Chemically, black carbon or BC is a component of fine particulate matter (PM ≤ 2.5 µm in aerodynamic diameter). Black Carbon consists of pure carbon in several linked forms. It is formed through the incomplete combustion of fossil fuels, biofuel, and biomass, and is emitted in both anthropogenic and naturally occurring soot.
In climatology black carbon is a climate forcing agent. Black carbon warms the Earth by absorbing heat in the atmosphere and by reducing albedo when deposited on snow and ice. Black carbon stays in the atmosphere for only several days to weeks, whereas carbon dioxide (CO2) has an atmospheric lifetime of more than 100 years.
The term black carbon is also used in soil sciences and geology, referring either to deposited atmospheric black carbon or to directly incorporated black carbon from vegetation fires. Especially in the tropics, black carbon in soils significantly contributes to fertility as it is able to absorb important plant nutrients.
- 1 Overview
- 2 Emission sources
- 3 Impacts
- 4 Control technologies
- 5 Biodegradation
- 6 Policy options
- 7 See also
- 8 References
- 9 Further reading
- 10 External links
||This section is written like a personal reflection or opinion essay that states the Wikipedia editor's particular feelings about a topic, rather than the opinions of experts. (February 2013)|
The term black carbon was coined by Tihomir Novakov, referred to as "the godfather of black carbon studies" by James Hansen, in the 1970s. Smoke or soot was the first pollutant to be recognized as having significant environmental impact yet one of the last to be studied by the contemporary atmospheric research community. Faraday recognized that soot was composed of carbon and that it was produced by the incomplete combustion of carbon-containing fuels.
Soot is composed of a complex mixture of organic compounds which are weakly absorbing in the visible spectral region and a highly absorbing black component which is variously called “elemental”, “graphitic” or “black carbon”. The term elemental carbon has been used in conjunction with thermal and wet chemical determinations and the term graphitic carbon suggests the presence of graphite-like micro-crystalline structures in soot as evidenced by Raman Spectroscopy. The term black carbon is used to imply that this soot component is primarily responsible for the absorption of visible light. The term black carbon is used as a synonym for both the elemental and graphitic component of soot. It can be measured using different types of devices based on absorption or dispersion of a light beam or derived from noise measurements.
Early mitigation attempts
The disastrous effects of coal pollution on human health and mortality in the early 1950s in London led to the UK Clean Air Act 1956. This act led to dramatic reductions of soot concentrations in the United Kingdom which were followed by similar reductions in US cities like Pittsburgh and St. Louis. These reductions were largely achieved by the decreased use of soft coal for domestic heating by switching either to “smokeless” coals or other forms of fuel, such as fuel oil and natural gas. The steady reduction of smoke pollution in the industrial cities of Europe and United States caused a shift in research emphasis away from soot emissions and the almost complete neglect of black carbon as a significant aerosol constituent, at least in the United States.
In the 1970s, however, a series of studies substantially changed this picture and demonstrated that black carbon as well as the organic soot components continued to be a large component in urban aerosols across the United States and Europe which led to improved controls of these emissions. In the less-developed regions of the world where there were limited or no controls on soot emissions the air quality continued to degrade as the population increased. It was not generally realized until many years later that from the perspective of global effects the emissions from these regions were extremely important.
Influence on Earth's atmosphere
Most of the developments mentioned above relate to air quality in urban atmospheres. The first indications of the role of black carbon in a larger, global context came from studies of the Arctic Haze phenomena. Black carbon was identified in the Arctic haze aerosols and in the Arctic snow.
In general, aerosol particles can affect the radiation balance leading to a cooling or heating effect with the magnitude and sign of the temperature change largely dependent on aerosol optical properties, aerosol concentrations, and the albedo of the underlying surface. A purely scattering aerosol will reflect energy that would normally be absorbed by the earth-atmosphere system back to space and leads to a cooling effect. As one adds an absorbing component the aerosol, it can lead to a heating of the earth-atmosphere system if the reflectivity of the underlying surface is sufficiently high.
Early studies of the effects of aerosols on atmospheric radiative transfer on a global scale assumed a dominantly scattering aerosol with only a small absorbing component, since this appears to be a good representation of naturally occurring aerosols. However, as discussed above, urban aerosols have a large black carbon component and if these particles can be transported on a global scale then one would expect a heating effect over surfaces with a high surface albedo like snow or ice. Furthermore, if these particles are deposited in the snow an additional heating effect would occur due to reductions in the surface albedo.
Measuring and modeling spatial distribution
Levels of Black carbon are most often determined based on the modification of the optical properties of a fiber filter by deposited particles. Either filter transmittance, filter reflectance or a combination of transmittance and reflectance is measured. Aethalometers are frequently used devices that optically detect the changing absorption of light transmitted through a filter ticket. A multiangle absorption photometer takes into account both transmitted and reflected light. Alternative methods rely on satellite based measurements of optical depth for large areas or more recently on spectral noise analysis for very local concentrations.
In the late 1970s and early 1980s surprisingly large ground level concentrations of black carbon were observed throughout the western Arctic. and modeling studies indicated that they could lead to heating over polar ice. One of the major uncertainties in modeling the effects of the Arctic haze on the solar radiation balance was limited knowledge of the vertical distributions of black carbon.
During 1983 and 1984 as part of the NOAA AGASP program, the first measurements of such distributions in the Arctic atmosphere were obtained with an aethalometer which had the capability of measuring black carbon on a real-time basis. These measurements showed substantial concentrations of black carbon found throughout the western Arctic troposphere including the North Pole. The vertical profiles showed either a strongly layered structure or an almost uniform distribution up to eight kilometers with concentrations within layers as large as those found at ground level in typical mid-latitude urban areas in the United States. The absorption optical depths associated with these vertical profiles were large as evidenced by a vertical profile over the Norwegian arctic where absorption optical depths of 0.023 to 0.052 were calculated respectively for external and internal mixtures of black carbon with the other aerosol components.
Optical depths of these magnitudes lead to a substantial change in the solar radiation balance over the highly reflecting Arctic snow surface during the March–April time frame of these measurements modeled the Arctic aerosol for an absorption optical depth of 0.021 (which is close to the average of an internal and external mixtures for the AGASP flights), under cloud-free conditions. These heating effects were viewed at the time as potentially one of the major causes of Arctic warming trends as described in Archives of Dept. of Energy, Basic Energy Sciences Accomplishments.
Presence in soils
Up to 30% of the total carbon stored in soils is contributed by black carbon. Especially for tropical soils black carbon serves as a reservoir for nutrients. Experiments showed that soils without high amounts of black carbon are significantly less fertile than soils that contain black carbon. An example for this increased soil fertility are the Terra preta soils of central Amazonia, which are presumably human-made by pre-Columbian native populations. Terra Preta soils have on average three times higher soil organic matter (SOM) content, higher nutrient levels and a better nutrient retention capacity than surrounding infertile soils. In this context, the slash and burn agricultural practice used in tropical regions does not only enhance productivity by releasing nutrients from the burned vegetation but also by adding black carbon to the soil. Nonetheless, for a sustainable management, a slash-and-char practice would be better in order to prevent high emissions of CO2 and volatile black carbon. Furthermore, the positive effects of this type of agriculture are counteracted if used for large patches so that soil erosion is not prevented by the vegetation.
Developed countries were once the primary source of black carbon emissions, but this began to change in the 1950s with the adoption of pollution control technologies in those countries. Whereas the United States emits about 21% of the world’s CO2, it emits 6.1% of the world’s soot. The European Union and United States might further reduce their black carbon emissions by accelerating implementation of black carbon regulations that currently take effect in 2015 or 2020 and by supporting the adoption of pending International Maritime Organization (IMO) regulations. Existing regulations also could be expanded to increase the use of clean diesel and clean coal technologies and to develop second-generation technologies.
Today, the majority of black carbon emissions are from developing countries and this trend is expected to increase. The largest sources of black carbon are Asia, Latin America, and Africa. China and India together account for 25-35% of global black carbon emissions. Black carbon emissions from China doubled from 2000 to 2006. Existing and well-tested technologies used by developed countries, such as clean diesel and clean coal, could be transferred to developing countries to reduce their emissions.
- the Indo-Gangetic plains of India
- eastern China
- most of Southeast Asia and Indonesia
- equatorial regions of Africa
- Mexico and Central America
- most of Brazil and Peru in South America.
Approximately three billion people live in these hotspots.
