Impact of Emerging Agricultural Contaminants on Global Warming

Boykoff and Mansfield (2008), in a recent paper in this journal, provide a detailedanalysis of the representation of climate change in the UK tabloid newspapers.They conclude that the representation of this issue in these papers ‘diverged fromthe scientific consensus that humans contribute to climate change’. That is,portrayal of climate change in tabloid newspapers contradicts the conclusions ofthe fourth Intergovernmental Panel on Climate Change (IPCC) assessment (IPCC2007). Is it healthy to have the scientific consensus challenged so frequently? Butshould we worry about systematic misrepresentation of scientific consensus? Webelieve the answer to both of these questions is yes. To present regular updates onclimate change issues in the popular press is important because the changes inbehaviour needed to achieve substantial reductions in greenhouse gas emissionsrequire a broad understanding of the basic facts. However, if the majority ofreaders receive misleading information, it will be difficult to achieve the level ofpublic understanding necessary to make such reductions needed to avoiddangerous climate change (Schellnhuber

Global warming is defined as an increase in the average temperature of the Earth’s atmosphere. Climate change is an effect of global warming that cause drastic changes in the weather. Volcanic eruptions, solar radiation, and movement of crustal plates are some of the natural causes of climate change. Additionally, modern lifestyle is a substantial contributor to climate change. Global warming influenced by society is caused through an increase in greenhouse gases. Some of these gases include water vapor, carbon dioxide, methane, fluorinated gases and nitrous oxide. These gases warm the Earth’s atmosphere by trapping heat. Fluorinated gases have the highest warming potential followed by nitrous oxide, methane, carbon dioxide and water vapor. In the environment, water vapor is released in enormous amounts followed by carbon dioxide, methane, nitrous oxide and fluorinated gases. Water vapor is a special gas because it has a low warming potential but is released in such high amounts, therefore, it has the highest warming effect. The carbon cycle circulates and transforms carbon back and forth between living species and the environment. Animal agriculture, transportation, and water utilities disrupt the carbon cycle by releasing stored carbon. As a result of global warming the following occur: intense heat, droughts, hurricanes, fires, floods, and rising of the sea level. Researchers created two experiments, the first experiment tested the warming potential of greenhouse gases at a constant rate. In contrast, the second experiment tested the warming potential of greenhouse gases at the rate they are released in the environment. In order to conduct these experiments greenhouses, ice sculptures, lights and thermometers were used. The results stated fluorinated gases had the greatest warming potential, while gases were distributed at a constant rate and carbon dioxide had the greatest warming potential when release in correlation to the environment. In conclusion, global warming is caused by greenhouse gases that are released by modern lifestyle. If global warming continues there will be fatal outcomes and congress has the power to prevent this by imposing a law in which methane is taxed.

This study reviews the global increase in atmospheric greenhouse gas (GHG) concentrations, including carbon dioxide (CO2), methane (CH4), and nitrous oxide (N2O), alongside the accelerated climatic change and its slow onset effects (or events) between 1992 and 2021. The establishment of the United Nations Framework Convention on Climate Change (UNFCCC) in 1992, and the simultaneous UN Earth Summit in Rio de Janeiro, generated the international efforts to tackle climatic change. Over the years, the UNFCCC-Conference of the Parties (COP) has led the efforts in climate change mitigation and adaptation, with many sequential meetings across the world. Three decades later, at the COP26 meeting in Glasgow in 2021, it is evident that climate change impacts have substantially worsened. Despite some uncertainties, it seems that over the last three decades, the climate change slow onset events, including 1) increasing temperatures, 2) glacial retreat, 3) sea level rise, 4) ocean acidification, 5) soil salinization, 6) land and forest degradation, 7) loss of biodiversity, and 8) desertification, have substantially exacerbated. Simultaneously, other (non-GHGs related) anthropogenic impacts, including habitat fragmentation, land-use and sea-use change and misuse, species overexploitation, environmental pollution, infrastructure constructions, and urbanization, have considerably increased. With the aim of achieving the Shared Socio-Economic Pathways 1.9 (SSP1-1.9) or SSP1-2.6 ultimate goals—keeping global warming in 2,100 below 1.5°C or 2.0°C, respectively, compared to preindustrial levels—it may still be possible to avoid climate change’s irreversible tipping points. To reach this target, policymaking must become more decisive and proactive, with continuous risks assessment, frequent monitoring of outcomes and their compatibility to goals, implementing practical legislation tools, and assigning specific financial instruments, aimed at effectively tackling climate change slow onset events and related environmental issues. Substantial efforts should be invested in boosting climate change mitigation, while simultaneously targeting effective climatic change adaptation measures and promoting environmental conservation and restoration. Relying on tools such as the UN Sustainable Development Goals (SDGs) will sustain provisioning, supporting, regulating, and cultural ecosystem services, thus improving water-, food-, environmental-, energy-, economic-, health-, and governance-security, while lessening the risks of social unrest, violent conflicts, mass migration, and other humanitarian catastrophes.

