High stratocumuliform clouds of the genus cirrocumulus form when moist air at high tropospheric altitude reaches saturation, creating ice crystals or supercooled water droplets. Limited convective instability at the cloud level gives the cloud a rolled or rippled appearance.
Some solutions found in living organisims are Carbon, Nitrogen, Oxegyn, and Hydrogen.
There are three possible concentrations of solution to consider: 1  Isotonic solution a solution of equal OP (or concentration) to a cell. 2  Hypertonic solution a solution of higher OP (or concentration) than a cell. 3  Hypotonic solution a solution of lower OP (or concentration) than a cell.