Approximately 20% of black carbon is emitted from burning biofuels, 40% from fossil fuels, and 40% from open biomass burning. Similarly estimates of the sources of black carbon emissions as follows:
- 42% Open biomass burning (forest and savanna burning)
- 18% Residential biofuel burned with traditional technologies
- 14% Diesel engines for transportation
- 10% Diesel engines for industrial use
- 10% Industrial processes and power generation, usually from smaller boilers
- 6% Residential coal burned with traditional technologies
Black carbon sources vary by region. For example, the majority of soot emissions in South Asia are due to biofuel cooking, whereas in East Asia, coal combustion for residential and industrial uses plays a larger role. In Western Europe, traffic seems to be the most important source since high concentrations coincide with proximity to major roads or participation to (motorized) traffic.
Fossil fuel and biofuel soot have significantly greater amounts of black carbon than climate-cooling aerosols and particulate matter, making reductions of these sources particularly powerful mitigation strategies. For example, emissions from the diesel engines and marine vessels contain higher levels of black carbon compared to other sources. Regulating black carbon emissions from diesel engines and marine vessels therefore presents a significant opportunity to reduce black carbon’s global warming impact.
Biomass burning emits greater amounts of climate-cooling aerosols and particulate matter than black carbon, resulting in short-term cooling. However, over the long-term, biomass burning may cause a net warming when CO2 emissions and deforestation are considered. Reducing biomass emissions would therefore reduce global warming in the long-term and provide co-benefits of reduced air pollution, CO2 emissions, and deforestation. It has been estimated that by switching to slash-and-char from slash-and-burn agriculture, which turns biomass into ash using open fires that release black carbon and GHGs, 12% of anthropogenic carbon emissions caused by land use change could be reduced annually, which is approximately 0.66 Gt CO2-eq. per year, or 2% of all annual global CO2-eq emissions.
Black carbon is a form of ultrafine particulate matter, which when released in the air causes premature human mortality and disability. In addition, atmospheric black carbon changes the radiative energy balance of the climate system in a way that raises air and surface temperatures, causing a variety of detrimental environmental impacts on humans, on agriculture, and on plant and animal ecosystems.
Public health impacts
Particulate matter is the most harmful to public health of all air pollutants in Europe. Black carbon particulate matter contains very fine carcinogens and is therefore particularly harmful.
It is estimated that from 640,000 to 4,900,000 premature human deaths could be prevented every year by utilizing available mitigation measures to reduce black carbon in the atmosphere.
Humans are exposed to black carbon by inhalation of air in the immediate vicinity of local sources. Important indoor sources include candles and biomass burning whereas traffic and occasionally forest fires are the major outdoor sources of black carbon exposure. Concentrations of black carbon decrease sharply with increasing distance from (traffic) sources which makes it an atypical component of particulate matter. This makes it difficult to estimate exposure of populations. For particulate matter epidemiological studies have traditionally relied on single fixed site measurements or inferred residential concentrations. Recent studies have shown that as much black carbon is inhaled in traffic and at other locations as at the home address. High peak concentrations are encountered during car driving. High in-vehicle concentrations of black carbon have been associated with driving during rush hours, on highways and in dense traffic.
Even relatively low exposure concentrations of Black Carbon have an inflammatory effect on the respiratory system of children.
The public health benefits of reduction in the amount of soot and other particulate matter has been recognized for years. However, high concentrations persist in industrializing areas in Asia and in urban areas in the West such as Chicago. The WHO estimates that air pollution causes nearly two million premature deaths per year. By reducing black carbon, a primary component of fine particulate matter, the health risks from air pollution will decline. In fact, public health concerns have given rise to leading to many efforts to reduce such emissions, for example, from diesel vehicles and cooking stoves.
Direct effect Black carbon particles directly absorb sunlight and reduce the planetary albedo when suspended in the atmosphere.
Semi-direct effect Black carbon absorb incoming solar radiation, perturb the temperature structure of the atmosphere, and influence cloud cover. They may either increase or decrease cloud cover under different conditions.
Snow/ice albedo effect When deposited on high albedo surfaces like ice and snow, black carbon particles reduce the total surface albedo available to reflect solar energy back into space. Small initial snow albedo reduction may have a large forcing because of a positive feedback: Reduced snow albedo would increase surface temperature. The increased surface temperature would decrease the snow cover and further increase surface albedo.
Indirect effect Black carbon may also indirectly cause changes in the absorption or reflection of solar radiation through changes in the properties and behavior of clouds. Research scheduled for publication in 2013 shows black carbon plays a role second only to carbon dioxide in climate change. Effects are complex, resulting from a variety of factors, but due to the short life of black carbon in the atmosphere, about a week as compared to carbon dioxide which last centuries, control of black carbon offers possible opportunities for slowing, or even reversing, climate change.
Estimates of black carbon’s globally averaged direct radiative forcing vary from the IPCC’s estimate of + 0.34 watts per square meter (W/m2) ± 0.25, to a more recent estimate by V. Ramanathan and G. Carmichael of 0.9 W/m2.
The IPCC also estimated the globally averaged snow albedo effect of black carbon at +0.1 ± 0.1 W/m2.
Based on the IPCC estimate, it would be reasonable to conclude that the combined direct and indirect snow albedo effects for black carbon rank it as the third largest contributor to globally averaged positive radiative forcing since the pre-industrial period. In comparison, the more recent direct radiative forcing estimate by Ramanathan and Carmichael  would lead one to conclude that black carbon has contributed the second largest globally averaged radiative forcing after carbon dioxide (CO2), and that the radiative forcing of black carbon is “as much as 55% of the CO2 forcing and is larger than the forcing due to the other greenhouse gasses (GHGs) such as CH4, CFCs, N2O, or tropospheric ozone.”
Table 1 : Estimates of Black Carbon Radiative Forcing, by Effect
|Source||Direct Effect||Semi-Direct Effect||Dirty Clouds Effect||Snow/Ice Albedo Effect||Total|
|IPCC (2007)||0.34 ± 0.25||-||-||0.1 ± 0.1||0.44 ± 0.35|
|Jacobson (2001, 2004, and 2006)||0.55||-||0.03||0.06||0.64|
|Hansen (2001, 2002, 2003, 2005, and 2007)||0.2 - 0.6||0.3 ± 0.3 ||0.1 ± 0.05||0.2 ± 0.1||
0.8 ± 0.4 (2001)
|Hansen & Nazarenko (2004)||-||-||-||~ 0.3 globally
|Ramanathan (2007)||0.9||-||-||0.1 to 0.3||1.0 to 1.2|
Table 2: Estimated Climate Forcings (W/m2)
|Component||IPCC (2007)||Hansen, et al. (2005)|
Effects on Arctic ice and Himalayan glaciers
According to the IPCC, “the presence of black carbon over highly reflective surfaces, such as snow and ice, or clouds, may cause a significant positive radiative forcing.” The IPCC also notes that emissions from biomass burning, which usually have a negative forcing, have a positive forcing over snow fields in areas such as the Himalayas.
According to Charles Zender, black carbon is a significant contributor to Arctic ice-melt, and reducing such emissions may be “the most efficient way to mitigate Arctic warming that we know of”. The “climate forcing due to snow/ice albedo change is of the order of 1.0 W/m2 at middle- and high-latitude land areas in the Northern Hemisphere and over the Arctic Ocean.” The “soot effect on snow albedo may be responsible for a quarter of observed global warming.” “Soot deposition increases surface melt on ice masses, and the meltwater spurs multiple radiative and dynamical feedback processes that accelerate ice disintegration,” according to NASA scientists James Hansen and Larissa Nazarenko. As a result of this feedback process, “BC on snow warms the planet about three times more than an equal forcing of CO2.” When black carbon concentrations in the Arctic increase during the winter and spring due to Arctic Haze, surface temperatures increase by 0.5 °C. Black carbon emissions also significantly contribute to Arctic ice-melt, which is critical because “nothing in climate is more aptly described as a ‘tipping point’ than the 0 °C boundary that separates frozen from liquid water—the bright, reflective snow and ice from the dark, heat-absorbing ocean.”
Black carbon emissions from northern Eurasia, North America, and Asia have the greatest absolute impact on Arctic warming. However, black carbon emissions actually occurring within the Arctic have a disproportionately larger impact per particle on Arctic warming than emissions originating elsewhere. As Arctic ice melts and shipping activity increases, emissions originating within the Arctic are expected to rise.
