9%, 
инан, 
M o T Sa 
Noris. enge Е 4 Ere irmond, Market-Kasen, Uineclusbire \ 
Ь АРИ Castle, Westmore 
Аана jm Jirencester, Gloucester 
Donne, Rev. Stephen, Т; Salop 
Bond, Robert, Thorington, Saxm undbam, Suffolk 
cota — Playford, Ipswich, n v 
all's roe Leathe 
aere m 
4 радай, Knockd 
H "d e > dea — "Bridge 
Ewens, се Samuel, 4, pred 
Wo , Wimborn 
ой Boultham Hall, Lin coln 
tus, Phil. D., R. A. Co ollege, Cirencester 
"Frost, Charles, Wi herstead, Ipswich, Suffo 
The names of 34 —9 for беш at the next. 
monthly meeting were 
FiwaANcEs —Mr. Ra өтт "Barker chairman of the 
Finance Com mmittee, read the report on o accounts of 
; from which it йге th at the current 
cash-balance then in the hands of the Bunkers (including 
“эй 9L 
oner 
Pepe "ot 
rogress, o of м 
Committee, andan obtained | farther time for nd 
"which the explanation о the law of rotation rests, viZ., that 
here are, properly speaking, only two ts on 
which our relations of weather g e 
flow ro over r the ot irs but 
w besi de e other in variable chann els. 
less et than warmer air, it 2" 
mplies а 
gm the northern he eiisphere); 
become south-westerly one 
an 
sir exis sting atmos 
preponderance of ore dh 
which from the earth's rotation 
n 
would appear "^ the east winds which prevailed 
d gave us such cold w eather, con- 
ching Liv Wm 
n longer іп n setting in 
s а good meet of 
w at the suríace of the 
nns compensatio n for Depos the barometer at а 
medium pr Matre: And besides, as Dove has т 
admitted that the prevalence ot north-west winds o 
be: east coast of the United carm and also in Canada 
= diture y 
i f th 4 | 
wem phong - n. Leslie Melville, Vice- flows into the Atlantie from th eriean continent 
of the "eni бнк» Committee presente 'This eurrent does not reach Е occa oast—if it 
: did so our winter would be vere, as it is 
mittee, whieh was postponed for 
motion of Mr. sure: seconded 
by Mr. Milwand, die "following resolution was pass 
“That it be an instruction to the stewards to endeavour 
if pem to decide all protests ас сес ards of 
he eonclusion 
ive 
such 
th 8, а he dire in 
yard, before 6 o'clock on the Thursday 
tlie show-week ; and that no protest shall be uei cd 
receive ved, unless satisfac aetory reasons be assigned for 
; i; by Me Thompeon, Sir Joh Fisher Hobbs, 
seconded mpson, Sir John Villiers Shelley, 
Bart, M.P., was eleeted one of the Trustees of the 
іп the vacancy о, by the decease of the 
Hon. k H. Clive. 
Солхо Зал, —Оп the motion of Mr. Fisher po 
seconded by 
namel 
rl of Be Si 
ке hme rein еы ir John "— Sir 
M.P., Mr. Barrow, M.P., Col. Chaloner, Mr. жуш 
‚ Mr. Woodwa r. Lawrence, 
er, Mr. Thom 
Mr. Caird, and Mr. Fisher Hobbs. ^R ud directed | It 
the s 
evening of | 80 
а divert into 
of | rotation. 
