TY - JOUR
T1 - Impingement of rain drops on a tall building
AU - Etyemezian, V.
AU - Davidson, C. I.
AU - Zufall, M.
AU - Dai, W.
AU - Finger, S.
AU - Striegel, M.
N1 - Funding Information:
This work was funded by the National Park Service Cooperative Agreements 042419005 and 00196035. Thanks to Curt Yeske and Shawn McClory who provided invaluable technical support. We appreciate the help from Paul Sides, Rob Verrenna, and the Department of Chemical Engineering on software issues. Christina Amon provided insightful suggestions for the preparation of this manuscript. Thanks are also due to Rich Palladini and Larry Young for permitting access to Warner Hall. Ivan Locke, David Iorio, and Judy Lee contributed to the CAD model of the Cathedral of Learning shown in Fig. 7 . Thanks to John Murray and Ivan Locke for their measurement work at the Cathedral of Learning. A special thanks to Susan Sherwood for her invaluable insights and guidance during the early phases of this work.
PY - 2000
Y1 - 2000
N2 - Soiling on the walls of limestone buildings can be washed off when the surface erodes due to rain impingement. In this study, the delivery of rain to the 42-story Cathedral of Learning in Pittsburgh, Pennsylvania, represented by a 30mx30mx160m rectangular block, was modeled using the RNG K-ε model for turbulence and Lagrangian trajectory calculations for individual rain drops. Local Effect Factors (LEF) for the rectangular block compared well with earlier work in the literature. LEFs increased with wind speed, raindrop size, and height along the block. Wind speed, direction, and rain intensity were measured continuously over a seven-week period and provided input parameters for modeling rain fluxes to the Cathedral of Learning. Model results suggested that sections of the building receiving larger amounts of rain corresponded to white areas, indicating that rain fluxes have a significant effect on the soiling patterns. Intermediate wind speeds (2.5 and 5ms-1) resulted in high rain fluxes. Although less frequent, high wind speeds also resulted in high rain fluxes. Much of the rain was delivered to the block as 1.25 and 2.5mm drops with 5mm drops having a smaller effect. Consideration of wind incidence angles other than 0°was shown to be important for future modeling efforts. Copyright (C) 2000 Elsevier Science Ltd.
AB - Soiling on the walls of limestone buildings can be washed off when the surface erodes due to rain impingement. In this study, the delivery of rain to the 42-story Cathedral of Learning in Pittsburgh, Pennsylvania, represented by a 30mx30mx160m rectangular block, was modeled using the RNG K-ε model for turbulence and Lagrangian trajectory calculations for individual rain drops. Local Effect Factors (LEF) for the rectangular block compared well with earlier work in the literature. LEFs increased with wind speed, raindrop size, and height along the block. Wind speed, direction, and rain intensity were measured continuously over a seven-week period and provided input parameters for modeling rain fluxes to the Cathedral of Learning. Model results suggested that sections of the building receiving larger amounts of rain corresponded to white areas, indicating that rain fluxes have a significant effect on the soiling patterns. Intermediate wind speeds (2.5 and 5ms-1) resulted in high rain fluxes. Although less frequent, high wind speeds also resulted in high rain fluxes. Much of the rain was delivered to the block as 1.25 and 2.5mm drops with 5mm drops having a smaller effect. Consideration of wind incidence angles other than 0°was shown to be important for future modeling efforts. Copyright (C) 2000 Elsevier Science Ltd.
KW - Acid rain
KW - Buildings
KW - CFD
KW - Driving rain
KW - Soiling
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U2 - 10.1016/S1352-2310(99)00443-4
DO - 10.1016/S1352-2310(99)00443-4
M3 - Article
AN - SCOPUS:0034112452
SN - 1352-2310
VL - 34
SP - 2399
EP - 2412
JO - Atmospheric Environment
JF - Atmospheric Environment
IS - 15
ER -