Evidence from Meteosat imagery of the interaction of sting jets with the boundary layer

Meteorological Applications

Volumn 11, Issue 4, 2004, Pages 277-289

  Browning, K A ^a   Field, M ^a  

^a UNIVERSITY OF READING   (United Kingdom)

Author keywords

[No Author keywords available]

Indexed keywords

STORMS;

CLOUD HEAD; DRY SLOT; EXTRA-TROPICAL CYCLONES; LOW-LEVEL CLOUDS; METEOSAT; SURFACE WINDS;

BOUNDARY LAYERS;

CLOUD COVER; INFRARED IMAGERY; JET FLOW; METEOSAT; MOMENTUM TRANSFER; TROPICAL CYCLONE; WIND FIELD;

EID: 14044273513     PISSN: 13504827     EISSN: None     Source Type: Journal    
DOI: 10.1017/S1350482704001379     Document Type: Article

References (6)

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2. Browning, K. A. (2004). The sting at the end of the tail: damaging winds associated with extratropical cyclones. Q. J. R. Meteorol Soc. 130: 375-399.
3. Browning, K. A. & Roberts, N. M. (1994) Structure of a frontal cyclone. Q. J. R. Meteorol. Soc. 120: 1535-1557.
4. Clark, P. A. & Browning, K. A. (2004) The sting at the end of the tail: model diagnostics of fine scale 3D structure of the cloud head. Q. J. R. Meteorol. Soc. submitted.
5. Grønås, S (11995) The seclusion intensification of the New Year's day storm 1992. Tellus 47A: 733-746.
6. Shapiro, M & Keyser, D. (1990) Fronts, jet streams and the tropopause. In Extratropical Cyclones: The Eric Palmén Memorial Volume, Am. Meteorol. Soc., Boston MA, pp. 167-191.