The New York Herald Newspaper, August 6, 1871, Page 6

4 STORM SCIENCE, |8s%=2% extending over only @ lew square mu bat whten still ten to avey the [ares lawa given the above table, ‘This 1 known as Bays Ral- tos Law of te Winds, from the name of the celebra- ted MELCOTOLO, Lat, who has long been the able director or theMereorologicalob servatory at Utrecht. Holland. ‘The conse- guent rule which Protossor Ballot med for prognos- tieating the cow of the wind—whicn has been rigidly found in experteauce t hold good ninety times in ahundred—is tis;— “Stand with your Jett hand toward ihe place Waere the ba- rometrical reading is lowest, And your right hand toward that where itte hich- ors and 708 - at pa peas . pave your back to The Storm Signal Bureaa at Washingtou bas just | ee uirection of the Pubhshed some of the resuits of its tirsi year's ob } wind which will servations, ‘This Issue, containing much that is | blow during the cow, though bref and concise, w a rick and invaine | 8." ccion of tne able addition to meteorology, Move than thirty | earth's suriace has & Interesting Description of ‘the Working of the Meteorological Burcan. Winds, Conds, Fogs, Rain, Snow, Hail, Tornadoes and Cyclones. The “Probabilities of the Weather’—The Pe- tuliarit es of American Climate. What Motecrology Has Done and Wiat it tesks to Accomplish. years ago Sir David Brewster, the renowned Eng: | eteuter infuence " wha (pon strong than lish philosopher, discussing te philosophy of | pon teebie winds, storms in the H2/hurg Review, graveiy prophesied | aud thus does more that if ence * G to retard the tangen- wt If sclence mnot bind over the disturoing tial than the centr. ciements to hoep the peace 1b may at least organize petal menon of the an eftoiens police te discover their ambush and | air iu the neighbor- Watch their movements.” Happily for oar day—a TY Bag ti aay of physi Wonders and commeions—thts | soquentiy im severe prophecy hus been veriied to an astomshing degree, | storms ou hend (he Happily, we sey; for, whea the paroxyrms of heat Wind 18 directed more nearly toward SUNDAY, AUGUST 6, 1871,—TRIPLE SHEsr, MAP. general way. In mak. In use of the weather the purpows of pre: dicuon for eon ‘of the count ic} ent from that in whieh we are atthe Moment residing, we ire, of course, cut of from the use of many local rules whic Wouid influence our judgment were we ab the time there preseut and able to know by personas Observauon all te Minuto of the almospherie condi. ti di deprived of 40°} Cuese tin portunt helps meme] wait Porced to rely ex clusively upon the bare numerical data otered by the butle- Un, we must call to our aid all euch kuowiledge as olcred by the preceaing brief statement of tie pro- =={niinent nieteorologi+ col principles, such CORINNERZC) BBG ECKFORD3 EXTINGUIGHED. A Onr-Sidet Gam» ou the Usien Grounds Yeso terday—Defeat of the Williamsburg Pets Score 13 to 1. All who saw the game on Friday afternoon be tween the Boston Ked Stockings and the Kekfords wore confident the Brooklyn boys would play an equally good game the next aay (yesterday); but they were greatly mistaken. When the two nines came together yesterday afternoon the bettlag was only silgitly in favor of the Boatons, and there was every indication that the game would be a close and exciting one, Having lost the toss the Reds went to the bat, and before retiring Wey scored a ran, which they got on a very bad overthrow by Shelly ‘to first base, The Kekfords retired from this inning, and, 1 fact, from the next seven, without scoring at all, wittle the Bostons, through errors Of Maviin, Swandell, Holdsworth and Hicks, soored three more rans in the fourth inning. In the eighth inning the Eckiords managed, through tn voriest Seratch, to get in tue single run which adorns tuetr seore, While the Jed Stockings in the ninth inning placed seven more runs to thetr account, and tov tb hey have to thank Hicks, Holdsworts and local taws 2s we may Know to hoid good for the disiriets 1 qaestion, and sucn more wenerat Laws ad have beem deduced by the study of emi- hent Mewworolozists. 30" A number of these = tetters wit be found in_the appendix. The loval laws re- a LC} ea ferred to are now PAN i 65 3019 6 being collecied by <0 us, and wil even- > tually be published insuch a mi bution of ihe prin- Cipal masses of cirrus { wIDMIe | and cold, the demons of the tempest, and the électric | the central area of and 6 ro-atratg Area combine (nd marshal themselves and march | the disturbance than clonds, combined 7 ving beveatl the in oceanic storms. with the stiibution forth with dosolating fury, driving iad a aay Thus in tornadoes = Nerd AS over or whirting into te air the floating and te Mxed | the inward ana vp- pay PHY, a iy Which tte tempera. divelllugs ©! moa und shivering che proud. { ward motions pre- ALE CEM los no Low: frow WaTH oe : a fure “and breseare est fabrica of