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contributor authorList, Roland
date accessioned2017-06-09T16:55:25Z
date available2017-06-09T16:55:25Z
date copyright2014/04/01
date issued2013
identifier issn0022-4928
identifier otherams-76538.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4218996
description abstractn all-encompassing new theory of heat and mass transfer (HMT) and growth equations have been developed for freely falling spherical hailstones with diameters of 0.5?8 cm. The initial six variables are diameter, liquid water content, air and hailstone surface temperatures, net collection efficiency, and ice fraction of spongy deposit. They are replaced by three or four new ones, depending on the three growth categories. Two new variables are products of ?old? ones: (i) the square root of the Reynolds number Re and the liquid water content and (ii) net collection efficiency and ice fraction of the spongy deposit. Only the products matter, not the individual parts. [The two variables in (ii) are as important as the two in (i).] Two old variables remain: air and surface temperatures. The HMT can be further compacted for hailstorms with specified pressure?air temperature?height profiles. Further, Re for free-fall reveals unexpected complexities?issues important to solve HMT problems.The ?new hailstone physics? is based on 55 years of in-house studies of all aspects of hailstone growth, followed by 5 years of shaping these puzzle pieces and assembling them into a coherent picture. This was only possible by recognizing the free-fall mode: a special gyration that allows hailstones to grow with a radial symmetry and, thus, homogeneous surface temperature.Part II will display the surprising solutions to growth and HMT and firmly link the hailstones to mostly spongy growth with shedding that favors a hail-coupled rain mechanism.
publisherAmerican Meteorological Society
titleNew Hailstone Physics. Part I: Heat and Mass Transfer (HMT) and Growth
typeJournal Paper
journal volume71
journal issue4
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/JAS-D-12-0164.1
journal fristpage1508
journal lastpage1520
treeJournal of the Atmospheric Sciences:;2013:;Volume( 071 ):;issue: 004
contenttypeFulltext


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