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Journal of Flow Visualization and Image Processing

Published 4 issues per year

ISSN Print: 1065-3090

ISSN Online: 1940-4336

The Impact Factor measures the average number of citations received in a particular year by papers published in the journal during the two preceding years. 2017 Journal Citation Reports (Clarivate Analytics, 2018) IF: 0.6 The Immediacy Index is the average number of times an article is cited in the year it is published. The journal Immediacy Index indicates how quickly articles in a journal are cited. Immediacy Index: 0.6 The Eigenfactor score, developed by Jevin West and Carl Bergstrom at the University of Washington, is a rating of the total importance of a scientific journal. Journals are rated according to the number of incoming citations, with citations from highly ranked journals weighted to make a larger contribution to the eigenfactor than those from poorly ranked journals. Eigenfactor: 0.00013 The Journal Citation Indicator (JCI) is a single measurement of the field-normalized citation impact of journals in the Web of Science Core Collection across disciplines. The key words here are that the metric is normalized and cross-disciplinary. JCI: 0.14 SJR: 0.201 SNIP: 0.313 CiteScore™:: 1.2 H-Index: 13

Indexed in

NUMERICAL FLOW VISUALIZATION AND THERMAL TRANSPORT PHENOMENON OF BENARD CONVECTION IN A THIN LIQUID LAYER INDUCED BY EVAPORATION

Volume 6, Issue 2, 1999, pp. 95-104
DOI: 10.1615/JFlowVisImageProc.v6.i2.20
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ABSTRACT

A numerical study is performed on heat transfer and fluid flow in natural convection in a very thin liquid layer induced by surface evaporation, irrespective of its being cooled below or adiabatic. The two-dimensional governing equations are discretized by means of a finite-difference technique and solved numerically. This study shows that (1) the flow structure and temperature distribution in the liquid layer are predicted; (2) the liquid layer consists of two strata: heat convection taking place in the upper stream and heat conduction taking place in the lower one; and (3) the wave motion appears in the upper liquid layer, and the fluid flow is stationary in the lower one.

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