The amount of precipitation varies greatly for the different desert
stations, usually becoming less as one goes south from the High
Plateau. As has already been mentioned, the average rainfall at
Laghouat, which lies at the southern base of the Saharan Atlas, is
198 mm., the average at Ghardaia is 114 mm., while that at El Golea
is 47 mm. The latter station is about 225 miles south of Laghouat, in
the midst of the Sahara. The amount of rainfall, however, is greatly
influenced by altitude, although lack of adequate precipitation data
for the desert makes impossible a detailed presentation of this phase
of the subject. As the amount of the yearly precipitation is less in
the extreme southern part of Algeria than it is nearer the Saharan
Atlas, where the altitude also is greater, it might be expected that
the number of rainy days would vary in a like manner. Such records as
are at hand, however, do not show this to be the case. For instance,
at Ouargla rain falls on an average 14.2 days, average of 7 years,
while the rainfall is 90.2 mm.; yet at El Golea, with a rainfall
of 47 mm., there are 23.4 rainy days each year.[4]
On the desert the rains are often of a torrential nature, as facts
presented above would indicate, and sometimes as much rain falls
within a few hours, or even a few minutes, as usually occurs in
an entire year. How much of the annual precipitation is of this
character and how much is of the non-torrential kind the usual
summaries leave entirely out of the account. It is well known that
the former type of storm is more destructive and less useful to
plants than the latter type. To illustrate the irregularity of
the rainfall in the northern Sahara the monthly precipitation at
Ouargla for several years is presented in table 2.
TABLE 2.—_Rainfall at Ouargla, in millimeters._
+----+-----+-------+----+----+----+-----+----+
| | |No. of | | | | | |
|Year| Amt.| days |Jan.|Feb.|Mar.| Apr.|May |
| | | rain | | | | | |
+----+-----+-------+----+----+----+-----+----+
|1900| | 1 | | | | | |
| | | | | | | | |
|1901| | 18 | | | | | |
| | | | | | | | |
|1902| 70.5| 8 | | |11.3| | |
| | | | | | | | |
|1903|135.6| 14 |55.0| | | | |
| | | | | | | | |
|1904| 35.0| 26 |20.0| | | | |
| | | | | | | | |
|1905| | | | | | | |
| | | | | | | | |
|1906| | |15.0| | 2.0| 4.0| |
| | | | | | | | |
|1907|210.0| 18 | |68.2| 67|325.0|16.2|
+----+-----+-------+----+----+----+-----+----+
[**Continued]
Public-domain text, read in full here on John Shaqi.
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