Effect of climate change is not confined to arthropod pests and their outbreaks; beneficial arthropods are also affected. Therefore, an attempt has been made to include effect of global warming on four beneficial arthropods viz., insects, mites, ticks and, spiders. Global warming is a great concern throughout the world. The ill effects of global warming like change in climate, temperature, rainfall, humidity, level of carbon dioxide have been found to have both positive and negative effects on insects, which in turn reduces the effectiveness of crop protection measures. Effect on human animal health is no exception. This creates the need for global warming to be taken as an important criterion in Entomology. Being poikilothermic in nature insects are greatly affected by changing temperature. The major cause of climate change is the increase in the concentration of greenhouse gases (GHG) viz., carbon dioxide (CO2), methane (CH4) and nitrous oxide (NO2) as a result of human activities from pre-industrial era. These gases keep the earth warm and cause global warming or greenhouse effect. Global warming is caused by natural factors as well as human activities. There are number of natural factors responsible for climate change. Some of the most prominent are volcanoes, ocean currents, forest fire etc. Among human activities, emissions of greenhouse gases, industrialization, deforestation, fuel burning, etc. are the most important factors contributing to global warming. It is not new that global warming can affect agriculture through their direct and indirect effects on crops, soils, pests, livestock and fish. Changes in climatic factors affect crops in various ways through ineffective pollination, salinity, drought, crop sterility, submergence, flash floods, plant mortality through inappropriate temperature level, hot air flush, cyclone, hailstorm etc. Climate change affects the biology of insects, spiders and mites. Global climate changes have significant impacts on agriculture and also on agricultural insect pests. Agricultural crops and their corresponding pests are irectly and indirectly affected by climate change. Direct impacts are on pests' reproduction, development, survival and dispersal, whereas indirectly the climate change affects the relationships between pests, their environment and other insect species such as natural enemies, competitors, vectors and mutualisms. Insects are poikilothermic organisms; the temperature of their body depends on the temperature of the environment. Thus, temperature is probably the most important environmental factor affecting insect behavior, distribution, development and reproduction. Therefore, farmers can expect to face new and intense pest problems in the coming years due to the changing climate. The spread of crop pests across physical and political boundaries threatens food security which is a global problem common to all countries and regions. Effects of different climatic factor on several aspects of insects, their natural enemies, insecticides, biopesticides and overall impact on crop production and food security are described here starting with effects on some beneficial and commonly known arthropods.

Radley Horton,1,a Daniel Bader,1,a Yochanan Kushnir,2 Christopher Little,3 Reginald Blake,4 and Cynthia Rosenzweig5 1Columbia University Center for Climate Systems Research, New York, NY. 2Ocean and Climate Physics Department, Lamont-Doherty Earth Observatory, Columbia University, Palisades, NY. 3Atmospheric and Environmental Research, Lexington, MA. 4Physics Department, New York City College of Technology, CUNY, Brooklyn, NY. 5Climate Impacts Group, NASA Goddard Institute for Space Studies; Center for Climate Systems Research, Columbia University Earth Institute, New York, NY

In the present world, climate change and global warming are the foremost problems in front of the human race. These problems have arisen due to the increase in Greenhouse gases (GHGs) concentration in the atmosphere. Most of the factors responsible for GHGs emissions are anthropogenic such as fossil fuel combustion, biomass burning, etc. Nature has developed its own way of fighting the GHGs problem by evolving microorganisms responsible for GHGs sequestration. These microorganisms can be utilized for solving the GHGs emission problem. Some of the methods that involve microorganisms for GHGs emission reduction are altering microbial community structure for altering GHGs flux into the atmosphere, microbial pathway engineering for more GHGs sequestration, and utilization of GHGs fixing enzyme derived from microbes to decrease emissions at the point source. Also, the biogeochemical cycling of elements such as C and N cannot be separated from climate change as the cycling of these elements involves the cycling of major GHGs such as carbon dioxide (CO2), methane (CH4), and nitrous oxide (N2O). The present chapter is about microbial role and solution to the GHGs emission problems.

