Show WI ICH WI The Tb opinion hu ha been et ax P that tb the winter sr growing less Ifill severe 1 than the they lied to be Old people seer remember lle toNg long winters sad of t their childhood perhaps that In the ages of af We life bath Mek and am wi winters seemed mid than they do to I Iii Ih Than uman hulle ever tiny da Is ll spent it In loma bUllY occupation nor nur that the snowdrift of recollection may Inky not hac hv bt bean n quite as 11 lar large a as pictured by the at that time Seather bureau statIstics are an n Invention of comparatively times timet but bul so 0 tr tar as they go 0 they do da donot not the supposition that the earths rth temperature is IK undergoing any perceptible pe ehI Winters and sum lum met mets are very rr much like they have bean wIthin the rech or of observation liS tot tory tells ot of unusually severe evere winters during which armies on ice Ie over Ih the straits that separate and In which wolves wole driven from Crom the tb mountains b by snow and nd frost the settled regions glons In alarming num bars but It allO aio tells or of mild winters and of a series rl of at such and the bURy I is that though we my may oo occasion occasionally ulon ally Uy he have beautiful Christmas weather such uch as al that enjoyed here lie for Cor ft en several years In succession lon we mr May In all 11 probability In the future hAve long and tHI severe V winters such as a have hem experienced In thu pat past The rha Milwaukee WI says Noah Webster I Is on one of the tint to inVestIgate this HII subject The Th he at is II quoted a as follow Trout From a careful comparison ot of MoW It appears that the weather weRther In modern winters Is I more Inore Inconstant than when the tho earth was covered with wood at the settlement ot of In thu country that the th warm weather or of autumn extends further Into winter Inter months and the cold rold weather ut of winter Inter and bd spring encroaches upon UllOn the cuin um mr men that the wind being more variable snow now Is Ie I lest permanent and the same aRm remark may b be applicable to ice Ic of oC th it rivers riveN These Thee effects seem Rem to result necessarily from the grunter quantity of heat accumulated In suni lum lummer tier mer since Inee Ih the ground has been cleared ot f wood and exposed to the of at th lIun and to the greater reater depth of frost frostIn In 11 the earth arth In winter by the exposure ot t It Its uncovered surface to the cold eold at But we lle can hardly infer InCer from the facts that have yet t bun col collected that t there Is Ie In modern In an diminution ot of the aggregate ot of ook In on either con oon mint |