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Name- Date Chapter 6 Laboratory Exercises 1. Consider the Coriolis force in the Southern Hemisphere and its effect on wind di
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1(a) It is due to the apparent force that acts on the moving objects causing the object to suddenly change the direction to the left in the southern hemisphere. Actually, the thing that happens is given in the picture below, if a person stands at some point along with the flow of current in the southern hemisphere facing the direction of current moving then the current suddenly changes its direction towards the left-hand side of the observer. This happens as a result of the rotation of Earth.

Nortz henaisphere, dofectio niget of te olosooer to the Clesenoer $zuotor defleation ma Olbsirves uteshn hemispesae 1 deflect

1(b) H & L indicates high and low pressure respectively. The winds move out in a counter-clockwise direction from the low-pressure zone and inward in the clockwise direction in the high-pressure zone. Both the images are given below.

t020 -1o16 - 10 12

989 980 62.The same thing happens as happens in the southern hemisphere with Coriolis force. See answer 1(b).A20 LO29 1016 l023t to 12

1000 1004 1008 1012 AAAA

In this pattern the arrows are shown as such that the wind is moving from lower pressure to higher pressure, it is just the representative version of the previous image of the question showing just a straight line pattern because if we notice we can see the exactly same thing happening, the wind is blowing from the low pressure region towards the high pressure region.

3(a). Average sea level pressure (P) = 1,000 Mb = 100000 Pa , C = 287 and T = 293 K

P = C*D*T

100000 = 287*D*293

D = 100000/(293*287) = 1.1891879 kg/m3

(b) Average sea level pressure (P) = 1,000 Mb = 100000 Pa , C = 287 and T = 298 K

100000 = 287*D*298

D = 100000/(298*287) = 1.169235 kg/m3

Density = Mass/Volume

V = 6*5*3 = 90 m3

Mass = D*V = 1.169235*90 = 105.23115‬ Kg

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