This article is a US Government work and is in the public domain in the USA.
Special Issue Article
Article first published online: 27 DEC 2010
This article is a US Government work and is in the public domain in the USA. Published in 2010 by John Wiley & Sons, Ltd.
Special Issue: Hydrometeorology of tropical montane cloud forests
Volume 25, Issue 3, pages 438–447, 30 January 2011
How to Cite
Giambelluca, T. W., DeLay, J. K., Nullet, M. A., Scholl, M. A. and Gingerich, S. B. (2011), Canopy water balance of windward and leeward Hawaiian cloud forests on Haleakalā, Maui, Hawai'i. Hydrol. Process., 25: 438–447. doi: 10.1002/hyp.7738
This paper is partly derived from a chapter previously published as T.W. Giambelluca, J.K. DeLay, M.A. Nullet, M.A. Scholl and S.B. Gingerich (2010). Interpreting canopy water balance and fog screen observations: separating cloud water from wind-blown rainfall at two contrasting forest sites in Hawai'i. In Tropical Montane Cloud Forests. Science for Conservation and Management, eds. L.A. Bruijnzeel, F.N. Scatena and L.S. Hamilton. Cambridge: Cambridge University Press, pp. 342–351. www.cambridge.org/9780521760355
- Issue published online: 20 JAN 2011
- Article first published online: 27 DEC 2010
- Manuscript Accepted: 6 APR 2010
- Manuscript Received: 24 NOV 2009
- US Geological Survey
- Water Resources Discipline
- Venture Capital Fund
- US National Science Foundation. Grant Number: EAR-0309731
- US Geological Survey
- Biological Resources Discipline
- tropical montane cloud forest;
- cloud water interception;
The contribution of intercepted cloud water to precipitation at windward and leeward cloud forest sites on the slopes of Haleakalā, Maui was assessed using two approaches. Canopy water balance estimates based on meteorological monitoring were compared with interpretations of fog screen measurements collected over a 2-year period at each location. The annual incident rainfall was 973 mm at the leeward site (Auwahi) and 2550 mm at the windward site (Waikamoi). At the leeward, dry forest site, throughfall was less than rainfall (87%), and, at the windward, wet forest site, throughfall exceeded rainfall (122%). Cloud water interception estimated from canopy water balance was 166 mm year−1 at Auwahi and 1212 mm year−1 at Waikamoi. Annual fog screen measurements of cloud water flux, corrected for wind-blown rainfall, were 132 and 3017 mm for the dry and wet sites respectively. Event totals of cloud water flux based on fog screen measurements were poorly correlated with event cloud water interception totals derived from the canopy water balance. Hence, the use of fixed planar fog screens to estimate cloud water interception is not recommended. At the wet windward site, cloud water interception made up 32% of the total precipitation, adding to the already substantial amount of rainfall. At the leeward dry site, cloud water interception was 15% of the total precipitation. Vegetation at the dry site, where trees are more exposed and isolated, was more efficient at intercepting the available cloud water than at the rainy site, but events were less frequent, shorter in duration and lower in intensity. A large proportion of intercepted cloud water, 74% and 83%, respectively for the two sites, was estimated to become throughfall, thus adding significantly to soil water at both sites. Published in 2010 by John Wiley & Sons, Ltd.