Abstract

Global warming is among the greatest terrible horrors of the modern times. The global carbon cycle is taking place in three main reservoirs (the oceans, the atmosphere, and terrestrial systems), which store carbon in different forms and varying amounts. The forest ecosystems have large potential to act as a temporary and long-term carbon (C) pool. Global forest vegetation stores 283 Gt of carbon in its biomass, 38 Gt in dead wood and 317 Gt in soils (top 30 cm) and litter. Globally, the litter C pool accounts for an estimated 5% (43 Pg) of all forest ecosystem C stocks. Agroforestry practices can reduce or remove significant amounts of GHGs through increased carbon storage in biomass above-ground and below-ground and in soil organic carbon. Roots are an important part of the C balance, because they transfer large amounts of C into the soil. Grasslands, including rangelands, shrublands, pastureland, and cropland sown with pasture and fodder crops, covered approximately 3.5 billion ha in 2000, representing 26 percent of the world land area and 70 percent of the world agricultural area, and containing about 20 percent of the world’s soil carbon stocks. Soils are the largest carbon reservoirs of the terrestrial carbon cycle 1500–1550 Gt of organic soil carbon and soil inorganic C approximate 750 Gt both to 1 m depth. On a global scale, carbon loss from soils is mainly associated with soil degradation, including accelerated erosion and mineralization, and land use change, and has amounted to 78+/- 12 Gt since 1850. The idea of Reducing Emissions from Deforestation and forest Degradation (REDD) was conceived by United Nations Framework Convention on Climate Change (UNFCCC) as the main carbon emission reduction mechanism by developing countries. The implementation of improved land management practices to build up carbon stocks in terrestrial ecosystems is a proven technology for reducing the concentration of carbon dioxide (CO2) in the atmosphere – offsetting emissions from other sources and drawing down atmospheric CO2. Keywords: Carbon sequestration, Terrestrial carbon, Global warming and Carbon stocks. DOI: 10.7176/JEES/10-8-04 Publication date: August 31 st 2020

Highlights

  • IntroductionCarbon is present in the nonliving environment as carbon dioxide (CO2) gas in the atmosphere, as dissolved carbon in water (forming bicarbonate and carbonate solutions), and in carbonate rocks, coal, petroleum, natural gas, and dead organic matter (humus)

  • Carbon is present in the nonliving environment as carbon dioxide (CO2) gas in the atmosphere, as dissolved carbon in water, and in carbonate rocks, coal, petroleum, natural gas, and dead organic matter

  • The greenhouse gases with special optical properties that are responsible for climate warming include carbon dioxide (CO2), water vapors, Methane (CH4), Nitrous oxide (N2O), Nitrogen oxides (NOx), stratospheric ozone (O3), carbon monoxide (CO) and Chlorofluorocarbons (CFC’s)

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Summary

Introduction

Carbon is present in the nonliving environment as carbon dioxide (CO2) gas in the atmosphere, as dissolved carbon in water (forming bicarbonate and carbonate solutions), and in carbonate rocks, coal, petroleum, natural gas, and dead organic matter (humus). Climate change 2007: The physical science basis (Cambridge University Press, Cambridge, UK and New York, USA, 2007). IPCC Special Report on Climate Change, Desertification, Land Degradation, Sustainable Land Management, Food Security, and Greenhouse gas fluxes in Terrestrial Ecosystems. Scenario analysis of the impacts of forest management and climate change on the European forest sector carbon budget. Soil Carbon Sequestration impacts on global climate change and food security. Carbon sequestration potential of agroforestry systems in Africa. In: Kumar BM, Nair PKR (eds) Carbon sequestration potential of agroforestry systems: opportunities and challenges. The Nature and Management of Ethiopian Soils, Alemaya University of Agriculture (AUA), Ethiopia. Soil carbon sequestration in tropical agroforestry systems: a feasibility appraisal. Adaptation to Climate Change through Sustainable Management and Development of Agroforestry Systems. Carbon Sequestration Potential of Traditionally Managed Forest: Contributions to Climate Change Mitigation, Ethiopia.

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