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<br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />t <br />t <br />t <br />t <br />t <br />t <br />t <br />t <br />t <br />t <br />t <br />t <br />t <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />~ <br />~ <br />. <br />. <br />. <br />. <br />. <br />I <br />l <br /> <br />airborne CCN counter that were visibly related 10 <br />air pollution. II was determined further that these <br />differences were related to the satellite retrievals. <br />which were validated by the aircraft <br />measurements. Pollution is certainly affecting <br />Sierra clouds and precipitation detrimentally, <br />Through the aircraft and satellite measurements <br />in SUPRECIP it has been noted that much of the <br />Sierra precipitation was produced by surprisingly <br />shallow pristine clouds_ This suggests that <br />pollution will act detrimentally on such clouds and <br />may help explain the long-term losses in Sierra <br />orographic precipitation. <br /> <br />Summary of the HEAT project <br /> <br />The Houston Environmental Aerosol <br />Thunderstorm Project (HEAT) is designed to <br />address the fadors responsible for the observed <br />enhancement in lightning frequency over <br />Houston. TX. An array of surface and airborne <br />equipment were operated during this study to <br />characterize the thermodynamic, environmental. <br />and cloud properties of the atmosphere within <br />and outside of the urban area. II has been <br />speculated that enhanced aerosol concentrations <br />arising from urban emissions suppress <br />precipitation and deepen the mixed layer within <br />urban douds. which may alter cloud <br />electrification. and possibly increase lightning <br />frequency . <br /> <br />. <br /> <br />4 I . ,~ <br /> <br /> <br />. <br />. <br /> <br />g <br />o <br /> <br />,.. <br />o <br /> <br />Figure 19 Mean annual flash density (flashes <br />'km2tyear) for the years 1989-2000, The Houston <br />metro area 1$ outlined in white, while the white box <br />represents the urban enhancement region (Orville et <br />al,.2oo1) <br /> <br />To address the merit of this hypothesis for the <br />Houston region. detailed measurements of <br />aerosol and doud properties were necessary. <br />Measurements were conducted onboard the <br />SOAR research aircraft with complementary <br />surface measurements of aerosol and cloud <br />properties throughout the approximately 6-week <br />intenSive field program. Nearly identical <br />instrumentation suites were used on the SOAR <br />Cheyenne II and at the 275 m Williams Tower on <br />the west side of Houston. to characterize size <br />distributions, size-resolved hygroscopic growth. <br />and cloud activation efficiency of the aerosol. The <br />SOAR research aircraft was equipped with <br />multiple wing probes for direcl measurement of <br />cloud droplet size distributions. <br /> <br />The primary goal of the Houston Environmental <br />Aerosol Thunderstorm (HEAT) project is to <br />examine the sources and causes of a 50% <br />enhancement of c1oud-to-ground lightning <br />discharges over Houston. Texas. Comparable <br />lightning enhancement has been observed also <br />over Lake Charles. Louisiana. Reaching this goal <br />will involve quantification of the effects of <br />pollution. the urban heat island. and the complex <br />coastline on storms and lightning characteristics <br />in the Houston area. <br /> <br />The SOAR and T AMU research team designed <br />flight patterns to accomplish three primary <br />objectives: <br /> <br />1. Provide additional detail of the properties of <br />the aerosol entering cloud base. and the size <br />distribution of cloud droplets in the liquid <br />phase region of target clouds. <br /> <br />2. Through flights extending beyond the <br />Houston urban area. statistically characterize <br />the differences between CCN spectra within <br />and outside of Houston. <br /> <br />3, Provide a link with the ground-based <br />measurements by flying spirals over the <br />surface site. <br /> <br />Airborne measurements from the SOAR <br />research aircraft prOvided the necessary spatial <br />coverage of the study region as well as the direct <br />in situ measurements of cloud properties. To <br />assess the degree to which the aerosol and CCN <br />properties during flight times are representative <br />of the region, complementary measurements <br />were made continuously al the surface site at the <br /> <br />34 <br />