THE WEATHER.
EXPLANATION OF THE CHART. temncrate latitudes in Australia and New Zealand. The dotted lines This diagram snows the -weather oyer i e . * eter at q a .,n. 0 n the above date, and thns indicate tha general •cv isobarh connect equal readings oi u>ef o Uowin.' these lines, changing its direction as they change, / circulation of the atmosphere, tne ■"?£" _ nt 0 f difference of barometer which they express. The arrows and increasing in force according_io ™° £ * contnuy direction to the movement of the hands of a clock, fly with the wind, which always o'°™". ~h tne c j ock oaD ds ronnd a low barometer or cyclonic area, round the area cf nion O baro^,f:" t h o eastward progress of these latter distnrbances, at the rate of 300 to Chances of weather chiefly ansa 'XjUom rfthY&ban, due to the shape of the land, are omitted. 500 miles in 24 hours. All local QB TQE WEATHER . ~.„ n (nt«OTte all over, most in the South: Northerly winds, except at the Bluff, KewZealand : Decre<™ <* " showers and gloomy at Wellington and Bluff. Australia: Slight S.K.: rain at Barometers : New Zealand-Russell. 30 1; Wellington, ; Portland, 29 0 ; Sydney, SOU '_
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Bibliographic details
New Zealand Herald, Volume XX, Issue 6819, 25 September 1883, Page 4
Word Count
196THE WEATHER. New Zealand Herald, Volume XX, Issue 6819, 25 September 1883, Page 4
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