Spons' Household Manual: A treasury of domestic receipts and a guide for home management
General
Spons' Household Manual: A treasury of domestic receipts and a guide for home management
Home economics
The amount of rain varies enormously in different parts of the
world, some districts being either absolutely rainless, or having
only a very few inches of rain in the year, whereas others have some
hundreds of inches in the year. Even in England itself there is
considerable variation. The average rainfall for the whole country
is about 30 inches a year, but the amount in different parts of the
country varies from about 20 inches to nearly 200 inches a year. The
eastern side of England, as Field remarks, has much less rain than
the western side, and, roughly speaking, if a line be drawn from
Portsmouth to Newcastle-on-Tyne, it will divide the country into a
dry portion and a wet portion. The portion of the country on the east
of this imaginary line will (with the exception of the south coast,
which is wetter) have only 25 inches of rain or less, and the portion
on the west of the line will have from 30 to 50 inches, with much
larger amount in the Cumberland and Welsh mountains, and at Dartmoor.
The rainfall of the wettest year is about double that of the driest
year. This gives a very useful rule for roughly ascertaining the
extreme rainfalls, which are really more useful for the purpose of
water supply than the rainfall for an average year. The fall in the
driest year may be assumed to be one-third less than the average, and
for the wettest one-third more. Thus, with an average rainfall of 30
inches, the fall of the driest year would be 20 inches, and that of
the wettest year 40 inches.
A portion only of the total rain which falls is available for water
supply, as there is always more or less loss. In the case of rain
falling on roofs, the loss is comparatively small, but in the case
of rain falling on the surface of the earth the loss is considerable.
The latter is disposed of in three different ways: part of it runs
directly into open watercourses and streams, part is taken up by
vegetation or lost by evaporation, and part percolates through the
surface ground and accumulates in the water-bearing strata which feed
the springs and wells.
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