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- W2175133722 abstract "Abstract An elongated cold-frontal maximum in the lower-tropospheric potential vorticity (PV) field accompanies some midlatitude cyclones. These PV maxima are often of diabatic origin, and are hypothesized to contribute substantially to the strength of the low-level jet (LLJ) and moisture transport in the cyclone warm sector. Diagnosis of a representative cyclone event from the central United States during February 1997 is presented with the goals of (i) elucidating the mechanisms of development and propagation of the cold-frontal PV band, and (ii) clarifying the relation between this PV maximum and the LLJ. A confluent upper trough and modest surface cyclone followed a track from the south-central United States northeastward into southern Ontario between 26 and 28 February 1997, accompanied by flooding and widespread straight-line wind damage. A LLJ, with maximum wind speeds in excess of 35 m s−1, was positioned at the western extremity of the cyclone warm sector, immediately east of an elongated PV maxi..." @default.
- W2175133722 created "2016-06-24" @default.
- W2175133722 creator A5088553581 @default.
- W2175133722 date "2002-01-01" @default.
- W2175133722 modified "2023-09-27" @default.
- W2175133722 title "Cold-Frontal Potential Vorticity Maxima, the Low-Level Jet, and Moisture Transport in Extratropical Cyclones" @default.
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- W2175133722 doi "https://doi.org/10.1175/1520-0493(2002)130<0059:cfpvmt>2.0.co;2" @default.
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