Oportunidades e vulnerabilidades do Brasil nas questões do clima e da sustentabilidade

As mudanças climáticas constituem um dos maiores desafios da humanidade hoje. É urgente entendermos como os ecossistemas brasileiros, a economia, a infraestrutura, as cadeias produtivas, a biodiversidade, a saúde, entre outros aspectos, estão sendo afetados pelas mudanças climáticas. O Brasil tem vantagens estratégicas enormes, como a possibilidade de reduzir fortemente as emissões de gases de efeito estufa, com ganhos importantes para a sociedade. Temos um potencial de geração de energia solar e eólica que nenhum outro país possui. Mas também temos vulnerabilidades, como um agronegócio dependente do clima e a geração de hidroeletricidade dependente da chuva. Temos também 8.500 km de áreas costeiras sensíveis ao aumento do nível do mar, e áreas urbanas vulneráveis a eventos climáticos extremos. Temos que construir uma socioeconomia mais justa e com clima e meio ambiente integrados de modo sustentável.Climate change constitutes one of the greatest challenges facing humanity today. It is urgent to understand how Brazilian ecosystems, the economy, infrastruc ture, produc tion chains, biodiversity, health, among other aspects, are being affected by climate change. Brazil has enormous strategic advantages, such as the possibility of strongly reducing greenhouse gas emissions, with important gains for society. We have a potential for generating solar and wind energy that no other country has. But we also have vulnerabilities, such as climate-dependent agribusiness and raindependent hydroelectricity generation. We also have 8,500 km of coastal areas sensitive to sea level rise, and urban areas vulnerable to extreme weather events. We have to build a fairer socio-economy, with climate and environment integrated in a sustainable way

Aerosol and precipitation chemistry in a remote site in Central Amazonia: the role of biogenic contribution

International audienceA long-term (2?3 years) measurement of aerosol and precipitation chemistry was carried out in a remote site in Central Amazonia, Balbina, (1°55' S, 59°29' W, 174 m above sea level), about 200 km north of Manaus city. Aerosols were sampled using stacked filter units (SFU), which separate fine (d<2.5 ?m) and coarse mode (2.5 ?

Uma nova era geológica em nosso planeta: o Antropoceno?

Nosso planeta seguiu uma evolução determinada pelas forças geológicas desde sua origem, há cerca de 4,5 bilhões de anos. Ao longo dessa jornada, passou por transformações significativas em sua crosta e atmosfera. Com o início da Revolução Industrial, na segunda metade do século XVIII, um novo agente de mudança se somou às transformações geológicas. O rápido crescimento populacional – somos 7,3 bilhões de habitantes hoje, e seremos cerca de 10 bilhões em 2050 –, associado ao uso excessivo de recursos naturais, fez com que muitos indicadores de saúde da Terra saíssem da região segura. A partir de 1950, o desenvolvimento humano e suas implicações no ecossistema terrestre crescem exponencialmente. Atualmente, uma grande fração das áreas continentais sem gelo é ocupada por atividades humanas como agricultura e urbanização, entre outras.Our planet has followed an evolutionary path determined by geological forces since its origin about 4.5 billion years ago. Throughout its evolution, the Earth has undergone significant changes in its crust and atmosphere. With the onset of the Industrial Revolution around 1750, a new agent of change has been added to the geological transformations. Rapid population growth (we are 7.3 billion people today, and we will be about 10 billion in 2050) associated with the excessive use of natural resources has brought several of the health indicators of our planet outside safe boundaries. Especially after 1950, human development and its implications on terrestrial ecosystem have grown exponentially. Currently, a large fraction of the continental areas without ice is occupied for human activities such as agriculture, grazing pastures, and urbanization, among others

Non-deforestation drivers of fires are increasingly important sources of aerosol and carbon dioxide emissions across Amazonia

