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Topoclimate effects on growing season length and montane conifer growth in complex terrain

Bibliographic Data

ID15548211
AuthorsDavid M Barnard (0000-0003-1877-3151, University of Colorado Boulder, corresponding author), Holly Barnard (0000-0003-1965-8542, University of Colorado Boulder, corresponding author), H R Barnard, N P Molotch (0000-0003-4733-8060, Institute of Arctic and Alpine Research)
Year2017
Volume12
Issue6
Pages064003-064003
Publication date2017-05-01
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueEnvironmental Research Letters (JOURNAL)
Journal identifiersISSN: 1748-9326 • E-ISSN: 1748-9326
PublisherIOP Publishing (PUBLISHER • GB)
DOI10.1088/1748-9326/aa6da8
OpenAlexW2619831090
LanguageEN
References cited63

Spatial variability in the topoclimate-driven linkage between forest phenology and tree growth in complex terrain is poorly understood, limiting our understanding of how ecosystems function as a whole. To characterize the influence of topoclimate on phenology and growth, we determined the start, end, and length of the growing season (GS(start), GS(end), and GSL, respectively) using the correlation between transpiration and evaporative demand, measured with sapflow. We then compared these metrics with stem relative basal area increment (relative BAI) at seven sites among elevation and aspects in a Colorado montane forest. As elevation increased, we found shorter GSL (-50 d km(-1)) due to later GS(start) (40 d km(-1)) and earlier GS(end) (-10 d km(-1)). North-facing sites had a 21 d shorter GSL than south-facing sites at similar elevations (i.e. equal to 200 m elevation difference on a given aspect). Growing season length was positively correlated with relative BAI, explaining 83% of the variance. This study shows that topography exerts strong environmental controls on GSL and thus forest growth. Given the climate-related dependencies of these controls, the results presented here have important implications for ecosystem responses to changes in climate and highlight the need for improved phenology representation in complex terrain

Atmospheric sciences · Basal area · Biology · Climate change · Ecosystem · Elevation (ballistics · Geography · Growing season · Growth function · Meteorology · Phenology · Physical geography · Precipitation · Terrain · Environmental Science · Mathematics · Plant Water Relations and Carbon Dynamics · Remote Sensing in Agriculture · Tree-ring climate responses · Ecology · Geology

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