Diurnal temperature range drives understory plant community composition in micro-climatically complex temperate montane forests

Cold air drainage is common in mountains, and leads to large, fine-scale differences in diurnal temperature range (DTR). DTR is hypothesized to drive plant community assembly, because areas with high DTR can be exposed to both extreme high and extreme low temperatures in the same day. We established...

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Bibliographic Details
Published in:Environmental research. Ecology Vol. 4; no. 3; pp. 35007 - 35021
Main Authors: Mahood, Adam L, Barnard, David M, Macdonald, Jacob A, Pittenger, David W, Hall, Sarah M, Fornwalt, Paula J
Format: Journal Article
Language:English
Published: IOP Publishing 30.09.2025
Subjects:
cold air drainage
diurnal temperature range
microclimate
plant ecology
topography
vapor pressure deficit
ISSN:2752-664X, 2752-664X
Online Access:Get full text
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Summary:Cold air drainage is common in mountains, and leads to large, fine-scale differences in diurnal temperature range (DTR). DTR is hypothesized to drive plant community assembly, because areas with high DTR can be exposed to both extreme high and extreme low temperatures in the same day. We established networks of temperature and relative humidity sensors along DTR gradients in two montane forest basins, and conducted plant surveys around each sensor ( n = 45). We studied the seasonal stability of DTR and its effects on fine-scale variation in plant community composition, and used topographic metrics to create spatial models of DTR. We found that mean DTR was stable throughout the year, although it was more variable around the mean (i.e. the standard deviation was higher) in winter months. It achieved both time series stability and distinguishability in less than 100 d, and was most strongly associated with daily minimum vapor pressure deficit. DTR measured in situ was the only variable that explained more than 50% of the within-basin variation in species composition for both basins, but among basins coarser-scale variables (actual evapotranspiration, topographic wetness index (TWI), and climatic water deficit) performed better. DTR had a small, negative effect on species richness. Our simple model of DTR explained 64% of the variation, using only TWI and elevation as predictors. These findings illustrate how at broad scales, average temperature and moisture conditions drive the regional species pool, but fine scale distribution of plant species within a basin is driven by microclimate. Accounting for fine-scale topoclimatic processes will lead to better models that capture abiotic gradients, allowing for improved representation of complex ecological processes in earth systems models. Future studies should account for microclimate, especially DTR, when designing experiments, as uneven sampling across microclimates will introduce bias into community observations.
Bibliography:ERE-100175.R2
ISSN:2752-664X
2752-664X
DOI:10.1088/2752-664X/adfa9e