his power, he trembles and becomes | Comnate over the Mon tangential. Prec D, CAT SIGNAL 7 ‘ a a oe ;, y NQTON. with abnormatrapid- the verisst siave of terrors wat ne ald net foresee, | weal, treeless WAR DEPARTMENT WEATHER MAP (SIGNAL SERVIOE), UNITRD STATES ARMY, SATURDAY, APRIL 8, A. M., WASHINGTON, Ty Wil een ae At was for imts reason thacso long ago the barome- | Water is greater that, The Numerals denole—1si-—The State of the Thermometer; 2d—That of the Barometer; and 8d—The Force of the Wind, oares He least for tne ter became the (aitaiui fried and monttor af the | over daud sy we find Tnimediate ssreging seaman and Murnt hin by its silent warming to | above meearib’s surface much greater than lower | annually occurs of cloads im the higher strata mov- ; Gulf there generally prevail in the higher regions ; Into wh Mie storm Will pass, and oecastonaily dor basile With the ele- reef his topsaits and prepay. ments. es per our, Lek furisce rarely So necessary are premonitions of atsospherte dis- | doubdess tis ha Vurbances io tue human family Mat, frem carly p riods of Ristory, they have been diligentiy studied. exceed Balloon voyages saow occasional velocities of Lhe highest gates on the eartn’s does and Momentary Kusts, ke. Lwace tae velocity of these observed on the sur.ace, even give # premonitio: portions, eac ‘Tue mere viol norliwest, * ofits breakrig up mio twe ording Lo the season rawn ta aimerent directions. st wiuds generally folow in the rng frou ny Other than a westerly point. During three ye sot very careful registry directed to tins | of the atmosphere soutiwe norih, or northeass winds a ehty-ve iites, though | particular port but Urree instances ef a contrary | and the distribution of abmnospheric pressure, been exceeded in certain torna- | direction Were observed, and these were during the | these ave those that provably deu rear aud on the south side of the advancing area of "The curreats only revalence of evtensive aud disastoous storms ou | ral movement of storms, lowest pressure ; those that precede the progress 0 a few hundred tect above the earth Nave frequently he Atlantic coas! stratum of air is comparatively quic. tint area may offen be more dangerous, however, TUL PROGRESS OF STORMS. didferent polats moving simultaneously im oppo. because of the accompanving fog, &e, ‘the Tatier wip ded Dv the cirrus and Unreat- Tits cerbam on tho coasts of the Meaiter au |] as sown by observaldon OL the velocity of passing We have hus tar considered ourselvesas studying | direotions, while overhead the whole “body of air is | Ia vinds are brece Adriatic Seas, eve slassic aes, stenal and | cloud shadows, a few Isoluted charts of the weather. But in com- | moving onward with a iar more Unxoria direction | CMe storm clouds; the rai that aecompantes or se wp beta a i ae he ir , ‘ . i Heavy gales (/. &., velocities of forty miles and up- paring we tadications of 4 series of these We are at | and velocity. | followa tnese generally ab and Gus gives wara- storm warnings were issned both to ma ward) ud me areas Wilhin which | once Strack with the regularity with which the | The westivard morton of thetower winds ts in onr | tng of the strong o u ada. ad, tu one form or anotlie: The is near to each otner and die | areas of ae nd cioar weather move over the | country, and especially ia tie antumn, winter a ‘ ert in ty be progression of Wwe area of cloud os bee ecognis scoas: Way sv soon as these lines are seen io separate. | surface. The ves of bigh and Jow pressure, the | sprig months, to be cousidered as Ul (cof a | and rai varies irom fiween to sixty mules im an mies been a recognized necessity for | Bray sy coou aS Tieut Dut very local storms the | areas of nigh aud low temperature, &¢., ace in'con- | tart inay orlgina:e on the tue | hocr, the actual velociy varyiag With te ladueaee au peopl statiuns will genorally fai to give more than @ | tinual motion generally to ty stward, except for | inface Of the ground, but tre ty ociet | Ol moisture, as ext Md IM dt Dre vious section. The honor oi applying the grand discovery of the | general indication of the disturbance, aud hence | the regions south of thirty d de, where | lower stratum of elonds ic is this dis. | ue average velocity of the curreuis, whica deter. ectric te ob to sigan ts 0 aa4 cannot be EXpecied of the Suzaal Bureau to give ne Movement 18 Westward L they may | the surface winds from the | mine general cerect, the progress of the Soon eae ple ects Ui Meuonett yk pret Meng Ore probabilities of such local dis- | change in the detalls, but their 1 are always taud soutueast which blow nearly toward | Nucleus of the storm, varies trom twenty to torty reserved, lt ‘or the great American meteors | Torpauces. indentifiable in each successive chart nati they nave a centre, while wes! $ prevail far | miles hourly, and rai wehes tne bigher limit, Mr. Win. O. Redfeia, of