SCIENTIFIC ABSTRACT TKACHUK, YU.V. - TKALICH, A.I.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001755930001-0
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: July 16, 2001
• Sequence Number: 1
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

GOV/ 11-9-58-12-13/17
Calculation of Horizontal Components of Wind with Consideration of
Internal Friction and Non-Linear Treatments of Acceleration
successive approximation. The assumption is made that the
pressure field is stationary, i.e. 6P/6t - 0 . Therefore,
the solution Eq.(5) will be found from the system of Eqs,(4).
The geostrophic wind at the point x = y = 0 flows along
the axis x with the speed uF and the condition:
6r/by =:6u/6x / 0 . This means that the air motion
converges when 6u/6xNO or diverges if 6u/6x