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Tree Physiology Advance Access originally published online on January 20, 2009
Tree Physiology 2009 29(4):517-528; doi:10.1093/treephys/tpn043
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© The Author 2009. Published by Oxford University Press. All rights reserved. For Permissions, please email: journals.permissions@oxfordjournals.org

Fog reduces transpiration in tree species of the Canarian relict heath-laurel cloud forest (Garajonay National Park, Spain)

Axel Ritter1, Carlos M. Regalado1,2 and Guido Aschan3

1 Instituto Canario de Investigaciones Agrarias (ICIA), Departamento Suelos y Riegos, Apdo. 60 La Laguna, 38200 S/C Tenerife, Spain
2 Corresponding author (cregalad{at}icia.es)
3 Applied Botany, University of Duisburg-Essen, Universitätsstr. 5, D-45117 Essen, Germany


   Abstract

The ecophysiologic role of fog in the evergreen heath-laurel ‘laurisilva’ cloud forests of the Canary Islands has not been unequivocally demonstrated, although it is generally assumed that fog water is important for the survival and the distribution of this relict paleoecosystem of the North Atlantic Macaronesian archipelagos. To determine the role of fog in this ecosystem, we combined direct transpiration measurements of heath-laurel tree species, obtained with Granier’s heat dissipation probes, with micrometeorological and artificial fog collection measurements carried out in a 43.7-ha watershed located in the Garajonay National Park (La Gomera, Canary Islands, Spain) over a 10-month period. Median ambient temperature spanned from 7 to 15 °C under foggy conditions whereas higher values, ranging from 9 to 21 °C, were registered during fog-free periods. Additionally, during the periods when fog water was collected, global solar radiation values were linearly related (r2 = 0.831) to those under fog-free conditions, such that there was a 75 ± 1% reduction in median radiation in response to fog. Fog events greatly reduced median diurnal tree transpiration, with rates about 30 times lower than that during fog-free conditions and approximating the nighttime rates in both species studied (the needle-like leaf Erica arborea L. and the broadleaf Myrica faya Ait.). This large decrease in transpiration in response to fog was independent of the time of the day, tree size and species and micrometeorological status, both when expressed on a median basis and in cumulative terms for the entire 10-month measuring period. We conclude that, in contrast to the turbulent deposition of fog water droplets on the heath-laurel species, which may be regarded as a localized hydrological phenomenon that is important for high-altitude wind-exposed E. arborea trees, the cooler, wetter and shaded microenvironment provided by the cloud immersion belt represents a large-scale effect that is crucial for reducing the transpirational water loss of trees that have profligate water use, such as those of the ‘laurisilva’.

Keywords: climate change, cloud immersion, Granier probes, sap flow, solar radiation reduction, transpiration monitoring

Received July 2, 2008; Accepted November 17, 2008


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