o; and the number of consecutive days when two
or more reefs have been kept tied down during the last few summers
has been remarkable--alternating at times with equally persistent
spells of calm and fog such as we are now passing through. Again,
we have had an unusually early appearance of ice in the Atlantic,
and most abnormal weather over Central Europe; while in a letter I
have just received from an old hand on board a large Australian
clipper, he speaks of heavy gales and big seas off that coast in
almost the height of their summer.
'Now, upon all this, in our season of long twilights, we have
bursting upon us some clear weather; with a display of cloud-forms
or vapor at such an elevation that, looking at them one day through
an opening in the nearer clouds, they seemed so distant as to
resemble nothing but the delicate grain of ivory upon a
billiard-ball. And yet with the fact that two-thirds of this earth
is covered with water, and bearing in mind the effect which a very
small increase of sun-power would have in producing cloud and
lifting it above its normal level for a time, we are asked to
believe that this sheen is all dust of some kind or other, in order
to explain what are now known as the "recent sunsets": though I
venture to think that we shall see more of them yet when the sun
comes our way again.
'At first sight, increased sun-power would seem to mean more
sunshine; but a little reflection would show us that this would not
be for long, while any considerable addition to the sun's power
would be followed by such a vast increase of vapor that we should
only see him, in our latitudes, at very short intervals. I am aware
that all this is most unscientific; but I have read column after
column of explanation written by those who are supposed to know all
about such things, and find myself not a jot the wiser for it. Do
you know anybody who is?--I am, Sir, your obedient servant,
'AN UNSCIENTIFIC OBSERVER. (R. LESLIE.)
_January 1_.']
[Footnote B: "I have been often at great heights on the Alps in
rough weather, and have seen strong gusts of storm in the plains of
the south. But, to get full expression of the very heart and
meaning of wind, there is no place like a Yorkshire moor. I think
Scottish breezes are thinner, very bleak and piercing, but not
substantial. If you lean on them they will let you fall, but one
may rest against a Yorkshire br
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