In some regions, such as the Himalayas, the impact of black carbon on melting snowpack and glaciers may be equal to that of CO2. Warmer air resulting from the presence of black carbon in South and East Asia over the Himalayas contributes to a warming of approximately 0.6 °C. An “analysis of temperature trends on the Tibetan side of the Himalayas reveals warming in excess of 1 °C.” A summer aerosol sampling on a glacier saddle of Mt. Everest (Qomolangma) in 2003 showed industrially induced sulfate from South Asia may cross over the highly elevated Himalaya. This indicated BC in South Asia could also have the same transport mode. And such kind of signal might have been detected in at a black carbon monitoring site in the hinterland of Tibet. Snow sampling and measurement suggested black carbon deposited in some Himalayan glaciers may reduce the surface albedo by 0.01-0.02. Black carbon record based on a shallow ice core drilled from the East Rongbuk glacier showed a dramatic increasing trend of black carbon concentrations in the ice stratigraphy since the 1990s, and simulated average radiative forcing caused by black carbon was nearly 2 W/m2 in 2002. This large warming trend is the proposed causal factor for the accelerating retreat of Himalayan glaciers, which threatens fresh water supplies and food security in China and India. A general darkening trend in the mid-Himalaya glaciers revealed by MODIS data since 2000 could be partially attributed to black carbon and light absorbing impurities like dust in the springtime, which was later extended to the whole Hindu Kush-Kararoram-Himalaya glaciers research finding a widespread darkening trend of -0.001 yr-1 over the period of 2000-2011. The most rapid decrease in albedo (more negative than -0.0015 yr-1) occurred in the altitudes over 5500 m above sea level.
In its 2007 report, the IPCC estimated for the first time the direct radiative forcing of black carbon from fossil fuel emissions at + 0.2 W/m², and the radiative forcing of black carbon through its effect on the surface albedo of snow and ice at an additional + 0.1 W/m². More recent studies and public testimony by many of the same scientists cited in the IPCC’s report estimate that emissions from black carbon are the second-largest contributor to global warming after carbon dioxide emissions, and that reducing these emissions may be the fastest strategy for slowing climate change.
Since 1950, many countries have significantly reduced black carbon emissions, especially from fossil fuel sources, primarily to improve public health from improved air quality, and “technology exists for a drastic reduction of fossil fuel related BC” throughout the world.
Given black carbon’s relatively short lifespan, reducing black carbon emissions would reduce warming within weeks. Because black carbon remains in the atmosphere only for a few weeks, reducing black carbon emissions may be the fastest means of slowing climate change in the near term. Control of black carbon, particularly from fossil-fuel and biofuel sources, is very likely to be the fastest method of slowing global warming in the immediate future, and major cuts in black carbon emissions could slow the effects of climate change for a decade or two. Reducing black carbon emissions could help keep the climate system from passing the tipping points for abrupt climate changes, including significant sea-level rise from the melting of Greenland and/or Antarctic ice sheets.
“Emissions of black carbon are the second strongest contribution to current global warming, after carbon dioxide emissions”. Calculation of black carbon’s combined climate forcing at 1.0–1.2 W/m², which “is as much as 55% of the CO2 forcing and is larger than the forcing due to the other [GHGs] such as CH4, CFCs, N2O or tropospheric ozone.”  Other scientists estimate the total magnitude of black carbon’s forcing between + 0.2 and 1.1 W/m² with varying ranges due to uncertainties. (See Table 1.) This compares with the IPCC’s climate forcing estimates of 1.66 W/m2 for CO2 and 0.48 W/m² for CH4. (See Table 2.) In addition, black carbon forcing is two to three times as effective in raising temperatures in the Northern Hemisphere and the Arctic than equivalent forcing values of CO2.
Jacobson calculates that reducing fossil fuel and biofuel soot particles would eliminate about 40% of the net observed global warming. (See Figure 1.) In addition to black carbon, fossil fuel and biofuel soot contain aerosols and particulate matter that cool the planet by reflecting the sun’s radiation away from the Earth. When the aerosols and particulate matter are accounted for, fossil fuel and biofuel soot are increasing temperatures by about 0.35 °C.
Black carbon alone is estimated to have a 20-year Global Warming Potential (GWP) of 4,470, and a 100-year GWP of 1,055–2,240. Fossil fuel soot, as a result of mixing with cooling aerosols and particulate matter, has a lower 20-year GWP of 2,530, and a 100-year GWP of 840-1,280.
The Integrated Assessment of Black Carbon and Tropospheric Ozone published in 2011 by the United Nations Environment Programme and World Meteorological Organization calculates that cutting black carbon, along with tropospheric ozone and its precursor, methane, can reduce the rate of global warming by half and the rate of warming in the Arctic by two-thirds, in combination with CO2 cuts. By trimming “peak warming”, such cuts can keep current global temperature rise below 1.5 ˚C for 30 years and below 2 ˚C for 60 years, in combination with CO2 cuts. (FN: UNEP-WMO 2011.) See Table 1, on page 9 of the UNEP-WMO report.
The reduction of CO2 as well as SLCFs could keep global temperature rise under 1.5 ˚C through 2030, and below 2 ˚C through 2070, assuming CO2 is also cut. See the graph on page 12 of the UNEP-WMO report.
Ramanathan notes that “developed nations have reduced their black carbon emissions from fossil fuel sources by a factor of 5 or more since 1950. Thus, the technology exists for a drastic reduction of fossil fuel related black carbon.” 
Jacobson believes that “[g]iven proper conditions and incentives, [soot] polluting technologies can be quickly phased out. In some small-scale applications (such as domestic cooking in developing countries), health and convenience will drive such a transition when affordable, reliable alternatives are available. For other sources, such as vehicles or coal boilers, regulatory approaches may be required to nudge either the transition to existing technology or the development of new technology.”
Hansen states that “technology is within reach that could greatly reduce soot, restoring snow albedo to near pristine values, while having multiple other benefits for climate, human health, agricultural productivity, and environmental aesthetics. Already soot emissions from coal are decreasing in many regions with transition from small users to power plants with scrubbers.”
Jacobson suggests converting “[U.S.] vehicles from fossil fuel to electric, plug-in-hybrid, or hydrogen fuel cell vehicles, where the electricity or hydrogen is produced by a renewable energy source, such as wind, solar, geothermal, hydroelectric, wave, or tidal power. Such a conversion would eliminate 160 Gg/yr (24%) of U.S. (or 1.5% of world) fossil-fuel soot and about 26% of U.S. (or 5.5% of world) carbon dioxide.” According to Jacobson’s estimates, this proposal would reduce soot and CO2 emissions by 1.63 GtCO2–eq. per year. He notes, however, “that the elimination of hydrocarbons and nitrogen oxides would also eliminate some cooling particles, reducing the net benefit by at most, half, but improving human health,” a substantial reduction for one policy in one country.
For diesel vehicles in particular there are a several effective technologies available. Newer, more efficient diesel particulate filters (DPFs), or traps, can eliminate over 90% of black carbon emissions, but these devices require ultra-low sulfur diesel fuel (ULSD). To ensure compliance with new particulate rules for new on-road and non-road vehicles in the U.S., the EPA first required a nationwide shift to ULSD, which allowed DPFs to be used in diesel vehicles in order to meet the standards. Because of recent EPA regulations, black carbon emissions from diesel vehicles are expected to decline about 70 percent from 2001 to 2020.” Overall, “BC emissions in the United States are projected to decline by 42 percent from 2001 to 2020. By the time the full fleet is subject to these rules, EPA estimates that over 239,000 tons of particulate matter will be reduced annually. Outside of the US diesel oxidation catalysts are often available and DPFs will become available as ULSD is more widely commercialized.
Another technology for reducing black carbon emissions from diesel engines is to shift fuels to compressed natural gas. In New Delhi, India, the supreme court ordered shift to compressed natural gas for all public transport vehicles, including buses, taxis, and rickshaws, resulted in a climate benefit, “largely because of the dramatic reduction of black carbon emissions from the diesel bus engines.” Overall, the fuel switch for the vehicles reduced black carbon emissions enough to produce a 10 percent net reduction in CO2-eq., and perhaps as much as 30 percent. The main gains were from diesel bus engines whose CO2-eq. emissions were reduced 20 percent. According to a study examining these emissions reductions, “there is a significant potential for emissions reductions through the [UNFCCC] Clean Development for such fuel switching projects.”
