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Dr. Jakub Bartyzel
AGH University of Science and Technology, Faculty of Physics and Applied Computer Science, Krakow, Poland

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0 Air Quality
0 Greenhouse Gas
0 Particulate Matter
0 Global warming and climate change
0 modelling and simulations

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Journal article
Published: 21 April 2021 in Sensors
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Winter smog episodes are a severe problem in many cities around the world. The following two mechanisms are responsible for influencing the level of pollutant concentrations: emission of pollutants from different sources and associated processes leading to formation of secondary aerosols in the atmosphere and meteorology, including advection, which is stimulated by horizontal wind, and convection, which depends on vertical air mass movements associated with boundary layer stability that are determined by vertical temperature and humidity gradients. The aim of the present study was to evaluate the performance of an unmanned aerial vehicle (UAV)-based measurement system developed for investigation of urban boundary layer dynamics. The evaluation was done by comparing the results of temperature, relative humidity, wind speed and particulate matter fraction with aerodynamic diameter below 10 μm (PM10) concentration vertical profiles obtained using this system with two reference meteorological stations: Jagiellonian University Campus (JUC) and radio transmission tower (RTCN), located in the urban area of Krakow city, Southern Poland. The secondary aim of the study was to optimize data processing algorithms improving the response time of UAV sensor measurements during the ascent and descent parts of the flight mission.

ACS Style

Piotr Sekula; Miroslaw Zimnoch; Jakub Bartyzel; Anita Bokwa; Michal Kud; Jaroslaw Necki. Ultra-Light Airborne Measurement System for Investigation of Urban Boundary Layer Dynamics. Sensors 2021, 21, 2920 .

AMA Style

Piotr Sekula, Miroslaw Zimnoch, Jakub Bartyzel, Anita Bokwa, Michal Kud, Jaroslaw Necki. Ultra-Light Airborne Measurement System for Investigation of Urban Boundary Layer Dynamics. Sensors. 2021; 21 (9):2920.

Chicago/Turabian Style

Piotr Sekula; Miroslaw Zimnoch; Jakub Bartyzel; Anita Bokwa; Michal Kud; Jaroslaw Necki. 2021. "Ultra-Light Airborne Measurement System for Investigation of Urban Boundary Layer Dynamics." Sensors 21, no. 9: 2920.

Journal article
Published: 12 July 2020 in Sustainability
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The concentration of indoor suspended particulate matter is considered to be one of the main factors that affect health and quality of life. In Poland, in response to the pressure of public opinion, a few thousand air purifiers have been installed in public buildings where children spend time. However, another factor that also impacts upon the quality of indoor air, namely increased CO2 mixing ratios, is frequently overlooked. The only way to remove CO2 excess from interiors is through intensive ventilation. This is often an action at odds with the need to maintain low concentrations of particulate matter in indoor air. Two methods are presented to assess the rate of air exchange using CO2 or particulate matter as a tracer. One of the methods using indoor/outdoor PM (particulate matter) concentrations is based on the use of box models for analysis. The second one uses indoor CO2 concentration change analysis. At the tested locations, they showed large deviations of the determined values of the air exchange coefficients from its limits. Both methods showed consistent ventilation parameters estimation.

ACS Style

Jakub Bartyzel; Damian Zięba; Jarosław Nęcki; Mirosław Zimnoch. Assessment of Ventilation Efficiency in School Classrooms Based on Indoor–Outdoor Particulate Matter and Carbon Dioxide Measurements. Sustainability 2020, 12, 5600 .

AMA Style

Jakub Bartyzel, Damian Zięba, Jarosław Nęcki, Mirosław Zimnoch. Assessment of Ventilation Efficiency in School Classrooms Based on Indoor–Outdoor Particulate Matter and Carbon Dioxide Measurements. Sustainability. 2020; 12 (14):5600.

Chicago/Turabian Style

Jakub Bartyzel; Damian Zięba; Jarosław Nęcki; Mirosław Zimnoch. 2020. "Assessment of Ventilation Efficiency in School Classrooms Based on Indoor–Outdoor Particulate Matter and Carbon Dioxide Measurements." Sustainability 12, no. 14: 5600.

