Please use this identifier to cite or link to this item: https://physrep.ff.bg.ac.rs/handle/123456789/365
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dc.contributor.authorĆurić, Mladjenen
dc.contributor.authorJanc, Dejanen
dc.contributor.authorVučković, Vladanen
dc.contributor.authorKovačević, Nemanjaen
dc.date.accessioned2022-07-12T15:23:41Z-
dc.date.available2022-07-12T15:23:41Z-
dc.date.issued2009-09-03en
dc.identifier.issn0177-7971en
dc.identifier.urihttps://physrep.ff.bg.ac.rs/handle/123456789/365-
dc.description.abstractSuccessful seeding of clouds in weather modification experiments essentially depends on the seeding time and dynamics, amount of seeding material and location of the initial seeding area. In the present study, we focus on the influence of the initial seeding zone location on the transport of seeding agent material into the target cloud. In addition, the inadvertent transport of seeding material is analysed. During weather modification activities, a lot of seeding material can be transferred far from the seeding zone in a downwind direction. The primary motivation for this research was to prove this statement. We use a three-dimensional, mesoscale cloud-resolving model to achieve our goal. We performed sensitivity tests with respect to the distance between the mass centres of the initial seeding area and the cloud. Different seeding scenarios are analysed. Our principal findings are as follows: (1) For distances between the mass centres of the initial seeding area and the cloud below 2.5 km, all seeding agent material would be activated after a short time. For distances above 10 km, most of the seeding agent would remain inactivated, because horizontal transport of the seeding agent becomes more important than transport induced by the main updraft. For these scenarios, the seeding agent is injected in the cold peripheral part of the cloud. (2) Sensitivity tests show that the inactivated seeding agent would remain close to the seeding area if the seeding is performed below cloud base. This effect occurs even for large distances between the seeding area and the target cloud (>20 km) due to low-level convergence. Thus, this seeding method suppresses the inert seeding material from being transferred far from the seeding zone. (3) The complete seeding material stays inactivated if the seeding is performed between the -8 and -12°C isotherms in front of the increased reflectivity zone. As a consequence, it would be transferred far from its initial area. The cloud would not be able to capture the seeding agent even during its greatest lateral extent. © Springer-Verlag 2009.en
dc.relation.ispartofMeteorology and Atmospheric Physicsen
dc.titleAn inadvertent transport of the seeding material as a result of cloud modificationen
dc.typeArticleen
dc.identifier.doi10.1007/s00703-009-0040-9en
dc.identifier.scopus2-s2.0-70349752902en
dc.identifier.urlhttps://api.elsevier.com/content/abstract/scopus_id/70349752902en
dc.relation.issue3-4en
dc.relation.volume105en
dc.relation.firstpage157en
dc.relation.lastpage165en
item.openairetypeArticle-
item.cerifentitytypePublications-
item.fulltextNo Fulltext-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.grantfulltextnone-
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