On the relationship of thunderstorm ice hydrometeor characteristics and total lightning measurements |
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| Authors: | Wiebke Deierling John Latham Walter A Petersen Scott M Ellis Hugh J Christian Jr |
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| Institution: | aUniversity of Alabama Huntsville, Department of Atmospheric Science, Huntsville, AL, United States;bNational Center for Atmospheric Research, Boulder, CO, United States;cEarth System Sciences Center, University Alabama Huntsville, 320 Sparkman Dr., Huntsville, AL 35899, United States;dNASA, Marshall Space Flight Center, Huntsville, AL, United States |
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| Abstract: | Satellite-borne and ground-based devices for the detection of lightning offer the opportunity to explore relationships–on all significant scales up to global–between lightning frequency, f, and other thundercloud parameters. Calculations predict that f is proportional to the product of the downflux p of solid precipitation and the upward mass flux, I, of ice crystals. This prediction has received support from limited computational studies. The physical reasons for such a relationship are explained in terms of the paramount role of ice in the electrification of thunderstorms. Herein, this prediction is subjected to further, preliminary examination through analysis of lightning and dual-polarimetric radar data collected during the STERAO experiment conducted in Northern Colorado during the summer of 1996. The analysis has yielded some highly provisional support for this flux hypothesis. Computed trends of radar derived hydrometeor fractions of solid precipitation and small ice show correlation to the total lightning frequency and raise the possibility of determining values of p and/or I from lightning measurements.It is shown that the extent to which the observed correlations between f and both solid precipitation and small ice trends are or are not strong can provide an indication as to whether the lightning activity is limited by the available concentrations of precipitating or non-precipitating ice in the upper regions of the charging zone of the thundercloud, where most of the charge transfer occurs. It is demonstrated that the most accurate determinations of precipitation rate p from measurements of lighting frequency f are likely to be for conditions where the field-growth is limited by the availability of graupel pellets. It is shown that the simultaneous time variations of f and solid precipitation trends of the type obtained in the STERAO experiment could enable us to determine the nature of the dominant glaciation process operative in the thunderclouds studied. |
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| Keywords: | Lightning Polarimetric radar Precipitation Ice |
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