✦ LIBER ✦

An anemometer for scale model environmental wind measurements

✍ Scribed by Sayed M. Ettouney; Fergus R. Fricke

Publisher: Elsevier Science
Year: 1975
Weight: 786 KB
Volume: 10
Category: Article
ISSN: 0007-3628
DOI: 10.1016/0007-3628(75)90004-3

No coin nor oath required. For personal study only.

✦ Synopsis

The limitations of existing methods available for the assessment of environmental wind conditions around buildings, using wind tunnel models, are discussed. The development of an alternative instrument which, in many situations, is more suitable than those more commonly used, is described. A drawing, circuit diagram and calibration curve for the instrument are presented and its limitations and future development outlined.

📜 SIMILAR VOLUMES

Hand anemometer for measuring winds near

Hand anemometer for measuring winds near the surface

📂 Article 📅 2007 🏛 John Wiley and Sons 🌐 English ⚖ 128 KB

Vortex anemometer for measurement of bot

Vortex anemometer for measurement of both speed and direction of the wind

✍ Sophie Goujon-Durand 📂 Article 📅 1993 🏛 Elsevier Science 🌐 English ⚖ 252 KB

Full-scale measurement of environmental

Full-scale measurement of environmental wind in the shinjuku new metropolitan center

✍ S. Sanada; Y. Iwasa; M. Yoshida 📂 Article 📅 1980 🏛 Elsevier Science 🌐 English ⚖ 920 KB

Full scale measurement of wind speeds in

Full scale measurement of wind speeds in an inner city

✍ C.W. Letchford; L.T. Isaacs 📂 Article 📅 1992 🏛 Elsevier Science 🌐 English ⚖ 574 KB

Measurement and data analysis methods fo

Measurement and data analysis methods for field-scale wind erosion studies and model validation

✍ Ted M. Zobeck; Geert Sterk; Roger Funk; Jean Louis Rajot; John E. Stout; R. Scot 📂 Article 📅 2003 🏛 John Wiley and Sons 🌐 English ⚖ 659 KB

Diffusion reduction in an arbitrary scal

Diffusion reduction in an arbitrary scale third generation wind wave model

✍ W.E. Rogers; J.M. Kaihatu; H.A.H. Petit; N. Booij; L.H. Holthuijsen 📂 Article 📅 2002 🏛 Elsevier Science 🌐 English ⚖ 359 KB

The numerical schemes for the geographic propagation of random, short-crested, wind-generated waves in third-generation wave models are either unconditionally stable or only conditionally stable. Having an unconditionally stable scheme gives greater freedom in choosing the time step (for given space