Deforestation rates have declined substantially across the Brazilian Legal Amazon (BLA) over the period from 2000–2017. However, reductions in fire, aerosol and carbon dioxide have been far less significant than deforestation, even when accounting for inter-annual variability in precipitation. Our observations and analysis support a decoupling between fire and deforestation that has exacerbated forest degradation in the BLA. Basing aerosol and carbon dioxide emissions on deforestation rates, without accounting for forest degradation will bias these important climate and ecosystem-health parameters low, both now and in the future. Recent increases in deforestation rate since 2014 will enhance such degradation, particularly during drought-conditions, increasing emissions of aerosol and greenhouse gases. Given Brazil’s committed Nationally Determined Contribution under the Paris Agreement, failure to account for forest degradation fires will paint a false picture of prior progress and potentially have profound implications for both regional and global climate

Robust relations between CCN and the vertical evolution of cloud drop size distribution in deep convective clouds

International audienceIn-situ measurements in convective clouds (up to the freezing level) over the Amazon basin show that smoke from deforestation fires prevents clouds from precipitating until they acquire a vertical development of at least 4 km, compared to only 1?2 km in clean clouds. The average cloud depth required for the onset of warm rain increased by ~350 m for each additional 100 cloud condensation nuclei per cm3 at a super-saturation of 0.5% (CCN0.5%). In polluted clouds, the diameter of modal liquid water content grows much slower with cloud depth (at least by a factor of ~2), due to the large number of droplets that compete for available water and to the suppressed coalescence processes. Contrary to what other studies have suggested, we did not observe this effect to reach saturation at 3000 or more accumulation mode particles per cm3. The CCN0.5% concentration was found to be a very good predictor for the cloud depth required for the onset of warm precipitation and other microphysical factors, leaving only a secondary role for the updraft velocities in determining the cloud drop size distributions. The effective radius of the cloud droplets (re) was found to be a quite robust parameter for a given environment and cloud depth, showing only a small effect of partial droplet evaporation from the cloud's mixing with its drier environment. This supports one of the basic assumptions of satellite analysis of cloud microphysical processes: the ability to look at different cloud top heights in the same region and regard their re as if they had been measured inside one well developed cloud. The dependence of re on the adiabatic fraction decreased higher in the clouds, especially for cleaner conditions, and disappeared at re?~10 µm. We propose that droplet coalescence, which is at its peak when warm rain is formed in the cloud at re~10 µm, continues to be significant during the cloud's mixing with the entrained air, canceling out the decrease in re due to evaporation

Rapid formation of isoprene photo-oxidation products observed in Amazonia

Isoprene represents the single most important reactive hydrocarbon for atmospheric chemistry in the tropical atmosphere. It plays a central role in global and regional atmospheric chemistry and possible climate feedbacks. Photo-oxidation of primary hydrocarbons (e.g. isoprene) leads to the formation of oxygenated VOCs (OVOCs). The evolution of these intermediates affects the oxidative capacity of the atmosphere (by reacting with OH) and can contribute to secondary aerosol formation, a poorly understood process. An accurate and quantitative understanding of VOC oxidation processes is needed for model simulations of regional air quality and global climate. Based on field measurements conducted during the Amazonian Aerosol Characterization Experiment (AMAZE-08) we show that the production of certain OVOCs (e.g. hydroxyacetone) from isoprene photo-oxidation in the lower atmosphere is significantly underpredicted by standard chemistry schemes. Recently reported fast secondary production could explain 50% of the observed discrepancy with the remaining part possibly produced via a novel primary production channel, which has been proposed theoretically. The observations of OVOCs are also used to test a recently proposed HO&lt;sub&gt;x&lt;/sub&gt; recycling mechanism via degradation of isoprene peroxy radicals. If generalized our observations suggest that prompt photochemical formation of OVOCs and other uncertainties in VOC oxidation schemes could result in uncertainties of modelled OH reactivity, potentially explaining a fraction of the missing OH sink over forests which has previously been largely attributed to a missing source of primary biogenic VOCs