Journal article
Published: 06 July 2020 in Nukleonika
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The city of Krakow located in southern Poland ranks among the most polluted urban agglomerations in Europe. There are persisting controversies with respect to impact of different pollution sources operating in Krakow agglomeration on air quality within the city. The presented pilot study was aimed at exploring the possibilities offered by elemental and carbon isotope composition of total suspended particulate matter (TSPM) for better characterization of its sources in Krakow atmosphere. The analyses of carbon isotope composition of total carbon in the investigated TSPM samples were supplemented by parallel analyses of radiocarbon content in atmospheric carbon dioxide (CO2). This study revealed large seasonal variability of carbon isotope composition in the analysed TSPM samples. This large variability reflects seasonally varying contribution of different sources of fossil and modern carbon to the TSPM pool. The elemental composition of TSPM also reveals distinct seasonal variability of the analysed elements, reflecting varying mixture of natural and anthropogenic sources of those elements. A linear relationship between the fossil carbon load in the TSPM samples and the fossil carbon load in the atmospheric CO2 was found, pointing to the presence of additional source of anthropogenic carbonaceous particles not associated with burning of fossil fuels. Wearing of tyres and asphalt pavement is most probably the main source of such particles.

ACS Style

Miroslaw Zimnoch; Filip Morawski; Tadeusz Kuc; Lucyna Samek; Jakub Bartyzel; Zbigniew Gorczyca; Alicja Skiba; Kazimierz Rozanski. Summer–winter contrast in carbon isotope and elemental composition of total suspended particulate matter in the urban atmosphere of Krakow, Southern Poland. Nukleonika 2020, 65, 181 -191.

AMA Style

Miroslaw Zimnoch, Filip Morawski, Tadeusz Kuc, Lucyna Samek, Jakub Bartyzel, Zbigniew Gorczyca, Alicja Skiba, Kazimierz Rozanski. Summer–winter contrast in carbon isotope and elemental composition of total suspended particulate matter in the urban atmosphere of Krakow, Southern Poland. Nukleonika. 2020; 65 (3):181-191.

Chicago/Turabian Style

Miroslaw Zimnoch; Filip Morawski; Tadeusz Kuc; Lucyna Samek; Jakub Bartyzel; Zbigniew Gorczyca; Alicja Skiba; Kazimierz Rozanski. 2020. "Summer–winter contrast in carbon isotope and elemental composition of total suspended particulate matter in the urban atmosphere of Krakow, Southern Poland." Nukleonika 65, no. 3: 181-191.

Original article
Published: 12 June 2018 in Mitigation and Adaptation Strategies for Global Change
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Anthropogenic emissions of carbon dioxide (CO2) and methane (CH4) in the atmosphere constitute an important component of the related carbon budget. The main source of anthropogenic CO2 is burning of fossil fuels, especially in densely populated areas. Similar emissions of CH4 are associated with the agricultural sector, coal mining, and other human activities, such as waste management and storage and natural gas networks supplying methane to large urban, industrial centers. We discuss several methods aimed at characterizing and quantifying atmospheric loads and fluxes of CO2 and CH4 in Krakow, the second largest city in Poland. The methods are based on atmospheric observations of mixing ratios as well as isotopic composition of the investigated gases. Atmospheric mixing ratios of CO2 and CH4 were measured using gas chromatography (GC) and cavity ring-down spectroscopy (CRDS). The isotopic composition of CO2 and CH4 was analyzed using isotope ratio mass spectrometry (IRMS), accelerator mass spectrometry (AMS), and CRDS techniques. These data, combined with auxiliary information characterizing the intensity of vertical mixing in the lower atmosphere (height of the nocturnal boundary layer [NBL] and atmospheric 222Rn concentration), were further used to quantify emission rates of CO2 and CH4 in the urban atmosphere of Krakow. These methods provide an efficient way of quantifying surface emissions of major greenhouse gases originating from distributed sources, thus complementing the widely used bottom-up methodology based on emission statistics.

ACS Style

Miroslaw Zimnoch; Jaroslaw Necki; Lukasz Chmura; Alina Jasek; Dorota Jelen; Michal Galkowski; Tadeusz Kuc; Zbigniew Gorczyca; Jakub Bartyzel; Kazimierz Rozanski. Quantification of carbon dioxide and methane emissions in urban areas: source apportionment based on atmospheric observations. Mitigation and Adaptation Strategies for Global Change 2018, 24, 1051 -1071.

AMA Style

Miroslaw Zimnoch, Jaroslaw Necki, Lukasz Chmura, Alina Jasek, Dorota Jelen, Michal Galkowski, Tadeusz Kuc, Zbigniew Gorczyca, Jakub Bartyzel, Kazimierz Rozanski. Quantification of carbon dioxide and methane emissions in urban areas: source apportionment based on atmospheric observations. Mitigation and Adaptation Strategies for Global Change. 2018; 24 (6):1051-1071.

