108 THE ROYAL SOCIETY OF CANADA 






Locality. Altitude Latitude N. | Longitude W. 
Feet. Deg. Min. | Deg. Min. 
Barkerville BC ster pene sa ee 4,180 Bey 121085 
Charlottetown, PIE TURN ep 38 46 14 63 10 
GChAYOQMOEN AIN CRE EEE 40 49 11 125 47 
Dawson NIET AN ior coo 1,052 64 4 139 20 
Bdmontonwaltacasesmess ce ane oe ae 2,158 58) Ss 115260 
Fort Vermilion: MEANS 58027 1162063 
Fredericton Noam Re ce 164 45 57 66 36 
Glacier S ER ee Ni em 4,072 Sa = 14 11722829 
Haileyiumy MONE ANRT EEE 687 47 29 192039) 
AIT AINES DRASS bos RER RARE re 88 44 39 63 36 
inetthatiolel SAS AE waa oe 1,924 50° 28 103 40 
RAMIOOpPS DIE oct. ote moo Soe ore 1,245 50 41 120 29 
Bong omits Opt LA cove 1 nel cn 42 36 80 20 
MOntreAlINOUE EE RAR PR oe ole oe 187 45 30 (BY ck) 
Ottawa ONE ce ee ose ere 286 45 26 15 42 
POneAt thins ONE ete cee ee eee 644 48 27 89 12 
OupAppellesSaskrcs rm Pr Neue. 7) ANAS) 50) 30 103 47 
Sable sand NES: scr sca de Seances 25 43 57 CONS 
SOUS IN RS tee tee AR 75 45 17 66 4 
SE JONN ENEMEM LE enr toes. a. 125 47 34 52 42 
HROrONtO ON EEE RARE te he hel sie: 379 43 40 79 24 
Hranples land Cr cnet te 680 50% 52 129 5 
Vancouver DNA Tee ae 136 49 17 125205 
NaCtOriaaV Ile: Biel ee 85 48 24 123049 
Winnipecss Vanier eee ser arene 760 49 53 LS pes | 



In the figures given below the results for only three years have, 
as a rule, been summarized. In some cases the results for only one 
or two years are given, as complete records for three years were not 
available. The figures are quoted chiefly to serve as examples of 
the method of measuring the variations found in different parts of 
Canada and are a sufficient approximation for this purpose. A 
ten-year record would give a fairly correct estimate of the climate 
of any place; for extreme departures it would probably be necessary 
to have records for a period of one hundred years. 
Most of the figures quoted below are based on the Annual Reports 
of the Meteorological Service of Canada and refer to that country 
only. No figures relating to evaporation are given in these reports, 
consequently I have had to fall back on other sources of information 
in respect to that factor. In the section dealing with Light no data 
appear to be available on sun-temperatures. | 
