Land Carbon Sequestration and Climate: Present and Future

A special issue of Atmosphere (ISSN 2073-4433). This special issue belongs to the section "Biosphere/Hydrosphere/Land–Atmosphere Interactions".

Deadline for manuscript submissions: closed (31 December 2015) | Viewed by 12587

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Guest Editor
Lawrence Berkeley National Lab, 1 Cyclotron Rd, Berkeley, CA 94720, USA
Interests: biosphere-atmosphere interactions; climate change; terrestrial remote sensing; GIS-ecology
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Special Issue Information

Dear Colleagues,

Atmospheric CO2 concentrations have increased dramatically over the past 150 years, from a pre-industrial value of 280 ppm to nearly 400 ppm today, and are projected to increase to 500–1,000 ppm by 2100. This increase in atmospheric CO2 will result in increases in global temperature and dramatic changes in the Earth Climate system. Land ecosystems draw down atmospheric CO2 through photosynthesis, and therefore play a key role in mitigating the effects of increased CO2 on the climate. Understanding (i) the functionality of land ecosystems, (ii) their climate feedbacks, and (iii) the role they play as atmospheric carbon absorbers is therefore critical to a proper understanding of Earth’s future climate.

Studies that address these research topics in the context of present and future Land carbon sequestration-Climate are welcome for publication in Atmosphere. Studies that integrate field data, remote sensing data, and modeling are especially encouraged.

Dr. Robinson I. Negron-Juarez
Guest Editor

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Keywords

  • land ecosystems
  • carbon sequestration
  • climate projections

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Published Papers (2 papers)

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Research

6127 KiB  
Article
Biophysical Impacts of Land Use Change over North America as Simulated by the Canadian Regional Climate Model
by Arlette Chacón, Laxmi Sushama and Hugo Beltrami
Atmosphere 2016, 7(3), 34; https://doi.org/10.3390/atmos7030034 - 26 Feb 2016
Cited by 4 | Viewed by 5757
Abstract
This study investigates the biophysical impacts of human-induced land use change (LUC) on the regional climate of North America, using the fifth generation Canadian Regional Climate Model (CRCM5). To this end, two simulations are performed with CRCM5 using different land cover datasets, one [...] Read more.
This study investigates the biophysical impacts of human-induced land use change (LUC) on the regional climate of North America, using the fifth generation Canadian Regional Climate Model (CRCM5). To this end, two simulations are performed with CRCM5 using different land cover datasets, one corresponding to the potential vegetation and the other corresponding to current land use, spanning the 1988–2012 period, driven by European Centre for Medium-Range Weather Forecasts Re-Analysis (ERA)-Interim at the lateral boundaries. Comparison of the two suggests higher albedo values, and therefore cooler temperatures, over the LUC regions, in the simulation with LUC, in winter. This is due to the absence of crops in winter, and also possibly due to a snow-mediated positive feedback. Some cooling is observed in summer for the simulation with LUC, mostly due to the higher latent heat fluxes and lower sensible heat fluxes over eastern US. Precipitation changes for these regions are not statistically significant. Analysis of the annual cycles for two LUC regions suggests that the impact of LUC on two meter temperature, evapotranspiration, soil moisture and precipitation are present year round. However, the impact on runoff is mostly restricted to the snowmelt season. This study thus highlights regions and variables most affected by LUC over North America. Full article
(This article belongs to the Special Issue Land Carbon Sequestration and Climate: Present and Future)
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902 KiB  
Article
Carbon Sequestration and Carbon Markets for Tree-Based Intercropping Systems in Southern Quebec, Canada
by Kiara S. Winans, Joann K. Whalen, David Rivest, Alain Cogliastro and Robert L. Bradley
Atmosphere 2016, 7(2), 17; https://doi.org/10.3390/atmos7020017 - 28 Jan 2016
Cited by 14 | Viewed by 6343
Abstract
Since agriculture directly contributes to global anthropogenic greenhouse gas (GHG) emissions, integrating trees into agricultural landscapes through agroforestry systems is a viable adaptive strategy for climate change mitigation. The objective of this study was to evaluate the carbon (C) sequestration and financial benefits [...] Read more.
Since agriculture directly contributes to global anthropogenic greenhouse gas (GHG) emissions, integrating trees into agricultural landscapes through agroforestry systems is a viable adaptive strategy for climate change mitigation. The objective of this study was to evaluate the carbon (C) sequestration and financial benefits of C sequestration according to Quebec’s Cap-and-Trade System for Greenhouse Gas Emissions Allowances (C & T System) or the Système de plafonnement et d’échange de droits d’émission de gaz à effet de serre du Québec (SPEDE) program for two experimental 10-year-old tree-based intercropping (TBI) systems in southern Quebec, Canada. We estimated total C stored in the two TBI systems with hybrid poplar and hardwoods and adjacent non-TBI systems under agricultural production, considering soil, crop and crop roots, litterfall, tree and tree roots as C stocks. The C sequestration of the TBI and adjacent non-TBI systems were compared and the market value of the C payment was evaluated using the net present value (NPV) approach. The TBI systems had 33% to 36% more C storage than adjacent non-TBI systems. The financial benefits of C sequestration after 10 years of TBI practices amounted to of $2,259–$2,758 CAD ha−1 and $1,568–$1,913 CAD ha−1 for St. Edouard and St. Paulin sites, respectively. We conclude that valorizing the C sequestration of TBI systems could be an incentive to promote the establishment of TBI for the purpose of GHG mitigation in Quebec, Canada. Full article
(This article belongs to the Special Issue Land Carbon Sequestration and Climate: Present and Future)
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