Taylor;

amounts

Table 1.

recorded

at

locations

in

the

Marshall

Islands

shown

in

Average annual rainfall in these islands ranges from 411 cm at 6°N

latitude

to

147 cm at

latitude.

The

estimate

mean

data

11.5°N latitude,

in Table

amounts

of

1

are

rainfall

indicating a strong correlation with

used

to

develop

on atolis

where

a

no

predictive

records

Eq. (1), L is the degrees north latitude of an atoll with
seconds

are

expressed

as

a

fraction

of

a

degree.

For

model

are

to

kept.

In

the minutes

and

example,

11°21'N,

the

latitude of Enewetak Atoll, is expressed as 11.35.

Annual mean rainfall (cm) = 696° - 48.92L .
Using

Eq.

(1),

the

predicted

mean

rainfall

compared to the measured annual mean of 147 cm.
used,

however,

to

estimate

mean

can be extremely variable and,
year.

amounts

of

for

Enewetak

is

135

cm

This equation should only be

rain.

The

annual

amount

of

rain

for the most part, unpredictable from year to

At Enewetak the annual rainfall in 1974 was

years recorded.

(1)

215 cm,

one of

the wettest

The next year there was only 102 cm of rain, which was one of

the driest years of the last two decades.
Because
stored

rainwater

and

especially
visited,

used
in

the

is

preferred

sparingly
Northern

in

to groundwater
anticipation

Marshall

for drinking,

of

Islands.

At

it must

unpredictable
the

inhabited

be

droughts,
atolls

we

there were a variety of cisterns that were used for the storage of

water drained through a series of troughs from residence or municipal
catchments.

roof

Ailinginae was the only uninhabited atoll with a cistern and it

collected only water that fell directly into it.
Cistern water sampled at Rongelap in 1956, 2 y after the Bravo event at
90... . 8
Bikini, was found to contain over 500 pCi/1 of
This concentration
present

was,

until

the

atoll.

reduced

water

the

would

associated

now,

were

the

Usage
be

U.S.

guidelines

and

dilution with

expected

so

that

to

correlate

lower

today

90 Sr

in drinking water

for 905,

activity

the

global

rainwater

of

expected

fallout

levels

fallout

recent
wet
deposition.
However,
as
239+
1
.
of
39 24054,
3705, and 906, in cistern
excess

but

in drinking water

radionuclide

with

with
.
in

for

only reported measurement

concentration

concentrations
Island

recommended

should
in

at

have

cistern

concentrations
late

as

water

at

1975,
ty
Bikini

.
3.4.
.
concentrations,
indicating

that

at some atolls there may be an additional source of radionuclide contamination.

em ee oe

exceeds

Select target paragraph3