Arkansas democratic banner., 1851-10-21
Direr.ifr nf Mana..

The Varsatfon os the winds $ considerable. v-f some places they are eousssag auY.nx thc wAase year. sIways blowing she sane direehoa ia osAers they caawge at eeFss;s pero8s and observe certain and regular laws. h tAe open sea, between the tropics. and fs ssne degrees beyoad tAeqn an eass ssiy ssna continues nI the year around without \ gay considerable variation. To the north Of the | line tho wind blows towards tAe nssaA-sass. aAs so the seeth Of the laas 4 Biows towards sse soasA- ! east and that or Jess according to tse position Of the sea. This. however, only strictly husas in the opca sea fos when islands and great continents oastraes the psogress of this wiad, tiey may chanse is cousSe, and in certain places make take a north direction. In thc southern parts ef the ocean westerly wind generally prevails TAe nearer we approach the eoaSsS the more var,ahle $ the wind. and Il is sail lsoe so as ws advance farther inland
 | The constant ess; wiAi $ ehsefy caused hy the beat which the sun Communicates to cur a;Enos phese. In sae India Sea theys srs winds named ] trade winds, os moasoosS which continue to blow in the same direction from three b SIX months Of the year, and dusing similar space of tase blow ! la gae oppost.e direction. The causes operating to pfo&see iktse scarcely yet satisfactorily ex- piala@a; but < cannot be doubted that the sItera- tons Of heat and cold, the inflammation of neteofS, the condensation of vspoEz into Easa. and other similar pno'neaa. have great effect ia then pro- tazctica- TsseFe are certain seas and countries which have winds and calus peculiar to them. h Egypt and the Perxlaa Calf during the summer, q burnias w.ad. wAseA s;Fes FesPsratlon and con saiaes everything. veFl 7ssfqseasly prevails. At the Cape of Good Hope 2 eto2d is sometimes seea to form, winch she inhabitants seTIn the fatal cIoad Of ox-eye; at first t s very sna bat soon vIssbly increases, and farious tempest proceeds from Ii, which oyersets sAips, and pTeepisates them is the bottom Of the sea.
 I Uncertain and variable wIRLs, whea have no aetcrEanase dfeetloa or duration. prevail over tke
 greatest part of s.e globe; for thougA certain winds may blow mare frequently a oa@ place thaa n anoter. they do nos return a. Exet. lnssrvas. but begin and end wisAoat aay regularity, anI vary ia proportion different causes interrupt the equili- etum of the alr Heat and cosd, ran and fine weather, mountains. straits, capes, and prononto- res may coztrs6ate, n considerable degree, to impede their course and change their directions No doubt many other causes, which are uRknow D as. iagaenee tke daEeEeut nbesacatoas and sgissssoas of the aiE.
 f What $ particularly TsmarkA5le. and sally oc- CUTS n almost every place, E, that htile calm, when n a few a1meats AftsE, jsst at the break of morning, pretty brsk east wIna begins to rise at the approach of the sun, and eontinaes some time after he has Fsea. Thls undoubtedly proceeds from she ar, hea1el by the rays Of the rising ssa becoming raFeGee, sad by Iss conseqGen expansion dlspiaees the contiguous air. and then produces an eaSt wind, which ceases as the surrounding air also becomes heated. For similar reasons as east wind ought always ts pseeeds the sun a tue tornd zone. and blow muck stronger than n thIs eoan ry because the suns power here s maeA less than In the regous bordering upon the lIne. Ths wind. then, in she t5rrid gone. eonstanrsy blows from east b west. wAilst west wiad very rarely pre- vsils ia those parts.
 FFan these o5sefvatioas are learn that winds are not the e5ects Of chance, uishogt el1ksr eaaSe or aesisa h these as Is eveFlh n, eise, tae Creator alaaf=sts Als wisdom and goodness; aaa he hAs 30 arranged them, tsa: they are scasinaaily rising, and dead cam very scidona aappens. Hs rega- .aIes the motion, power and duration of tAe aai aad Psescr.5es to taen the course they ought so ,ake. Tseir veFy a4yeEsity s sf use; for WAen a ioag drought has raadg pants aad snssaas laagash ss3 4rocp, a wind pgaeee5s ffoza tAe sea esast, loaded w.ta sxAalsss5fs. w4igfz sh= HsatsSs aad gIves aew aa,ssaatsoa ia aasss@ W hen faas object
 s aeeou1pgsAei, x ssttiaseaiag sron Inc eass restores the sesenssy ssg fhe lag. aaa stngs back ina wea.a4ss. Tse E11LA wlaa brings sigag w4sa '. naassroas tnszaa Parssezss, aaa 2anaes the z2- ;anaa4l ar from ils noxioas vapor. LAslIss to the sharp sessa wla4 seeses1s the soa'h wind. and eos.ng fEsEa tse southern reigouz, E aliases a gratefAi warmth through iae 1lx< Thus sb@se soa. unG4l variations of the wlnaS tend ss preserve healEA asd srrtslslY a gae eastA.
 Y JxNST LsSD n 0FEzA.--Tae New York 2 haes states wtat he eaIs .'Feiiahle authos1ty, tka; Jsaay Lin wls setsra b skzt city "a saort Gsae, and ui anner al (aste T1arsen d. sarlx ln Iar,aar,r