Chicago/Turabian Style

Miroslaw Zimnoch; Jaroslaw Necki; Lukasz Chmura; Alina Jasek; Dorota Jelen; Michal Galkowski; Tadeusz Kuc; Zbigniew Gorczyca; Jakub Bartyzel; Kazimierz Rozanski. 2018. "Quantification of carbon dioxide and methane emissions in urban areas: source apportionment based on atmospheric observations." Mitigation and Adaptation Strategies for Global Change 24, no. 6: 1051-1071.

Journal article
Published: 10 February 2016 in Isotopes in Environmental and Health Studies
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A dedicated, GC-based analytical system is presented which allows detection of four anthropogenic trace gases (SF6, SF5CF3, CFC-12 and Halon-1301) in a single water sample, with detection limits and measurement uncertainties sufficiently low to employ them as quantitative indicators of groundwater age. The gases dissolved in water are extracted in the field using the method based on a dynamic head-space concept. In the laboratory, the investigated gases are cryogenically enriched, separated and measured using an electron capture detector. Reproducibility of the analyses is in the order of 2-5 %. The investigated tracers were measured in several production wells located in the recharge area of an intensively exploited aquifer in southern Poland. While the piston-flow ages of groundwater in the investigated wells revealed internal consistency, they appeared to be generally smaller than the ages derived from time series of tritium content in those wells, interpreted by lumped-parameter models. This difference stems mainly from significantly longer travel times of tritium through the unsaturated zone, when compared to the gaseous tracers being used. The results of this study highlight the benefits of using multiple tracing in quantifying timescales of groundwater flow in shallow aquifer systems.

ACS Style

Jakub Bartyzel; Kazimierz Rozanski. Dating of young groundwater using four anthropogenic trace gases (SF6, SF5CF3, CFC-12 and Halon-1301): methodology and first results. Isotopes in Environmental and Health Studies 2016, 52, 393 -404.

AMA Style

Jakub Bartyzel, Kazimierz Rozanski. Dating of young groundwater using four anthropogenic trace gases (SF6, SF5CF3, CFC-12 and Halon-1301): methodology and first results. Isotopes in Environmental and Health Studies. 2016; 52 (4-5):393-404.

Chicago/Turabian Style

Jakub Bartyzel; Kazimierz Rozanski. 2016. "Dating of young groundwater using four anthropogenic trace gases (SF6, SF5CF3, CFC-12 and Halon-1301): methodology and first results." Isotopes in Environmental and Health Studies 52, no. 4-5: 393-404.

Journal article
Published: 01 January 2016 in Aerosol and Air Quality Research
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Records of trace gas composition of the atmosphere originating from mountain stations are difficult to interpret in terms of continental gas balances due to complex topography and local wind patterns. Kasprowy Wierch station, located in the High Tatra Mountains, Poland, provides datasets to European GHG databases and can be used for regional and continental balances of trace gases in Earth’s atmosphere. Although it suffers from strong influence of local valley winds, the concentration record obtained at Kasprowy Wierch contains also a discernible fraction of methane (up to 100 ppb) emitted mainly by large regional source of this gas (Silesian Coal Basin) located ca. 150 km north-west of Kasprowy Wierch. Comparison of GOSAT satellite CH4 record in the pixel including High Tatras at the level of 850 hPa with the data obtained at Kasprowy Wierch mountain station revealed surprisingly good correlation, even for relatively short time intervals

ACS Style

Jarosław M. Nęcki; Michał Gałkowski; Łukasz Chmura; Christoph Gerbig; Miroslaw Zimnoch; Damian Zięba; Jakub Bartyzel; Wojciech Wołkowicz; Kazimierz Różański. Regional Representativeness of CH4 and N2O Mixing Ratio Measurements at High-Altitude Mountain Station Kasprowy Wierch, Southern Poland. Aerosol and Air Quality Research 2016, 16, 568 -580.

AMA Style

Jarosław M. Nęcki, Michał Gałkowski, Łukasz Chmura, Christoph Gerbig, Miroslaw Zimnoch, Damian Zięba, Jakub Bartyzel, Wojciech Wołkowicz, Kazimierz Różański. Regional Representativeness of CH4 and N2O Mixing Ratio Measurements at High-Altitude Mountain Station Kasprowy Wierch, Southern Poland. Aerosol and Air Quality Research. 2016; 16 (3):568-580.

