<?xml version="1.0" encoding="UTF-8"?><xml><records><record><source-app name="Biblio" version="6.x">Drupal-Biblio</source-app><ref-type>27</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Djurfors, S.</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">On the rise of buoyant plumes in turbulent environments</style></title></titles><keywords><keyword><style  face="normal" font="default" size="100%">air emissions</style></keyword><keyword><style  face="normal" font="default" size="100%">climate</style></keyword><keyword><style  face="normal" font="default" size="100%">plume measurement and movement</style></keyword><keyword><style  face="normal" font="default" size="100%">Syncrude</style></keyword><keyword><style  face="normal" font="default" size="100%">weather</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">1977</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://era.library.ualberta.ca/files/5q47rq09m/1977-4%20-%20PP%20-%20Djurfors%20-%20Bouyant%20Plume.pdf</style></url></web-urls></urls><publisher><style face="normal" font="default" size="100%">Syncrude Canada Ltd. </style></publisher><pub-location><style face="normal" font="default" size="100%">Edmonton, AB  </style></pub-location><pages><style face="normal" font="default" size="100%">10 pages </style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">A plume rise model is derived from the equations of turbulent motion, retaining the turbulent flux terms. The solutions are similar to those proposed earlier by Csanady but containing an exponential decay term. The model finds particular value in predicting a leveled-off plume trajectory in neutral atmospheric conditions. In unstable atmospheric conditions the ultimate mode of behavior depends on whether the atmospheric turbulence or the unstable stratification finally dominate the plume motion. </style></abstract><notes><style face="normal" font="default" size="100%">Professional Paper 1977-4.</style></notes><custom3><style face="normal" font="default" size="100%">http://www.worldcat.org/oclc/15914967</style></custom3><custom4><style face="normal" font="default" size="100%">OSEMB</style></custom4></record></records></xml>