Eldh irertfcal imerspaoe TEpresents one flegreeTlhrenheii, and the fractional parts of a degree are indinateil as exactly as possible hi die pilotfing q£ the curves- Each fiflh 

 ! isreprestaitEa bya. slighfly heaviei; line., The transverse iuterspaces inclosed by the heavier lines represent periods of ton 3ays each, as indicated 1^. the flates on the 

 leftiand Hde-o'f the -plate.--'' Ttie Tfghfer transversra' IhieS^'Intenneaiale IretweEJi 6x bea:\^ier onea are'ttaEmded tonrejirBSEmifhe mean of. each ten days^ and flia curves erf tEinjEP» 

 Biate-Hre i3oned w^TfeSirenEBtatlKse Ihiesk The lefthandiTerfical division Is devottfl to thta flfr temjjerataresfbr'rS8r,\r882 anxl- tSSjjtoftflMdle dlvldim" to fhs sml^ 

 iKa/ai tEmparamres fof the same yesrsi thus pemiMiSg- of a campsfisaa of the two: ainJ 'tha/ighBhanS division ta fho vraten temperamres for 1884 ami 1885; 



