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‘Breathing’ of the terrestrial biosphere: lessons learned from a global network of carbon dioxide flux measurement systems

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TLDR
Key findings reported include: ecosystems with the greatest net carbon uptake have the longest growing season, not the greatest FA; many old-growth forests act as carbon sinks; and year-to-year decreases in FN are attributed to a suite of stresses that decrease FA and FR in tandem.
Abstract
Published eddy covariance measurements of carbon dioxide (CO2) exchange between vegetation and the atmosphere from a global network are distilled, synthesised and reviewed according to time scale, climate and plant functional types, disturbance and land use. Other topics discussed include history of the network, errors and issues associated with the eddy covariance method, and a synopsis of how these data are being used by ecosystem and climate modellers and the remote-sensing community. Spatial and temporal differences in net annual exchange, FN, result from imbalances in canopy photosynthesis (FA) and ecosystem respiration (FR), which scale closely with one another on annual time scales. Key findings reported include the following: (1) ecosystems with the greatest net carbon uptake have the longest growing season, not the greatest FA; (2) ecosystems losing carbon were recently disturbed; (3) many old-growth forests act as carbon sinks; and (4) year-to-year decreases in FN are attributed to a suite of stresses that decrease FA and FR in tandem. Short-term flux measurements revealed emergent-scale processes including (1) the enhancement of light use efficiency by diffuse light, (2) dynamic pulses in FR following rain and (3) the acclimation FA and FR to temperature. They also quantify how FA and FR respond to droughts and heat spells.

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Journal ArticleDOI

Seasonal and inter-annual variability of energy exchange above a boreal Scots pine forest

TL;DR: In this paper, 12 years of eddy-covariance measurements conducted above a boreal Scots pine forest in Hyytiala, Southern Finland were analyzed to assess the seasonal and inter-annual variability of surface conductance (gs) and energy partitioning.
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An improved isotopic method for partitioning net ecosystem–atmosphere CO2 exchange

TL;DR: In this article, the authors extended the theory of isotopic flux partitioning to include photorespiration, foliar daytime respiration, and other refinements, arriving at a general yet practical formulation from which all previous formulations can be derived as simplifying approximations.

A Review of Global Terrestrial Evapotranspiration: Observation, Modeling, Climatology, and Climatic Variability

TL;DR: In this article, the authors survey the basic theories, observational methods, satellite algorithms, and land surface models for terrestrial evapotranspiration, including a long-term variability and trends perspective.
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Ecosystem CO2 fluxes of arbuscular and ectomycorrhizal dominated vegetation types are differentially influenced by precipitation and temperature.

TL;DR: This study represents the first large-scale assessment of terrestrial CO(2) fluxes in multiple vegetation types classified according to dominant mycorrhizal association and supports and complement the hypothesis that bioclimatic conditions influence the distribution of AM and EM systems across large geographical distances.
References
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Journal ArticleDOI

The Strategy of Ecosystem Development

TL;DR: The principles of ecological succession bear importantly on the relationships between man and nature and needs to be examined as a basis for resolving man’s present environmental crisis.
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Climate Extremes: Observations, Modeling, and Impacts

TL;DR: Results of observational studies suggest that in many areas that have been analyzed, changes in total precipitation are amplified at the tails, and changes in some temperature extremes have been observed.
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Correction of flux measurements for density effects due to heat and water vapour transfer

TL;DR: In this article, the basic relationships are discussed in the context of vertical transfer in the lower atmosphere, and the required corrections to the measured flux are derived, where the correction to measurements of water vapour flux will often be only a few per cent but will sometimes exceed 10 percent.
Journal ArticleDOI

Aerosols, climate, and the hydrological cycle

TL;DR: Human activities are releasing tiny particles (aerosols) into the atmosphere that enhance scattering and absorption of solar radiation, which can lead to a weaker hydrological cycle, which connects directly to availability and quality of fresh water, a major environmental issue of the 21st century.
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