This paper examines the 27-yr record of precipitation measurements at
Ocean Weather Station ''P'' (50-degrees-N, 145-degrees-W). The credibi
lity of the rainfall observations is assessed, and the testing of cert
ain extraordinary features of the fall and winter seasonal precipitati
on time series is outlined. Using the portion of the record establishe
d to be close to ''ground truth'' (1954-1967), the authors have statis
tically related present weather observations to seasonal precipitation
amounts at Ocean Weather Station ''P.'' With this approach, the autho
rs have reproduced the first half (1954-1967) and predicted the second
half (1969-1980) of the precipitation time series to compare to obser
vations. Precipitation is physically estimated by determining the vert
ical moisture convergence at Ocean Weather Station ''P'' and comparing
the relative consistency of the moisture convergence time series to t
he contemporaneous seasonal rate of measured precipitation. The analys
is suggests that the Ocean Weather Station ''P'' record of measured pr
ecipitation is a substantial improvement over previous estimates of pr
ecipitation in the northeast Pacific for the period between 1954 and 1
967, but that the second half of the record, particularly during the e
arly 1970s, remains questionable. Reliable rainfall estimates along wi
th measurements for the 27-yr record are given to aid studies dealing
with energy balance calculations and the verification of oceanic preci
pitation generated by global climate models.