Aboveground sink strength in forests controls the allocation of carbon below ground and its [CO2]-induced enhancement - Test2 - elhamkhani - TriplyDB

Aboveground sink strength in forests controls the allocation of carbon below ground and its [CO2]-induced enhancement

Aboveground sink strength in forests controls the allocation of carbon below ground and its [CO2]-induced enhancement

http://www.wikidata.org/entity/Q35539972

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Where does the carbon go? A model-data intercomparison of vegetation carbon allocation and turnover processes at two temperate forest free-air CO2 enrichment sites Evaluation of 11 terrestrial carbon-nitrogen cycle models against observations from two temperate Free-Air CO2 Enrichment studies The space-time continuum: the effects of elevated CO2 and temperature on trees and the importance of scaling.A synthesis of the effects of atmospheric carbon dioxide enrichment on plant hydraulics: implications for whole-plant water use efficiency and resistance to drought.Increased litterfall in tropical forests boosts the transfer of soil CO2 to the atmosphere.A stomatal optimization theory to describe the effects of atmospheric CO2 on leaf photosynthesis and transpiration The spatial factor, rather than elevated CO₂, controls the soil bacterial community in a temperate Forest Ecosystem Relative information contributions of model vs. data to short- and long-term forecasts of forest carbon dynamics.Pulse-labelling trees to study carbon allocation dynamics: a review of methods, current knowledge and future prospects.Forest water use and water use efficiency at elevated CO2 : a model-data intercomparison at two contrasting temperate forest FACE sites.Canopy leaf area constrains [CO2]-induced enhancement of productivity and partitioning among aboveground carbon pools Increases in nitrogen uptake rather than nitrogen-use efficiency support higher rates of temperate forest productivity under elevated CO2.Dynamics of soil CO2 efflux under varying atmospheric CO2 concentrations reveal dominance of slow processes.Annual climate variation modifies nitrogen induced carbon accumulation of Pinus sylvestris forests.The likely impact of elevated [CO2], nitrogen deposition, increased temperature and management on carbon sequestration in temperate and boreal forest ecosystems: a literature review.Are above- and below-ground phenology in sync?Allometric constraints on, and trade-offs in, belowground carbon allocation and their control of soil respiration across global forest ecosystems.Increases in the flux of carbon belowground stimulate nitrogen uptake and sustain the long-term enhancement of forest productivity under elevated CO₂.Production and turnover of ectomycorrhizal extramatrical mycelial biomass and necromass under elevated CO2 and nitrogen fertilization.Re-assessment of plant carbon dynamics at the Duke free-air CO(2) enrichment site: interactions of atmospheric [CO(2)] with nitrogen and water availability over stand development.Relationship between fine-root exudation and respiration of two Quercus species in a Japanese temperate forest.Increases in atmospheric CO2 have little influence on transpiration of a temperate forest canopy.Stem compression reversibly reduces phloem transport in Pinus sylvestris trees.Enhanced root exudation induces microbial feedbacks to N cycling in a pine forest under long-term CO2 fumigation.Sustained effects of atmospheric [CO2] and nitrogen availability on forest soil CO2 efflux.Increased resin flow in mature pine trees growing under elevated CO2 and moderate soil fertility.Moving beyond photosynthesis: from carbon source to sink-driven vegetation modeling.Redefinition and global estimation of basal ecosystem respiration rate Optimal Function Explains Forest Responses to Global Change Terrestrial nitrogen feedbacks may accelerate future climate change Linking plant functional trait plasticity and the large increase in forest water use efficiency Carbon allocation in forest ecosystems Carbon allocation in boreal black spruce forests across regions varying in soil temperature and precipitation Total belowground carbon flux in subalpine forests is related to leaf area index, soil nitrogen, and tree height

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P2860

Aboveground sink strength in forests controls the allocation of carbon below ground and its [CO2]-induced enhancement

http://www.wikidata.org/entity/Q35539972

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2006 nî lūn-bûn

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2006 թուականի Դեկտեմբերին հրատարակուած գիտական յօդուած

@hyw

2006 թվականի դեկտեմբերին հրատարակված գիտական հոդված

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2006年の論文

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2006年論文

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2006年論文

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2006年論文

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2006年論文

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2006年論文

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2006年论文

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Aboveground sink strength in f ...... its [CO2]-induced enhancement

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Aboveground sink strength in f ...... its [CO2]-induced enhancement

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Aboveground sink strength in f ...... its [CO2]-induced enhancement

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P1433

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PNAS.0609492103

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Proceedings of the National Academy of Sciences of the United States of America

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Aboveground sink strength in f ...... its [CO2]-induced enhancement

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P2093

Kurt H Johnsen

http://www.w3.org/2001/XMLSchema#string

Sari Palmroth

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William H Schlesinger

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P2860

Forest response to elevated CO2 is conserved across a broad range of productivity.

Limited carbon storage in soil and litter of experimental forest plots under increased atmospheric CO2.

Canopy leaf area constrains [CO2]-induced enhancement of productivity and partitioning among aboveground carbon pools

Fine-root production dominates response of a deciduous forest to atmospheric CO2 enrichment.

Belowground carbon cycling in a humid tropical forest decreases with fertilization.

Effects of elevated concentrations of atmospheric CO2 and tropospheric O3 on leaf litter production and chemistry in trembling aspen and paper birch communities.

Leaf dynamics of a deciduous forest canopy: no response to elevated CO2.

Soil fertility limits carbon sequestration by forest ecosystems in a CO2-enriched atmosphere.

Tropospheric O(3) compromises net primary production in young stands of trembling aspen, paper birch and sugar maple in response to elevated atmospheric CO(2).

Foliage, fine-root, woody-tissue and stand respiration in Pinus radiata in relation to nitrogen status.

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19362-19367

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scholarly article

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10.1073/PNAS.0609492103

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51

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103

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Heather R McCarthy

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2006-12-11T00:00:00Z

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6640835

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17159142

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1748231

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