828 research outputs found

    Quantifying the carbon sequestration costs for Pinus elliottii afforestation project of China greenhouse gases voluntary emission reduction program: a case study in Jiangxi province

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    Afforestation and reforestation (AR) is an important component of China’s Greenhouse Gases (GHG) Voluntary Emission Reduction Program, acting as a valuable nationwide carbon sink. Although a number of studies have explored the costs of creating a carbon sink, such an assessment is lacking for China’s GHG Voluntary Emissions Reduction Program. This study develops an economic carbon sink costs measurement model for the Pinus elliottii afforestation project, based on the land opportunity cost method, which incorporates carbon sink transaction costs and leakage costs. From this, an empirical analysis on the carbon sink costs and its sensitivity factors was conducted. The results show that, firstly, the carbon sequestration costs of afforestation projects are generally high, ranging from 44.2 Yuan/tCO2e to 425.4 Yuan/tCO2e with and without considering the benefits of wood, respectively. This is higher than the current average carbon sink price of 20 Yuan/tCO2e. Secondly, forestry carbon sink transaction costs have a positive impact on carbon sequestration costs, but the impact is weak. Thirdly, carbon sequestration costs are negatively affected by timber prices but positively influenced by increasing labor prices and discount rate, which is not conductive to the development of carbon sink afforestation projects. In order to strengthen role of forestry in combating climate change, the study holds that the government departments should take measures to reduce carbon sink transaction costs, establish and improve the forestry carbon sink compensation mechanism in the future, and encourage wood-processing companies to make technological innovations to produce and sell durable wood products. The project owners can explore multiple operating models to increase their revenue, including market and non-market benefits, when the carbon sink afforestation project has been launched according to relevant methodologies

    Preliminary Analysis of the Metabolic Rate Monitor System

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    Metabolic rate monitor system analysi

    Orbital-scale climate variability in Arabia as a potential motor for human dispersals

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    The Arabian Peninsula is situated at an important crossroads for the movement of Pleistocene human populations out of, and into, Africa. Although the timings, routes and frequencies of such dispersals have not yet been confirmed by genetic, fossil or archaeological evidence, expansion into Arabia would have been facilitated by humid periods driven by incursions of monsoon rainfall, potentially from both Indian Ocean and African monsoon systems. Here we synthesise terrestrial and marine core palaeoclimatic data in order to establish the spatial and temporal variability of humid periods in Arabia between late Marine Isotope Stage (MIS) 7 and 3. Incursions of monsoon rainfall occurred during periods of insolation maxima at ca. 200–190, 170, 155, 130–120, 105–95, 85–75 and 60–55 ka, providing multiple ‘windows’ of favourable climatic conditions that could have facilitated demographic expansion through Arabia. Strong summer monsoons are generally associated with mid-high latitude interglacials, however, enhanced monsoon convection also brought rainfall into Arabia during global glacial phases, possibly due to a strengthened winter monsoon and a greater influence of southern hemispheric temperature changes. Key periods for dispersal into northern regions of Arabia correspond with the synchronous intensification of both eastern Mediterranean and monsoon rainfall systems at insolation maxima during MIS 7 and MIS 5, which may have facilitated demographic connectivity between the Levant and the Arabian interior. Environmental conditions throughout southern and southeast regions were also favourable to expansion during these times, although strong monsoons in these regions during MIS 6 and MIS 3 suggest further opportunities for demographic expansion and exchange. Terrestrial and marine evidence show that during early MIS 3 (ca. 60–50 ka), a strengthened monsoon led to the activation of interior drainage systems and increased productivity in coastal zones, indicating that favourable environmental conditions existed along both coastal and interior routes at that time
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