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气候变化、过敏与哮喘以及热带森林的作用

Climate change, allergy and asthma, and the role of tropical forests.

作者信息

D'Amato Gennaro, Vitale Carolina, Rosario Nelson, Neto Herberto Josè Chong, Chong-Silva Deborah Carla, Mendonça Francisco, Perini Josè, Landgraf Loraine, Solé Dirceu, Sánchez-Borges Mario, Ansotegui Ignacio, D'Amato Maria

机构信息

Division of Respiratory and Allergic Diseases, Department of Respiratory Diseases, High Specialty Hospital A. Cardarelli, Napoli, Italy.

School of Specialization in Respiratory Diseases, University of Napoli Federico II, Napoli, Italy.

出版信息

World Allergy Organ J. 2017 Mar 7;10(1):11. doi: 10.1186/s40413-017-0142-7. eCollection 2017.

Abstract

BACKGROUND

Tropical forests cover less than 10 per cent of all land area (1.8 × 107 km) and over half of the tropical-forest area (1.1 × 107 Km) is represented by humid tropical forests (also called tropical rainforests). The Amazon basin contains the largest rainforest on Earth, almost 5.8 million km, and occupies about 40% of South America; more than 60% of the basin is located in Brazil and the rest in Bolivia, Colombia, Ecuador, French Guiana, Guyana, Peru, Suriname and Venezuela. Over the past decade the positive role of tropical rainforests in capturing large amounts of atmospheric carbon dioxide (CO) has been demonstrated. In response to the increase in atmospheric CO concentration, tropical forests act as a global carbon sink.

MAIN BODY

Accumulation of carbon in the tropical terrestrial biosphere strongly contributes to slowing the rate of increase of CO into the atmosphere, thus resulting in the reduction of greenhouse gas effect. Tropical rainforests have been estimated to account for 32-36% of terrestrial Net Primary Productivity (NPP) that is the difference between total forest photosynthesis and plant respiration. Tropical rainforests have been acting as a strong carbon sink in this way for decades. However, over the past years, increased concentrations of greenhouse gases, and especially CO, in the atmosphere have significantly affected the net carbon balance of tropical rainforests, and have warmed the planet substantially driving climate changes through more severe and prolonged heat waves, variability in temperature, increased air pollution, forest fires, droughts, and floods. The role of tropical forests in mitigating climate change is therefore critical. Over the past 30 years almost 600,000 km have been deforested in Brazil alone due to the rapid development of Amazonia, this is the reason why currently the region is one of the 'hotspots' of global environmental change on the planet.

CONCLUSION

Deforestation represents the second largest anthropogenic source of CO to the atmosphere, after fossil fuel combustion. There are many causes of deforestation, including socioeconomic and natural factors, such as clear-cutting for agriculture, ranching and development, unsustainable logging for timber, as well as droughts, fires and degradation due to climate change. About natural causes of forest degradation, in the context of the Amazon, the major agent of change in the forest ecosystem would most likely be decreased dry-season precipitation. Of the 23 global climate models employed by the Intergovernmental Panel on Climate Change (IPCC) in their 2007 report, 50-70% predict a substantial (above 20%) reduction of dry-season rainfall in eastern Amazonia under mid-range greenhouse gas emissions scenarios, 40% in central Amazonia and 20% in the west. While annual carbon emissions from fossil-fuel combustion have been continually increasing since 1960s, historical trends of deforestation and associated carbon emissions have remained poorly understood.

摘要

背景

热带森林覆盖面积不到全球陆地总面积(1.8×10⁷平方千米)的10%,而超过一半的热带森林面积(1.1×10⁷平方千米)为湿润热带森林(又称热带雨林)。亚马孙河流域拥有地球上最大的雨林,面积近580万平方千米,约占南美洲面积的40%;该流域60%以上位于巴西,其余分布在玻利维亚、哥伦比亚、厄瓜多尔、法属圭亚那、圭亚那、秘鲁、苏里南和委内瑞拉。在过去十年中,热带雨林在捕获大量大气二氧化碳(CO₂)方面的积极作用已得到证实。为应对大气中CO₂浓度的增加,热带森林起到了全球碳汇的作用。

主体

热带陆地生物圈中的碳积累有力地减缓了CO₂排入大气的速率,从而减少了温室气体效应。据估计,热带雨林占陆地净初级生产力(NPP)的32% - 36%,净初级生产力即森林总光合作用与植物呼吸作用的差值。几十年来,热带雨林一直以这种方式充当着强大的碳汇。然而,在过去几年中,大气中温室气体浓度的增加,尤其是CO₂浓度的增加,已显著影响了热带雨林的净碳平衡,并使地球大幅升温,通过更严重和持久的热浪、温度变化、空气污染增加、森林火灾、干旱和洪水推动了气候变化。因此,热带森林在缓解气候变化方面的作用至关重要。在过去30年里,仅巴西就因亚马孙地区的快速发展砍伐了近60万平方千米的森林,这就是为什么该地区目前是全球环境变化的“热点”地区之一。

结论

森林砍伐是仅次于化石燃料燃烧的第二大人为CO₂排放源。森林砍伐有许多原因,包括社会经济和自然因素,如为农业、牧场和开发进行的皆伐、不可持续的木材采伐,以及气候变化导致的干旱、火灾和退化。关于森林退化的自然原因,在亚马孙地区的背景下,森林生态系统变化的主要因素很可能是旱季降水量减少。政府间气候变化专门委员会(IPCC)在其2007年报告中采用的23个全球气候模型中,50% - 70%预测在中等温室气体排放情景下,亚马孙东部旱季降雨量将大幅减少(超过20%),亚马孙中部减少40%,西部减少20%。自20世纪60年代以来,化石燃料燃烧的年度碳排放量一直在持续增加,而森林砍伐及相关碳排放量的历史趋势仍鲜为人知。

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