New York. ‘This On TEMPERATCRE. ‘a passed 01 3 1 other phenomena have 5: | and also on the oppo: nie, On the ease qane snenges aes ow tarice datly reported st otou! fenttst—the New: Although the average temperature ts higher at the | 2€ rapidity of the easterly movement | side of a winter storm, aud got far rom is centre, ‘out Mune ashtugion drequentiy afford indica- modest bal, Hrotound sclenlse—wie “Newton: \00)|,. Coo catony then ar fie. norern ones; And”) asionally amount to Airy ilies per hour, | these casterly surtace Wiads may extend for two | Mons of the movement of the great | equatoe storm physi¢s—in bis colepraced paper apoa Nur | higher in the day than at night time, yet tue Weatner | but probably averages less than thirty miles, | miles upward above the earth, but ata greater dis- currents, and hence aq preinont- ricanes, p 1 in the early part of the y Liap Wiil disclose Wnumerable depariares from thts With but very lew cxeeptions the storma that | tax advance of the central region they H of & ef a the generai character of the i egimthe | have been traced to any distance trom Anril to Oc: Had more and more super H ut froqueney f ow the law nal of vo urgne sustrate the feasibility of using ihe tele. ning and announcing the approach the #7 1si6 Sctenca on Sept and } in sure or uy marily, inde for agd di graph for usc aud force of storms, closing hts paper with ihese stern ‘oO space; bul, in addition to this, the heat | terior of the contine: *hese great areas of high | in the trade-wind regions the easterly snrface | Me optical phenomena of t ithe Ar ie ports of the United States | netu latent np Gie Vapor that floats mm the air 18 at | pressure are, howe ever varying in Outline and | winds are the permanent and nor. ndition ef | veniuaily to arrive ai the approach of: le, when the storm 13 yet on the | times Loeraved by the condensation of the vapor | position, thus g) se tO the Changés ia tue | the atmosphere, ually so are the southwest over r regio ne aprons y . e * | ince fog, rala ond snow, ana then it becomes sensi- | storm patas. | winds that prev we. The liae that divides the | are propag Gull of Me ef im the Soaihern or Wesier bie to ine thermometer. Daring the day & motst ‘{hore 18 a very noticeable tendency of aroas of low | tromical from tempe: eteorolovical Isr May bo nade Avown by sof the ele ato phere will become warmer (han one thatis dry, | Pressure to move north Ward more randy | | changes: af . ' curing the mahe the radiation of heat through | we & result aparently in accordance w months, so th at this time tho region | ymuiag, fort graph, whe jy ly wali Soon exten AUC CLUS SR ee “ ‘ eee omen tak rahe cad Sea. vere will be less than that tarough | theoretical manence of the daily roration o1 the | south of Lake snpeno nerally covered by a r ‘ore the wind accu co the & this will euable tur my cloudy or hazy Weatuver tae redte UPPER ATMOSPHERIC CURRENTS. | Westerly current high above tae geutle current from mids (oO OLoW or Hie ram fo fall: thus they mey he avold exposing his Vessel to a invions gale alfver | 3 nost Wholly cut off, so tigt & very Uniform The general progress of atmo: changes, as | the southeas' | nit to cnable us to feel the pulse ef the atmos. aie he teleg " exten’ | temperature prevat other haud stuicient | above a!uded to, Seis to depend upon t he motion of | AMERICAN STORMS AND CYCLONES | Hi mast not be forgotten that the | deaving her port.” ‘The telograpa did soon extent | WD or cornea ( ry becomes latent) in che pro- | theupper stratum of air, Over tie country north of we The storms 24 States are or four | “le which passes between the first appeara from Maine fo Mississipm, and, m ihe rear 1843 | cess of evaporation to materially reduce the tem~ change of weather and its ac tauuary 6), Professor Henry, borrowing the sugges- | p eof the air; 80 rg hd silting nae me oe eee ee _ Nee . “ AGRE ao |} coulis. C1 bara) SSUrC, S| ) ur tO. succeed.a Yon of Afr. Keailou, made a year and & Natt belore, | AVON ine the eapachty of tie alt for MOWLUEE, than when The opposite chang ngressional attention and provision. | serves io stmuiate evaporation and temporarily ace, Hf the barometer rises steadily ory of this NEW sciences, It nee the remperatures nean height wile the weather ge ‘au, tne lower strata of air recetve heat from the alr becomes «rier, nortwesterly, pi the volume now ediciatly | issued by the Pur contalus te gon. re on the earti’s surt iS ow may y be expected. Un the eralization that meletfe ogists, im carrying out change. Inthe normal rary, if t Srvemaninn alization “ro Sy rryimg ow § warmer and t mes danrner, Redfeld's saggestion, Rive found tt sate to lay | aown, } abnormat c nid @speciady so Lf any great aigerenc: ended cloudia The temperature of the lower i, upon the amount of h down upon tne earch by the saa, and od by (ae wit, as the tt is generally the © rais that pass dire is by mereasing te mown! ¢ Such balou observauous as And specrly by the study of the torm Mokons, height’ and velocity of the southwest and northwest sides of a storm a westerly winds which blow may be rogardec upper curcent of alt extending down to the suriace, Dut Weakened by the retarding © friction. ex! tober are found to move abont the tropical area of hisa barometer in the direction corresponding to the movement of tae bands of & watch, and those traced durimg the wiater months move tn the same Girection abont the ares of bign barometer in the in- u an be a and by arth radiates its heat f Cancer) norehward during the | ate back to th: hortueasterly winds, OF less wind, less emperature above otiing below, ‘The equence td rain may ly looked Jor Le ui the 3 otne remons nigh 2 general principica, Scelly, €ach of whom committed unpardonable errors. he following {5 the score;— BOSTON, Eokronp, RABT. PA, Be Players, RAVB.! ry 1 Nelson, c. f,. 0 0 Chapman tf. 0 1 Hicks, ¢° .. 0 swith, aa elly, 3d b ney, I. t wandell, 2db .Wrightyns. 3 Raraes, Ub. 1 Bir isall, vf. 0 MeVey, H.Wright Gould, ist b- Schatier, Sd. et le ito Sl meena eee comoseenet emma souencwem’ earn uma’ ‘Totals. Cube. Boston. Gokford Sh cm msecese: z Ze! pounce 9h. ta oot oh, 0 a8 Ga. Dh, Gth. Teh, BA. ee ee o 09 0 fb INNING, oF, = ot Po! 1» th, Th, Bir. Brick 0 3 a z. Ath. 0 6 o mpire—d. Wildoy, of the Mutual ‘Time of gamo--One hour and forty minutes, 0 Ci) h Cad. C Wes ae Tae Athictics of Philadelphia « of Washington. PHILADELPMIA, Aagust 5, 1871. Viiteen nundred persons assembled to-day te witness (he game of base ball between the Olympica of Washington and the Atliteu The Olympics were short of Allison und Waterman, aid in order not to disappomt the people Halbach and Pastalt yolanterred to fll the vaca 3. {b proved a one- sid game, ‘Toe Alalelics scored 16, only two of which were earned; the Olymoiws scored one om each ef the first and eighth aud wound up wun three on the ninth, ‘The following is the se 1 Ou it, 2h Uh. Athlet sae aa 3 OYympicc id 0 8 8 8 8 LACROSSE, The Wild Indian Game Alive and Flouvishe ing=The Match Played Yesterday Betyreca clud, of Terente, Ont, and the Knickerbocker Club, ot New York== The Sublects of Victorian torigus Again. The wid Indian game of Lacrosse bids fair to establish its claim as an exetting and enticing sport pre-emmently. There are two excellent Lacrosse cluds ia this city and vicinity, and the devouon of the members to their favorite game borders on the enthustasttc. These are the Knickerbocker and the Manhattan cluys, Last year the Knickeroockers Went down to Toronto to play the Toronto Clab and got fairly beaten, the Torontonians winning three aud the Knickeroockers two out of the five games, AN INVITATION was then extended by the Knickerbockers to their athietle opponents to come on to this City this year and try conclusions once more in the explosive and uarul, Mmosphere of Gotham. The Toronto gentle- Men Came ou here last week, 294 the contest cama ol yesterday afternoon m the Capitoline grounds, Brookiyn. ‘The following were the parues whe igared in the game :— KNICKERBOCKERS, Meld Captain—John Rroen, who did not piay, Mry L. x In his place as facer, al-R. W. Hopaiis. int—F. J. Taylor, Marhattan Lacrosse Club. ver Point—W, Harper, eter, James Foster, the Larressr sheppard. ham. Leit Home. t Mome—Kdward Ciut. nm . Field Captain and Facer-.f. Haghea, METEOROLUGICAL RETO D WEATHRE Wars. cf the eleva woal-—H, Alexand 4 papi spa Lepr abov he condensation of 18 Mos , Correspotd to tae various | Goal—H Alexani By a comomavion of telegrapuic cirenits, as oar | Bove AP cicn the expenmon of oe athe - readers Know, three times every day tustrumental | vhe undue heat tas generated mse upper ¢ s warmer while the barome- |p ieideps_ vbservations of ihe Weather are taken syuchronousiy | Straut hated down to the earth ag well as : vache pe i] 4 4. Beatty, ¢ at aeventy select points In the United States, and | ON! inte at: ent Mibiatian’ chat Wit other band, the weathers yy reece tag transmitied by telegraph weather vuiletia, | show thal tt ture varies much less over colder Wi wmd Is south pA gr gginty te} 33 which is pablisic u any prouti | yr QISEPICS; Mat tt Varies 1ess barometer tow, and then we may look for a a . . | ed regious; that itis warmer sudden sqitail, or perhaps a storm from tae no: t S * y a hence ta tts cou » ‘Phe first t tone to iow or mgh pressure Most striking exceptions to te | Of & five agreed pon Was Wor In two and a halt ascertain the atmospherke changes Likely to occur Is | ner carmen in ad= ~d by Adatirat Pirzroy Tinities by the Teroutonians, the ball Naviag been ta ; ui noftheast sent ytog through te goat’ by RK. B. Mateuell, ieft 1AUOD Con taine ue bulletin or, What js inore eounomical, to { tushed at cost by the Signal | nsag faice. Thus the inquirer Was 3 grapiuc or