Meteorology of Whitehaven. 



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* The evaporation for 1842 is computed from the evaporation force, in proportion to the respective values of the estimated and 

 measured evaporation in the corresponding months of the years 1843 and 1844. The result, calculated for the mean of the whole 

 period (1843-1846) during which the evaporating force and the spontaneous evaporation were registered daily together is 39-870 

 inches: — ° J ' 



Grains. Inches. Grains. Inches. 

 Thus, if 19-99 : 30-908 :: 25-8 : 39-87 

 t The evaporation in 1843 is somewhat too small in amount, from the gauge not being sufficiently exposed to wind and sun dur- 

 ing the first half of the year. 



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