The summers throughout the transition province are hot, with little rain
in the western portion, but refreshing showers and occasional
destructive storms in the humid eastern portion. Owing to the latitude
of the main transcontinental belt of the province, the number of hours
of sunlight each day in summer is increased beyond what it is in the
main portions of the austral provinces, thus favouring the growth of
vegetation. There is also a lengthening of the morning and evening
duration of twilight, and magnificent sunrises and sunsets are frequent.
The mean summer temperature is in the neighbourhood of 70 deg. F., but hot
spells, lasting for days, and even weeks, are of common occurrence.
During these trying and frequently unhealthy intervals the temperature
in the shade reaches or even exceeds 100 deg. F., and sunstrokes or
prostrations by reason of the heat, particularly in the cities, are
numerous. The four seasons of the year are better marked and have
more pronounced characteristics in this division of the continent than
in any other, and it is the region of greatest seasonal climatic changes
as well as of marked weekly and even daily variations in weather
conditions. The most delightful months to most people are May, when the
returning migratory birds are nesting, the trees unfolding their many
tinted leaves, and the air laden with the perfume of multitudes of
blossoms, and October, when the rich colours of ripened leaves give to
the forests a marvellous variety and brilliancy of colour and the
tranquil, hazy atmosphere is undisturbed by storms for days and even
weeks together. This annual period of tranquil weather, extending
frequently far into November, is known as Indian summer.
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.
Elsewhere in the archive
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account