Show UT AH Brie on It Physical Pea Fea Feay I turc Development Dy y J 3 n H Paul Paul 11 vlis CYCLONIC Tue ho amount ut M our raInfall his has not yet ct be beun n It le leIlh hod lily Anti e ably ubly ibis nt not G In II a Clr That or of time the Ills arIes tom tommi G tl tO ti IncItes just It sit time the Sierra Nevadas soUth Mouth of oC tIme to roil S 8 to 10 16 re In ill the thelle or of the tha II in A lle ml comma the ml n rail II Is II loss tutu tIm rue titi tIme Ilche It fly sf or thil United States At II in three time tho mo t ever tel fell II Iii heavy precIpitation ore oel tIme tho 10 wih with Ic pencils domIng which time the continued cold fro I time the nell acts upon time the wInds that cIrculate about rat thu Iho r clono or storm ti fails THE CANYON CANYO rImo rho moot delightful ot of our In Is time thu slimmer Those who Ivo live II in or far car flun float the lower cud II Pt any gorge mire nrc familiar wih with this II tilt which Is II Iii nees n anti n fO almost regular lIt me ot of the tho year ell lS its II IC Lie tIme tho land and sea s of 11 the COl coasts ts rho wind blowN up UI Ii the I canyon lit In and down the tho 1101 tl lt at night Tho rho lind I tho velocIty ot of this timis breeze t 1 lil vary wih local anti I it itIs II Is hy larger lnell wind I Ihl rums breeZe e OCCUrS thought though often hut but butI I 01 on time of ni all the tho larger mountains The transition tar for thu night II to the tho or of ortho tIm tho da day is 18 In tho but h Ia Ilow slow In time the valleys and the Iho ot of the breeze varies 1 a good eal with tIme the local Tue ho wind from the tho natural Slope of tIm hJ surface which clr car carmie riel mie the Iho cold aIr ot of luch Ile like n a dOn Illo into the thc warmer valley Thu eln can yonH owing to 10 theIr greater their forest areas the proxImIty ot of places od and time tho shorten time during they direct sUI tire are cooler than the alleys lt at so that the wind front time tho cooler lal rJ o th the broader valleys or lower dowl al cud the tho lay tnt ii luch this wInd throughout most of oC the Iho day dayTime Time Tho now ot of time the up tIme tho ellon canyon or tilde Is nol mid erI the tho or of a without u usa o u I If however we Imagine thc I its In one column o river I time tho thoa th the valley a 01 mind In column upon I It I Is apparent that the tat lat I tim shorter by time Iho amount of the tho ot of tho above the valley As time tho nil ale next to 10 the earth b heated llo time air ah ox x the tho expansion being proportIon mite I Ic their r respectIve lengths the air nearest to the Iho earth This b by sonic lt of the lower all air the mun of air lt at I a given lovi Over oer the Iho valey valley t to be hemler gen than lt itt lie this base or of the tho at the tho same samo level on fl hillside The Th column titer Ier time the valley lcy therefore to 10 time Ildo sIde and en causes uses 1 a breeze Ut tile or 01 up time tho canyon generally noon or afternoon dying I IY IS as the limo sinking nears the tho western horizon I It I is this which affects most mos favorably the Hummer or of time the semiarid vanes valleys At the writers home Ju just t withIn the of tle CIty Creel Creek thIs blows 11 every summer night and seems to bring time the his lulls cooled oled hy by tIme tho fresh tresh of ozone ald amid vigor sor It breathing I mm outdoor I mm covet cd This cool fragrant wInd vInd orel time the balsam odors ot of pine and cedar leml ls one aims of the days of at Ind and early I It SIghs html but Is cheerful and Invigorating and amid p puts ts Into hun I a pam pel pelIon Ion son the of oC for or ln an another other dl day ReclIning Oil the earth ot of mime Iho slope lopo Iho words of II an olden Iulia Dime to Ilee sleep III am nt at In olle other anti antiOno Ono again as ot f oll old hen time tho tine breeze blows Mid Ic time the quakIng asp groves Id 10 lIe gleams and th the columbine glows Near time the cool stream by THE Cyc Cyclone ono Is Ia the word now used to descrIbe our greater IHs In a a cyclonic storm six Ix conditIons are arc 1 flero Is I IL central region of nt low light air duo duo to 10 warmth and mimic ture tire arund which the I is moving In great cures curvos from rIght to ler counterclockwise 2 There Ther Is a great cloud murea from whIch rain multi or Inow emmett raUl falls 3 There hero are arc winds successive I 1 thol thou and ida lS as time tho It atOm rm arises os in Ind mOVeS on eastward 4 The amass a or air Mout lh central A Y AU JI amen uren ot of tow low nut ot extend to tn n a vel very great h th the 1 earth hut bUI ls Its l 11 b r or C I I el G or Of this storm tIme the blow tIle tho southwest front th tie