Terrestrial ecosystem carbon dynamics and climate feedbacks

By Martin Heimann, Markus Reichstein. Nature, 2008

1,599 citations recorded by the source corpus.

Subfields: Global and Planetary Change, Plant Science

View Paper: https://www.semanticscholar.org/paper/6446a4ee2ff9618519dc028eb41fb419533075c6

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Global and Planetary Change

In Plant Science

Citations in the corpus

Microbial contributions to climate change through carbon cycle feedbacks (2008, background): “Of these, perhaps the greatest is the need to better understand the biological mechanisms regulating carbon exchanges between the land, oceans and atmosphere and how these exchanges will respond to climate change through climate–ecosystem feedbacks, which could amplify or dampen regional and global ”
The REFLEX project: Comparing different algorithms and implementations for the inversion of a terrestrial ecosystem model against eddy covariance data (2009, background): “54 55 Fox, Williams et al. 5 Introduction 56 The carbon cycle is a critical determinant of the Earth‟s climate, but the carbon-climate 57 relationship is complicated by feedbacks between the climate, the terrestrial biosphere and the 58 atmosphere (Heimann and Reichstein 2008).”
Microbial mediation of carbon-cycle feedbacks to climate warming (2012, neutral): “dtd" [ ]> Understanding the mechanisms of biospheric feedbacks to climate change is critical to project future climate warmin”
Identification of 100 fundamental ecological questions (2013, background): “Another suite of human impacts is more indirect but perhaps even more pervasive; through our alteration of the climate (both its mean state and variability; IPCC 2007; Hannah 2011) and changes in the biogeochemistry of the atmosphere and oceans (Heimann & Reichstein 2008; Doney et al. 2009).”
Root-induced changes in nutrient cycling in forests depend on exudation rates (2014, neutral): “The degree to which such shifts affect long-term ecosystem C storage in forests, and subsequent feedbacks to global climate, warrants further study (Heimann and Reichstein, 2008).”
The Future of Earth Observation in Hydrology. (2017, neutral): “…mission would have provided key insights into permafrost processes, particularly the freeze/thaw state, which acts as a proxy for monitoring methane and carbon release (Heimann and Reichstein, 2008), forest productivity (Kimball et al., 2001) and sub-surface flow processes (Bayard et al., 2005).”
Global response patterns of terrestrial plant species to nitrogen addition. (2008, background): “Thus, the central question of carbon–climate interactions is how N availability impacts the capacity of the terrestrial ecosystem to sequester C from the atmosphere (Gruber & Galloway, 2008; Heimann & Reichstein, 2008 ).”
Does accelerated soil organic matter decomposition in the presence of plants increase plant N availability (2009, neutral): “rhizosphere priming effect should be considered as an important mechanism affecting the global C cycle (Heimann and Reichstein, 2008).”
Effect of temperature on metabolic activity of intact microbial communities: Evidence for altered metabolic pathway activity but not for increased maintenance respiration and reduced carbon use efficiency (2011, background): “Understanding the response of microbial metabolism to increased temperature is critical to predicting the future size of the terrestrial C sink (Bradford et al., 2008; Davidson and Janssens, 2006; Heimann and Reichstein, 2008).”
Climate control of terrestrial carbon exchange across biomes and continents (2010, neutral): “Yi, C, Ricciuto, D, Li, R, Wolbeck, J, Xu, X, Nilsson, M, Aires, L, Albertson, JD, Ammann, C, Arain, MA, de Araujo, AC, Aubinet, M, Aurela, M, Barcza, Z, Barr, A, Berbigier, P, Beringer, J, Bernhofer, C, Black, AT, Bolstad, PV, Bosveld, FC, Broadmeadow, MSJ, Buchmann, N, Burns, SP, Cellier, P, Chen,”
The global nitrogen cycle in the twenty-first century (2013, methodology): “This may be compared with a rough estimate made using the annual terrestrial global C sequestration [79] and Churkina et al.”