Technologies are also in development to reduce some of the 133,000 metric tons of particulate matter emitted each year from ships. Ocean vessels use diesel engines, and particulate filters similar to those in use for land vehicles are now being tested on them. As with current particulate filters these too would require the ships to use ULSD, but if comparable emissions reductions are attainable, up to 120,000 metric tons of particulate emissions could be eliminated each year from international shipping. That is, if particulate filters could be shown reduce black carbon emissions 90 percent from ships as they do for land vehicles, 120,000 metric tons of today’s 133,000 metric tons of emissions would be prevented. Other efforts can reduce the amount of black carbon emissions from ships simply by decreasing the amount of fuel the ships use. By traveling at slower speeds or by using shore side electricity when at port instead of running the ship’s diesel engines for electric power, ships can save fuel and reduce emissions.
Ramanathan estimates that “providing alternative energy-efficient and smoke-free cookers and introducing transferring technology for reducing soot emissions from coal combustion in small industries could have major impacts on the radiative forcing due to soot.”  Specifically, the impact of replacing biofuel cooking with black carbon-free cookers (solar, bio, and natural gas) in South and East Asia is dramatic: over South Asia, a 70 to 80% reduction in black carbon heating; and in East Asia, a 20 to 40% reduction.”
Many countries have existing national laws to regulating black carbon emissions, including laws that address particulate emissions. Some examples include:
- banning or regulating slash-and-burn clearing of forests and savannas;
- requiring shore-based power/electrification of ships at port, regulating idling at terminals, and mandating fuel standards for ships seeking to dock at port;
- requiring regular vehicle emissions tests, retirement, or retrofitting (e.g. adding particulate traps), including penalties for failing to meet air quality emissions standards, and heightened penalties for on-the-road "super-emitting" vehicles;
- banning or regulating the sale of certain fuels and/or requiring the use of cleaner fuels for certain uses;
- limiting the use of chimneys and other forms of biomass burning in urban and non-urban areas;
- requiring permits to operate industrial, power generating, and oil refining facilities and periodic permit renewal and/or modification of equipment; and
- requiring filtering technology and high-temperature combustion (e.g. super-critical coal) for existing power generation plants, and regulating annual emissions from power generation plants.
The International Network for Environmental Compliance & Enforcement issued a Climate Compliance Alert on Black Carbon in 2008 which cited reduction of carbon black as a cost-effective way to reduce a major cause of global warming.
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- V. Ramanathan & G. Carmichael, supra note 1, at 221 ("Until about the 1950s, North America and Western Europe were the major sources of soot emissions, but now developing nations in the tropics and East Asia are the major source problem.").
- Jacobson Testimony, supra note 9, at 4
- Clean Air Fine Particle Implementation Rule, 72 Fed. Reg. 20586, 20587 (April 25, 2007) (to be codified as 40 C.F.R. pt. 51), available athttp://www.epa.gov/fedrgstr/EPA-AIR/2007/April/Day-25/a6347.pdf; Press Release, European Union, Environment: Commission welcomes final adoption of the air quality directive, (April 14, 2008), available at http://europa.eu/rapid/pressReleasesAction.do?reference=IP/08/570&type = HTML&aged=0&language=EN&guiLanguage=en.
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- Tami Bond, Testimony for the Hearing on Black Carbon and Climate Change, U.S. House Committee on Oversight and Government Reform 2-3 (October 18, 2007), available athttp://oversight.house.gov/images/stories/documents/20071018110647.pdf [hereinafter Bond Testimony]
- Jacobson Testimony, supra note 9, at 5.
- Tami Bond, Summary: Aerosols, Air Pollution as a Climate Forcing: A Workshop, Honolulu, Hawaii, April 29-May 3, 2002, available at http://www.giss.nasa.gov/meetings/pollution2002/
- V. Ramanathan & G. Carmichael, supra note 1, at 226
- Ramanathan Testimony, supra note 4, at 4
- V. Ramanathan & G. Carmichael, supra note 1, at 221
- V. Ramanathan & G. Carmichael, id
- V. Ramanathan & G. Carmichael, id. at 224.
- See Bond Testimony, supra note 42, at 2 (figure 1)
- Bond Testimony, id. at 1-2.
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- Dons, E; Int Panis, Luc; Van Poppel, Martine; Theunis, Jan; Willems, Hanny; Torfs, Rudi; Wets, Geert (2011). "Impact of time-activity patterns on personal exposure to black carbon". Atmospheric Environment 45 (21): 3594–3602. Bibcode:2011AtmEn..45.3594D. doi:10.1016/j.atmosenv.2011.03.064.
- Jacobson Testimony, supra note 13, at 5-6 (showing that shipping emissions produce more than 3 times as much black carbon as POC, while off-road vehicles produce 40% more black carbon than POC, and on-road vehicles produce 25-60% more black carbon than POC).
- Although shipping only accounts for 1.7% of the global black carbon inventory, given the expected increase in shipping throughout regions especially sensitive to black carbon like the Arctic, it still represents a strong option for black carbon reductions. Lack, D., B. Lerner, C. Granier, T. Baynard, E. Lovejoy, P. Massoli, A. R. Ravishankara, and E. Williams, Light absorbing carbon emissions from commercial shipping, 35 Geophysical Res. Letters L13815 (2008).
- J. Hansen et al., Efficacy of Climate Forcing, supra note 27
- Mark. Z. Jacobson, The Short-Term Cooling but Long-Term Global Warming Due to Biomass Burning, 17 J. OF CLIMATE 2909, 2923 (". . . whereas aerosol particles emitted during burning may cause a short-term cooling of global climate, longer-lived greenhouse gases may cause warming (or cancel the cooling) after several decades. As such, reducing biomass burning may cause short-term warming but long-term cooling or no change in temperature. Although the eventual cooling may not appear for many years, its magnitude may be as large as 0.6 K after 100 yr.").
- Surabi Menon, James Hansen, Larissa Nazarenko, & Yunfeng Luo,Climate Effects of Black Carbon, 297 SCIENCE 2250, 2250 (27 September 2002) (Black Carbon emissions are "a product of incomplete combustion from coal, diesel engines, biofuels, and outdoor biomass burning . . .").
- Lehmann, et al., Bio-Char Sequestration in Terrestrial Ecosystems – A Review, 11 MITIGATION AND ADAPTATION STRATEGIES FOR GLOBAL CHANGE 403, at 403-07, 418 (Springer 2006), available at http://www.css.cornell.edu/faculty/lehmann/publ/MitAdaptStratGlobChange%2011,%20403-427,%20Lehmann,%202006.pdf ; See id. at 407 (Researchers estimate that between 38-84% of the biomass carbon in vegetation is released during the burn, whereas converting the biomass into bio-char by means of simple kiln techniques sequesters more than 50% of this carbon in bio-char).
- Id. at 407-08
- Raupach, Michael, et al., Global and Regional Drivers of Accelerating CO2 Emissions, 104 Proceedings of the National Academy of Sciences of the United States of America 24, (underlying data available at http://www.pnas.org/cgi/content/full/0700609104/DC1) (indicating that between 2000 and 2005 land use emissions annually represented on average 1.5 GtC of the total 8.7 GtC global emissions or 5.5 Gt CO2 eq. of 31.9 Gt CO2 eq. of global emissions—17.25% of total. A reduction of 12% of land use emissions equals 0.66 Gt CO2 eq., approximately 2% of annual global CO2 eq. emissions. Lehmann’s original estimates were based on a 0.2 GtC offset of the 1.7 GtC emissions from land use change estimated in 2001 by the IPCC). See also Lehmann, et al., supra note 49, at 407-08. (Given the increase in fossil fuel emissions to 8.4 GtC, total anthropogenic emissions in 2006, including the estimated 1.5 GtC from land use change, were 9.9 GtC. Thus, despite an increase in overall CO2 eq. emissions, using Lehmann’s original 0.2 GtC reduction still results in an approximate 2% reduction in global CO2 eq. emissions). See Global Carbon Budget Team, Recent Carbon Trends and the Global Carbon Budget, the Global Carbon Project, (15 November 2007), available at http://www.globalcarbonproject.org/global/pdf/GCP_CarbonCycleUpdate.pdf (giving 2006 global carbon emissions estimates).
- Black carbon: Better monitoring needed to assess health and climate change impacts - European Environmental Agency
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- Dons, E; Van Poppel, M; Kochan, B; Wets, G; Int Panis, L (2013). "Modeling temporal and spatial variability of traffic-related air pollution: Hourly land use regression models for black carbon". Atmospheric Environment 74: 237–246. Bibcode:2013AtmEn..74..237D. doi:10.1016/j.atmosenv.2013.03.050.
