2013
DOI: 10.1175/waf-d-12-00021.1
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An Intercomparison of UW Cloud-Top Cooling Rates with WSR-88D Radar Data

Abstract: The University of Wisconsin Convective Initiation (UWCI) algorithm utilizes geostationary IR satellite data to compute cloud-top cooling (UW-CTC) rates and assign CI nowcasts to vertically growing clouds. This study is motivated by National Weather Service (NWS) forecaster reviews of the algorithm output, which hypothesized that more intense cloud-top cooling corresponds to more vigorous short-term (0–60 min) convective development. An objective validation of UW-CTC rates using a satellite-based object-trackin… Show more

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Cited by 11 publications
(20 citation statements)
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“…In fact, any georeferenced dataset, including nonmeteorological data, can be fused with the cloud objects through the statistical postprocessing system with the ability to monitor temporal trends in all data fields. Two research projects at UW-CIMSS are utilizing the convective cloud object tracking system and publications from those projects will further demonstrate the utility of the system (e.g., Hartung et al 2013).…”
Section: Discussionmentioning
confidence: 99%
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“…In fact, any georeferenced dataset, including nonmeteorological data, can be fused with the cloud objects through the statistical postprocessing system with the ability to monitor temporal trends in all data fields. Two research projects at UW-CIMSS are utilizing the convective cloud object tracking system and publications from those projects will further demonstrate the utility of the system (e.g., Hartung et al 2013).…”
Section: Discussionmentioning
confidence: 99%
“…In addition, a lead-time analysis of cloud-top cooling rates as a function of the same NEXRAD fields was generated to highlight the prognostic value of satellitebased cooling rates in operational forecasting. Such an in-depth analysis is not presented in this text, but the reader is referred to Hartung et al (2013) for complete details. A second research project leverages the two systems to compute the time rate of change of an array of satellite cloud-retrieved fields (e.g., « tot , cloud phase, visible optical depth), combined with NWP data and NEXRAD data to probabilistically nowcast the likelihood that a developing convective cloud will produce surface severe weather reports in the subsequent 0-2-h time frame.…”
Section: Application Of Convective Cloud Object Tracking Methodologymentioning
confidence: 99%
“…Spatial correlation problems also exist when comparing satellite brightness-temperature values with reflectivity. Objects identified objectively as convection by satellite would need to be appropriately backtracked to the correct preconvective cloud object, which would introduce several unwanted tracking errors at a low temporal resolution (Sieglaff et al 2013). Parallax is resolved using a method similar to that in Sieglaff et al (2011) in which indications are assumed to be at a height of 7 km.…”
Section: A Defining Convection Initiationmentioning
confidence: 99%
“…Previous studies have done basic validations to test the skill of CI products (Mecikalski et al 2008;Hartung et al 2013), but only a few have speculated on the impact of the preconvective environment on CTC-based predictions of CI (Mecikalski et al 2008;Sieglaff et al 2011;Walker et al 2012). Validations range from radar-based CI detection (Mecikalski and Bedka 2006;Mecikalski et al 2008;Walker et al 2012) to occurrence of lightning near CTC indications (Sieglaff et al 2011).…”
Section: Introductionmentioning
confidence: 99%
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