Experiments on the Load Convective Mass Transfer of Smooth and Rough Hailstone ModelsSource: Journal of Applied Meteorology:;1971:;volume( 010 ):;issue: 005::page 1018Author:Schuepp, Peter H.
DOI: 10.1175/1520-0450(1971)010<1018:EOTLCM>2.0.CO;2Publisher: American Meteorological Society
Abstract: The local convective mass transfer (i.e., the mass transfer as a function of polar angle) of smooth and rough particles has been investigated with an electrochemiluminescence technique at a Schmidt number Sc ≈ 103 for Reynolds numbers 3 ? 103 < Re < 105. Comparative qualitative wind tunnel observations were made of the evaporation of naphthalene-coated rough spheres with Sc = 2.4 and, wherever possible, the findings were compared with existing heat transfer measurements in order to minimize their dependence on the molecular properties of the fluid. Although some uncertainty still exists, it is possible to present estimates of the qualitative and quantitative effect of surface roughness on the local convective heat and mass transfer of hailstones, and especially to show the large increase in local transfer at polar angles around 90° for Re > 104, which may help to explain the growth of big hailstones.
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contributor author | Schuepp, Peter H. | |
date accessioned | 2017-06-09T17:16:53Z | |
date available | 2017-06-09T17:16:53Z | |
date copyright | 1971/10/01 | |
date issued | 1971 | |
identifier issn | 0021-8952 | |
identifier other | ams-8234.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4225445 | |
description abstract | The local convective mass transfer (i.e., the mass transfer as a function of polar angle) of smooth and rough particles has been investigated with an electrochemiluminescence technique at a Schmidt number Sc ≈ 103 for Reynolds numbers 3 ? 103 < Re < 105. Comparative qualitative wind tunnel observations were made of the evaporation of naphthalene-coated rough spheres with Sc = 2.4 and, wherever possible, the findings were compared with existing heat transfer measurements in order to minimize their dependence on the molecular properties of the fluid. Although some uncertainty still exists, it is possible to present estimates of the qualitative and quantitative effect of surface roughness on the local convective heat and mass transfer of hailstones, and especially to show the large increase in local transfer at polar angles around 90° for Re > 104, which may help to explain the growth of big hailstones. | |
publisher | American Meteorological Society | |
title | Experiments on the Load Convective Mass Transfer of Smooth and Rough Hailstone Models | |
type | Journal Paper | |
journal volume | 10 | |
journal issue | 5 | |
journal title | Journal of Applied Meteorology | |
identifier doi | 10.1175/1520-0450(1971)010<1018:EOTLCM>2.0.CO;2 | |
journal fristpage | 1018 | |
journal lastpage | 1025 | |
tree | Journal of Applied Meteorology:;1971:;volume( 010 ):;issue: 005 | |
contenttype | Fulltext |