well known the nineto mpidly кач кл» с 
h во if the 
beer oes to the north-west; and 
truth in the law that the earth mien n its a 
converts а nd into a westerly one, we should 
ows into 
also — that the sabia wind whie 
the Atlan mer should be converted, first 
into à ee one and afters rwa - toan east wind. "That 
thi p n the opens of 
e solution of this matter appears y" be, that part 
of this — American eurrentr — Europe by 
еч пррег ч t. This is а very с 
rum 
west win nds ну the А 
strata best һи, рез ien 
ne gi ng ixture of the air of differ 
gravities through vertici] gyrat d This is 
forces c; propel the south-west winds in fario us 1s gales, 
not свз ар pec wind is sometimes 
n east one as the effect of the earth's 
There i ise vidently a great sympathy or con 
wt ood гене ае north hes east yis. — as those 
of December But instead of the polar current 
— in aps rete as s this physical (ma жыла 1еаа 
only i 
servati 
Hum пае К this о ago, on 
the 
eve Ty por 
A A 
Ё , с 
h-west winds in our 
wind, instead of producing rain, as in Jerse 
inosculation m A relatively warmer ч... d 
south-west, bro about a remarka t 
the vim part *i England, duri 
d th, 
da oet 
mentioned. At Bath, 
t 
our corres 
4 К 4 ernoon, and con | 
Же Sb. When lle e day w na баз | 
was misty, and the bes was ME its Жы the темме | 
int of the compass. ub | 
e proceed further north, we find the 
be t the two antagonistie curren nts—the so uth- 
upper, and Ше, Rud rth- rai nder—a a later i 
mencing, but h longer in termina ER Й. 
In the middle districts К р 
ear uc ca 
re stealing over the zenith 
Another night a - frolla er 
n the 4th, th n an SE to 
^, and eontinued at this polit form gen 
re strong gale had set in fron, the east. The 
: A and north coast of Engl ө ta 
“vexed” 
s Pap oceurred for years 
ie e ese days, 
bad again fa Пеп еа ше чий Eu the 
to 30°, 
the temperature was 11° 
temperature wa sed by a stron 
the south-west, бөөн the north-eas 
furiously below, and it swept all the 
temperature of 38^ Fei а continue 
-— е until it drove eie 
gradually fell, rà on the 10th the « $a 
as sime нд with 4 inches of snow. 
T is w d of green that bern € snow fell 
on the 4th and 5th of January on the east coast 
Scotland, more fell in t the 
the no rth of Ireland. 
able fall of snow on the 
no ast 
ESR 
it was rs чин 
Bir 
ted In 
believe t quito as Aeg rain falls c on v west coast 
of Britai e and also in Ireland, ж кее: өс as on the 
east coast, but the excess of mo e former. 
rales arises from the greater quad whieh falls 
with w inds. rather curious and tan 
r 
the committee to be ned for Wednesday next, | flowing side by side with the equatorial, mor - 
and Mr. Fisher Hobbs to act asits Ch x, m Anci monly flows as an upper win from hoci Es Mir t itle dryness * east winds on the € 
Heir т fo exhibition at the Lin: M4 Pages et = o two currents is ery common in our while they were raining in the more — parts ts of the. 
bee qe ts ame bulled before the 31st н March, | latitude, o also Sn from this action ; | 2!htry» осештей last season in Scotland, For a fer 
y com e prizes that may be awarded to | but we меба enter farther - this subject at present. miles inland, along the coast of East Lothian, Fife 
nM Ont their producing live elvis before wipe wel Өйгө In Aber. | OTT, and also r a great part of the county o 
the 31st of January doni n hs cul al DONE E (from the 26th to | Aberdeenshire, the summer was the driest which b 
the 3th of March. 3lst) seems to have been a mere modification. of whati is occurred since in some localities there was 
; enough moisture to braird the late-sown Barley andthe 
i 7 "т thi Hacen 1, | Lurnips, while a few miles to the westward the rains 
АЁ ЕП т some сезсин but the mcs wind c к ada to a more | Were In great excess — pe was mosily 
те: Distribution P Heat over не Surf. weste rl ra dem and brought more moisture witlrit; | 12002 the tonc hirci upper rom ү 
Globe. Taylor and Franeis, тоёбу, 1 pe E the on the north u rrent ing its sway at th ,|west. It is only de such conditions ISI. | 
TuE maps, presented by P s E гм surface of the ground snow was precipitated, and е | T^! snow Bri ith east winds. Bi 
of Berlin, to -— British Association for the ad quantity was greater as the country was more el 4 | how delicately are the conditions of precipitation often 
