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Abstract
Based on a high-resolution dataset, this note re-examines the recently developed potential vorticity (PV) metrics for determining extratropical transition (ET) onset and completion times. The PV metrics use average 330-K isentropic potential vorticity (IPV) to determine the ET onset time, defined as the 330-K IPV minimum time. However, the suggested 330-K IPV threshold fails to determine the ET completion time using the 20-km resolution data, and this IPV method cannot resolve reintensifying and weakening tropical cyclone cases due to the absence of differentiation of lower-level IPV tendencies after ET onset between these two groups of cases.
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Citation
LI Qingqing, WANG Qian. 2013: Re-Examination of the Potential Vorticity Metrics for Determining Extratropical Transition Onset and Completion Times Using High-Resolution Data. Journal of Meteorological Research, 27(4): 502-508. DOI: 10.1007/s13351-013-0404-4
LI Qingqing, WANG Qian. 2013: Re-Examination of the Potential Vorticity Metrics for Determining Extratropical Transition Onset and Completion Times Using High-Resolution Data. Journal of Meteorological Research, 27(4): 502-508. DOI: 10.1007/s13351-013-0404-4
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LI Qingqing, WANG Qian. 2013: Re-Examination of the Potential Vorticity Metrics for Determining Extratropical Transition Onset and Completion Times Using High-Resolution Data. Journal of Meteorological Research, 27(4): 502-508. DOI: 10.1007/s13351-013-0404-4
LI Qingqing, WANG Qian. 2013: Re-Examination of the Potential Vorticity Metrics for Determining Extratropical Transition Onset and Completion Times Using High-Resolution Data. Journal of Meteorological Research, 27(4): 502-508. DOI: 10.1007/s13351-013-0404-4
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