| Description |
The optical properties of lightning observed by the Lightning Imaging Sensor (LIS) aboard the Tropical Rainfall Measuring Mission (TRMM) satellite between 1998 and 2010 are described and examined in the context of how they interrelate, when and where they occur globally, the nature of the cloud environment they illuminate, and the properties of the parent thunderstorm. Daytime (nighttime) flashes that occur over the open ocean are shown to be 31.7% (39.8%) larger and 55.2% (75.1%) brighter than flashes over land. Three factors are proposed that determine the size of the illuminated region: the brightness of the flash, the scattering properties of the cloud medium, and the structure of the electrical breakdown. Some of these results are explored using a Monte-Carlo radiative transfer model. The properties of TRMM Radar Precipitation Features (RPFs) that produce exceptionally large, long-lasting, and optically bright lightning flashes are compared to typical storms. RPFs over land with exceptionally large lightning flashes are up to three times larger than typical RPF thunderstorms and are considerably stronger. Coastal and oceanic RPFs with exceptionally large lightning flashes, as well as RPFs with exceptionally long lasting or bright flashes are also considerably larger and stronger than typical thunderstorms. Finally, high-altitude aircraft passive microwave and electric field observations taken by the NASA ER-2 over the course of multiple field campaigns are used to examine relationships between the properties of electrified clouds and above-cloud electric fields. A retrieval algorithm is created that is capable of estimating above-cloud electric fields from 85 GHz or 37 GHz passive microwave observations. The 37 GHz estimates are only valid over land since the ocean surface appears "cold" at 37 GHz and can reproduce the observed electric fields to within a factor of two 60% of the time. By comparison, the 85 GHz estimates fall within a factor of two of observations more than 70% of the time over land, but the 85 GHz routine is valid for both land and ocean cases. Individual cases are examined, and methods for improving the routine before applying it to satellite observations to study the Global Electric Circuit are discussed. |
