TY - JOUR
T1 - The vertical structure of a tornado near Happy, Texas, on 5 May 2002
T2 - High-resolution, mobile, W-band, doppler radar observations
AU - Bluestein, Howard B.
AU - Weiss, Christopher C.
AU - Pazmany, Andrew L.
PY - 2004/10
Y1 - 2004/10
N2 - A mobile, W-band Doppler radar scanned, at close range, portions of a tornado near Happy, Texas, on 5 May 2002. Simultaneous boresighted video images were also recorded, which facilitated correlating the radar-observed features of the tornado with its visual features. Range-height indicators (RHIs) of radar reflectivity and Doppler velocity were collected that detail, with high spatial resolution, aspects of the vertical structure of the tornado near the ground. Most of the RHIs showed a column of a weak-echo hole from about 60 m above the ground up to the top of the domain at 800-1000 m above the ground; the hole was roughly 40% broader about 100 m above the ground as it was above, resulting in a characteristic pear-shaped vertical cross section of reflectivity. In this tornado, the condensation funnel was much narrower than the width of the weak-echo hole; the visible debris cloud near the ground was approximately just as wide as the hole above 150 m. The mean depth of the debris cloud was around 200 m. The vertical structure of the Doppler-velocity field exhibited a narrow band of high wind speeds about 200-400 m above the ground, consistent with airflow inward toward and cyclonically about the tornado. Possible reasons for the observed structure of the tornado are offered.
AB - A mobile, W-band Doppler radar scanned, at close range, portions of a tornado near Happy, Texas, on 5 May 2002. Simultaneous boresighted video images were also recorded, which facilitated correlating the radar-observed features of the tornado with its visual features. Range-height indicators (RHIs) of radar reflectivity and Doppler velocity were collected that detail, with high spatial resolution, aspects of the vertical structure of the tornado near the ground. Most of the RHIs showed a column of a weak-echo hole from about 60 m above the ground up to the top of the domain at 800-1000 m above the ground; the hole was roughly 40% broader about 100 m above the ground as it was above, resulting in a characteristic pear-shaped vertical cross section of reflectivity. In this tornado, the condensation funnel was much narrower than the width of the weak-echo hole; the visible debris cloud near the ground was approximately just as wide as the hole above 150 m. The mean depth of the debris cloud was around 200 m. The vertical structure of the Doppler-velocity field exhibited a narrow band of high wind speeds about 200-400 m above the ground, consistent with airflow inward toward and cyclonically about the tornado. Possible reasons for the observed structure of the tornado are offered.
UR - http://www.scopus.com/inward/record.url?scp=7744238614&partnerID=8YFLogxK
U2 - 10.1175/1520-0493(2004)132<2325:TVSOAT>2.0.CO;2
DO - 10.1175/1520-0493(2004)132<2325:TVSOAT>2.0.CO;2
M3 - Article
AN - SCOPUS:7744238614
SN - 0027-0644
VL - 132
SP - 2325
EP - 2337
JO - Monthly Weather Review
JF - Monthly Weather Review
IS - 10
ER -