- Dons, E; Int Panis, L; Van Poppel, M; Theunis, J; Willems, H; Torfs, R; Wets, G (2011). "Impact of time-activity patterns on personal exposure to black carbon". Atmospheric Environment 45 (21): 3594–3602. Bibcode:2011AtmEn..45.3594D. doi:10.1016/j.atmosenv.2011.03.064.
- Dons, E; Int Panis, L; Van Poppel, M; Theunis, J; Wets, G (2012). "Personal exposure to Black Carbon in transport microenvironments". Atmospheric Environment 55: 392–398. Bibcode:2012AtmEn..55..392D. doi:10.1016/j.atmosenv.2012.03.020.
- Dons, E; Temmerman, P; Van Poppel, M; Bellemans, T; Wets, G; Int Panis, L (2013). "Street characteristics and traffic factors determining road users' exposure to black carbon". Science of the Total Environment 447: 72–79. doi:10.1016/j.scitotenv.2012.12.076. PMID 23376518.
- De Prins, S (2014). "Airway oxidative stress and inflammation markers in exhaled breath from children are linked with exposure to black carbon". Environment International 73: 440–446. doi:10.1016/j.envint.2014.06.017.
- Lydersen, Kari (April 21, 2011). "Black Carbon Testing Finds High Levels". The New York Times. Retrieved April 22, 2011.
Major American cities generally have background levels of one to three micrograms of black carbon per cubic meter.
- Koch, D.; A.D.Del Genio (2010). "Black carbon semi-direct effects on cloud cover: review and synthesis" (PDF). Atmospheric Chemistry and Physics 10: 7685–7696. doi:10.5194/acp-10-7685-2010.
- T. C. Bond; S. J. Doherty, D. W. Fahey, P. M. Forster, T. Berntsen, B. J. DeAngelo, M. G. Flanner, S. Ghan, B. Kärcher, D. Koch, S. Kinne, Y. Kondo, P. K. Quinn, M. C. Sarofim, M. G. Schultz, M. Schulz, C. Venkataraman, H. Zhang, S. Zhang, N. Bellouin, S. K. Guttikunda, P. K. Hopke, M. Z. Jacobson, J. W. Kaiser, Z. Klimont, U. Lohmann, J. P. Schwarz, D. Shindell, T. Storelvmo, S. G. Warren, C. S. Zender (Submitted 26 March 2012; published online January 15, 2013). "Bounding the role of black carbon in the climate system: A scientific assessment". Journal of Geophysical Research-Atmospheres (Wiley) 118 (11): 5380–5552. Bibcode:2013JGRD..118.5380B. doi:10.1002/jgrd.50171. Check date values in:
- Elisabeth Rosenthal (January 15, 2013). "Burning Fuel Particles Do More Damage to Climate Than Thought, Study Says". The New York Times. Retrieved January 17, 2013.
- Mollie Bloudoff-Indelicato (January 17, 2013). "A Smut Above: Unhealthy Soot in the Air Could Also Promote Global Warming: Atmospheric black carbon is not only bad for the lungs, but can also act as greenhouse particles under certain circumstances". Scientific American. Retrieved January 22, 2013.
- IPCC, Changes in Atmospheric Constituents and in Radiative Forcing, in CLIMATE CHANGE 2007: THE PHYSICAL SCIENCE BASIS. CONTRIBUTION OF WORKING GROUP I TO THE FOURTH ASSESSMENT REPORT OF THE INTERGOVERNMENTAL PANEL ON CLIMATE CHANGE 129, 132 (2007), available at http://www.ipcc.ch/ipccreports/ar4-wg1.htm. (Magnitudes and uncertainties added together, as per standard uncertainty rules)
- V. Ramanathan and G. Carmichael, Global and regional climate changes due to black carbon, 1 NATURE GEOSCIENCE 221-22 (23 March 2008) ("The BC forcing of 0.9 W m–2 (with a range of 0.4 to 1.2 W m–2) … is as much as 55% of the CO2 forcing and is larger than the forcing due to the other GHGs such as CH4, CFCs, N2O or tropospheric ozone.")
- Mark Z. Jacobson, Effects of Anthropogenic Aerosol Particles and Their Precursor Gases on California and South Coast Climate, California Energy Commission, 6 (Nov. 2004), available athttp://www.stanford.edu/group/efmh/jacobson/CEC-500-2005-003.PDF (BC’s semi-direct effect occurs when "solar absorption by a low cloud increases stability below the cloud, reducing vertical mixing of moisture to the cloud base, thinning the cloud.").
- Carbon’s Other Warming Role, GEOTIMES (May 2001), available at http://www.geotimes.org/mar01/warming.html (BC produces "dirty cloud droplets, causing an "indirect" impact that reduces a cloud's reflective properties.").
- IPCC, Changes in Atmospheric Constituents and in Radiative Forcing, in CLIMATE CHANGE 2007: THE PHYSICAL SCIENCE BASIS, CONTRIBUTION OF WORKING GROUP I TO THE FOURTH ASSESSMENT REPORT OF THE INTERGOVERNMENTAL PANEL ON CLIMATE CHANGE, 129, 163-64, and 185 (2007) (estimating the direct radiative forcing of BC at 0.2 W/m2 + 0.15 and the indirect of effect of BC on snow and ice surface albedo at 0.1 W/m2 + 0.1).
- Mark Z. Jacobson, Strong Radiative Heating Due to the Mixing State of Black Carbon in Atmospheric Aerosols, NATURE, 409, 695-697 (2001) ("The final yearly averaged direct forcing due to BC in the external mixture, the multiple-distribution coated-core, and the single internally mixed, coated-core distribution cases from Fig. 3 were 0.31, 0.55 and 0.62 W/m2, respectively. The multiple-distribution BC direct forcing (0.55) falls between direct-forcing estimates for CH4 (0.47 W/m2 and CO2 (1.56 W/m2) from IPCC .").
- Mark Z. Jacobson, Climate response of fossil fuel and biofuel soot, accounting for soot’s feedback to snow and sea ice albedo and emissivity, 109 J. GEOPHYS. RES. D21201 (2004). (Dirty Clouds Effect of .03 W m-2)
- Mark Z. Jacobson, Effects of Externally-Through-Internally-Mixed Soot Inclusions within Clouds and Precipitation on Global Climate, 110 J. PHYS. CHEM. A. 6860-6873 (2006). (Snow/Ice Albedo Effect of .06 W m-2) This figure has been obtained by adding Jacobson’s estimates for BC’s direct and indirect forcings. See supra, notes 76-78 and accompanying text.
- James E. Hansen and Makiko Sato, Figure 1 in Trends of Measures Climate Forcing Agents, 98 PROC. OF THE NAT’L ACAD. OF SCI. 14778, 14779 (2001). (Hansen 2001 estimate – Direct Forcing – 0.6 W/m2 Total forcing – 0.8 + 0.4 W/m2); J. Hansen, supra note 11, at 435 (Hansen 2002 estimate – "My present estimate for global climate forcings caused by BC is: (1) 0.4 + 0.2 W/m2 direct effect, (2) 0.3 + 0.3 W/m2semi-direct effect (reduction of low level clouds due to BC heating; Hansen et al., 1997), (3) 0.1 + 0.05 W/m2 ‘dirty clouds’ due to BC droplet nuclei, (4) 0.2 + 0.1 W/m2 snow and ice darkening due to BC deposition. … The uncertainty estimates are subjective. The net BC forcing implied is 1 + 0.5 W/m2."); J. Hansen, et al., Climate Change and Trace Gases, 365 PHIL. TRANS. R. SOC. 1925, 1942 (2007) (Hansen 2007 estimate – "Soot from fossil fuel burning, i.e. highly absorbing aerosols that contain black carbon (BC) and organic carbon (OC), are estimated to cause a global climate forcing of 0.22 W m-2. This is a conservative estimate for fossil fuel BC forcing . . . because it assumes a high OC/BC ratio for fossil fuel emissions. In addition, it assigns 50% of the aerosol indirect effect (which causes cooling) to soot (BC/OC).").
- . Hansen, supra note 11, at 435 (Hansen 2002 estimate – "My present estimate for global climate forcings caused by BC is: (1) 0.4 + 0.2 W/m2 direct effect, (2) 0.3 + 0.3 W/m2 semi-direct effect (reduction of low level clouds due to BC heating; Hansen et al., 1997), (3) 0.1 + 0.05 W/m2 ‘dirty clouds’ due to BC droplet nuclei, (4) 0.2 + 0.1 W/m2 snow and ice darkening due to BC deposition. … The uncertainty estimates are subjective. The net BC forcing implied is 1 + 0.5 W/m2.").