ment of Science, representing the t dvance- over which the currents rise. Nearly 20 inches of snow balanced, and ho ly are their limits prescris A 
the e different mouths of the year over чле ХЗ - are seem to have fallen with the north wind in Aberdeen confound those who ignorantly pretend PE 
аг Ка shire, while = ANN of Scotland were visited with nature of the ther in particular localities qu 
t they bespeak the i industry of their distinguished | a hard blac After thesnow-storm in the south of Englan 7 
we wish to make a few remarks in to Throughout he greater part - Б paeniter the winds | 5i» а09 5th nuary, the temperature РО УШИ 
his views оп the atm eric currents of our northern | ly or noórtherly in Britain, e warming | 2017 and the wind went to the south-west, 1 yt 
асан qe the HoW Romis cre] т he south-west winds was little felt. The of Scotland there was a much greater r store 0 А 
weather, ho т, t tt y h long me i 
e has been led (0 eonsider that th еге | Devonshire. The rains in that count т although it is ve —— X it existed in the 
MEN ivo smomhoce which flow E ps »used by the equatorial current tting ч basea = di cl Qu x eid а ше 5 ol бе " 
in the northern latitudes ; one | Wind, while the east wind still i p ive 4 dd articulars of the weather at a station 9 
Н t g prevailed below, and at |5 à : 
s the poles, the towards the rend k the west wind above, and resto d miles and 600 feet above its 
equator, In his view, when a -west wind is . | the cold ег. t wind, indeed, s ems t Mus in Strathdon, A "Айген, for the purpose | 
latitude, a north ind vere maintained its supremacy till the beginning DE compar 
here else to maintain the equilibrium ват confliet took place between the east vind Jan. 3. fumes frost, 5? below zero; barometer falling. | 
pressure. In tances which haye | 25 21 under eu üth-west wind asan , | Jan. 4. Intense frost, 69 below zero at night; 1° at noone ы, | 
*ome under our observation opposi ic ting in the latter gaining th Upper, | Jan. 5. Minimum temperature 12? ; cirrus s from the south gil 
existing in two d fons. | length freely flowing over the whol por к x below south-east with dry hail showers; baromi} , 
distances from ses other, and the a great rise in a fore SÍDE | an. 6 6. "уша east-sonth-east; frequent showers of snow; WF 
amie US а very sa expl about, an imm nse quantity of snow iba and чен "a meter 28.42; minimum tem perat ture 10? ini 00 | 
er led to believe that storms about by severe d qm. of which was driven | Jan. 7. Cirrus still passing from the south- be 1 
; ien гу “чыбыз wisis did Ri their mode we shall shortly n notice j o e тан w falling all ni io ро temperature 89 ub - $ 
ENE e т п. 8. ast-n 
minds come itr содае with each other, Fe the end а х year the frost was current south-w est; [rmn Be rising. : шю 
to the mind, ho it this view із | OUT island ; the south-west wind, howe very intense over | Jan. 9. Suet fall of dry snow, with cumulo stratus | 
R dy of rotation which has been | à Surface wind in J ета wüéfliwingas| east; galo ebating; cirrus та magees 600 a ci 
| апа by many others, and a thaw was ee Агачы y as the 2d of last mont ep qme d nearly calm; 890" 
C 'ori 4s ished. . 10, à t ture 6? ; clear an ME 
says : two theories | Fur fes nd there back d to the ea east, an чача ше 3d M ха now Iyleg 98. i posee hw beer removed үм um j 
му. са the researches that I have already oderit ts d the аси fall АП of the barometer м Due rentur aao а until te шө, 4 
eonditions of weather um ations of temperature, that opposite I, fowis ng as an t wind was still | th е таит emere ыр 7 The warm S009. - 
i usually prevail simuitaneousi: pper eurrent, A: the ice being 10 to 18 inches. P : 
and Euro usually. Es and that iy in the same the south d za: to tho Ith winds were at length sw ver Grampian 5 
а severe winter here corresponda ts а n ап opposition, so that | The wind see in Jersey.  |Lowland by the 17th, and this Polar scene S05 eggs 
versa, On Dhenome bonds to a mild one there, and vice north-east b i r f i the river Yig 
phenomena is grounded the ln east over th England delle from е | {о dissolve. « the whole ice on "pack the 
3 m n са! tinued n the same direction on the 4th and 5th. T1. "d con- | in motion ;" here and there a bridge damme ер ie 
east | torrent for a time, till it gai strength to 91^? 
