Reading the WeatherLongstreth, T. Morris (Thomas Morris)
Science
Reading the Weather
Longstreth, T. Morris (Thomas Morris)
Weather forecasting
Of course many valleys are so large as to be affected, not by these local
causes, but by the larger movements of the anticyclones when the
sure-clear west wind may blow up the valley for three days at a time. But,
nevertheless, for most mountainous places the logic holds and you may
expect rain if the wind does not blow coolly down the ravine at night. Of
course watch your clouds for confirmation.
In times of calm prepare for storm. An eminent meteorologist has frowned
upon me for saying that. It is not the whole truth, I admit, but there is
a certain kind of calm which happens often enough to justify the remark.
It happens this way. A severe storm has passed. The customary anticyclone
with its brisk northwest winds has arrived and is blowing with all the
vigor necessary to induce one to believe that the clear weather is to
continue for the usual length of time; that is, three or four days. But
suddenly in the early afternoon, just when it should be blowing its
hardest, the wind drops, lulls, shows a tendency to change its direction.
There is only one explanation. Another cyclone has developed off in the
west. It has knocked the anticyclone on the flank, taken the teeth out of
the gale.
The wind shows this before clouds can. The absence of wind when there
ought to be a lot shows it before even the first cirrus swims overhead.
The chance is that when the flow of anticyclonic air has been thus rudely
cut off and stillness follows, it will be storming by morning. It is best
to keep an eye on these abnormal, precipitous calms. In times of peace
prepare for rain.
But the eminent meteorologist was eminently right when he said that the
statement was misleading unless explained. For there are many kinds of
calms that do not portend coming storms. Nearly every day, winter and
summer, but particularly in summer, the wind drops to a calm at sunset.
That is a time of adjustment. After sunset when the accounts are all in
the wind springs up with as much force as it had in the afternoon and
continues until dawn. At sunrise, however, there is another truce. If this
truce is neglected either at sunrise or at sunset it is a sign that either
a cyclone on an anticyclone is very much in the ascendency. These truces
are most often observed at the seashore when you are out sailing and the
smell of supper fills your nostrils but is not sufficient to fill your
sails. These calms are normal and the best sign of a fair day on the
morrow, provided the other signs agree.
During the great transition period from summer to winter comes that
autumnal truce, Indian Summer, which is the chief claim to fame of
American weather. For day after day a brooding haze sleeps in the air,
sometimes for weeks there is no wind of any strength. Winter advances
insidiously in the fall but retreats in commotion, and the cooling off
process permits of these still days while they are uncommon in the spring.
The wind checks off more mileage in March than in any other month.
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account