Laserfiche WebLink
<br /> <br />V. ANALYSIS <br /> <br />PIBAL POINTS <br />Ie FEB. 1965 <br /> <br />, \ <br />~ <br /> <br />A- 1600' <br />.- 1000' <br /> <br />PREDICTED _ MEASURED ....-- Ale TRACKS <br />Figure 43c.-Plume Dimensions and Pibal Soundings for 18 <br />February 1965. <br /> <br />it does not seem likely that the natural freezing <br />nuclei are being scavenged, but are being used. <br />It would be desirable to confirm this by electron <br />microscope technique with replicas taken from the <br />Park Range; facilities for doing this work are availa- <br />ble at the National Center for Atmospheric Re- <br />search, Boulder, Colo. <br />Of the snowcrystal replicas taken during the past <br />winter season, 33 were examined in detail. About <br />50 percent showed collected water drops and/or <br />riming and 50 percent did not. Those showing <br />water drops and/or riming were collected during <br />the early winter (January and early February); <br />those without water drops and/or riming were col- <br />lected in late February and March. It appears that <br />the presence or absence of water drops characterizes <br />a storm. Figure 48 is an example taken from the <br />28 January 1965 storm. <br />About 40 percent of the replicas contain simple <br />crystals only; the remaining 60 percent consist of <br /> <br />35 <br /> <br />aggregates. The presence of water drops or riming <br />on aggregates exceeded that on simple crystals by a <br />2: 1 ratio, and the dendritic form-which is pre- <br />dominant among all other forms-is most favored <br />for the collection of water drops. <br />If artificial nucleation is effective, the quantity <br />of such drops should decrease when artificial nuclei <br />are provided, The seasonal history of supercooled <br />drop population will show whether the effectiveness <br />of nucleation operations can be expected-on a <br />physical basis-to vary with time, and whether- <br />through neutron activation analyses of replicas-the <br />variation is due to the abundance of natural nuclei <br />or to carry-over effects of AgI nuclei. <br />The measurement of Ag concentration in artifi- <br />cial snow replicas3-snow formed by nucleating <br />supercooled water drops in a cold box-show that <br /> <br />3 Schaefer, V. and Fuquay, ]., 1965: "The Detection of <br />Silver Iodide in Snow by Neutron Activation Analysis", <br />Journal of Recherches des Atmospheriques, Vol. II, April- <br />June 1965, No.2, <br /> <br />l!5mi R. <br />- ------------ <br /> <br /> <br />IOmi R. <br /> <br />.~~ <br />.;,," 'If <br />!f.... .......'~..."A1 <br />.. ""-, '?;J7'''-= <br />. '- Y ."... <br />.... - =."~:.~iI;"'.J'4$o...4t!i'~ <br />. 'i. .,,4 <br /> <br />~. <br />y~- <br /> <br /> <br /> <br />OAK CREEK ( <br /> <br /> <br />/ <br /> <br />,/ <br /> <br />~ PREmCTEO <br /> <br />_ MEASURED <br /> <br />------ TRUCK <br /> <br />Figure 43d.-Plume Dimensions and Pibal Soundings for 22 <br />February 1965. <br />