Show u jH t tt t L I i CLIMATE Aw Away back In 1776 1170 Father Vales d de white man manto manto to set t toot foot on Utah all wrote rote In his hla diary referring to Utah Uth here lIere the climate Is so 10 delicious dUclo tb the air so 10 balmy that It 1 II a pleasure leure to breathe by b day and nd b by night Since that da day hundreds hundred ot of thou thousands sands unda have felt the urns m pleasure In breathing the pure air tr ot of that the rood good padre a century and a quarter ago when hen II he clued but a tw few mil miles from the lit site of salt lAke City Ctt SUITS ALL CLASSES CLANE Willie While the State Itte presents the wonder tut tul variety rIty ot of climate found nowhere IM else perhaps ll oU outside of California the condition In Salt Lake seem to cult all 11 el classes Within the region are ure min mingled Bled the tr fresh b breezes from the great lak lake and nd soft ott cool air from canyon canon and nd lt mountain peak tk Th The hen he here are re no 10 greater than good health and or dinar activity require and with its Ita changes the climate Itt et Salt Lake CIt City le a perpetual 1 tonic DISTINCTION WITH A DIF r Then Thill a Is a rut t difference between the effects ot of Ii a temperature ot of degrees In Nw New York or Chicago and nd Salt LakeIn lAke lAkeIn In those eastern tern clues phi air Ir tern tempera tra tore tur or the temperature actually felt elt corresponds to that ot of the ther thermometer In Utah during the summer months month tb the air Ir or sensible temperature may he bt u Ii or 10 q degrees lower than that shown own b by the thermometer A QUESTION OI OF One who has been greatly struck with this Ulia writ writes In explanation It le a evaporation Evaporation oration a le a cooling and nd It is III going golar on from the surface of the body Th The moisture that I per perspired b by the lady body a le evaporated with greater or lees rapidity It la Ia greater when hen the atmosphere he In addition to being worn I also Ito dry I Is alto also accelerated by br th the wind and Ad In a windy d day the lea evaporation po ration le greater and then thre is a cones quent at greater of tb the surface of the body The use of a tn fan In an ease Illustrates tha this fact t t Th The action ot of the tn fan no mutter maUer how vigorously ap applied plied piled and nd In hi what numbers numbe will not re reduce duce dUle the temperature lit ut the auditorium It a 8 in aea the tare tem temperature t f th the N 11 r but tit It Ill the tho t m rf t the Ih peran using It by I accelerating the evaporation ot of mote molt turf ture from the skin It bas been found Ut that Ue the tempera 1 ture tun ot of Ute the wet t bulb ear responds to the temperature ot of persons perean standing In the shade ot of tree and exposed to a natural brue of at t least six mil miles an n hour So 80 that the wet t bulb temperature which It is the temperature of evaporation hu has come eom to be known u the sensible temperature and the reo re recording cording ot of this temperature alongside of the air tm temperature has baa now became a part ot of th the work ork ot of the States Weather Buu observers This Thle departure from the usual custom ot of tAkIng observations should be elated by the ot of the ark and States EAST AND WET It I Is shown In this way ay that the un Hn sible Ible tern temperature ot of Bait Lake Cit City responds bout about that ot of toba Sault Ste Marie Mrie and nd Halifax I during the Ule months ot of July and nd August Augut Nw New York City h has a sensible tm tem temperature I 10 degrees higher than salt Lake lak City or Se 16 degrees At the earns m j time th the maximum air Ir temperature at t I New York I is bout about band at t Sail It lAke City U So that we hue have the phnom phenomenon Ii non nen ot of a higher air Ir temperature at Salt Lake Ike City than at t N New York but a lower lowr temperature Salt hit Lake City sensible temperature for Jul Juland July I and August I is about II 01 dg degrees or a J reduction ot of 10 q degrees due to anon atlon Chicago and Bolton ha have uh each a sensible temperature ot of bout about p a de greo tr San kl l lIco isco bout about the came San Ian Francisco oo h has a humid atmosphere 4 t Ilk like Chicago and hence It its I sensible I 1 temperature is II aiso higher t tl This I is all 11 VIr very w to the t t I arid region It It Is seen Hen that tbt though the theair t tair air temperature In our dry climate is II considerably b higher than that t ot of the I t r humId Stat States the sensible temperature the temperature actually felt by the t human hod body I is so 10 much lower lor In the theand arid and region that It my may be pleasant In the mountain valleys valley and Ull At Atthe atthe the once m time decidedly oppressive t toften often otten tally fatally so 10 In the humid I It Il will therefore be that j although the readings of oC the there ther my may be the urn same at sea level leveland el eland and In the altitudes on tb the urns m dy day the sensible temperature of the two J places placa will he be widely different |