Variations in the intensity of the global hydrological cycle can have far-reaching effects on living conditions on our planet. While climate change discussions often revolve around possible consequences of future temperature changes, the adaptation to changes in the hydrological cycle may pose a bigger challenge to societies and ecosystems. Floods and droughts are already today amongst the most damaging natural hazards, with floods being globally the most significant disaster type in terms of loss of human life (Jonkman 2005). From an economic perspective, changes in the hydrological cycle can impose great pressures and damages on a variety of industrial sectors, such as water management, urban planning, agricultural production and tourism. Despite their obvious environmental and societal importance, our understanding of the causes and magnitude of the variations of the hydrological cycle is still unsatisfactory (e.g., Ramanathan et al 2001, Ohmura and Wild 2002, Allen and Ingram 2002, Allan 2007, Wild et al 2008, Liepert and Previdi 2009).

The changing climate is unequivocal, and it is generally recognised as a threat to the terrestrial environment due to its cross-sectoral and irreversible impacts. Since the inception of industrial revolution (1750), the concentration of greenhouse gases (carbon dioxide, methane and nitrous oxide) in the atmosphere has been compromised. Until the past two centuries, the quantity of carbon dioxide and methane in the atmosphere had never surpassed about 280 part per million (ppm) and 790 part per billion (ppb), respectively. Rise in greenhouse gases (GHGs) has impacted almost every biotic component on the surface of the earth, and regions which have low adaptive capacity and greatly depend on agriculture and biodiversity for livelihood are hard hit. This phenomenon has resulted in global warming, extinction of some fora and fauna species, precipitation variability, extreme weather conditions, migration of biotic creatures from one geographical area to another, melting of icecap, sea level rise, coral breach and so on during the last century. The contribution of emission of greenhouse gases of Africa is insignificant, however, the repercussion of the changing climate is crucial in the region due to the presence of other stressors such as poverty, corruption, diseases, geographical position of the continent, low adaptive capacity, rain-fed agriculture etc., and this has led to conflict over resources usage, food insecurity, forced migration, ill-health and many more.

In recent years, the diverse industrial practices and human inputs widely disseminated emerging contaminants (ECs) throughout environmental matrices, which is of great concern. Even at low concentrations, ECs pose major ecological problems and threaten human health and the environment’s biota. Consequently, people’s interest and concerns on the widespread dissemination of environmentally connected ECs of great concern as developed due to their scientific understanding, technical innovation, and socioeconomic awareness. Increased detection of contaminants may occur from climatic, socioeconomic, and demographic changes and the growing sensitivity of analytical techniques. Hence, this article reviews the determination of ECs in ecological specimens, from aquatic setup (river water, marine water, and wastewater), sludge, soil, sediment, and air. Sample collection and the quality measures are summarized. The preparation of samples, including extraction and cleanup and the subsequent instrumental analysis of ECs, are all covered. Traditional and recent extraction and cleanup applications to analyze ECs in samples are reviewed here in this paper. The detection and quantification of ECs using gas chromatography (GC) and liquid chromatography (LC) linked with various detectors, particularly mass spectrometry (MS), is also summarized and explored, as are other possible techniques. This study aims to give readers a more excellent knowledge of how new and improved approaches are being developed and serve as a resource for researchers looking for the best method for detecting ECs in their studies.

