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Side 16
The advantage Water Barometers might be supposed to possess in showing
changes of atmospheric pressure on a large scale , is more than
counterbalanced by a serious objection . The space in the tube above the water
is not a true vacuum ...
The advantage Water Barometers might be supposed to possess in showing
changes of atmospheric pressure on a large scale , is more than
counterbalanced by a serious objection . The space in the tube above the water
is not a true vacuum ...
Side 17
1 shows the Cistern Barometer in its essential and simplest form , and it only
requires a scale , extending from the surface of the mercury in the cistern to the
top of the tube , to make it complete . Cistern barometers are subject to two sorts
of ...
1 shows the Cistern Barometer in its essential and simplest form , and it only
requires a scale , extending from the surface of the mercury in the cistern to the
top of the tube , to make it complete . Cistern barometers are subject to two sorts
of ...
Side 18
Hence , then , owing to the incessant changes in the level of the cistern , the
readings on the fixed scale are sometimes too high and sometimes too low . The
simplest and rudest way of compensating for this error is to ascertain ( 1 ) the
neutral ...
Hence , then , owing to the incessant changes in the level of the cistern , the
readings on the fixed scale are sometimes too high and sometimes too low . The
simplest and rudest way of compensating for this error is to ascertain ( 1 ) the
neutral ...
Side 19
zontal lines on the ivory float and supports , which are drawn so as to lie in the
same straight line only when the surface in the cistern is at the neutral point from
which the scale , G , of the instrument has been graduated . Hence , then , with ...
zontal lines on the ivory float and supports , which are drawn so as to lie in the
same straight line only when the surface in the cistern is at the neutral point from
which the scale , G , of the instrument has been graduated . Hence , then , with ...
Side 21
A graduated scale passes along the whole length of the tube , and when an
observation is made , the readings at the lower and upper limbs are taken , and
the difference between them is the height . There is another form of this
instrument , in ...
A graduated scale passes along the whole length of the tube , and when an
observation is made , the readings at the lower and upper limbs are taken , and
the difference between them is the height . There is another form of this
instrument , in ...
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America amount appear Asia Atlantic atmosphere atmospheric pressure average barometer becomes blow Britain calm causes centre changes charts climate cloud coast cold column compared consequently continued countries course daily diminished direction earth east Edition effect electricity Europe evaporation examined falls feet flow force frequently give given greater greatest heat height Hence higher hour Illustrations important inches increase indicate influence January July land least less light lines lower maximum mean mean temperature mercury Meteorological miles months nearly night northern observations occur ocean passed period Plate position pressure prevail Professor quantity radiation rain rainfall regarded regions relation rises round scale Scotland season seen side soil storms summer surface Table temperature thermometers tion tube upper vapour vols weather whole wind winter
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