![In the given figure for u = u0/3 . Find the height from the ground at which the block the leaves the hemisphere. [where u0 = √(gr3) ]](https://dwes9vv9u0550.cloudfront.net/images/155360/7e76d485-f4b7-40e8-9c5b-04c66f609950.jpg "In the given figure for u = u0/3 . Find the height from the ground at which the block the leaves the hemisphere. [where u0 = √(gr3) ]")
In the given figure for u = u0/3 . Find the height from the ground at which the block the leaves the hemisphere. [where u0 = √(gr3) ]
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![Collected reprints / Atlantic Oceanographic and Meteorological Laboratories [and] Pacific Oceanographic Laboratories. Oceanography Periodicals.. 422 JOURNAL OF PHYSICAL OCEANOGRAPHY Volume 5 U = U0 U = 0. Fig. 1. Schematic diagram](https://c8.alamy.com/comp/REHBNH/collected-reprints-atlantic-oceanographic-and-meteorological-laboratories-and-pacific-oceanographic-laboratories-oceanography-periodicals-422-journal-of-physical-oceanography-volume-5-u-=-u0-u-=-0-fig-1-schematic-diagram-of-a-rossby-wave-propagating-into-a-zonal-current-which-is-independent-of-longitude-while-the-waves-phase-velocity-cp-is-away-from-the-current-the-group-velocity-cg-carries-the-wave-energy-into-the-current-illustrated-in-fig-2-0km-rtx-i-ry-4-when-lateral-viscosity-is-present-the-wave-is-damped-as-it-propagates-although-the-energy-loss-per-wave-length-is-REHBNH.jpg "Collected reprints / Atlantic Oceanographic and Meteorological Laboratories [and] Pacific Oceanographic Laboratories. Oceanography Periodicals.. 422 JOURNAL OF PHYSICAL OCEANOGRAPHY Volume 5 U = U0 U = 0. Fig. 1. Schematic diagram")
Collected reprints / Atlantic Oceanographic and Meteorological Laboratories [and] Pacific Oceanographic Laboratories. Oceanography Periodicals.. 422 JOURNAL OF PHYSICAL OCEANOGRAPHY Volume 5 U = U0 U = 0. Fig. 1. Schematic diagram
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