Airflow above changes in surface heat flux, temperature and roughness; an extension to include the stable case

✍ Scribed by P. A. Taylor

• Publisher: Springer
• Year: 1971
• Tongue: English
• Weight: 790 KB
• Volume: 1
• Category: Article
• ISSN: 0006-8314
• DOI: 10.1007/bf00184785

✦ Synopsis

OkE

Non-dimensional absolute humidity gradient. OH Non-dimensional temperature gradient of heat flux. ObM Non-dimensional wind shear. ~b ~' = OM = H = WE, an assumption used in stable conditions. Q Air density. e, Absolute humidity. Qw Density of water. T Kinematic shear stress. Logarithmic height scale (=In(z+z)/z,).