- J. Hansen, supra note 11, at 435 (Hansen 2002 estimate – "My present estimate for global climate forcings caused by BC is: (1) 0.4 + 0.2 W/m2 direct effect, (2) 0.3 + 0.3 W/m2 semi-direct effect (reduction of low level clouds due to BC heating; Hansen et al., 1997), (3) 0.1 + 0.05 W/m2 ‘dirty clouds’ due to BC droplet nuclei, (4) 0.2 + 0.1 W/m2 snow and ice darkening due to BC deposition. … The uncertainty estimates are subjective. The net BC forcing implied is 1 + 0.5 W/m2.").
- J. Hansen, supra note 11, at 435 (Hansen 2002 estimate – "My present estimate for global climate forcings caused by BC is: (1) 0.4 + 0.2 W/m2 direct effect, (2) 0.3 + 0.3 W/m2 semi-direct effect (reduction of low level clouds due to BC heating; Hansen et al., 1997), (3) 0.1 + 0.05 W/m2 ‘dirty clouds’ due to BC droplet nuclei, (4) 0.2 + 0.1 W/m2 snow and ice darkening due to BC deposition. … The uncertainty estimates are subjective. The net BC forcing implied is 1 + 0.5 W/m2.").
- James E. Hansen and Makiko Sato, Figure 1 in Trends of Measures Climate Forcing Agents, 98 PROC. OF THE NAT’L ACAD. OF SCI. 14778, 14779 (2001). (Hansen 2001 estimate – Direct Forcing – 0.6 W m-2, Total forcing – 0.8 + 0.4 W m-2); J. Hansen, supra note 11, at 435 (Hansen 2002 estimate –"My present estimate for global climate forcings caused by BC is: (1) 0.4 + 0.2 W/m2 direct effect, (2) 0.3 + 0.3 W/m2 semi-direct effect (reduction of low level clouds due to BC heating; Hansen et al., 1997), (3) 0.1 + 0.05 W/m2 ‘dirty clouds’ due to BC droplet nuclei, (4) 0.2 + 0.1 W/m2 snow and ice darkening due to BC deposition. … The uncertainty estimates are subjective. The net BC forcing implied is 1 + 0.5 W/m2."); Makiko Sato, James Hansen, Dorthy Koch, Andrew Lacis, Reto Ruedy, Oleg Dubovik, Brent Holben, Mian Chin, and Tica Novakov, "Global Atmospheric Black Carbon Inferred from AERONET, 100 PROC. OF THE NAT’L ACAD. OF SCI. 6319, at 6323 (2003) (… we estimate the anthropogenic BC forcing as »0.7 + 0.2 W/m2."); J. Hansen, et al., Climate Change and Trace Gases, 365 PHIL. TRANS. R. SOC. 1925, 1942 (2007) (Hansen 2007 estimate –"Soot from fossil fuel burning, i.e. highly absorbing aerosols that contain black carbon (BC) and organic carbon (OC), are estimated to cause a global climate forcing of 0.22 W m-2. This is a conservative estimate for fossil fuel BC forcing . . . because it assumes a high OC/BC ratio for fossil fuel emissions. In addition, it assigns 50% of the aerosol indirect effect (which causes cooling) to soot (BC/OC).").
- J. Hansen & L. Nazarenko, supra note 14, 426 ("the effective forcing for the assigned snow albedo change in the most realistic cases 1 and 2 is Fe ~0.6 W/m2 in the Northern Hemisphere or Fe ~0/3 W/m2 globally.").
- James E. Hansen and Makiko Sato, Figure 1 in Trends of Measures Climate Forcing Agents, 98 PROC. OF THE NAT’L ACAD. OF SCI. 14778, 14779 (2001). (Hansen 2001 estimate – Direct Forcing – 0.6 W/m2, Total forcing – 0.8 + 0.4 W/m2); J. Hansen, supra note 11, at 435 (Hansen 2002 estimate – "My present estimate for global climate forcings caused by BC is: (1) 0.4 + 0.2 W/m2 direct effect, (2) 0.3 + 0.3 W/m2 semi-direct effect (reduction of low level clouds due to BC heating; Hansen et al., 1997), (3) 0.1 + 0.05 W/m2 ‘dirty clouds’ due to BC droplet nuclei, (4) 0.2 + 0.1 W/m2 snow and ice darkening due to BC deposition. … The uncertainty estimates are subjective. The net BC forcing implied is 1 + 0.5 W/m2."); Makiko Sato, James Hansen, Dorthy Koch, Andrew Lacis, Reto Ruedy, Oleg Dubovik, Brent Holben, Mian Chin, and Tica Novakov, Global Atmospheric Black Carbon Inferred from AERONET, 100 PROC. OF THE NAT’L ACAD. OF SCI. 6319, at 6323 (2003) (… we estimate the anthropogenic BC forcing as »0.7 + 0.2 W/m2."); J. Hansen, et al., Climate Change and Trace Gases, 365 PHIL. TRANS. R. SOC. 1925, 1942 (2007) (Hansen 2007 estimate – "Soot from fossil fuel burning, i.e. highly absorbing aerosols that contain black carbon (BC) and organic carbon (OC), are estimated to cause a global climate forcing of 0.22 W m-2. This is a conservative estimate for fossil fuel BC forcing . . . because it assumes a high OC/BC ratio for fossil fuel emissions. In addition, it assigns 50% of the aerosol indirect effect (which causes cooling) to soot (BC/OC).").
- Id., at 425 (The "climate forcing due to snow/ice albedo change is of the order of 1 W/m2 at middle- and high-latitude land areas in the Northern Hemisphere and over the Arctic Ocean.")
- Ramanathan Testimony, supra note 4.
- IPCC, supra note 3.
- J. Hansen, et al., Efficacy of Climate Forcing, supra note 22.
- IPCC, supra note 13, at 397. ("While the radiative forcing is generally negative, positive forcing occurs in areas with a very high surface reflectance such as desert regions in North Africa, and the snow fields of the Himalayas."); J. Hansen & L. Nazarenko, supra note 14, at 425. (The brown haze over India, heavy with fossil fuel and biofuel soot, reaches to the Himalayas. If prevailing winds deposit even a fraction of this soot on glaciers, the snow black carbon content could be comparable to that in the Alps.").
- J. Hansen, et al., Efficacy of Climate Forcing, 110 J. GEOPHYS. RES. D18104, 1 (2005), available at http://pubs.giss.nasa.gov/docs/2005/2005_Hansen_etal_2.pdf (Accounting for forcing efficacies and for indirect effects via snow albedo and cloud changes, we find that fossil fuel soot, defined as black carbon + OC (organic carbon), has a net positive forcing while biomass burning black carbon + OC has a negative forcing).
- IPCC, supra note 13, at 397.
- Zender Testimony, supranote 3, at 6.
- J. Hansen & L. Nazarenko,supra note 14, at 425.
- J. Hansen & L. Nazarenko, id. at 428
- J. Hansen & L. Nazarenko,id. at 425
- See supra note 18
- P.K. Quinn, T.S. Bates, E. Baum, N. Doubleday, A.M. Fiore, M. Flanner, A. Fridlind, T.J. Garrett, D. Koch, S. Menon, D. Shindell, A. Stohl, and S.G. Warren. Short-lived Pollutants in the Arctic: Their Climate Impact and Possible Mitigation Strategies, 8 ATMOS. CHEM. PHYS. 1723, 1731 (2008); See David Shukman, Vast Cracks Appear in Arctic Ice, BBC NEWS (23 May 2008), available at http://news.bbc.co.uk/2/hi/science/nature/7417123.stm (A recent expedition study by Canada confirmed vast cracks stretching for more than 10 miles on Ward Hunt)
- Charles Zender, Written Testimony for the Hearing on Black Carbon and Climate Change, U.S. House Committee on Oversight and Government Reform 1 (18 October 2007),available at http://oversight.house.gov/images/stories/documents/20071018110919.pdf [hereinafter Zender Testimony].
- P.K. Quinn,supra note 34, at 1732.
- P.K. Quinn, id
- P.K. Quinn, id. at 1732; J. Hansen & M. Sato,et al., Dangerous Human-Made Interference with Climate: a GISS modelE Study 7 ATMOS. CHEM. PHYS. DISCUSS. 2287, 2298, 2296 (2007)("We suggest that Arctic climate change has been driven as much by pollutants (03, its precursors CH4 and soot) as by CO2 ... Thus, in that case, reduction of some of the pollutants [including soot] may make it possible to keep further Arctic warming very small and thus probably avoid loss of all sea ice.")
