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!coast; and secondly by the fact that the Piru Creek Drain-
lage Basin experiences drastic se&sonal changes in temp-
lerature from warm, dry summers to damp, roj_ld winters ..
!
i Generally, precipitation is moderate with 90% of the
I
!total annual rainfall occurring during the period between
i
!October to April. In the course of my research I was
1
able to compile a table of precipitation relating the
iPiru Creek Drainage Basin for the period from 1769 to
1972. (Figure 1)~ This came mainly from early historical
journals, the records of Fort Tejon, the records of
Missions San Buenaventura and San Fernando and from the
records of the various agricultural service agencLes in
the area. While not 100% accurate, this table does reveal
some interesting facts; for instance the average annual
rainfall since 1769 has been 17.01 inches~ The Sandberg
weather station, located in the northeastern quarter of
the basin at an altitude of 4~517 feet or about 400 feet
higher than the mean altitude for the whole basin, at
present has the only known long term precipitation and
temperature profiles for the area. (Figures 2 & 3)~
At Sandberg, annual precipitation ranges from 12 in-
ches at the station to about 24 inches at the Temescal
;station, in the southwestern portion of the basin~ Mean
annual rainfall for the entire basin based upon informa-
!tion collected since 1933 supports the previously stated
figure of 17 .. 01 inches. (Figure 4) .. 'rhe data collected