Evaluation
The AAQM provides a full list of categories by which airport emissions are grouped, each representing a specific operational scenario as well as a number of subcategories. The categories are: 1a) aircraft main engine; 1b) Auxiliary Power Unit (APU); 2a) Ground Support Equipment (GSE); 2b) Airside air traffic of vehicles such as cargo loaders; 2c) Aircraft refueling, in the form of evaporation through fuel tanks/vents, trucks, and pipeline systems; 2d) De-icing and anti-icing substances during the winter season, in particular during snowstorms; 3a) Sources related to the main airport infrastructures, such as cooling and heating plants; 3b) Emergency power generators, such as those ensuring that runway lights can operate even in the case of power shortages; 3c) Activities and facilities related to the maintenance of aircraft, such as engine test beds, and washing; 3d) Activities focused on the maintenance of airport facilities and equipment; 3e) The storage, handling and distribution of fuel; 3f) Construction activities connected to the development of an airport; 3g) Activities related to fire training with various types of fuel; 3h) Surface de-icing, this time applied to the infrastructure, with a focus on access roads; 4a) Vehicle traffic linked to the airport as a whole, accounting for curbsides, drive-ups, parking lots, etc. Though it is believed by the author that any estimate on these emission categories is grossly challenged by uncertainties, this paper will address the issues related to specific disciplines and their fields.
In the simplest scenario, a given airport has one runway (intended as an actual linear infrastructure) which in turn has two bearings, identified by QFU (Magnetic bearing of the runway in use). The bearing identifies the orientation of the runway, RWY from now on, with respect to the magnetic north pole, divided by a factor of 10 (e.g., 30 for 300 °N); the two headings have a 180° difference from each other. Other, more articulated scenarios with parallel runways having the same orientation would introduce the identifiers L and R (Left and Right, respectively) to differentiate them, but these examples are now ignored for the sake of conciseness. Airport runways are not built at random, as they are the result of studies on local wind circulation meant to ensure the safety of air traffic on the principle by which both take-offs and landings need to be performed against the wind: this leads to a very important assumption by which the local influence of emissions is distinct from contributions to the global output. In fact, local emissions (intended as those affecting the airport workforce and nearby suburbs) should take in consideration wind speed and direction, while 100% of the emission output does however add up to total atmospheric pollution levels. Moreso, this should at least indicate that emission outputs related to take-off and landing maneuvers are concentrated on an axis that is coincident with the runway in use, plus a buffer zone accounting for high pollutant concentration levels, which would then be reduced as the distance from the axis increases: it doesn’t seem the case, however, of the main state of the art on the literature of the field, as classifications are performed on a per radius basis that – for example – attributes the label of “near-airport” range category to everything located in a 10-kilometer radius from the airport itself, a range deemed of particular attention in terms of health hazards, as reported by both Carslaw et al. (2006)5 and Carslaw & Beevers (2013)6. In fact, many annual deaths caused by a number of diseases linked to air pollution are attributable to people either living or spending working hours within this radius.
The point is that wind circulation, broadly characterized by the key parameters of wind speed (WS) and wind direction (WD), does influence the transport of pollutants on local to large scales. Models such as NOAA’s (National Oceanic and Atmospheric Administration) HYSPLIT7 (Hybrid Single-Particle Lagrangian Integrated Trajectory) allow to backtrack – or even make short-term future predictions – based on these wind parameters and are frequently used to monitor the distribution of pollutants that follow major events, such as large wildfires. The introduction of WS and WD (plus their intrinsic variability over time, linked to synoptic atmospheric circulation), even if fully integrated with air traffic below 915m/3000ft, does pose new challenges in the correct estimation of local pollutants caused by aircraft: one rather uncommon exception, though worth a mention due to its implications, is the Circle-To-Land procedure by which an aircraft would approach a given airport for landing, then perform a short turn (normally a left turn, according to the Rules of the Air), reach the other side of the aerodrome and land on the opposite RWY. Such a landing pattern completely invalidates any local scale pollution distribution model, as the sources of emission throughout the entire maneuver (hereby intended as points in space, the engine exhausts) follow a completely different path, and at different altitudes/orientations, each with different WS/WD parameters (especially the former, which is notoriously dependent on altitude). Moreso, at the time of writing there’s no tangible evidence that such landing procedures are tracked and a recorded in a nation-wide or international database, open to researchers and their institutions, up to a point that could be used to provide reasonable pollution estimates on a local scale. Even the emission estimate on an absolute scale, in this case, is challenged by different flight times (a Circle-To-Land maneuver and a standard landing are likely to be performed with different timing and fuel consumption settings). As said before, the Circle-To-Land scenario may be regarded as a rare circumstance, but it’s worth noting that training procedures performed by military airplanes of various air forces operating at commercial airports follow a similar pattern several times in a row during each training session and the exercises themselves frequently involve large airplanes with remarkable emission outputs. These odds may be considered an example of “Missing information” as intended by the AAQM: inventories not fully integrated with air traffic control, local civil aviation authority records and precise meteorological stations would systematically fail to account for these non-standard maneuvers.
In addition to the challenges posed by local pollution and emission estimates, even the accounting of released compounds itself is challenged by intrinsic degrees of uncertainties: at the time of writing, in fact, there are no comprehensive and detailed data on specific methane releases by aircraft that could be used to provide adequate assessments. Methane (CH4), though not a pollutant per se, is a potent GHG (greenhouse gas) due to its global warming potential (GWP) exceeding that of CO2 by nearly two orders of magnitude over the time period of two decades and is nearly 30 times higher over the course of a century8; despite this, methane levels in the atmosphere are about 200 times lower than those of CO2, thus making carbon dioxide the biggest threat to climate (this compound also tends to persist in the atmosphere for longer periods of time, potentially one millennium, so that’s why it’s currently the focus of social, political and economic debates). Unlike carbon dioxide however, methane has showed degrees of variability (both in terms of global growth rates and carbon isotope fractionation, the latter being a characteristic that will be described later on in this section) which have a now confirmed influence on social sciences such as Sociology and Psychology, as evidenced by an earlier study9 analyzing the side-effects of a complex compound when it comes to climate change communication and its numerous implications for present day society.
Prior to the analysis of engine emissions, in this context is deemed relevant to make a number of references to the Covid-19 pandemic and the consequent collapse of commercial aviation that followed, in particular with respect to the complexity of atmospheric chemistry it allowed to highlight. Globally, the disruption of aircraft operations resulted in notable atmospheric NOx reductions which are well documented, and totally compromised long term predictions on worldwide air traffic growth, such as the environmental trends to 2050 by Fleming & de Lepinay (2019)10 issued just one year prior to the pandemic. It’s worth noting that research on the effects of aviation on climate change showed spatial variations depending on where operations occur, so the net effects may change locally; several uncertainties in estimations have been highlighted too11. Air traffic reductions related to the Covid-19 outbreak are perhaps the most documented reduction of human activities during that period, as others would be subject to gross uncertainties; therefore, airports may be considered a good environmental indicator for the major lockdowns that took place all over the world. Recent models created by Lee et al. (2021)12 reported baseline values for methane radiative forcing sensitivity to aviation NOx emissions, a result that was converted by Stevenson et al. (2022)13 to a sensitivity of methane to a pulse change in aviation NOx emissions of 1.12 ppb (parts per billion) (CH4)/Tg(NO2)yr−1. These estimates indicate a tangible influence of NOx emissions dropping to CH4 levels, in accordance with past research from over a decade before. The broad effects of NOx are such that recent research proposed a reduction of these emissions as more favorable compared to a slight increase in CO2 emissions, a result that is hereby showed to demonstrate how the driving mechanisms of climate change and atmospheric pollution oftentimes rely on an intricate set of interactions between compounds, and the release (or increase) of certain emissions should not be regarded as an independent parameter. The climate altering balance tradeoff proposed by this research could eventually spark new advances in the development of sustainable fuels.
Speaking of methane, aircraft engines are confirmed to release certain quantities of this compound during idle, taxi, take-off, approach, and cruise phases, and its role in climate change is considerable, as remarked by Lee et al. (2009)14 and other research teams. In general, with all released compounds considered, the climate change potential of aircraft is also related to side effects such as contrails, as reported by Burkhardt et al. (2010)15 and others. Research on such impact has been performed in areas where domestic traffic is very heavy, such as the United States of America. Research on the local impact of air traffic on the environment is generally focused on LTO cycles, in accordance with the AAQM, while research on broader effects of air traffic also considers cruise phases16. In Europe, the currently available databases issued by regulators such as EASA17 on air transportation safety and environmental impact use “HC” as a generic parameter for released hydrocarbons that includes, but is not limited to, methane. The parameters used by EASA provide information on the grams (g) of HC released per kilogram (kg) of fuel during different phases based on an Emission Index (EI), and they do so on a per-engine basis; for instance, a HC EI Idle (g/kg) of 4.6 for the CFM56-5B7/P engine, which is now out of production, indicates an emission of 4.6 grams of hydrocarbons per kilogram of fuel consumed when the engine is set to idle, a condition typical of the engine startup sequence, which normally lasts several minutes and precedes the taxi procedure, as well as holdings on ground due to nearby aircraft movements. Directives on airport air quality do specify “NMHC” (Non-methane Hydrocarbons) as released pollutants, but they’re not quantified in EASA reports on engine outputs, thus making methane impossible to factor out by subtracting NHMC from HC data.
That said, before addressing into the detail the odds of several emission estimate uncertainties with respect to engine outputs, it’s worth explaining what the main AAQM (and, consequently, ICAO) directives on engine emissions are based on in terms of computations. As per the referenced document, these emissions depend on three key parameters, which are Time-In-Mode (TIM), the Emission Index (EI) already mentioned before, and fuel flow through the main engine. Extra parameters include fleet sizes and types, as well as the number of operated aircraft movements, which both propagate the low-end values to higher scales, depending on traffic intensity. TIM is essentially the time period in minutes that satisfies the specific conditions by which the engines are operating at a given setting. The EI, as stated before, provides a value representing the mass of pollutant that is released per unit mass of fuel burned, classified by compound or category of compounds (NOx, CO, and HC – note again how hydrocarbons are grouped into one category). A multiplication between the mode-specific EI and TIM-specific fuel flow results into the estimation of units of grams of pollutant per LTO. Consequently, modal emissions for a given aircraft plus engine combination are equal to TIM multiplicated by the amount of fuel used at a given power level, which is then multiplied by the EI (also at the related level), and the number of engines on the aircraft, which is generally equal to two. Inventories based on these methodology approaches are grouped by levels of detail and range from “simple” to “sophisticated”, with “advanced” being the intermediate tier. “Hybrid” models combining characteristics of more than one approach exist, though the AAQM warns on a caveat when it comes to relying on such models.
Speaking of the accuracy of these estimates, a precise calculation of HC values emitted by aircraft movements and related activities would be nearly impossible to achieve: HC values are engine, not aircraft specific, and even in the context of the same commercial operator, aircraft of the same type such as the Airbus A320 may have different engines mounted on them, so the analysis may have to be performed on a per-airplane basis, and precise registrations or tail numbers of aircraft are no longer available in the records after a given amount of time, which is normally two years. Even if they were available, these estimations would not take into account the emissions caused by ground equipment and vehicles which rely on regular fuel whose combustion does release quantities of methane (e.g., Ground Power Unit or GPU, Air Starter Unit or ASU, Air Conditioning Unit or ACU), which themselves are various in nature depending on the aircraft’s technical conditions during transit (e.g., a faulty Auxiliary Power Unit or APU would require the GPU and ASU be employed), airline, cargo loads (e.g., cargo on commercial aircraft requires extra personnel and equipment for unloading/loading), aircraft type (e.g., turboprop planes like the Bombardier Dash Q-400 require the GPU be connected during the first phase of engine start), PRM figures (Passengers with Reduced Mobility who require ad hoc equipment and vehicles for disembarkation and boarding), logistics and infrastructure (e.g., remote stands require personnel and passengers be transferred via ground vehicles, instead of walking) and so on. As per the AAQM, these would all qualify as “Missing information” on local emissions: the absence of a precise log on these activities, as well as their integration with meteorological data, would lead to these emissions being ignored by inventories.
In purely operational terms, records do not provide precise information on the duration of engine running periods on ground, as on-block and off-block times may diverge from them depending on airline-specific operating procedures, technical issues, and operational ACARS (Aircraft Communication Addressing and Reporting System) devices. In this study, it is concluded that a precise estimation of emissions from aircraft, ground equipment and vehicles is not possible.
A case could be made that the integration of airports with advanced air quality and emission monitoring instruments, placed at key locations to cover most of the traffic or at least the most notable influence of local traffic, could at least overcome the reported uncertainties via quantitative data. Such monitoring efforts could indeed provide relevant information should certain thresholds be crossed for hours, but even in this case the uncertainties would be gross: unless the airport is built far away from its respective city, pollution levels would be affected by nearby industrial and urban activities, and even in the case of airports located far from urban/industrial areas, any spike detected at a given moment may not be necessarily connected to air traffic (wildfire and landfill emissions result into notable peaks, just to report two examples)18. A possible solution would be an integrated monitoring system accounting for carbon isotopes, relying on the VPDB standard (Vienna Pee Dee Belemnite19, the shell of a Late Cretaceous belemnite cephalopod) to detect deviations from the 0‰ (per mille) value of both CH4 and CO2, the so defined δCH4 and δCO2 (delta C) parameters. However, not only are these instruments very expensive to implement – even the main atmospheric monitoring stations lack a total coverage of carbon isotope data on the atmosphere, so the extension of said network to airports would be a challenge under several points of view – but any detection at an airport would have to be reanalyzed and validated in order to consider observed δCO2 and δCH4 values attributable to natural processes, as well as anthropic processes distinct from aircraft emissions. A possible solution would be the integration of 14C (carbon-14) measurements as an indicator of fossil versus present-day sources:20 due to its radiogenic nature, 14C tends to decay over the course of thousands of years, up to the point where it becomes nearly impossible to detect (this normally occurs after the equivalent of ten half-times, which are equivalent to approximately 57300 years – modern technology fails at detecting 14C past this threshold). Fossil fuels, which are much older than that (their age is in the range of several dozen millions of years, at times hundreds of millions of years) are depleted in 14C; with adequate analysis, it’s therefore possible to distinguish CO2 peaks derived, for instance, from a wildfire affecting modern plants from the CO2 released by aviation emissions, which relies on fuel totally depleted in 14C. A continuous, integrated analysis accounting for all three main carbon isotope compounds would provide strategic details, except it’s not impossible to implement with present-day technologies: standard δCO2 measurements are still in their implementation phase throughout international networks of atmospheric monitoring, and 14C evaluations require samples be collected and sent to laboratories for precise analyses, thus making a coordinated and instantaneous integration between the two methods all but impossible at this point. In addition to that, the AAQM does not include any mention of carbon isotopes as tools to differentiate emission sources around airports as guidelines for air quality indicators, and the broader academic research is lacking with respect to that, so standards and guidelines may have to be developed first. At the time of writing, in fact, not a single comprehensive study on a notable-scale employment of such standards with respect to ground-level aviation emissions has been reported.
If these extra technologies were to be implemented one day, depending on operating costs, human resources and instrument availability, they could mitigate “Error estimations” as intended by the AAQM when it comes to emission inventories. According to the document, these errors are divided into the subcategories of Measured, Calculated, and Estimated: the efficient integration of advanced atmospheric analyses, combined with meteorological and ATC data, could not only mitigate errors affecting inventories but could also provide insights and tools meant to improve the inventories themselves. For instance, in one hypothetical scenario by which the local CO2 inventory levels at a given airport operating under regular conditions are systematically underestimated by ≈150ppm compared to observed values, research efforts could then be redirected to the estimation vs. observation anomaly and perhaps pinpoint the gap or error leading to that difference. That, in turn, could be used to upgrade the algorithm not only on a local scale, but also globally should the air traffic and environmental settings at that airport be somewhat relatable to other conditions elsewhere.
Restrictions on the accuracy of atmospheric measurements at airports may be overcome by the actual need behind the measurements themselves. In fact, it is recognized that continuous (or sporadic) measurements could be the result of a legal requirement at various levels, asking for an assessment of atmospheric pollution in a given area (this principle is applicable to various contexts other than airports – see core industrial areas, for example). Other reasons leading to more accurate measurements could have “voluntary” baselines as the driving factor behind them, in the form of airport authorities willing to perform more detailed analyses, or public concern over pollution levels in a given area (again, this may be applicable to a number of scenarios unrelated to aviation) that result into the central government funding these measurements. In an ideal scenario, these measurements would be performed globally, with standardized procedures, and their accuracy/frequency could be adjusted depending on the intensity of local air traffic (e.g., busy airports may have to be monitored at a higher rate), as well as precise local meteorological conditions (e.g., weak local circulation may lead to the accumulation of pollutants and, consequently, the need for continuous or more frequent evaluations), as well as the overall urban setting (e.g., distance to, and population density of, urban centers). In addition to these procedures, which need to be discussed on a global scale, regulating factors such as the maximum amount of data gaps (e.g., caused by lack of reports or unrepaired instruments) allowed before a sanction takes place, as well as precise legal requirements on the accuracy of reported data, need to be implemented. An integrated and well-regulated international network would then be beneficial for all authorities and countries involved, especially in terms of source apportionment (SA), a key tool by which emission sources can be detected. Right now, SA seems poorly developed in the context of atmospheric measurements at airports, for the reasons stated above.
Despite the gaps in source apportionment (SA) methodology, the AAQM however acknowledges the complexity of monitoring aviation-related emissions in geographic contexts where other emission sources are present: it is recognized, in fact, that the airport inventory – intended, by the AAQM, as a local scale source emission estimate – might constitute a “small percentage to the overall area emissions inventory”. The same document also reports that railway systems and trains, though considered part of local emission sources due to their infrastructural relevance (sometimes, train stations are perfectly integrated into airports, so the two sources coexist and each one of them has a direct influence on the other), are not covered by the document itself. This, combined with the odds of precise carbon compound analysis in atmosphere mentioned before, significantly contributes to the degrees of uncertainty that form up the core of this research paper.