II;
STORM MOTION;
ERIN;
2001;
INTENSITY;
EVOLUTION;
D O I:
10.1175/MWR-D-12-00334.1
中图分类号:
P4 [大气科学(气象学)];
学科分类号:
0706 ;
070601 ;
摘要:
Following a recent demonstration of multicase compositing of axisymmetric tropical cyclone (TC) structure derived from airborne Doppler radar measurements, the authors extend the analysis to the asymmetric structure using an unprecedented database from 75 TC flights. In particular, they examine the precipitation and kinematic asymmetry forced by the TC's motion and interaction with vertical wind shear. For the first time they quantify the average magnitude and phase of the three-dimensional shear-relative kinematic asymmetry of observed TCs through a composite approach. The composite analysis confirms principal features of the shear-relative TC asymmetry documented in prior numerical and observational studies (e.g., downshear tilt, downshear-right convective initiation, and a downshear-left precipitation maximum). The statistical significance of the composite shear-relative structure is demonstrated through a stratification of cases by shear magnitude. The impact of storm motion on eyewall convective asymmetry appears to be secondary to the much greater constraint placed by vertical wind shear on the organization of convection, in agreement with prior studies using lightning and precipitation data.
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页码:2949 / 2969
页数:21
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