[HTML][HTML] Finescale vertical structure of a cold front as revealed by an airborne Doppler radar
B Geerts, R Damiani, S Haimov - Monthly weather review, 2006 - journals.ametsoc.org
B Geerts, R Damiani, S Haimov
Monthly weather review, 2006•journals.ametsoc.org… Here Δx is computed as the shortest distance between a station in the cold air and the
cold front. The location of the latter is fine-tuned based on a fine line observed in the
displays of the Amarillo and Vance, TX, NEXRAD radars and S-band dual-polarization
Doppler radar (S-Pol), although between 1600 and 1800 UTC none of the radars clearly
locates this fine line. The value of ΔT is obtained from the station in the cold air, and the
closest station in the warm air. Mobile mesonet temperatures are not included …
cold front. The location of the latter is fine-tuned based on a fine line observed in the
displays of the Amarillo and Vance, TX, NEXRAD radars and S-band dual-polarization
Doppler radar (S-Pol), although between 1600 and 1800 UTC none of the radars clearly
locates this fine line. The value of ΔT is obtained from the station in the cold air, and the
closest station in the warm air. Mobile mesonet temperatures are not included …
Bond, NA, and MA Shapiro, 1991: Research aircraft observations of the mesoscale and microscale structure of a cold front over the eastern Pacific Ocean. Mon. Wea. Rev, 119, 3080–3094.
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