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June 1 - 3 , 1978 - University of Hawaii at Manoa

June 1 - 3 , 1978 - University of Hawaii at Manoa

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ACID RAIN IN HAWAI 'I*<br />

John M. Miller, and Alan M. Yoshinaga<br />

Mauna Loa Observ<strong>at</strong>ory<br />

N<strong>at</strong>ional'Oceanic and Atmospheric Administr<strong>at</strong>ion<br />

Hilo, <strong>Hawaii</strong><br />

Precipit<strong>at</strong>ion samples have been collected for chemical anal-<br />

ysis on the island <strong>of</strong> Hawai'i since <strong>June</strong> 1975. Though the number<br />

<strong>of</strong> collection sites varied from 5 to 10, the permanent sites<br />

included Kapoho (sea level), Hilo (60 m), Kulani Mauka (2500 m),<br />

and Mauna Loa Observ<strong>at</strong>ory (3400 m). Samples were collected<br />

either on an event basis or every three days depending on the<br />

accessibility <strong>of</strong> the site. The pH and conductivity tests were<br />

performed immedi<strong>at</strong>ely after collection <strong>of</strong> all samples. Anion<br />

analysis was made on selected samples using an ion chrom<strong>at</strong>ograph.<br />

The results show th<strong>at</strong> pH values in precipit<strong>at</strong>ion ranged from 3.7<br />

to 5.5 with an all-island average <strong>of</strong> 4.5. The acidity <strong>of</strong> the<br />

precipit<strong>at</strong>ion increased with elev<strong>at</strong>ion from sea level to 3400 m.<br />

Analysis in terms <strong>of</strong> air trajectories and surface winds <strong>at</strong> the<br />

Mauna Loa site indic<strong>at</strong>es the more acidic rains come from the<br />

northern quadrant. The effects <strong>of</strong> the volcano on the acidity<br />

will also be discussd.<br />

* Abstract

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