- V. Ramanathan & G. Carmichael, supra note 1, at 221.
- V. Ramanathan & G. Carmichael, supranote 1, at 224
- Jing Ming, Dongqi Zhang, Shichang Kang et al., 2007. Aerosol and fresh snow chemistry in the East Rongbuk Glacier on the northern slope of Mt. Qomolangma (Everest), J. Geophys. Res., 112, D15307, doi:10.1029/2007JD008618
- Jing Ming, Cunde Xiao, Junying Sun et al., 2010. Carbonaceous particles in the atmosphere and precipitation of the Nam Co region, central Tibet. J. Environ. Sci.-CHINA, 22(11), 1748–1756.
- Jing Ming, Cunde Xiao, Helene Cachier et al., 2009. Black carbon in the snow of glaciers in west China and its potential effects on albedos, Atmos. Res., 92(1), 114-123.
- Jing Ming, H. Cachier, C. Xiao et al., 2008. Black carbon record based on a shallow Himalayan ice core and its climatic implications. Atmos. Chem. Phys., 8(5), 1343–1352
- Lester R. Brown, Melting Mountain Glaciers Will Shrink Grain Harvests in China and India, PLAN B UPDATE, Earth Policy Institute (20 March 2008), available athttp://www.earth-policy.org/Updates/2008/Update71.htm (Melting Himalayan glaciers will soon reduce water supply for major Chinese and Indian rivers (Ganges, Yellow River, Yangtze River) that irrigate rice and wheat crops that feed hundreds of millions and "could lead to politically unmanageable food shortages.").
- Jing Ming, Zhencai Du, Cunde Xiao et al., 2012. Darkening of the mid-Himalaya glaciers since 2000 and the potential causes. Environ. Res. Lett., 7(1): 014021.
- Ming, J, Wang, Y, Du, Z, Zhang, T, Guo, W, Xiao, C, Xu, X, Ding, M, Zhang, D, Yang, W, 2015. Widespread albedo decreasing and induced melting of Himalayan snow and ice in the early 21st century. Plos One 10:e0126235.
- Ming, J, Wang, Y, Du, Z, Zhang, T, Guo, W, Xiao, C, Xu, X, Ding, M, Zhang, D, Yang, W, 2015. Widespread albedo decreasing and induced melting of Himalayan snow and ice in the early 21st century. Plos One 10:e0126235.
- IPCC, Changes in Atmospheric Constituents and in Radiative Forcing, in CLIMATE CHANGE 2007: THE PHYSICAL SCIENCE BASIS. CONTRIBUTION OF WORKING GROUP I TO THE FOURTH ASSESSMENT REPORT OF THE INTERGOVERNMENTAL PANEL ON CLIMATE CHANGE 129, 136, 163 (2007), available at http://www.ipcc.ch/ipccreports/ar4-wg1.htm
- "Third-World Stove Soot Is Target in Climate Fight" article by Elizabeth Rosenthal in The New York Times April 15, 2009
- See id. at 164, 170, 174–76, 217–34 (citing studies by Ramanathan, Jacobson, Zender, Hansen, and Bond); supra notes 3-4 (Zender Testimony and Ramanathan Testimony); infra notes 9 and 42 (Jacobson Testimony and Bond Testimony).
- V. Ramanathan, Testimony for the Hearing on Black Carbon and Climate Change, U.S. House Committee on Oversight and Government Reform 4 (18 October 2007), available at http://oversight.house.gov/images/stories/documents/20071018110734.pdf [hereinafter Ramanathan Testimony] (The developed nations have reduced their black carbon emissions from fossil fuel sources by a factor of 5 or more. Thus the technology exists for a drastic reduction of fossil fuel related black carbon); but compare Bond, T. C., E. Bhardwaj, R. Dong, R. Jogani, S. Jung, C. Roden, D. G. Streets, and N. M. 'Trautmann Historical emissions of black and organic carbon aerosol from energy-related combustion, 1850–2000, 21 Global Biogeochemical Cycles GB2018 (2007) (Previous work suggests a rapid rise in [global] black carbon emissions between 1950 and 2000; this work supports a more gradual, smooth increase between 1950 and 2000).
- Ramanathan Testimony, supra note 8, at 3 ("Thus a drastic reduction in BC has the potential of offsetting the CO2 induced warming for a decade or two.").
- Timothy Lenton, Hermann Held, Elmar Kriegler, Jim Hall, Wolfgang Lucht, Stefan Rahmstorf, and Hans Joachim Schellnhuber, Tipping elements in the Earth’s climate system, 105 PROC. OF THE NAT’L ACAD. OF SCI. 6 (12 February 2008) ("The greatest threats are tipping the Arctic sea-ice and the Greenland ice sheet. . ."); J. Hansen, Climate Catastrophe, NEW SCIENTIST (28 July 2007) (...the primary issue is whether global warming will reach a level such that ice sheets begin to disintegrate in a rapid, non-linear fashion on West Antarctica, Greenland or both.").
- V. Ramanathan and G. Carmichael, supra note 1, at 221 (". . . emissions of black carbon are the second strongest contribution to current global warming, after carbon dioxide emissions.") Numerous scientists also calculate that black carbon may be second only to CO2 in its contribution to climate change, including Tami C. Bond & Haolin Sun, Can Reducing Black Carbon Emissions Counteract Global Warming, ENVIRON. SCI. TECHN. (2005), at 5921 ("BC is the second or third largest individual warming agent, following carbon dioxide and methane."); and J. Hansen, A Brighter Future, 53 CLIMATE CHANGE 435 (2002), available at http://pubs.giss.nasa.gov/docs/2002/2002_Hansen_1.pdf (calculating the climate forcing of BC at 1.0±0.5 W/m2).
- V. Ramanathan and G. Carmichael, supra note 4, at 222.
- IPCC, "Technical Summary", in Climate Change 2007: The Physical Science basis,. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change, 21 (2007) available at http://www.ipcc.ch/ipccreports/ar4-wg1.htm.
- James Hansen & Larissa Nazarenko, Soot Climate Forcing Via Snow and Ice Albedos, 101 Proc. of the Nat'l. Acad. of Sci. 423 (13 January 2004) ("The efficacy of this forcing is »2 (i.e. for a given forcing it is twice as effective as CO2 in altering global surface air temperature)"); compare Zender Testimony, supra note 7, at 4 (figure 3); See J. Hansen & L. Nazarenko, supra note 18, at 426. ("The efficacy for changes of Arctic sea ice albedo is >3. In additional runs not shown here, we found that the efficacy of albedo changes in Antarctica is also >3."); See also Flanner, M.G., C.S. Zender, J.T. Randerson, and P.J. Rasch, Present-day climate forcing and response from black carbon in snow, 112 J. GEOPHYS. RES. D11202 (2007) ("The forcing is maximum coincidentally with snowmelt onset, triggering strong snow-albedo feedback in local springtime. Consequently, the "efficacy" of black carbon/snow forcing is more than three times greater than forcing by CO2.").
- Gross global warming should result in about 2 °C (4 °F) temperature rise. However, observed global warming is only about 0.8 °C because cooling particles off set much of the warming. Reducing fossil fuel and biofuel soot would reduce about 40% of the observed warming and about 16% of the gross warming. Jacobson Testimony, supra note 13, at 3. ("The figure also shows that fossil-fuel plus biofuel soot may contribute to about 16% of gross global warming (warming due to all greenhouse gases plus soot plus the heat island effect), but its control in isolation could reduce 40% of net global warming.").
- Jacobson Testimony, id. at 4.
- Jacobson Testimony, id
- Jacobson Testimony, id. As an aerosol, there is not standardized formula for developing global warming potentials (GWP) for black carbon. However, attempts to derive GWP100 range from 190 – 2240 relative to CO2. Jacobson M Z 2005 Correction to `control of fossil-fuel particulate black carbon and organic matter, possibly the most effective method of slowing global warming' 110 J. Geophysical Res. D14105 (2005) (GWP BC – 190); Hansen, J., Mki. Sato, P. Kharecha, G. Russell, D.W. Lea, and M. Siddall, 2007: Climate change and trace gases. Phil. Trans. Royal. Soc. A, 365, 1925 (GWP BC – 500); Bond, T. and Haolin, Sun, "Can Reducing Black Carbon Emissions Counteract Global Warming?" Envtl. Sci. & Tech., 5921 (August 2005) (GWP BC – 680); Jacobson Testimony, supra note 9 at 4 (GWP BC – 2240)
- Jacobson Testimony, supra note 9, at 4.
- UNEP and World Meteorological Organization, INTEGRATED ASSESSMENT OF BLACK CARBON AND TROPOSPHERIC OZONE, SUMMARY FOR DECISION MAKERS (June 2011).
- Ramanathan Testimony, supra note 4, at 4.
- J. Hansen & L. Nazarenko,supra note 14, at 428
- Jacobson Testimony, supra note 9, at 9.
- Jacobson offers an estimate of total U.S. CO2 emissions in 2005 of 6270 metric tonnes, 26% of which is 1630. Id.
- Jacobson Testimony, supra note 9, at 9
- Manufacturers of Emission Controls Association (MECA), "Emission Control Technologies for Diesel-Powered Vehicles," 9 (December 2007) ("Diesel oxidation catalysts installed on a vehicle’s exhaust system can reduce total PM typically by as much as 25 to over 50 percent by mass, under some conditions depending on the composition of the PM being emitted"), available at:http://www.meca.org/galleries/default-file/MECA%20Diesel%20White%20Paper%2012-07-07%20final.pdf.
- Id., ("DPFs can achieve up to, and in some cases, greater than a 90 percent reduction in PM. High efficiency filters are extremely effective in controlling the carbon fraction of the particulate, the portion of the particulate that some health experts believe may be the PM component of greatest concern").
- Id., at 5, ("Mobile source black carbon emissions are estimated at 234 Gg in 2001, representing 54 percent of the nationwide black carbon emissions of 436 Gg. Under Scenario F, mobile source emissions are projected to decline to 71 Gg, a reduction of 163 Gg."
- Bahner, Mark A., Weitz, Keith A., Zapata, Alexandra and DeAngelo, Benjamin, Use of Black Carbon and Organic Carbon Inventories for Projections and Mitigation Analysis," 1, (2007) available at: http://www.epa.gov/ttn/chief/conference/ei16/session3/k.weitz.pdf.
- EPA, Heavy-Duty Highway Diesel Program, available at: http://www.epa.gov/oms/highway-diesel/index.htm ("Once this action is fully implemented…Soot or particulate matter will be reduced by 110,000 tons a year"); EPA, Clean Air Nonroad Diesel Rule—Facts and Figures, available at: http://www.epa.gov/nonroad-diesel/2004fr/420f04037.htm ("Environmental Benefits When the Fleet of Older Nonroad Engines Has Fully Turned Over by 2030: Annual reductions of Fine PM (PM2.5): 129,000 tons").
- Conor C. O. Reynolds & Milind Kandlikar, Climate Impacts of Air Quality Policy: Switching to a Natural Gas-Fueled Public Transportation System in New Delhi, ENVIRON. SCI. TECHNOL. (forthcoming 2008) ("When aerosol emissions are included, the switch to CNG fueling results in a climate benefit, largely because of the dramatic reduction of black carbon emissions from the diesel bus engines"). The fuel switching policy was implemented with the aid of the Indian Supreme Court. See Urvashi Narain and Ruth Greenspan Bell, Who Changed Delhi’s Air? The Roles of the Court and the Executive in Environmental Policymaking, Resources for the Future Discussion Paper 05-48 (December 2005) http://www.rff.org/rff/documents/rff-dp-05-48.pdf ("[T]he main role of the Supreme Court was to force the government to implement previously announced policies. … [T]he Delhi experience for instituting change has become a model for other Indian cities as well as neighboring countries.")
- Conor C. O. Reynolds & Milind Kandlikar, Climate Impacts of Air Quality Policy: Switching to a Natural Gas-Fueled Public Transportation System in New Delhi, ENVIRON. SCI. TECHNOL. (forthcoming 2008) ("However, when aerosol emissions are taken into account in our model, the net effect of the switch is estimated to be a 10% reduction in CO2(e), and there may be as much as a 30% reduction in CO2(e)").
- Id., at Section 3.1 ("In total there is about a 10% reduction of net CO2(e) emissions, and if buses are considered separately, net CO2(e) emissions are reduced by about 20%").
- C. O. Reynolds & Milind Kandlikar, Climate Impacts of Air Quality Policy: Switching to a Natural Gas-Fueled Public Transportation System in New Delhi, 1, ENVIRON. SCI. TECHNOL. (forthcoming 2008).
- Lack, D., B. Lerner, C. Granier, T. Baynard, E. Lovejoy, P. Massoli, A. R. Ravishankara, and E. Williams, Light absorbing carbon emissions from commercial shipping, 35 Geophysical Res. Letters L13815 (2008).
- That is, if particulate filters could be shown reduce black carbon emissions 90 percent from ships as they do for land vehicles, 120,000 metric tons of today’s 133,000 metric tons of emissions would be prevented.
- Conor C. O. Reynolds & Milind Kandlikar, Climate Impacts of Air Quality Policy: Switching to a Natural Gas-Fueled Public Transportation System in New Delhi, ENVIRON. SCI. TECHNOL. (forthcoming 2008) ("Between 2001 and 2003, public transport vehicles in New Delhi were required to switch their fuel to natural gas in an attempt to reduce their air pollution impacts. …[W]hen [black carbon and other] aerosol emissions are taken into account in our model, the net effect of the switch is estimated to be a 10% reduction in CO2 (eq), and there may be as much as a 30% reduction…. There is a significant potential for emissions reductions through the [UNFCCC] Clean Development for such fuel switching projects.") The fuel switching policy was implemented with the aid of the Indian Supreme Court. See Urvashi Narain and Ruth Greenspan Bell, Who Changed Delhi’s Air? The Roles of the Court and the Executive in Environmental Policymaking, Resources for the Future Discussion Paper 05-48 (December 2005) http://www.rff.org/rff/documents/rff-dp-05-48.pdf ("[T]he main role of the Supreme Court was to force the government to implement previously announced policies. … [T]he Delhi experience for instituting change has become a model for other Indian cities as well as neighboring countries.")
- V. Ramanathan & G. Carmichael, supra note 4, at 226.
- V. Ramanathan & G. Carmichael, id.
- Hockaday WC; Grannas AM; Kim S,; Hatcher PG (2006). "Direct molecular evidence for the degradation and mobility of black carbon in soils from ultrahigh-resolution mass spectral analysis of dissolved organic matter from a fire-impacted forest". Organic Chemistry soil 37 (4): 501–510. doi:10.1016/j.orggeochem.2005.11.003.
- O. Boucher and M.S. Reddy, Climate trade-off between black carbon and carbon dioxide emissions, 36 ENERGY POLICY 193, 196-198 (2007) (Particulate traps on diesel engines reduce black carbon emissions and associated climate forcing but are partially offset by an increase in fuel consumption and CO2 emissions. Where the fuel penalty is 2-3%, black carbon reductions will produce positive benefits for the climate for the first 28-68 years, assuming reduction in black carbon emission is 0.150.30 g/mile, CO2 emissions are 15002000 g/mile, and a 100-year GWP of 680 is used for black carbon. The net positive benefits for climate will continue for up to centuries in northern regions because of black carbon's effect on snow and ice albedo).
- "Jump-Starting Climate Protection: INECE Targets Compliance with Laws Controlling Black Carbon" analysis by International Network for Environmental Compliance and Enforcement, June 12, 2008, accessed April 22, 2011
- Stone, R. S., Sharma, S., Herber, A., Eleftheriadis, K., & Nelson, D. W. (2014) A characterization of Arctic aerosols on the basis of aerosol optical depth and black carbon measurements. Elementa. Retrieved 24 November 2014. doi:10.12952/journal.elementa.000027
- Integrated Assessment of Black Carbon and Tropospheric Ozone, 2012, United Nations Environmental Programme.
- Why Black Carbon and Ozone Also Matter, in September/October 2009 Foreign Affairs with Veerabhadran Ramanathan and Jessica Seddon Wallack.
- The Climate Threat We Can Beat, in May/June 2012 Foreign Affairs with David G. Victor, Charles F. Kennel, Veerabhadran Ramanathan
- UCSD Researchers: Where International Climate Policy Has Failed, Grassroots Efforts Can Succeed; Control of greenhouse agents other than CO2 needs to reach the local level, according to a new Foreign Affairs essay April 26, 2012 University of California, San Diego