Chicago/Turabian Style

Jarosław M. Nęcki; Michał Gałkowski; Łukasz Chmura; Christoph Gerbig; Miroslaw Zimnoch; Damian Zięba; Jakub Bartyzel; Wojciech Wołkowicz; Kazimierz Różański. 2016. "Regional Representativeness of CH4 and N2O Mixing Ratio Measurements at High-Altitude Mountain Station Kasprowy Wierch, Southern Poland." Aerosol and Air Quality Research 16, no. 3: 568-580.

Journal article
Published: 01 January 2016 in Papers on Global Change IGBP
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An overview of systematic observations of the trace-gas composition of the atmosphere over southern Poland is presented, against the background of data available for other greenhouse gas (GHG) monitoring stations in Europe. The results of GHG monitoring for three major greenhouse gases (CO2, CH4, N2O) are discussed. Measurements were performed at two locations of contrasting characteristics, i.e. (i) the high-altitude mountain station of Kasprowy Wierch in the High Tatras, representing atmospheric conditions relatively free of local influences, and (ii) an urban station located in the Krakow agglomeration. The GHG data available for the Kasprowy Wierch station were compared with relevant data available for two marine reference stations (Mace Head, Ireland and Terceira Island, Azores), and two continental stations (Hohenpeissenberg, Germany and Pallas-Sammaltunturi, Finland). The growth rates for the CO2 mole fraction recorded at these five stations reveal only small temporal changes that almost coincide, leading to a quasi-linear increase of the CO2 mixing ratio over the European continent over the past 20 years. While N2O observations also reveal a steady increase over this time period, the mole fraction accounted for by CH4 is increasing again, after a period of stagnation in the years 2001–2007. The impact of continental sources of CH4 and N2O is seen clearly in the Kasprowy Wierch records. The mean departure between the CH4 mixing ratios recorded at Kasprowy Wierch and at the marine reference stations in the period 1994–2014 is of 27.3 ppb, and stems from continental emissions of this gas originating mainly from anthropogenic activities (leaking natural-gas distribution networks, landfills and livestock). For N2O, a departure of 1 ppb was observed for the period 2009–2014. Comparison of quasi-continuous measurements of CO2, CH4 and N2O mixing ratios made in the urban atmosphere of Krakow and at the regional reference site Kasprowy Wierch (located approximately 100 km away), allows for a deeper insight into the mechanisms controlling daily variations in atmospheric mixing ratios of these gases at the two sites. The development of a nocturnal inversion layer in the atmosphere above the city leads to local enhancements of CO2, CH4 and N2O mole fractions in the Krakow atmosphere during the night hours, with these exceeding the baseline level significantly.

ACS Style

Kazimierz Różański; Łukasz Chmura; Michał Gałkowski; Jarosław Nęcki; Mirosław Zimnoch; Jakub Bartyzel; Simon O’Doherty. Monitoring of Greenhouse Gases in the Atmosphere – A Polish Perspective. Papers on Global Change IGBP 2016, 23, 111 -126.

AMA Style

Kazimierz Różański, Łukasz Chmura, Michał Gałkowski, Jarosław Nęcki, Mirosław Zimnoch, Jakub Bartyzel, Simon O’Doherty. Monitoring of Greenhouse Gases in the Atmosphere – A Polish Perspective. Papers on Global Change IGBP. 2016; 23 (1):111-126.

Chicago/Turabian Style

Kazimierz Różański; Łukasz Chmura; Michał Gałkowski; Jarosław Nęcki; Mirosław Zimnoch; Jakub Bartyzel; Simon O’Doherty. 2016. "Monitoring of Greenhouse Gases in the Atmosphere – A Polish Perspective." Papers on Global Change IGBP 23, no. 1: 111-126.

Journal article
Published: 10 April 2014 in Geological Quarterly
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ACS Style

Kazimierz Rozanski; Jarosław Nęcki; Łukasz Chmura; Ireneusz Śliwka; Mirosław Zimnoch; Jarosław Bielewski; Michał Gałkowski; Jakub Bartyzel; Janusz Rosiek. Anthropogenic changes of CO2, CH4, N2O, CFCl3, CF2Cl2, CCl2FCClF2, CHCl3, CH3CCl3, CCl4, SF6 and SF5CF3 mixing ratios in the atmosphere over southern Poland. Geological Quarterly 2014, 58, 1 .