pie. | early in tial represents iion Oi tne greal aerial o as itis | fernd to be onthe given day. Toe S charts are | tins as on trausine paper, and it is posaibie to see | Vapor di ahrongh several sheets, and thus more readily com- | Srystals whenest pare successive PR f the weather. Tue record | sy ts iv with the for cach siation bemg entered on the chart init © cubic £90 ppropriate piace (the wind and weather So Irausfer tue ink d+ a common map die blank charts ine m ves, WH hold 4. sailed DY arToWs aud black oF White circles), wh is at ‘ is Wolk Of Jat a tow mulautes, we are fealy io | UES picstte of the eit, there Will resblt a de~ Aechange in this direction ts cavied . eer et tee anes ate vos! ta portion o: ihe water, and that either Thus an east wind shits to west throngn Sei Sci RDOR Cie ans Gh qi | Mithe form of jog, dew, rai, frst, cr snow and southeast, south iud southwest, snd a west epi! marine ahaa ps vik | nai. Ou the otter hand, tf We tucrease the tem- Wind shifts to ust through. north: srars DoasiDIe to waen | Demitune or she pressure, te ait becomes capa- amt nortiesste 1 tte wind sh hose potuts w mnevet Sie cent? | ble of holding a larger ‘quantly ot vapor aud east’ the clinnges call bine: anaene If from two gpoinis there are reporte ri staration by 100 per ‘cent and seldom accurs vuless When the Weusher 1$ une sen * inem, S ajare ae 1 ago s by zero, We indicate ol our souled. press A dha khe barotene of | map at € moisture of the wit al ihe Uuite- eoaah are, Bins) Of. the peibotnat: Taws walcti, pou y ide S rartaeieen eames | rent siauon D at 30,00, ting wih red lead pet s . é observation, ar * n Ti: sseiiannaeiaes “satan The absolute quantity of moisture tn the nor- wea y, are all the points Of equal pressure tus Cecvermined | mai conaition of tue atmosphere decreases as we mMeELeOrOLOgists “All prrortae| negen cme artisan sgt be ye avove ihe earth's suriace, but the law of Se eee Bi her having crawn the mena five oi go.oo | CECT, canals and tale, weather | aoc ah cs Ted teadl pencil Les wie projected, BLOWIN | Cogroe of sAiuTaton oF Ihe AtMOsphere increases ere the barometer stands 1.80, 0% | un to the low d siratuu, and rapidly de- dnc i of | creases above the tp of that stratuin, 3 ¥ and hits Sime « line: bg aud dew attend the eupersaturation of tne n ment thts one may draw tines aca of iatn and show wre merety tered and disjointed. i Soe ee ere ace wepesited from pecsaturated sonably expecied These fics of eunal we Weather chart Wil slow us * Weat twobarics ¢ se Witt n eT : lower than a ore else on Uwe Tap. . Tai TOR C Lie mo 1 Pg t : nals — than over eoid or ¢ clog ofe a oF Ire on th ater areas vi ti and ate I a witnin the barometer ove brie su ressnre Wilt ¥ nes, tornadoes and ( 7 ver stores ussocisicl. It ts bbe wi Be . areas of Wy and low meter that new particue | Die cetaited repr larly Latere ye meieord iuese at Coie, Tae froin a few, | UTS PALL sare a ind ter hus t Wryns AND Ty tttat re by 4 the up sin ist y found of any siorm cenre and coiter tn he By attention to the po snd fatiing te tion Of app Thia unpertant clement is given in 0 percentage of inti satnration. ature we receive an pacD1Ug SOrMs. the wind 13 northessteriy and ticht, and the TURE, barometer begins to fall, rain may set'm verore ¢ bnlle the wind ¢ 3 sf, vatery Besides un there olves iu air very much as satt dis~ fs a rule about the way in which the wind ted tn changes watch Is very important, It is well ater, and as te salt ts depo: or the Water 18 fully saturated, spheric vapor. of air, having a temperature of degrees aud under a uniform pressure of 80.00 8 grains of water when fully w, compared with dry y clouds x to the rel. re and pressure existiag their motions er cul ¢ near bodies of w extensive fore: Wa ne by . alihough c other on of the areas of On ine and Pisin hand, whea knowa to every Sailor, and is contained In the following couplet: — When the wind ebifts against the aun, Trust is not, for back it wil can, The wind usually shifts with the sun— from left to right in the no} nology ts yet not of certamtics. te riment. the Signal Office 13 not chargeal ‘6 ont or act j por I anettut theories at of wir, Phe casent of expanding Warm alr gives rise A the atmosphere. Ui us chier has nad ta mov cumulus clouds, Waose at bases are all forward in tue dark ve appears to Mave feit hrs | apreiy uniform jevel. 