In this study, the strength of the regional changes in near-surface climate associated with a global warming of 2°C with respect to pre-industrial times is assessed, distinguishing between 26 different regions. Also, the strength of these regional climate changes is compared to the strength of the respective changes associated with a markedly stronger global warming of 4.5°C. The magnitude of the regional changes in climate is estimated by means of a normalized regional climate change index, which considers changes in the mean as well as changes in the interannual variability of both near-surface temperature and precipitation. The study is based on two sets of four ensemble simulations with the ECHAM5/MPI-OM coupled climate model, each starting from different initial conditions. In one set of simulations (1860–2200), the greenhouse gas concentrations and sulphate aerosol load have been prescribed according to observations until 2000 and according to the SRES A1B scenario after 2000. In the other set of simulations (2020–2200), the greenhouse gas concentrations and sulphate aerosol load have been prescribed in such a way that the simulated global warming does not exceed 2°C with respect to pre-industrial times. The study reveals the strongest changes in near-surface climate in the same regions for both scenarios, i.e., the Sahara, Northern Australia, Southern Australia and Amazonia. The regions with the weakest changes in near-surface climate, on the other hand, vary somewhat between the two scenarios except for Western North America and Southern South America, where both scenarios show rather weak changes. The comparison between the magnitude of the regional changes in near-surface climate for the two scenarios reveals relatively strong changes in the 2°C-stabilization scenario at high northern latitudes, i.e., Northeastern Europe, Alaska and Greenland, and in Amazonia. Relatively weak regional climate changes in this scenario, on the other hand, are found for Eastern Asia, Central America, Central South America and Southern South America. The ratios between the regional changes in the near-surface climate for the two scenarios vary considerably between different regions. This illustrates a limitation of obtaining regional changes in near-surface climate associated with a particular scenario by means of scaling the regional changes obtained from a widely used “standard” scenario with the ratio of the changes in the global mean temperature projected by these two scenarios.

Performance and mechanisms of reactive substrates in constructed wetlands: Emerging contaminant removal and greenhouse gas mitigation—A comprehensive review

Climate change is a complex and contentious public issue, but the risk-management options available to us are straightforward and have well-characterized strengths and weaknesses.

Increases in the concentrations of atmospheric greenhouse gases, carbon dioxide (CO2), methane (CH4), nitrous oxide (N2O) due to human activities are associated with global climate change. CO2 concentration in the atmosphere has increased by 33% (to 380 ppm) since 1750 ad, whilst CH4 concentration has increased by 75% (to 1,750 ppb), and as the global warming potential (GWP) of CH4 is 25 fold greater than CO2 it represents about 20% of the global warming effect. The purpose of this review is to: (a) address recent findings regarding biophysical factors governing production and consumption of CH4, (b) identify the current level of knowledge regarding the main sources and sinks of CH4 in Australia, and (c) identify CH4 mitigation options and their potential application in Australian ecosystems. Almost one-third of CH4 emissions are from natural sources such as wetlands and lake sediments, which is poorly documented in Australia. For Australia, the major anthropogenic sources of CH4 emissions include energy production from fossil fuels (~24%), enteric fermentation in the guts of ruminant animals (~59%), landfills, animal wastes and domestic sewage (~15%), and biomass burning (~5%), with minor contributions from manure management (1.7%), land use, land-use change and forestry (1.6%), and rice cultivation (0.2%). A significant sink exists for CH4 (~6%) in aerobic soils, including agricultural and forestry soils, and potentially large areas of arid soils, however, due to limited information available in Australia, it is not accounted for in the Australian National Greenhouse Gas Inventory. CH4 emission rates from submerged soils vary greatly, but mean values ≤10 mg m−2 h−1 are common. Landfill sites may emit CH4 at one to three orders of magnitude greater than submerged soils. CH4 consumption rates in non-flooded, aerobic agricultural, pastoral and forest soils also vary greatly, but mean values are restricted to ≤100 μg m−2 h−1, and generally greatest in forest soils and least in agricultural soils, and decrease from temperate to tropical regions. Mitigation options for soil CH4 production primarily relate to enhancing soil oxygen diffusion through water management, land use change, minimised compaction and soil fertility management. Improved management of animal manure could include biogas capture for energy production or arable composting as opposed to open stockpiling or pond storage. Balanced fertiliser use may increase soil CH4 uptake, reduce soil N2O emissions whilst improving nutrient and water use efficiency, with a positive net greenhouse gas (CO2-e) effect. Similarly, the conversion of agricultural land to pasture, and pastoral land to forestry should increase soil CH4 sink. Conservation of native forests and afforestation of degraded agricultural land would effectively mitigate CH4 emissions by maintaining and enhancing CH4 consumption in these soils, but also by reducing N2O emissions and increasing C sequestration. The overall impact of climate change on methanogenesis and methanotrophy is poorly understood in Australia, with a lack of data highlighting the need for long-term research and process understanding in this area. For policy addressing land-based greenhouse gas mitigation, all three major greenhouse gases (CO2, CH4 and N2O) should be monitored simultaneously, combined with improved understanding at process-level.

Introduction to <i>Climate Change Adaptation in New York City: Building a Risk Management Response</i>

Uniting the Global Gastroenterology Community to Meet the Challenge of Climate Change and Non-Recyclable Waste