The effect of atmospheric aerosol particles and clouds on net ecosystem exchange in the Amazon

Carbon cycling in the Amazon is closely linked to atmospheric processes and climate in the region as a consequence of the strong coupling between the atmosphere and biosphere. This work examines the effects of changes in net radiation due to atmospheric aerosol particles and clouds on the net ecosystem exchange (NEE) of CO₂ in the Amazon region. Some of the major environmental factors affecting the photosynthetic activity of plants, such as air temperature and relative humidity, were also examined. An algorithm for clear-sky irradiance was developed and used to determine the relative irradiance, <i>f</i>, which quantifies the percentage of solar radiation absorbed and scattered due to atmospheric aerosol particles and clouds. Aerosol optical depth (AOD) was calculated from irradiances measured with the MODIS (Moderate Resolution Imaging Spectroradiometer) sensor, onboard the Terra and Aqua satellites, and was validated with ground-based AOD measurements from AERONET (Aerosol Robotic Network) sun photometers. Carbon fluxes were measured using eddy covariance technique at the Large-Scale Biosphere-Atmosphere Experiment in Amazonia (LBA) flux towers. Two sites were studied: the Jaru Biological Reserve (RBJ), located in Rondonia, and the Cuieiras Biological Reserve at the K34 LBA tower (located in a preserved region in the central Amazon). Analysis was performed continuously from 1999 to 2009 at K34 and from 1999 to 2002 at RBJ, and includes wet, dry and transition seasons. In the Jaru Biological Reserve, a 29% increase in carbon uptake (NEE) was observed when the AOD ranged from 0.10 to 1.5 at 550 nm. In the Cuieiras Biological Reserve, the aerosol effect on NEE was smaller, accounting for an approximate 20% increase in NEE. High aerosol loading (AOD above 3 at 550 nm) or high cloud cover leads to reductions in solar flux and strong decreases in photosynthesis up to the point where NEE approaches zero. The observed increase in NEE is attributed to an enhancement (~50%) in the diffuse fraction of photosynthetic active radiation (PAR). The enhancement in diffuse PAR can be done through increases in aerosols and/or clouds. In the present study, it was not possible to separate these two components. Significant changes in air temperature and relative humidity resulting from changes in solar radiation fluxes under high aerosol loading were also observed at both sites. Considering the long-range transport of aerosols in the Amazon, the observed changes in NEE for these two sites may occur over large areas in the Amazon, significantly altering the carbon balance in the largest rainforest in the world

Spatiotemporal assessment of particulate matter (PM10 and PM2.5) and ozone in a Caribbean urban coastal city

Air pollution has become a critical issue in urban areas, so a broad understanding of its spatiotemporal characteristics is important to develop public policies. This study analyzes the spatiotemporal variation of atmospheric particulate matter (PM10 and PM2.5) and ozone (O3) in Barranquilla, Colombia from March 2018 to June 2019 in three monitoring stations. The average concentrations observed for the Móvil, Policía, and Tres Avemarías stations, respectively, for PM10: 46.4, 51.4, and 39.7 μg/m3; for PM2.5: 16.1, 18.1, and 15.1 μg/m3 and for O3: 35.0, 26.6, and 33.6 μg/m3. The results indicated spatial and temporal variations between the stations and the pollutants evaluated. The highest PM concentrations were observed in the southern part of the city, while for ozone, higher concentrations were observed in the north. These variations are mainly associated with the influence of local sources in the environment of each site evaluated as well as the meteorological conditions and transport patterns of the study area. This study also verified the existence of differences in the concentrations of the studied pollutants between the dry and rainy seasons and the contribution of local sources as biomass burnings from the Isla Salamanca Natural Park and long-range transport of dust particles from the Sahara Desert. This study provides a scientific baseline for understanding air quality in the city, which enables policy makers to adopt efficient measures that jointly prevent and control pollution