7 oe side and bi Rapatty “e . me yas me grat : ft wave When tley s¢ Lo be ted by rising cur- he ni Which led to the selection of ue siege te ts of a fhe cirras clouds are probably wous fines of tes Verdras, in te old Peningi. Gon 0 hae el independentiy oy tiation of ~* PB Itlou from witch (he occu. veries ay - outward into thehignest regions of ab cANNOT be forced to retreat, and Which gives poe ne a obey og 4 aunosphere, in Which case they v every facthity for wa advan ato given io miles p on ey un the | are composed — of pene of ee snd = = ot pre ae Winds, as & as ‘ «med af the remnants o r ‘ 5 "0 tron the great | (Cy are, Mee gee dm whict 1. Cirrus, 3. Cirro-stratus. FARM FUGitT. y section, aad bow eral winds appear to be pri- | storm clouds, erally composed of rents of air t marily cevondeurt upon existence and position } 7 ofthe ureas wand Lgl pressure: toe great | Winds that currenis, 4 Hipg as Mey do over Whole conu as Heuts ani enearcilng the earth, are directly aepen- | OP” wren im which case tuey are gen- warmer vapor. atrend areas of ive rise, through the influence Of iriction, Ki before stated, air, in which, by expausion or The strong barometer 4, Ciunulo-stratus, Nimbus, 2. Cirro-camutus, . Cumulus, Stratis. low Wor’t Accept the Sitmation=Rearrest of | Folice Captain MangiamAnother West, chester ‘“‘Dogherry.”” to ascending strata Oe ala inj arent nan en the winds wit | COMME, as the cage may be, are produced the scud | types, as Tollows:— , ooasr of Contral and North America a moist south. | In Yonkers, Westchester county. te Jaw- abt be fant te Le biowing Meray tum the eenire, wut | #nd rath clouds of waich we have a tue exampie im | Frrsi—the West India cyciones, originating in | west wins ts forced up over the Sorta Nevadas and | ing portion of the community are ot present defected towaris wht as t move forwar tue easteriy raims of the Atlanue coast, Whts send | the southern region of tie zone of terily trade | Rocky Mor Vs moi deposited and a | | furattly Geetviad over cet ate x Wil in rea Ol 1OW pressure the < bow tes , Cloud, which is an amorphous cumulus, spreads 1 Wiuds, aud generaliy east of the Windward Islands. | of rarefied & baoly dry alr is started on ,; Siderably exercised over un atleged outrage on the ward the aud are also dedected toward ihe | *to broad sheets of stratus, . . | Alow pressure and iarge humidity mark thet cen rihoast of eastern comts | Captain of Pouce m that village py a Justices of the right han nove forward. tue tolion. | 2 TO layers of ciouds wimost Invariably coexist | tral region; towards this tie winds blow from all ¢ Storms pass over Wwithoat Ta Peace, named Shannon, tast frkiay evening. Ing table shows Which winds generally prevail on | Whereever extended raia storm@s prevail, the Upper | points, and, deflecting to the right, pursue their | . | ae done y 5 mdgs © of these arcas of hig! 1) low pres: | Maver stretebing far In advance of the lower, but | spiral course inward and upward, at least this i# | cause may be ‘raced Duck to the changes going on Some few we ago, a4 nas already been re- Ss or ace Prem | descending uid joutlng to the lower in the rear of | the omy satisiactory explanation that has yet been | m the southern aud we-tern limits of the Cuded | ported im the Henatn, Captain Mangin, alter div aor =the Prevatiing Winds w j the area over wien rain 1s Jalling. A geueral sur. | odered for the various phenomena. Tne motsture | States—at jcast two such have been actually f0l- | possessing sume parties who biel heen defeated in a The orwerver B Lowe Pressures } vey of the map wil show that cumoali or the cirrifirst | brought by this wind condenses as the press | lowed during the four or six days occupied in pass: | a had ated € “y on Me aii f | mentioned are uot {nconst+tent with fair weather. reduced, and clouds are formed, with heavy rain. Yng from the Pacific Coas! to Nova Scona. | Protracted jaw suit regardiag the ownership of a ‘edb oy ikea ’y. and Aa tacreasel accumulation of cammlous clouds At the centre of a cyclone an upward carrent 13 | — furd-—Karely we have a well-defined, though | yaiuatie farm, in answer (oa warrant, appea Ga the BW. aoe: - | Decomes cloudy weather, but does Not generally pre | supposed to exist, aud uigh above are formed the | generally weak disturbance, pass from the mort t9 | sore shannon, and having pat in On the W, side Wo ane wn th On the sec S. side Ou the SB. On the KB. side... } ciguds of winter au ‘ in an arca of abnormally low pressure and on the porihwest side of its centre he sgvuld Qud tie wind blowing | from some potui in the horizon betwe northwest and hortheast. if le is within ay area Of lugh pres- sure and on the hortiwest side of irs centre he should find the wind blowing from some pointio tue quadrant between soutiiedst and soutuwest, Waen no well marked central areas are actnaily Accordiughy, | sage the extended storms of winter. nu class, sotuettmes called cirro-stratus, al- st always precedes at § of samiuer. If we xeep in mind the existence of two immense | Quainted with the signs of the weather, ihe equatorial current 18 nghter than that of the polar, and so southerly winds will begin to blow aloli Delore they are felt on the ground, Wille porth- erly wiuds will begin to Liow close to the ground, southwest warning of their co ning than noriheasterly ones, atheast, ant probaoly only in midwinter, when tle nortieast Winds