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Final Comprehensive Conservation Plan - U.S. Fish and Wildlife ...

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Hakalau Forest National <strong>Wildlife</strong> Refuge<br />

<strong>Comprehensive</strong> <strong>Conservation</strong> <strong>Plan</strong><br />

humidity during the winter months is about 70 percent. In the spring <strong>and</strong> summer months, daily<br />

humidity increases to about 85 percent. Daily differences in humidity are also present, with the<br />

strongest humidity in the late afternoon <strong>and</strong> early evening (USFWS 2002a).<br />

3.1.2 Kona Forest Unit Climate<br />

Compared to the HFU on windward Mauna Kea, the climate on the Kona side (leeward) of Hawai‘i<br />

Isl<strong>and</strong> is drier. In particular, South Kona is considered one of the most drought-prone regions in the<br />

Hawaiian archipelago (USFWS 2008a). The moisture patterns in the area are driven primarily by<br />

daytime surface heating <strong>and</strong> upslope winds that yield convective rainfall from roughly 2,000 -<br />

5,900 ft. Unlike most areas in the State, the rainy season in Kona occurs during the summer months,<br />

with peaks in June-September <strong>and</strong> low periods from November-February (Juvik <strong>and</strong> Juvik 1998).<br />

Rainfall clearly decreases with elevation at KFU. Areas above 5,000 ft <strong>and</strong> below 2,000 ft elevation<br />

are generally dry (Atkinson et al. 2005). Average annual rainfall at the lower <strong>and</strong> upper area of KFU<br />

can differ by 39 in (USFWS 2008a). Between April 1995-November 1998, the average annual<br />

rainfall varied from 5.63 inches at 2,000 ft to 2.05 inches at 6,000 ft. The climatic differences<br />

between the elevations affect the types of species present <strong>and</strong> species distributions. Seasonal<br />

fluctuations have also been observed at the Refuge. Annual <strong>and</strong> monthly rainfall averages are listed<br />

in Table 3-1.<br />

Table 3-1. Average Monthly Rainfall (inches) at the Kona Forest Unit, April 1995-<br />

November 1998.<br />

Month Elevation<br />

2,000 ft 3,000 ft 4,000 ft 5,000 ft 6,000 ft<br />

January 3.31 2.80 3.00 2.78 2.73<br />

February 1.61 2.07 2.25 1.71 0.82<br />

March 5.28 6.12 6.09 5.42 4.08<br />

April 3.89 4.40 3.26 2.57 1.64<br />

May 4.76 5.77 4.04 2.15 1.30<br />

June 8.45 8.19 7.06 4.74 3.17<br />

July 6.94 5.45 4.10 3.17 1.95<br />

August 6.99 6.48 4.02 2.29 1.73<br />

September 12.2 9.89 6.19 3.07 2.35<br />

October 6.16 4.79 2.19 2.03 1.25<br />

November 3.11 2.85 2.10 1.79 1.42<br />

December 2.37 4.25 4.15 4.01 2.71<br />

Annual Ave. 5.63 5.39 4.05 2.93 2.05<br />

Source: USFWS, unpubl.<br />

Rain is the primary moisture source at elevations from 2,000 - 2,700 ft, while areas above this<br />

elevation also receive moisture from fog drip. The maximum amount of fog drip occurs from 3,000-<br />

6,500 ft. Fog density peaks at about 5,000 ft (USFWS 2008a). “Vog”, volcanic gases <strong>and</strong> particulates<br />

emitted from Kīlauea volcano, is another aspect of the climate on the Isl<strong>and</strong> of Hawai‘i. Vog forms a<br />

distinctive haze <strong>and</strong> has been implicated in causing decreased rainfall <strong>and</strong> plant damage in Kona<br />

forests (USFWS 2008a).<br />

Chapter 3. Physical Environment 3-3

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