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Seasonal patterns and environmental control of carbon dioxide and water vapour exchange in an ecotonal boreal forest
Author(s) -
Hollinger D. Y.,
Goltz S. M.,
Davidson E. A.,
Lee J. T.,
Tu K.,
Valentine H. T.
Publication year - 1999
Publication title -
global change biology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 4.146
H-Index - 255
eISSN - 1365-2486
pISSN - 1354-1013
DOI - 10.1046/j.1365-2486.1999.00281.x
Subject(s) - environmental science , taiga , ecosystem respiration , ecotone , carbon sink , boreal , carbon dioxide , boreal ecosystem , ecosystem , canopy , atmospheric sciences , photosynthetically active radiation , carbon cycle , ecology , eddy covariance , photosynthesis , botany , biology , geology , shrub
Summary Carbon dioxide, water vapour, and sensible heat fluxes were measured above and within a spruce dominated forest near the southern ecotone of the boreal forest in Maine, USA. Summer, mid‐day carbon dioxide uptake was higher than at other boreal coniferous forests, averaging about – 13 μmol CO 2 m –2 s –1 . Nocturnal summer ecosystem respiration averaged ≈ 6 μmol CO 2 m –2 s –1 at a mean temperature of ≈ 15 °C. Significant ecosystem C uptake began with the thawing of the soil in early April and was abruptly reduced by the first autumn frost in early October. Half‐hourly forest CO 2 exchange was regulated mostly by the incident photosynthetically active photon flux density (PPFD). In addition to the threshold effects of freezing temperatures, there were seasonal effects on the inferred photosynthetic parameters of the forest canopy. The functional response of this forest to environmental variation was similar to that of other spruce forests. In contrast to reports of carbon loss from northerly boreal forest sites, in 1996 the Howland forest was a strong carbon sink, storing about 2.1 t C ha –1 .