center from th limo east imd Ht o of como troll trout hc north amid on thu tho vest wesl Ilde side ot of time the northwest Il II The Tho or area ot of low NI If lt Itt time matO GOO 1100 butt but mIl of miles pel iam II to the l or er II mis It begins ill time Iho vicinity ot of i tOi Ti The stormi tais falls to 10 tim It i Great h to time the Cult caine tl tim l 11 ill tIme littler COIO case I It the Ol areat ut lakes 01 omi ls Its W way tu to time tho Atlantic CYCLONIC W iN TIlE THE ILA ThoUgh the HoCky Inter copt the nearly nt at right angles yet simmee the wl westerly terlY winds uro during most ot of time the year ll thu Ihu as ascent ascent cent from tho kent rent Ia BasIn ln to the tho I lm of oC time the Is grad gradual ual Iho cooling effect due to 10 ci I not 10 so In the plateau Ie mc ns as It otherwIse he be The Tho flow ot of warm lt rom the Pacific Is but little retarded l are In out on tho HII 1111 on om the tho farther cast Cold ot of originate In lm reg region o Mon Momi lali tuna and amid travel rime cyclone or storm I is warmest at the southwest quadrant or 01 front of starIn and c on the circle or rear or nr it Is the elt I coldest on mm the tho west cs side when tIme the trough of low how extendS due amid n south JI lii these theo tOI toni B 13 on Ih the s 31 south l on omm the 49 Ind and northeast 26 Time Jho rain areas attending time the cyclone are aro very rr guIDI Wih us mis southeast precede tho th storm These the tho theaIr aIr und amid I It and before the limo cold aIr ah tie time Pacific Th sky over overcast cast minor or falls thon the winds In roma 0 mi from time the Ind and I a cold WIo itte follows 1 IVY nil air amid cell clear kl with I a wInd to iii 1 time the cyclone hence called the tho now pr pro vail nt Cy Cyclone lono anti together last about days weather l alU cloudy kie and aIr tel tol lowed ti b by rain or snow weather hat baa clear skies lIght winds amid fair skies The halt bait ot of tIme Iho Utah Arona Now Mexico and amid souther alc are less fru visited by cyclonic than time tho r and the wInds 1 front from the Pacific bring Itlo little The fhe fail lit In thereat ot of the I not 10 so pro on the tho laoc coast nul amid ov over r the plateau Iteal t ns I it I Iii In dl dIstrIcts east ot of the Iho Rocky To The In front Is heated tw the tho ot of a a cyclone II iy wurl from the tho south amid by local cloudiness which prevents tIme tho heat trOn the II vinter nn an or period ot of cold clear elcar weather wi will oren often statIonary for tor ocr 1 tIu plateau passing east ot of the tho This hll II is by easterly winds Is Its cause has not yet yot been explained PLATEAU S OF The fossil beds or of and tnt In Inn n It degree ot of Utah tend I to to that tim the great climatic changes grel whIch time Iho earth hUM has subject In lel ages been INon very vcr marked II In Inthe region Skeletons o or of the tho plateau rellon r that her lier when thu th clImate yams nl much cooler ali much more moIst and or of others that were here when time the WI ivins Ilch mud warmer than I It now Is are the tho mOlt most strikIng evIdences to the title readier of the clImatic changes lie But Dut oilier indications mort general It icS strIking are not difficult to unit unitt t II is that repeated hanes In hi I have Imae occurred In the Rocky nock areas Ind and that time the records left lett bY the former ot of the tho Great flash lio time greatest hoty lody of l o In establIshing thIs fact ocl Gilbert has haR shon that tero there were waro five tho Gibert stages In the ot of Like Luke Bonneville The Tho first was wac along a per le toil ot of drier and of oC lo low water which alluvIal comics now 1010 more or 1 less h l Inter hater hIke deposits maro bui buIlt along timo tho base bases Qt of time tho tile lake rite fhe second WI was a period or of Ild or of high which dId not result In rime third period Wil omme of dryIng imp l lit hum ho lakes lake ater after Ul thin tho ot of the rivers were not lado lit In wlter ater on the tho lund land or of the dry There WIS was a perl pen 11 01 oil lit hi which time tho water ruse rose 11 tilt I it over overflowed owed ut at th the corner of Limo tho The Thc lake was waR 8 feet above the tho pres Ont ont ot of time tho and 1 a 18 fett cH lute nto the tho river 11 ln O I 1 I cliEnt times tiny 1 11 Ii r ur it time 1 ii IRk If IA od ur of high 11 with th the lit t tIme tho ut of g Kuila ocl In n 1 lImO hy by ii a ad r dr In tnt II ot of n t tu oral n 1 time ho ol la lake 10 hl TImi ho fl In Inn of time ot of the hake Inko fu thUs face hmo rapid time SmIl ur hOl riM rit Iso In tl time or of ii fir C shi ate Is Borne 3 4 i In I WI hail mies wide IU l i |