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INTRODUCTION: The Hawaiian Islands proper consist of eight major islands:
Hawaii, Maui, Molokai, Kahoolawe, Oahu, Kauai, and Niihau; comprising a total land
area of approximately 6,450 square miles, of which the island of Hawaii comprises
about 62 percent. The islands are all mountainous and of volcanic origin. Their
coastlines are indented by numerous bays and coves, and in many places long stretches
of white sand beaches, alternating with rocky shores and headlands, rise from the
shallow waters inside the reefs. At other places there are no beaches at all; the
steep cliffs often drop directly into deep water, or their bases are strewn with
FISHERY RESEARCH BIOLOGIST, SECTION OF BIOLOGY AND OCEANOGRAPHY, PACIFIC OCEANIC FISHERY
INVESTIGATIONS, U. S. FISH AND WILDLIFE SERVICE, HONOLULU, T. H.

1/PARTI THE HAWAIIAN LONG-LINE FISHERY BY THE SAME AUTHOR APPEARED IN COMMERCIAL FISHERIES

REVIEW, JANUARY 1950, PP. 1-23; ALSO AVAILABLE AS SEPARATE NO. 244.

2/DR. SIDNEY SHAPIRO, FISHERY RESEARCH BIOLOGIST, U. S. FISH AND WILDLIFE SERVICE, COLLABORATED

IN THE PRELIMINARY PHASES OF THIS INVESTIGATION.

3/THE VARIOUS TUNA SPECIES CONSIDERED HERE INCLUDE: YELLOWFIN TUNA (NEOTHUNNUS MACROPTERUS),

BIG-EYED TUNA PARATHUNNUS SIBI), ALBACORE (THUNNUS GERMO), OCEANIC SKIPJACK (KATSUWONUS

PELAMIS), AND KAWAKAWA (EUTHYNNUS YAITO).

lava rocks. In general, the fringing reef extends only a few hundred yards from shore.

Climate is fairly uniform through the year. Mean monthly air temperature at Honolulu varies from 71° F. in January to 78.4° F. in August. Northeast trade winds prevail throughout the year, but from October to April they are occasionally interrupted by "Kona" (southerly or southwesterly) winds. "Kona" weather is often accompanied by rainstorms which may last from a few hours to three or four days.

SEA TEMPERATURES:

The average annual sea-surface temperature in the Hawaiian area is about 770 F. Maximum and minimum monthly averages are shown in table 1.

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It is at once apparent that,
at the surface, the differ-
ences between the monthly
maximum and minimum temper-
atures become smaller dur-
ing the summer season and
larger during the winter.
The same condition exists
at a depth of 100 feet,
while at 200 and 300 feet,
the differences appear to
remain relatively constant.
The horizontal distribution
of sea temperatures at the
surface, 100 feet, 200 feet,
and 300 feet, at the two ex-
tremes of the year (February
and August), is shown in
figure 1. The thermocline,
therefore, generally lies
between 250 and 300 feet dur-
ing the winter months, ris-

Since the tunas are primarily warm-water forms, it is to be expected that the vertical and horizontal distribution of the various species is to some extent governed by sea temperature conditions. The results of the Japanese exploratory investigations in the region of the Inner South Seas, for example, indicate that sea temperature had a close bearing on the occurrence of skipjack and yellowfin tuna, especially in the region of the equatorial countercurrent, where the main fishing grounds for these species were located. Their findings indicate that when temperatures in this zone were below normal, a marked decrease in the catches of skipjack and yellowfin tuna occurred, followed by an increase in the long-line catches of big-eyed tuna and albacore.

Although no basic studies on the relation of sea temperatures to the occurrence and abundance of tunas in Hawaiian waters have been completed, the Territorial Division of Fish and Game has been gathering data on the relation of subsurface temperatures to tuna long-line fishing. The commercial catch records indicate a marked increase in the landings of yellowfin tuna and skipjack, as the waters in this region become progressively warmer during the summer months. As the season advances and the waters again become cooler, the numbers of these two species entering the commercial catches show a decided decline. Big-eyed tuna and albacore, which may be less tolerant of the higher summer temperatures, occur in the catches in fewer

numbers during the summer season. These two species enter the catches in the greatest abundance during the winter months, and their increased appearance follows closely the decline of the yellowfin and skipjack.

OCEAN CURRENTS: The waters surrounding the Hawaiian Islands are subject to strong and variable currents through the year (figure 3).

In general, currents run southwesterly and westerly offshore, due to the influence of the northeast trade winds. Close inshore, however, the flow is northward along the coastlines, except off the Puna (southeast) coast of Hawaii, where the inshore current flows in a southwesterly direction. In the channels

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between the islands, the currents are tidal, but to some extent, are influenced by the prevailing winds and the position of the islands with respect to each other.

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In Kauai Channel, the main current approaches from the northeast, but abruptly changes its direction of flow to the northwest as it strikes the shallow water bank that extends northwestward off Kaena Point, Oahu. It continues northwestward until it reaches the east coast of Kauai; here it divides in the vicinity of Nawiliwili Bay. North of the bay it follows the coastline and joins the main current north of the island. South of Nawiliwili Bay it joins a large eddy movement that exists south and west of Kauai. This eddy rotates in a clockwise pattern, extending a maximum of about 30 miles offshore. The north

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