AMA Style

Kazimierz Rozanski, Jarosław Nęcki, Łukasz Chmura, Ireneusz Śliwka, Mirosław Zimnoch, Jarosław Bielewski, Michał Gałkowski, Jakub Bartyzel, Janusz Rosiek. Anthropogenic changes of CO2, CH4, N2O, CFCl3, CF2Cl2, CCl2FCClF2, CHCl3, CH3CCl3, CCl4, SF6 and SF5CF3 mixing ratios in the atmosphere over southern Poland. Geological Quarterly. 2014; 58 (4):1.

Chicago/Turabian Style

Kazimierz Rozanski; Jarosław Nęcki; Łukasz Chmura; Ireneusz Śliwka; Mirosław Zimnoch; Jarosław Bielewski; Michał Gałkowski; Jakub Bartyzel; Janusz Rosiek. 2014. "Anthropogenic changes of CO2, CH4, N2O, CFCl3, CF2Cl2, CCl2FCClF2, CHCl3, CH3CCl3, CCl4, SF6 and SF5CF3 mixing ratios in the atmosphere over southern Poland." Geological Quarterly 58, no. 4: 1.

Journal article
Published: 01 July 2013 in European Journal of Soil Science
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Uptake of atmospheric hydrogen by soils constitutes the most important sink of this gas at the global scale. However, little is known about the strength and spatio‐temporal variability of this sink. We present the results of a systematic study aimed at characterizing hydrogen uptake by urban soils. The study was carried out at two field sites in Krakow, southern Poland. The measured fluxes of hydrogen to soils revealed distinct seasonality, with large values (up to 40 µmol hour−1 m−2) recorded during summer months and small values (between 5 and 10 µmol hour−1 m−2) during winter. Temperatures in the top 6 cm of the soil profile varied during the study from −9 to +24°C, while volumetric soil water content fluctuated between 15 and 50%. Measurable hydrogen fluxes were also observed when soil temperatures were less than zero. The results were interpreted in the context of seasonal changes of local climate and air and soil temperature, soil water content and amount of rainfall. Mixing conditions at the air–soil interface were also considered. Modelling of H2 uptake was performed with a two dimensional diffusion transport model, with contrasting assumptions about distribution and intensity of the hydrogen sink in the soil profile. The model results suggest that conditions in the uppermost soil layer exert a decisive control on measured hydrogen uptake rates. The measured hydrogen flux can be reproduced by the transport model only if significant reduction of the soil water content in the uppermost layer of the soil is postulated. This finding has important implications for the parameterization of hydrogen uptake rates in models of the global H2 budget.

ACS Style

Jakub Bartyzel; J. M. Necki; Damian Zięba; K. Rozanski; M. Gasiorek. Uptake of atmospheric hydrogen by soils: a case study from southern Poland. European Journal of Soil Science 2013, 64, 597 -609.

AMA Style

Jakub Bartyzel, J. M. Necki, Damian Zięba, K. Rozanski, M. Gasiorek. Uptake of atmospheric hydrogen by soils: a case study from southern Poland. European Journal of Soil Science. 2013; 64 (5):597-609.

Chicago/Turabian Style

Jakub Bartyzel; J. M. Necki; Damian Zięba; K. Rozanski; M. Gasiorek. 2013. "Uptake of atmospheric hydrogen by soils: a case study from southern Poland." European Journal of Soil Science 64, no. 5: 597-609.

Short communication
Published: 22 March 2013 in Journal of Chromatography A
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Atmospheric concentrations of anthropogenic trace gases, such as sulfur hexafluoride, SF6, chlorotrifluoromethane, CF3Cl, and bromotrifluoromethane, CF3Br, are increasing. Their long lifetimes and limited chemical reactivity make them attractive environmental tracers for hydrology and oceanography. While ambient SF6 concentrations can be readily measured using GC-ECD, the simultaneous analysis of CF3Cl and CF3Br is hampered due to their low ECD sensitivity. The response of a commercial ECD for those gases was enhanced using the resonance detection mode which is based on shifting the mean energy of electrons in the ECD detector towards the region where the electron-capture reaction reveals a distinct maximum. A custom electronic system enabled operation of a commercial ECD in the resonance detection mode. An approximately 50-fold amplification of the ECD signal was obtained for CF3Cl by application of high-frequency electric field (amplitude of 50 V and frequency of 40 MHz). For CF3Br, a 3.5-fold increase of the ECD signal was obtained, with a lower HF field (20–30 V). In the case of SF6 the application of the HF field reduces the magnitude of ECD signal by a factor of 40. The electron-capture coefficients for SF6, CF3Cl and CF3Br were determined from 453 to 633 K in the standard and the resonance modes. The electron-capture coefficients for CF3Cl and CF3Br increase with increasing temperature for both modes, while that for SF6 decreases slightly with increasing temperature. The application of the resonance detection mode to a commercial ECD provides an attractive and cost-effective alternative to GCMS for high-quality quantitative analyses of CF3Cl and CF3Br as environmental tracers.

