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<br />- <br /> <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />With a new conceptual model suggesting seeding for dynamic effect can also <br />produce a substantial increase in rainfall without causing a sizeable increase in the <br />maximum height of the seeded cloud (Rosenfeld and Woodley, 1993), further research in <br />Texas in the 1990s documented the physical processes operative within the vigorous <br />supercooled convective towers at the time of treatment with glaciogenic material. In <br />addition to finding that the internal cloud structure is strongly dependent upon cloud base <br />temperature, evidence was produced strongly suggesting seeding works well in clouds <br />having an abundance of supercooled water, especially where such water in a vigorous, <br />supercooled updraft region is available for artificial nucleants having a greater cross- <br />sectional area for accretion of cloud water (Rosenfeld and Woodley, 1997), It was also <br />observed that the time to reduce the maximum amount of cloud water in seeded <br />convective towers to half of its initial value was lessened by some 2 to 3 minutes from <br />that in the unseeded cases, <br /> <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />Additional exploratory research in the Montana HIPLEX (1975-1980), and later <br />in North Dakota (1987-1993) further examined the precipitation processes in cumuliform <br />clouds. In the North Dakota work, many of the new technologies cited in the NRC report <br />were applied. In addition to the tracer techniques cited in the brief review of the NOAA <br />Atmospheric Modification Program (AMP) elsewhere in this response, the North Dakota <br />researchers used dual-channel microwave radiometers, in situ cloud microphysical <br />measurements, including within hailstorms themselves (Detwiler et aI., I 994a, b), and <br />numerical cloud models. Some of the modeling was done in real-time, for predictive <br />purposes, much else was done post hoc, to gain a better understanding of the observations <br />made, and to allow further improvements to the models. These modeling efforts are also <br />discussed elsewhere within this response, <br /> <br />Our point here is two-fold, First, contrary to the implications of the NRC report, <br />there has been quality research in conjunctions with ongoing operational programs <br />published in the refereed literature. Secondly, the research ceased only when federal <br />involvement at a significant scale ended. We wholeheartedly endorse the NRC <br />recommendation that a renewed long-term research effort be undertaken, and agree that a <br />number of critical issues remain to be fully answered. <br /> <br />We also maintain that coupling physical experiments with ongoing operational <br />programs for exploratory experiments would be a productive, cost-effective approach to <br />answering many ofthe questions posed in the NRC report. We acknowledge, however, <br />that only conducting randomization apart from existing operational programs will afford <br />the strength of statistical design necessary for confirmatory experiments, <br /> <br />24 <br />