Tuesday, 24 January 2017: 10:30 AM
Conference Center: Tahoma 1 (Washington State Convention Center )
This study provides, for the first time, detailed climatological diurnal variations in lightning flash optical energetics observed from the Tropical Rainfall Measuring Mission Lightning Imaging Sensor (TRMM/LIS). The analysis of 13 years (2002-2014) of LIS global-scale (~38°S-38°N) flash radiances (ε) as a function of the local solar time (LST) reveals remarkably consistent regional and seasonal patterns. The diurnal variation of ε (over both continental and oceanic regions) is characterized by a monotonic increase from late afternoon (~20:00 LST), attaining a maximum around 09:00 LST, followed by a decreasing trend. In particular, the continental (oceanic) ε values reach a broader minimum spanning from ~15:00-19:00 LST (~18:00-20:00). The relative diurnal amplitude variation in continental ε is about 45%, compared to only about 15% for oceanic ε. The study confirms that the results are not affected by diurnal biases associated with instrument detection characteristics, or other statistical artifacts. A notable agreement is shown between the diurnal variations of ε and the global-scale (~38°S-38°N) Mesoscale Convective Systems diurnal areal extent. Comparisons with recently published diurnal variations of cloud-to-ground lightning peak current over the US also exhibit a marked similarity. Given the novelty of these findings, few tentative hypotheses about the underlying physical mechanism(s) are discussed.
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