and high pressure prevail in British America. Fourth. —The storms which are geueratly confined within our own country are tue northers, tornadoes ‘The cirrus of the soudh, or ihe northwest to the cirrus clouds, Which streaw far away in advance on bs These st rms are carried | i taey pass into the me- where the prevailing rol their motions. This : & PLEA OF NOT GUILTY | to the charge Of asequiting the persons who were Gispossessed, Waived examination and gare bonds the Upper currents of air, To the north and west, 0 teorological temperate south and west wiuds con ome distance tae st | and ever-fowing currents of air, one from the pole | generally happens on or opposite the Soath Atlantic | and thander storms. The Jatter are geuerally spread | to answer Suy Indictment that might be aud the other from the Equator, one cola and ary, | coast, and as the storms then purse a course Rearly | Over a very Narrow space, so that they may attimes | found against him by the Grand Jury. the other bot and moist, We shail soon get ac- | wide gee) with the Gull Siream, with Its attendant | pass between the stations from which we receive | As Was contidenti " ° ‘e G ie The air of | band of moist air, they produce heavy casierly gales | our reports, These storms evidently onginate 1m Bh! Uy expected the Grand inenest prov ignored the frivolons accusation At the instan { the ejected parties, however, Shannon tssuea on the day named what he styied “peace warrants" for the arrest of Captam Mangia, George B. Skinaer (the owner. of the property al- the lower cioud stratum, in locai but intense differ- oisture and pressure, and to prevail only oa the West- pressure, arms te | ratner pay on our bast Atlautc coast, and finally are lost in the Northern Atianuec, but occasionally, foubtiess, reacn Iceland aud the coast of Great Britat Instances are not wanting im which these heavy storms of the Eastern Gull have passed to Texas, Ulence borthward to the lakes and northeast to | ences of temperatur } are believed in general ern side orin the rear of areas of hig The pen winds give much more yratory movements of are smali f upon local curreuts and fresistan: Within the limits of whe map the winds stil wuite | “Tne southwest wind Will often show itself firstby | Maine, widening the area of disturbances, and | than on the earth's rotation; they may, tnerefore, | Iuded to), and ent others, The Capua of with the lines of po all adage -nind Magee ne ba ova long streaks of cirrus clouds ata great hetgnt, called | gradually coanging into extended ratus with mode: | ther towara rhe rigut or the left. Tn these | Police, through his counsel, demanded a discharge ATEAS AS EXISTING De ON AS ee ee dear | soimetiines ‘‘Mare’s Tails;" or, wheu a gale ts very | rate winds, tausdidering frow the Atiantic storius cumnnius clouds are particularly remark- | onthe ground that’ the accusation set forth in the wet ester plaits tnaicate the low pressure. that | Beat, by dfiving scud. only in the direction. able for their height anu te citrus clouds for ther | warrant Was preciscly ike same ae that tne Meer ised Ii, the Missoult Valle). Wien | Dr. Gthbons pottced with great care at San Fran. Serond—The autumn, winter and spring rains, | suall exte’ which tne Grand Jury had recenuy thrown exists at that season iasiderabie area is very ant | ciseo the the course of the higher strata of | which generally frst announce theiaseives on our THE PREDICTION OF STORMS. out. Notwithstanding " the fact apthat — the Oe ee emee iooal wodeences (auch Clouds--the cirrns ana the very high stratus—when | southwest or western plains may be regarded as | ‘Tne wind ts (hat element which most affects the | warrant Was fssued” for assault, the obtuse form then minor local 1 disturbances origiating on the uorthern coutines of | commercial interest of the country, aud in forecast. ogberry” bound each aud all, of the parties over cannot generally be exactly iveated by Jimited number of reports hat We at present receive) adect the geutic winds that then @Xist; on such oc- casions local dierences of temperature and mots. lure. electing ae they do Uhg local pressures, give | where au ave irom some westerly for many yoaTs at Pai the | they were visible, and found gem .o come uniformly ut, dade long OWserved the same [act rave Of wor in $250 to Keep the peace for cae year. It is under- stood that lezal stops Will at, once be taken to keep this mode! ()) J ce wibhia ‘tue Lames of tat Octal durisdichou, * jug the approach of a storm We at present natne- ally give our pritctpal attentton to this element, ‘the prevalence of fog, rain or snow and the temper. ature of Hie air May, however, be esugated mm a the tropical zone ana oa the Paciie siope (as dis- timet from those of the preceding class that onal. nate In the West Indies). From (ue area Of niga pregsure OW the Pacidc he had also observed iua. The writer