ACS Style

J. Rosiek; Jakub Bartyzel; K. Rozanski; I. Sliwka. The use of a custom mode electron capture detector to determine mixing ratios of environmental tracers: Sulfur hexafluoride, chlorotrifluoromethane and bromotrifluoromethane. Journal of Chromatography A 2013, 1282, 194 -198.

AMA Style

J. Rosiek, Jakub Bartyzel, K. Rozanski, I. Sliwka. The use of a custom mode electron capture detector to determine mixing ratios of environmental tracers: Sulfur hexafluoride, chlorotrifluoromethane and bromotrifluoromethane. Journal of Chromatography A. 2013; 1282 ():194-198.

Chicago/Turabian Style

J. Rosiek; Jakub Bartyzel; K. Rozanski; I. Sliwka. 2013. "The use of a custom mode electron capture detector to determine mixing ratios of environmental tracers: Sulfur hexafluoride, chlorotrifluoromethane and bromotrifluoromethane." Journal of Chromatography A 1282, no. : 194-198.

Journal article
Published: 11 April 2011 in Atmospheric Chemistry and Physics
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This paper presents an analysis of the recent tropospheric molecular hydrogen (H2) budget with a particular focus on soil uptake and European surface emissions. A variational inversion scheme is combined with observations from the RAMCES and EUROHYDROS atmospheric networks, which include continuous measurements performed between mid-2006 and mid-2009. Net H2 surface flux, then deposition velocity and surface emissions and finally, deposition velocity, biomass burning, anthropogenic and N2 fixation-related emissions were simultaneously inverted in several scenarios. These scenarios have focused on the sensibility of the soil uptake value to different spatio-temporal distributions. The range of variations of these diverse inversion sets generate an estimate of the uncertainty for each term of the H2 budget. The net H2 flux per region (High Northern Hemisphere, Tropics and High Southern Hemisphere) varies between −8 and +8 Tg yr−1. The best inversion in terms of fit to the observations combines updated prior surface emissions and a soil deposition velocity map that is based on bottom-up and top-down estimations. Our estimate of global H2 soil uptake is −59±9 Tg yr−1. Forty per cent of this uptake is located in the High Northern Hemisphere and 55% is located in the Tropics. In terms of surface emissions, seasonality is mainly driven by biomass burning emissions. The inferred European anthropogenic emissions are consistent with independent H2 emissions estimated using a H2/CO mass ratio of 0.034 and CO emissions within the range of their respective uncertainties. Additional constraints, such as isotopic measurements would be needed to infer a more robust partition of H2 sources and sinks.

ACS Style

C. E. Yver; I. C. Pison; A. Fortems-Cheiney; M. Schmidt; Frédéric Chevallier; M. Ramonet; A. Jordan; O. A. Søvde; Andreas Engel; Rebecca Fisher; D. Lowry; E. G. Nisbet; I. Levin; S. Hammer; J. Necki; Jakub Bartyzel; Stefan Reimann; M. K. Vollmer; Martin Steinbacher; T. Aalto; M. Maione; Jgor Arduini; S. O'doherty; A. Grant; W. T. Sturges; G. L. Forster; C. R. Lunder; V. Privalov; N. Paramonova; A. Werner; Philippe Bousquet. A new estimation of the recent tropospheric molecular hydrogen budget using atmospheric observations and variational inversion. Atmospheric Chemistry and Physics 2011, 11, 3375 -3392.

AMA Style

C. E. Yver, I. C. Pison, A. Fortems-Cheiney, M. Schmidt, Frédéric Chevallier, M. Ramonet, A. Jordan, O. A. Søvde, Andreas Engel, Rebecca Fisher, D. Lowry, E. G. Nisbet, I. Levin, S. Hammer, J. Necki, Jakub Bartyzel, Stefan Reimann, M. K. Vollmer, