Cities account for more than 70% of global total greenhouse gas (GHG) emissions. Quantifying GHG emissions from cities, which are often the smallest administrative unit, is thus a key challenge towards effective emissions management. Emission inventories (EI) are a fundamental tool to keep track of emission changes (e.g., national emission inventory (NEI)). However, most cities do not even compile EIs although they have been recognized as practical emission reduction target, even when motivated by international consortiums (e.g., C40 cities climate leadership group). Moreover, EIs are prone to systematic biases from both the emission calculation methodology and the inadequate quality of the underlying activity data (e.g., Guan et al., 2012; Liu et al., 2015). In the absence of a transparent protocol to provide reliable activity data and a robust calibration method, EIs remain uncertain, therefore limited in their ability to measure GHG emission reduction efforts in metropolitan areas (Hutyra et al., 2014). At the country scale (e.g., Kyoto Protocol), EIs aim to determine the level of contribution of various sectors to national carbon budgets thereby supporting the implementation of carbon mitigation for which accurate quantification of emissions is of major importance. The authors believe it is important for the science community to contribute to establishing a framework prefacing the implementation of a complete Monitoring/Reporting/Verification (MRV) practice for cities, guiding stakeholders and emission management policies.
Cities’ roles for emission management and emission reduction potential have been identified. However, only few megacities are compiling their EI with the required granularity. Especially, quantification of emissions from cities is preferably done by developing fine-grained bottom-up EI where emission accounting and geolocating are available at the same spatial scale, as done by Gurney et al. (2012) as opposed to most gridded datasets based on disaggregation of national/sectoral emissions (e.g., Andres et al., 1996; Olivier et al., 2005; Janssens-Maenhout et al., 2012; Rayner et al., 2010; Oda and Maksyutov, 2011; Kurokawa et al., 2013; Asefi-Najafabady et al., 2014). The links between human activities and emissions described in a bottom-up framework provide more information on energy use than top-down estimates, which are limited by the ambiguity of mixed source signals in atmospheric observations. However, the development of fine scale EI is often labor intensive and difficult to be completed in a timely manner (i.e., annual basis). In fact, such fine-grained city emission datasets are only available for few locations. Over the continental US, only few EI’s have been compiled at the building-level resolution: Indianapolis (Gurney et al., 2012), Los Angeles (Feng et al., 2016), Baltimore (Gurney et al., in preparation) and Salt Lake City (Patarasuk et al., 2016). Furthermore, error quantification and characterization associated with EI’s is another emerging issue (e.g., Andres et al., 2016). Especially for fine-grained EI’s, uncertainty assessment is non-trivial and involves complex parametric and structural uncertainties (Gurney et al., same issue). Those information should be included in city scale inversion to obtain robust city emission estimates (Lauvaux et al., 2016).
Beyond their original use for city emission accounting, EI is also a key component in top-down methods as they provide a first guess in the optimization problem to help identify the source distribution (Enting, 1995). The use of atmospheric data to verify EI’s has been encouraged by several studies (e.g., Nisbet and Weiss, 2010; Pacala et al., 2010) and supported by the analysis of various types of instrumentation (e.g., Kort et al., 2012, Janardanan et al., 2016 for satellite CO2 data; Basu et al., 2016 for C14 radiocarbon data). Recently, an inversion analysis from the Indianapolis Flux experiment (INFLUX) project, as the first of its kind, has achieved a top-down emission estimate for a single city and demonstrated the use of atmospheric CO2 tower data to constrain urban emissions (Lauvaux et al., 2016). The inversion system used the “Hestia” fine-grained emission dataset (Gurney et al., 2012, data available from http://hestia.project.asu.edu/) as a priori emission and derived emission corrections using atmospheric CO2 data from the dense tower network within the city domain. The inverse methodology produced 1-km resolution adjustments to the first guess (Hestia) modifying the total emissions by about 20%, a statistically significant change reflecting possible discrepancies between the two methods including the presence of additional sources beyond anthropogenic emitters (e.g., soil respiration – Gurney et al., 2016). The study also illustrated the impact of assimilating coarser resolution prior emissions taken from the Open-source Data Inventory for Anthropogenic CO2 (ODIAC) global 1 × 1 km fossil fuel emissions dataset (Oda and Maksyutov, 2011; Oda et al., 2016, data available from http://db.cger.nies.go.jp/dataset/ODIAC/) and its impact on the spatial structures of the emission corrections.
Potentially being applicable to any cities, top down approaches are currently being tested across few metropolitan areas (e.g., Feng et al., 2016), mostly due to the lack of atmospheric GHG networks to constrain city emissions. The deployment of ground-based instruments require an existing infrastructure (i.e. accessible tall towers or high buildings) and expert knowledge to calibrate the instruments (Richardson et al., 2017). Other observing strategies such as future satellite missions (e.g., Orbiting Carbon Observatory-3 – Eldering, 2015; CarbonSAT – Buchwitz et al., 2013; GeoCARB – Polonsky et al., 2014) are currently under development and could provide the required constraint on urban emissions in the near future. In this study, we present the space-based emission field at fine resolution to inform a top-down urban-scale framework. We evaluate the product against an existing fine-grained EI, Hestia, and assess the impact of the fine-scale structures on the posterior emissions estimate. The original ODIAC emissions is a global data set based on disaggregation of national emissions using point source profiles (power plant emission estimates and geolocation) and satellite-observed nighttime lights (e.g., Oda and Maksyutov, 2011). The total emission for the Indianapolis domain taken from ODIAC for a priori was remarkably close to Hestia as shown by Lauvaux et al. (2016), meaning the national emission disaggregation in ODIAC was sufficient for an annual estimate of the whole-city emissions. We present here an improved product at a higher level of granularity with the ambition of achieving the required accuracy in emissions estimates, i.e. sufficient to inform city-scale mitigation policies (i.e. less than 10% annually). However, the emission disaggregation technique using proxy geospatial data, while applicable to the large scale, is limited by the spatial heterogeneity of sources at finer scales. Therefore, proxy data-based emission disaggregation approaches would not work at higher resolutions, especially at the city level when light intensity and population are decorrelated from large emitters. We thus focus on creating better emission spatial structures by determining locations of specific aggregated emission sectors and attempt to make the method applicable to other metropolitan areas.
We created a fine-grained emission field from the ODIAC emissions used in Lauvaux et al. (2016). Following the emission disaggregation commonly done in global and region gridded EI studies (e.g. Streets et al., 2003; Janssens-Maenhout et al., 2012; Kuenen et al., 2014), city emission fields can be approximated by three principal emission type components: point, line and diffused (area) emission sources. Table 1 shows the sector emission breakdown for Hestia. Values are updated from Gurney et al. (2012). It is often fairly straightforward to categorize emissions into few major sectors. For Indianapolis, and likely for many other cities over North America, emissions from transportation can account for a major fraction of the city total (about half – or 49% – for Indianapolis). In the original ODIAC emissions, power plant emissions, which are often the major emitting sector at the national scale, are already distributed using geolocation of power plants taken from CARMA (www.carma.org) (Oda and Maksyutov, 2011; Oda et al., 2017). The transportation sector emissions are distributed as a diffused source. Thus, we preserved the power plant emission information from the ODIAC dataset and disaggregated the non-point source emissions (total minus point source emissions) using geospatial datasets. We used both the global road network data and satellite-data driven surface imperviousness data at 30 × 30 m resolution to generate a final product at a spatial scale similar to Hestia. We distributed the residual (non-point emissions) using the Global Roads Open Access Data Set (gROADS) v1 developed by the SocioEconomic Data and Applications Center (SEDAC) (CIESIN/ITOS/University of Georgia, 2013, http://sedac.ciesin.columbia.edu/data/set/groads-global-roads-open-access-v1) for transportation sector emissions (i.e. line source emissions) and used the satellite-data driven 30 m surface imperviousness data (National Land Cover Dataset (NLCD) 2011 http://www.mrlc.gov/nlcd2011.php) for diffused source emissions (i.e. area source emissions). ODIAC does not distinguish emissions from the different sectors as emission estimates are based on country scale fuel consumption statistics (Oda et al., 2017). In this study, we calculated the fraction of transportation emissions using Hestia (see Table 1). The sectoral emission approach is applicable to any city assuming that sectoral total estimates are available. If not, an average of sectoral contributions from other cities across the country should provide a fairly similar distribution. The impervious surface used here indicate four levels of development (high, medium, low and open space, see Figure 1), but the four categories are aggregated to one as the surface imperviousness does not directly inform CO2 emission sectors (e.g. industrial, residential and commercial), but potential locations for area sources. We thus used population data taken from Census (www.census.gov for the year 2011) to create spatial gradient on sector emission areas indicated by gROAD data and impervious data. The use of population is a classic proxy for human emissions (e.g., Andres et al., 1996) even applied for transportation emission (e.g., Olivier et al., 2002) as population and traffic density are highly correlated. The use of population data is therefore a reasonable approach as a first order approximation. We found a difference of 0.3% in total emissions when projecting our 1 × 1 km ODIAC into the impervious surface data fields (30 m resolution). We corrected the iODIAC emissions of the difference by adjusting the entire field.
|Hestial emission sector||Type||Emissions
The flux inversion analyses in this study were done using the urban high-resolution atmospheric CO2 inversion system developed by Lauvaux et al. (2016). The urban inversion system is built around the Weather Research Forecasting model coupled with Chemistry (WRF-Chem) modified for passive tracers described as Lauvaux et al. (2012). The version of WRF model used in Lauvaux et al. (2016) has Four Dimensional Data Assimilation (FDDA) capability and the World Meteorological Organization (WMO) observations were assimilated in order to simulate atmospheric CO2 concentration with the best accurate meteorological conditions (Deng et al., 2017). Lauvaux et al. (2016) used three WRF model grid configurations in nested mode (9km, 3km and 1km, see Figure 1 of Lauvaux et al., 2016). This study focuses on the Indianapolis metropolitan area that is defined by 87 × 87 grid points at 1 km resolution. The urban inversion system employs the Lagrangian Particle Dispersion Model (LPDM) described by Uliasz (1994) as an adjoint model for the WRF-Chem model. Lagrangian particles are released from CO2 observation locations and transported backward in time to yield the contributions from surface fluxes and boundary contributions. As in Lauvaux et al. (2016), we used CO2 data from nine towers of the INFLUX network, all of them operational over the period September 2012 to April 2013 (Miles et al., 2017). The system assimilates CO2 data and solves for 5-day corrections to surface anthropogenic emissions over the dormant season during which the biospheric contribution is small (about 5% of the total CO2 emissions, reported by Turnbull et al., 2015). Additional modeling details are available in Lauvaux et al. (2016).
We will evaluate the different prior emissions by computing the final mismatch in CO2 mixing ratios referred here as goodness-of-fit after inversion, both over the whole city and for each individual tower site. Because prior error covariances are also constructed according to the prior emissions, the goodness-of-fit depends on the distribution of sources across the inversion domain and their associated errors. The error variances will be a function of the emissions for each pixel whereas the error covariances will correspond to an exponentially decaying function assuming a correlation length scale of 4 km between urban pixels (similar to Lauvaux et al., 2016). We note here that inverse emissions depend on the a priori but the relative performances will reflect the consistency between atmospheric data and the different prior emission products. Therefore, higher correlations between the posterior mixing ratios and the observations are evidences of a better agreement between the prior emissions and the true fluxes.
Figure 1 shows the impervious surface data over Indianapolis. We extracted three categories that indicate the level of development (high, medium and low) and a category for open space. According to NCDC categorization (http://www.mrlc.gov/nlcd06_leg.php), high density indicates 80–100% imperviousness, medium indicates 50–79%, low indicates 20–49% and open space indicates less than 20%. Although a single category is unlikely to correspond to one particular emissions sector, the city structures are clearly depicted with developed areas and open spaces, the major road transport network (e.g., beltway and interstate highways) and blocky patterns in residential areas. Compared to the spatial structures of ODIAC (see Figure 2a), the use of impervious data significantly reduces the mapping error by distributing the emissions over well-identified urban areas rather than smoothed zones overlapping with non-emitting areas. The impervious data might be able to identify particular emission sectors, but no clear relationship between the imperviousness categories and emission sectors can be established. In this study, we aggregated the four imperviousness categories and used them with population density maps as a proxy for diffused emissions.
The 30 × 30 m improved emission field (iODIAC) and the other fields are shown in Figure 2. The emission gradients over the areas depicted by the impervious surface data were driven by population. Thanks to the use of 1 × 1 km gridded population data, the blocky features are visible across the area (see Figure 2b). As expected, the emission mapping error is significantly reduced in iODIAC field compared to ODIAC, with iODIAC field being more closely related to Hestia, although emission gradients are modeled rather than being determined by sectoral information. We present a quantitative assessment of the iODIAC emissions in the following section by performing inversions over the city and by computing statistical metrics to evaluate the improved representation of urban CO2 emissions.
Table 2 shows the summary of the 8-month inverse estimates over Indianapolis. Assuming Hestia is the best estimate of Indianapolis CO2 emissions, the nightlight-based disaggregation emissions from ODIAC (only for non-point sources) are performing reasonably well for a middle-size city like Indianapolis. When the inversion was performed using the 30 × 30 m improved emission field (iODIAC) as a priori, the inverse estimate differed by only 0.4 Mt/yr over 8 months (about 8% of the total emissions) compared to the Hestia-based inversion. The inversion result with ODIAC was slightly closer to the Hestia inversion result by 0.2 MtC/yr, within the uncertainty range of 0.6 MtC/yr. The spatial structure of the prior emissions has an indirect impact on the inverse emissions. Because the error variances are scaled with prior emissions, specific areas or points may be more or less susceptible to adjustments. Therefore, the differences in the total emissions will depend on the presence of sources near the observation locations which defines the degree of freedom of the prior emissions (i.e. error variances of the prior emissions). Overall, the sharp spatial emission gradients in iODIAC affected the whole-city inverse emissions producing a lower estimate over the entire period (lower by 0.17 MtC/yr). Assuming that iODIAC emissions represent the urban area more accurately than ODIAC, this result shows the sensitivity of the top-down estimate to the fine-scale structure as described by the prior emissions.
|iODIAC –this study
Figure 3 shows the prior and posterior emission fields for the three inversion cases, i.e. invHestia, invODIAC and inviODIAC emissions. Although the total inviODIAC emission estimate differs from invHestia, the two inverse emission distributions shared major spatial patterns especially with high emissions. The correlation with Hestia was increased from 46% to 52% and the Mean absolute Error (MAE) was reduced by 14% compared to invODIAC. Both statistics are significant considering that the increased resolution of iODIAC artificially decreases the correlation (i.e. increases the MAE) due to misplacements of larger gradients in iODIAC. Smoother structures in ODIAC tend to have better correlations, attributable to smaller spatial gradients. We also note here that the power plant emissions were removed to avoid artificially high correlation values (the three maps share identical power plant information). Figure 3 illustrates the high resemblance between Hestia and iODIAC (upper row, left and right panels) compared to the smoothed pattern of emissions in ODIAC (upper row, middle panel). The inversion shows more diffuse emission corrections when using ODIAC (lower row, middle panel), while emission adjustments are guided by the spatial patterns in the iODIAC prior field and the error variances constructed accordingly (lower row, right panel).
In Figure 4, the temporal variations in the posterior emissions are shown. As shown in previous inversion cases by Lauvaux et al. (2016), atmospheric data constrain the temporal variability while prior emissions have no significant impact on the inverse 5-day variations. The inverse results confirm that while spatial information remains a limiting factor despite the large number of towers over the city, temporal variations in the emissions being primarily constrained by observations rather than a priori information. Therefore, the lack of diurnal and sub-monthly variability in iODIAC is overcome by the observational constraint. This result is discussed further in Section 4.3 with potential implications for the development of future high resolution EI’s.
We calculated the model-observation mismatch for the three inversion cases as a measure of the goodness-of-fit before and after inversion. Because the prior errors are fairly similar over the whole city, this result illustrates the capability of the inversion to fit the observed mole fractions and therefore the quality of the prior. If the prior structures are inconsistent with the gradients in the atmospheric observations, the goodness-of-fit will not improve after the inversion. Table 3 summarizes the values calculated from all the atmospheric measurements used in the inversion. We found that both iODIAC and inviODIAC showed smaller model-observation mismatch compared to ODIAC and invODIAC emissions (–0.382 ppm vs. –0.487 ppm after inversion, and –0.819 ppm vs. –1.05 ppm before inversion), with iODIAC being further away than the Hestia case. This result confirms that iODIAC emission distribution is closer to that of Hestia, allowing the inversion to improve the fit to the atmospheric observations, which indirectly confirms a better distribution of the posterior emissions. The authors would like to highlight that, unlike the Hestia case, weekly to diurnal temporal patterns were not applied to neither ODIAC nor iODIAC.
|iODIAC – this study
We further looked at model-observation mismatch for each tower assimilated in the inversion. Figure 5 shows the model-observation mismatch on a per-tower basis. In this analysis, only the posterior fit was used. The fit of Hestia emissions are available in Miles et al. (same issue). Here we only consider the fit to the posterior emissions. This analysis revealed that the posterior model-observation goodness-of-fit are similar or even better with inviODIAC compared to invHestia emissions for most of the sites, except for sites #04 and #12 which are located on the south side of the city. For the site within the beltway (site #02, 03, 05, 07, and 10) where the emissions are most intense, the iODIAC case outperformed the other two cases. For site #04, the model-observation fit is similar for the three cases, indicating a missing adjustment in all cases. For site #12, the invODIAC and inviODIAC model-observation differences are much larger than for the Hestia case.
Given the use of generic geospatial data that are available globally, our downscaling approach is applicable to any city in a systematic and timely manner, although the accuracy of the disaggregation method could vary due to errors/biases from larger scale EIs and/or solely due to the potential regional errors/biases in emission disaggregation. The use of very high-resolution satellite-driven data such as impervious surface data for emission mapping can be computationally expensive. For similar studies over multiple cities, the collection of impervious data for urban emissions only represents a small fraction of the surface of the globe which decreases significantly the amount of data and processing of such application. As pointed out by Lauvaux et al. (2016), error quantification and characterization for city scale inversion is often extremely difficult to implement due to the lack of information and the computational expense when considering large volume of data in EI’s. Our approach could also provide a limited but meaningful opportunity to perform error quantification and characterization by providing alternative emission field to be compared. Thus, the authors believe that emission downscaling approach will help informing city emissions in a global framework for city top-down MRV, especially with future space-based carbon-observing missions. Here we discuss current limitations and future perspectives of this study in a context of city MRV implementation.
As pointed out earlier, the lack of EI reported by cities is a fundamental, limiting factor in city MRV. Although the authors believe that development of a fine-grained EI such as Hestia is an ideal way to accurately quantify city emissions and inform top down methods in a city MRV framework, emission accounting for cities via compilation of EIs needs to be more commonly available and following existing guidelines, such as the Global Protocol for Community-Scale Greenhouse Gas Emission Inventories (GPC, http://www.ghgprotocol.org/city-accounting). With sector-specific information, more accurate emission modeling can be implemented instead of making crude assumptions about sectoral contributions (e.g., applying national-level sectoral distributions or averaged city sectoral fractions to every city). Spatially defined EIs or geolocation information will also greatly support the introduction of the complexity and the diversity of anthropogenic sources in the resulting emission field at fine scale.
The quality of EI is often correlated with the goodness of statistical data collected from various institutions or directly from private organizations (e.g., Olivier and Peters, 2002; Marland, 2008; Andres et al., 2012). Most of the countries that are thought to be producing lower quality EIs are unlikely to be able to compile high-accuracy EIs at the city scale. Collecting accurate data at large scales for aggregated EIs (e.g., national and province levels) remains more practical than city-scale emissions. Therefore, the construction of fine-grained top down estimates to support city-scale EIs is an attractive solution to produce more accurate estimates in any country, and possibly offer a monitoring of the reported emissions, consistent with estimates from larger scales. As an example, Guan et al. (2012) reported a 1 Gt CO2 difference between estimates based on national and province level statistics in China.
Initially, the agreement between ODIAC and Hestia total emissions suggests that the downscaling approach can give us a reasonable estimate for whole-city emissions (within 10%). However, disaggregation (mapping) error can be more significant when moving to higher spatial resolutions. Especially at very high spatial resolution, source locations have to be determined rather than estimated or approximated using proxy data. As seen in the emission pattern, ODIAC provides maps of CO2 emissions over areas that are unlikely to be emitting (see Figure 2). Other than the resolution mismatch (1 km vs. 30 m), the underlying nightlight data used in ODIAC, provided by the Defense Meteorological Satellite Program (DMSP) Operational Linescan System (OLS) nightlight data (https://ngdc.noaa.gov/eog/dmsp.html), have known limitations (e.g., Elvidge et al., 2013). The authors are working on applying new nightlight environmental product developed from data collected by Visible Infrared Imaging Radiometer Suites (VIIRS) on Suomi National Polar-orbiting Partnership (NPP) satellite (Román and Stokes, 2015) to the ODIAC emission model (Oda et al., 2017). There are a number of improvements in VIIRS over the previous instrument which will mitigate the mapping error originating from the use of current nightlight data.
Although the satellite-driven data used in this study for downscaling (e.g., nightlights and impervious surface data) turned out to be useful for determining source regions within a city, nightlights intensity, or development density in impervious surface data, does not fully explain any emission spatial gradients within the emitting area. In this study, we used population data to model the spatial emission gradient. In future study, we will examine the impact of emission gradients on the posterior emission estimates constrained by other proxies, which could be a source of bias in the current inversion setup.
Given the absence of other EI estimates, the evaluation of biases in the emission field remains unachievable. However, geolocation information used to map the emissions can be addressed from various data sources. Although emissions estimates could be significantly biased for sources such as power plants and transportation, we could determine the precision of the geolocation at a minimum (e.g., locations of power stacks and road networks). This first step is critical for city-scale inversions because atmospheric data are unlikely to determine the locations of large sources within the city limits. The verification of intense sources is also limited to few proxies such as public information from Google Map/Earth. However, the limited numbers of large point sources remain manageable within each city compared to the national scale EIs (e.g., Oda and Maksyutov, 2011). This type of error/uncertainty has been discussed in other studies (e.g., Oda and Maksyutov, 2011; Woodard et al., 2014)
In this study, we focused on the impact of spatial emissions distributions on the inverse emissions without including any temporal variations in the a priori beyond monthly time scale (except Hestia). The seasonality in ODIAC is taken from estimates made by the Carbon Dioxide Information Analysis Center (CDIAC) at Oak Ridge National Laboratory (Oda et al., 2016). The CDIAC seasonality is based on national monthly fuel statistics, rather than subnational (e.g., state) monthly statistics. Thus, the actual subnational seasonality might be different. According to GPC inventory guidelines, future products may include an annual (i.e. 12 month) inventory. The development of monthly emissions would greatly improve the current level of information in EIs. Climatology may also be used for modeling purposes such as Nassar et al. (2010). The response to environmental conditions and human events (e.g., regular weekday/weekends vs. holidays) should be detectable and therefore quantifiable, if applied. Overall, the authors would like to highlight that the inversion with iODIAC was able to show a very good match with the atmospheric observations comparable to Hestia inversion case over an 8-month period. Future work will aim to assess the impact of temporal profiles in the emissions relative to the impact of finer spatial distributions.
The lack of the error quantification/characterization in the fine-grained emission dataset was discussed by Lauvaux et al. (2016). As mentioned earlier, many sources of uncertainties can affect the emissions and need to be carefully considered depending on the flux resolution (e.g., time and space) of interest. Most of the emission datasets are based on disaggregation of emissions (e.g., CDIAC, EDGAR) where proxy data are used at many different levels. The proxy data are used to approximate the spatial emissions and thus are usually not appropriate at urban scales where individual processes are identifiable. Emission intercomparison may not be highly meaningful but given the lack of physical measurements or EIs constructed at comparable spatial resolutions, model intercomparison remains valid. In the current inversions, the absence of definition for emissions errors is critical, impairing the ability of top down methods (Lauvaux et al., 2016). Given the relatively good performance of iODIAC and the presence of detailed spatial structures, the assessment of emissions errors is a critical objective for urban inversions to improve both the distribution and the total emissions of the city.
We present the first space-based emission field at fine resolution to inform a top-down urban-scale framework. Following the INFLUX inversion case with a global 1 × 1 km ODIAC fossil fuel CO2 emission dataset as a prior, we further improved the 1 × 1 km emission field from the global ODIAC dataset to describe higher levels of emission granularity at the city-scale such as roads and point sources, often missing in coarser resolution products. We approached city emission fields with three types of geometrical objects to represent the principal emission sector components: point, line and diffused (area) emission sources. While preserving the point source information in the ODIAC dataset, we disaggregated the non-point source emissions using geospatial dataset such as global road network data and satellite-data driven surface imperviousness data to generate a 30 × 30 m resolution emission field, comparable to the spatial scale of Hestia. Our disaggregation theoretically can be applied to any global cities and provide an emission estimate with spatial distributions even EI are not compiled locally. The posterior emission estimate summed over the whole city was about 5.1 MtC/yr and remains statistically similar to the previous inversion using ODIAC (5.3 MtC/yr, as reported by Lauvaux et al., 2016). However, the inversion with the 30 × 30 m emission field yielded flux corrections with major spatial patterns matched with those of the inverse using a state-of-the-art building-level emission product, and the optimized model-observation mismatches were similar across the city despite the absence of hourly variability in the prior emissions.
Although emission disaggregation is not often the best approach to inform emissions at a high spatial resolution, our result showed that the use of the geospatial data allowed us to improve the prior emission spatial structure within the city and the potential for providing city emissions where fine-grained emissions data are not available. Beyond the simple mapping of GHG emissions, we quantify here the indirect gain of information by using better-informed a priori emissions, further increasing the potential of the top down approach. This combined approach is particularly useful as fine-grained emission products like Hestia are rarely available for a vast majority of the large metropolitan areas across the globe. Currently, city scale emissions are reported for some cities within local climate action such as Compact of Mayors (https://www.compactofmayors.org/). If we were to start with such activities using atmospheric information, the reported EI (often without spatial distributions) needs to be disaggregated, in order to be incorporated into models. Our method offers a potential approach to a global verification system of city emissions (MRV) using a disaggregation method and an atmospheric inversion system at the urban scale. Given the availability of generic geospatial data, our approach could provide fine-scale city emissions in various locations as future CO2 observations from ground-based or space missions become more systematically available.
The ODIAC global emission dataset is available at http://db.cger.nies.go.jp/dataset/ODIAC/. “Hestia” fine-grained emission dataset is avaialbe from http://hestia.project.asu.edu/. The Global Roads Open Access Data Set (gROADS) v1 is available from http://sedac.ciesin.columbia.edu/data/set/groads-global-roads-open-access-v1. National Land Cover Dataset (NLCD) 2011 is available from http://www.mrlc.gov/nlcd2011.php. The atmospheric CO2 tower data used in this study are available at http://sites.psu.edu/influx/data/.
The authors would like to thank Junmei Tang for providing her expertise to data processing of geospatial data.
TO is supported by NASA Carbon Cycle Science program (Grant #NNX14AM76G). TL is supported by the National Institute for Standards and Technology (INFLUX project #70NANB10H245) and the National Oceanic and Atmospheric Administration (grant #NA13OAR4310076).
The authors have no competing interests to declare.
Andres RJ Boden TA Bréon F-M Ciais P Davis S et al. 2012. A synthesis of carbon dioxide emissions from fossil-fuel combustion. Biogeosciences 9: 1845–1871, DOI: http://dx.doi.org/10.5194/bg-9-1845-2012
Andres RJ, Boden TA and Higdon DM 2016. Gridded uncertainty in fossil fuel carbon dioxide emission maps, a CDIAC example. Atmos. Chem. Phys 16: 14979–14995, DOI: http://dx.doi.org/10.5194/acp-16-14979-2016
Asefi-Najafabady S Rayner PJ Gurney KR McRobert A Song Y et al. 2014. A multiyear, global gridded fossil fuel CO2 emission data product: Evaluation and analysis of results. J. Geophys. Res. Atmos 119: 10213–10231, DOI: http://dx.doi.org/10.1002/2013JD021296
Buchwitz M Reuter M Bovensmann H Pillai D Heymann J et al. 2013. Carbon Monitoring Satellite (CarbonSat): assessment of atmospheric CO2 and CH4 retrieval errors by error parameterization. Atmos. Meas. Tech 6: 3477–3500, DOI: http://dx.doi.org/10.5194/amt-6-3477-2013
Center for International Earth Science Information Network – CIESIN – Columbia University Information Technology Outreach Services – ITOS – University of Georgia 2013. Global Roads Open Access Data Set, Version 1 (gROADSv1) In: Palisades, NY: NASA Socioeconomic Data and Applications Center (SEDAC), DOI: http://dx.doi.org/10.7927/H4VD6WCT
Deng A, Lauvaux T, Davis KJ, Gaudet BJ, Miles N, Richardson SJ, Wu K, Sarmiento DP, Hardesty RM, Bonin TA, Brewer WA and Gurney KR 2017. Toward reduced transport errors in a high resolution urban CO2 inversion system. Elem Sci Anth, In press for the INFLUX Special Feature.
Elvidge CD, Baugh K, Zhizhin M and Hsu FC 2013. Why VIIRS data are superior to DMSP for maping nighttime lights. Proc. the Asia-Pacific Advanced Network 35: 62–69, DOI: http://dx.doi.org/10.7125/APAN.35.7
Enting IG, Trudinger CM and Francey RJ 1995. A synthesis inversion of the concentration and d13C atmospheric CO2. Tellus B 47: 35–52, DOI: http://dx.doi.org/10.3402/tellusb.v47i1-2.15998
Feng S Lauvaux T Newman S Rao P Ahmadov R et al. 2016. Los Angeles megacity: a high-resolution land–atmosphere modelling system for urban CO2 emissions. Atmos. Chem. Phys 16: 9019–9045, DOI: http://dx.doi.org/10.5194/acp-16-9019-2016
Guan D, Liu Z, Geng Y, Lindner S and Hubacek K 2012. The gigatonne gap in China’s carbon dioxide inventories. Nature Climate Change 2: 672–675, DOI: http://dx.doi.org/10.1038/nclimate1560
Gurney K Razlivanov I Song Y Zhou Y et al. 2012. Quantification of fossil fuel CO2 emission on the building/street scale for a large US city. Environ. Sci. & Technol 46: 12194–12202, DOI: http://dx.doi.org/10.1021/es3011282
Gurney KR Liang J Patarasuk R O’Keeffe D Huang J et al. 2016. Reconciling the differences between a bottom-up and inverse-estimated FFCO2 emissions estimate in a large US urban area. Elem Sci Anth, In press for the INFLUX Special Feature.
Hutyra L Duren R Gurney KR Grimm N Kort E et al. 2014. “Urbanization and the carbon cycle: Current capabilities and research outlook from the natural sciences perspective”. Earth’s Future, DOI: http://dx.doi.org/10.1002/2014EF000255
Janardanan R, Maksyutov S, Oda T, Saito M, Kaiser JW, Ganshin A, Stohl A, Matsunaga T, Yoshida Y and Yokota T 2016. Comparing GOSAT observations of localized CO2 enhancements by large emitters with inventory-based estimates. Geophys. Res. Lett 43DOI: http://dx.doi.org/10.1002/2016GL067843
Janssens-Maenhout G Dentener F Van Aardenne J Monni S Pagliari V et al. 2012. EDGAR-HTAP: a Harmonized Gridded Air Pollution Emission Dataset Based on National Inventories In: JRC68434, EUR report No EUR. Ispra (Italy): European Commission Publications Office, 25pp. 299–2012. 978-92-79-23122-01831-9424
Kort EA, Frankenberg C, Miller CE and Oda T 2012. Space-based observations of megacity carbon dioxide. Geophys. Res. Lett 39: 17–22, DOI: http://dx.doi.org/10.1029/2012GL052738
Kuenen J, Visschedijk A, Jozwicka M and Gon H 2014. TNO-MACC_II emission inventory; a multi-year (2003–2009) consistent high-resolution European emission inventory for air quality modelling. Atmos Chem Phys 14(20): 10963–10976, DOI: http://dx.doi.org/10.5194/acp-14-10963-2014
Kurokawa J Ohara T Morikawa T Hanayama S Janssens-Maenhout G et al. 2013. Emissions of air pollutants and greenhouse gases over Asian regions during 2000–2008: Regional Emission inventory in ASia (REAS) version 2. Atmos. Chem. Phys 13: 11019–11058, DOI: http://dx.doi.org/10.5194/acp-13-11019-2013
Lauvaux T et al. 2016. High-resolution atmospheric inversion of urban CO2 emissions during the dormant season of the Indianapolis Flux Experiment (INFLUX). J. Geophys. Res. Atmos 121DOI: http://dx.doi.org/10.1002/2015JD024473
Liu Z et al. 2015. Reduced carbon emission estimates from fossil fuel combustion and cement production in China. Nature 524: 335–8, DOI: http://dx.doi.org/10.1038/nature14677
Marland G 2008. Uncertainties in Accounting for CO2 From Fossil Fuels. J. Industrial Ecology 12: 136–139, DOI: http://dx.doi.org/10.1111/j.1530-9290.2008.00014.x
Miles NL et al. 2017. Detectability and quantification of atmospheric boundary layer greenhouse gas dry mole fraction enhancements in an urban landscape: Results from the Indianapolis Flux Experiment (INFLUX). Elem Sci Anth, In press for the INFLUX Special Feature.
Nassar R Jones DBA Suntharalingam P Chen JM Andres RJ et al. 2010. Modeling global atmospheric CO2 with improved emission inventories and CO2 production from the oxidation of other carbon species. Geosci. Model Dev 3: 689–716, DOI: http://dx.doi.org/10.5194/gmd-3-689-2010
Nisbet E and Weiss R 2010. Top-down versus bottom-up. Science 328: 1241–1243, DOI: http://dx.doi.org/10.1126/science.1189936
Oda T and Maksyutov S 2011. A very high-resolution (1 km × 1 km) global fossil fuel CO2 emission emission inventory derived using a point source database and satellite observations of nighttime lights. Atmos. Chem. and Phys 11: 543–556, DOI: http://dx.doi.org/10.5194/acp-11-543-2011
Olivier JGJ, Aardenne JAV, Dentener FJ, Pagliari V, Ganzeveld LN and Peters JAHW 2005. Recent trends in global greenhouse gas emissions: Regional trends 1970–2000 and spatial distribution of key sources in 2000. J. Integr. Env. Sci 2: 81–99, DOI: http://dx.doi.org/10.1080/15693430500400345
Olivier JGJ and Peters JAHW 2002. Uncertainties in global, regional, and national emissions inventories In: Van Ham, J, Baede, APM, Guicherit, R and WIlliams-Jacobse, JFGM eds. Non-CO2 greenhouse gases: Scientific understanding, control options and policy aspects. New York, USA: Springer, pp. 525–540.
Pacala SW et al. 2010. Verifying Greenhouse Gas Emissions: Methods to Support International Climate Agreements In: Committee on Methods for Estimating Greenhouse Gas Emissions; National Research Council. National Academy of Sciences, p. 124.
Patarasuk P Gurney KR O’Keeffe D Song Y Huang J et al. 2016. Application of high-resolution fossil fuel CO2 emissions quantification to urban climate policy in Salt Lake County, Utah USA. Urban Ecosystems, DOI: http://dx.doi.org/10.1007/s11252-016-0553-1
Polonsky IN, O’Brien DM, Kumer JB, O’Dell CW and the geoCARB Team 2014. Performance of a geostationary mission, geoCARB, to measure CO2, CH4, and CO column-averaged concentrations. Atmos. Meas. Tech 7: 959–981, DOI: http://dx.doi.org/10.5194/amt-7-959-2014
Rayner PJ, Raupach MR, Paget M, Peylin P and Koffi E 2010. A new global gridded data set of CO2 emissions from fossil fuel combustion: Methodology and evaluation. J. Geophys. Res 115(D19): 306.DOI: http://dx.doi.org/10.1029/2009JD013439
Richardson SJ Miles NL Davis KJ Lauvaux L Martins DK et al. 2017. CO2, CH4, and CO tower in situ measurement network in support of the Indianapolis FLUX (INFLUX) Experiment. Elem Sci Anth, In press for the INFLUX Special Feature.
Román MO and Stokes EC 2015. Holidays in Lights: Tracking cultural patterns in demand for energy services. Earth’s Future, DOI: http://dx.doi.org/10.1002/2014EF000285
Streets D et al. 2003. An inventory of gaseous and primary aerosol emissions in Asia in the year 2000. J. Geophys. Res 108(D21): 8809.DOI: http://dx.doi.org/10.1029/2002JD003093
Turnbull JC et al. 2015. Toward quantification and source sector identification of fossil fuel CO2 emissions from an urban area: Results from the influx experiment. J. Geophys. Res. Atmos 120: 292–312, DOI: http://dx.doi.org/10.1002/2014JD022555
Woodard D Branham M Buckingham G Hogue S Hutchins M et al. 2014. A spatial uncertainty metric for anthropogenic CO2 emissions, Greenhouse Gas Measurement and Management (2014). 2–4: 139–160, DOI: http://dx.doi.org/10.1080/20430779.2014.1000793