has in Western New York, (e than one instance | The Music. the Me: Lome of the Toronto Cinb. THE SECOND GAME jasted eighteen minutes and Was won also by the 1 lemen, Mr. ©. Nelson sending the vait threuga the goal. THE THIRD GAME, Which, like rhe orhers, had tts every inch vigorously contested by the Knickerbvockers, Was wou in like manuer by the iilusirious strangers in turteen n thus giving the Bine Noses the frst ames out of five, and ending the most signativ tn their favor. Tho piay turoughout Was Very spirited, and the run Ding on both sides was magnificent. The batl on The fast game was sent througu the fags by the lett home Of the Toronto Cinb, Mr. Mutchell, who kindly treated Amickerbockers to a similar exhibilion on tue Lirst game, When the third game was ended, ut twenty minutes past jive o’c.ock both clubs as- sembved in the middie of the feid, shook mands and cheered oneanotier heartily, the vast and respecta ble Larong who assembled fo witness the game jotn- tug tn the plaudits. ‘The Toronto Clab will have to TRY TP AGAIN norrow afternoon atthe same place, When they | play the first three out of five games against @ ub made ap of six men from the Manat ana six from the Knickerbockers. to w tau Clan CENTRAL PARK. au ‘The copious rains we have lately had nave at least it one Rood effet. The “ram is good 8, anyLOW,” Say COOd-natared poopie to aru x tricnds who have lost their pmbrelias; Dalit is even better forthe grass, Central Park is vow m its brightest and most charming dress, ‘th is carpeted with brilliant veraure, amt trees are rejoicing in the lealy glorios of a mfd- Meith, dol thing more than summer that hag certainly, whatever niay ve ts nouncing the app f ti ot shortcomings, not been unpleasantly dry, The storms, 18 bitlletins of the gr “are | eforts of the Park Conimissioners, im the wi nd sky we comp yersaliy FQught alier and ted, and its dy aha — seaie c way atahon of the atmospheric sphere of ladue every day | Of flower beds and hedg ace already crowned by their kinds and widening. Its pr ¢ certamty | with deserved success, The holiday-making citizea ive tempera- iu its processes of mvesiigation ans tis pnd- a at bigh “i Storm Warnings iinuaily mprev- | i they iudicute tue There se wo no haste to | fe, Velloved now and then by patches of ming Nowers, with he: statue, sud there the dull fasw Yesterday was qu day. The ar ments at the music stand are excel There are chairs and benches im abundance, ana temporary uwnuigs have been spread over them as a necded ev from the perils of a July sun, Al around fora co: ‘opie stroit, Y, occasion, eof pleasant lours, thousands and firs and make themselves . ly dropping into the cool saloon venrath the grand stone stairway that Jeads to the Lake to indulge in a water ice or a sherry cobbler. ‘The music Was very good, and the programme was Mate tip principally of seiections from popular and Siinpic operas, Whose music ts Tamuliar to all, Wke “righa det Regimento.” Music, however, was by nO means the sole reerea- itou golbg. On the common ot Parties were busily cagaged in cur “nttional game,” and the drives were thronged with elegant vehicies. & number oc gentemen on horsevack abroad, and there are indica- tons th horsemanship 18 growing to be @ more popalar amusement than it used to be. The Lake Was gay Win bowling parties, who were for a few fractional stamps rowed aronnd the islands a tars, Deatly dressed in white boating shirts, wi oan of bine falling on tne breast and neck. le mevagerie, however, Was, NeXt to the music stand, te grand centre of interest, Within the past three months the new house nas been 0} ned, and the lion that tas once so sullen now condescends to y at short intervals, to the sntemse satisfaction ofthe small boys. The zebras have become qu te tame, aud cat sweet cakes [rom the hans of visit. ors wilh the docitity of lambs, The otner wonders: the menagerie, are they not known to all! In me way, however, the seem now to be kept much cleaner than formerty, and ali the animais, except the monkeys, smett a litte jess ofensively ihan your African fellow traveller? up town on & ‘Third avenne car, And, as to the monkeys, every one KNOWS (hat they arc @ hopeless case, Onter Juarick CHASE.—A gentleman tn this city has just recetVed a letter from Chief Justice Chase, In reply to & series of resolutions subuaitted to him tor considerauion, in Winch he takes ground upon the late ameudmenis—holding that they are valid ant are parts of the Constitution ana are to be ree verted and obeyed as such, and this without quatin- catiow or reservation of any kind, The resolutions here, referred to are 10 be publisked at an early day. His many political and personal friends will ve Pleased to learn that his health continues to improve, Me is at present stopping at the Magnetic Springs, St. Louis, Gratiot county, Michigan, Lurkersburg (West Fan Journal, Angas! .