|  | British Rainfall 1895 page 22 
 OTHER GAUGES AT SEATHWAITE.
 
 I wish to direct particular attention to the double rule  
separating the first three columns on p.25 from the others,  
because anyone who looks at that table without attending to  
that double rule, and without reading the following  
sentence, is sure to be confused and to think that there is  
some mistake.
 The fact is, that the first three columns are devoted to the 
record of Gauge I., the standard record; the subsequent  
columns are to be considered solely as confirmatory - and  
for that purpose the ratios in the latter columns have  
nothing to do with the relative wetness or dryness of the  
years, but express the ratio of the amount collected in each 
year by each gauge to the amount collected by Gauge I. -  
e.g., Gauge I. in 1847 collected 129.24 in., but  
Gauge II. collected only 126.80 in., which was 98 per cent.  
of the amount collected by Gauge I. - and so of all the  
other values given on that side of the double rule.
 Gauge II. - It will be remembered that at first Gauge 
I. was said to be only 6 inches above the ground; Gauge II.  
was 1 ft. 6 in. above it, and therefore should have  
collected slightly less.
 Gauge III. - This was 1 ft. 10 in. above the ground,  
and therefore the same argument applies as with reference to 
Gauge II.
 Gauge IV. - This gauge is, as regards the collection  
of snow, so badly designed that I do not understand why,  
from 1872 to 1894, it has practically collected as much as  
Gauge I.; the deficiency, as shown by the first few years,  
seems more probable, and the sudden change at the beginning  
of 1872 is very puzzling. Of course, the same arithmetical  
result would follow if the readings of Gauge I. for the  
years 1865-71 were too high, but there does not seem to be  
any reason to accept that explanation.
 Gauge V. This gauge shows rather less than I  
expected; perhaps its position in the garden was slightly  
sheltered.
 Gauge VI. - This gauge is practically perfect, and in 
an excellent position; it shows a mean deficiency of 5.2 per 
cent. as compared with Gauge I.
 Gauge VII. - This gauge is close to Gauge I., and (as 
already explained) has practically supplanted it. It is  
therefore satisfactory to find that it agrees with Gauge I.  
within less than 2 per cent.
 
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