Publication | Closed Access
Multiscale analysis of temporal variability of soil CO<sub>2</sub> production as influenced by weather and vegetation
169
Citations
78
References
2009
Year
EngineeringTerrestrial Ecosystem ProductivityCanopy MicrometeorologyTemporal VariabilityEarth ScienceTerrestrial EcosystemMultiscale AnalysisVegetation-atmosphere InteractionsMicrometeorologyWavelet Coherence AnalysisClimate ChangeCarbon SequestrationBiogeochemistryEarth's ClimateClimatologySoil Carbon CycleSoil ModelingAbstract Ecosystem ProcessesSoil Carbon Sequestration
Abstract Ecosystem processes are influenced by weather and climatic perturbations at multiple temporal scales with a large range of amplitudes and phases. Technological advances of automated biometeorological measurements provide the opportunity to apply spectral methods on continuous time series to identify differences in amplitudes and phases and relationships with weather variation. Here we used wavelet coherence analysis to study the temporal covariance between soil CO 2 production and soil temperature, soil moisture, and photosynthetically active radiation (PAR). Continuous (hourly average) data were acquired over 2 years among three vegetation types in a semiarid mixed temperate forest. We showed that soil temperature and soil moisture influence soil CO 2 production differently at multiple periods (e.g. hours, days, weeks, months, years), especially after rain pulse events. Our results provide information about the periodicity of soil CO 2 production among vegetation types, and provide insights about processes controlling CO 2 production through the study of phase relationships between two time series (e.g. soil CO 2 production and PAR). We tested the performance of empirical models of soil CO 2 production using the continuous wavelet transform. These models, built around soil temperature and moisture, failed at multiple periods across the measured dates, suggesting that empirical models should include other factors that regulate soil CO 2 production at different temporal scales. Our results add a new dimension for the analysis of continuous time series of biometeorological measurements and model testing, which will prove useful for analysis of increasing sensor data obtained by environmental networks.
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