EXAMINATION OF THE GRAVITATION THEORY OF OCEANIC
CIRCULATION.—LIEUT. MAURY’S THEORY.—(_Continued._)
Methods of determining the Question.—The Force resulting from
Difference of Specific Gravity.—Sir John Herschel’s Estimate
of the Force.—Maximum Density of Sea-Water.—Rate of Decrease
of Temperature of Ocean at Equator.—The actual Amount of
Force resulting from Difference of Specific Gravity.—M.
Dubuat’s Experiments 115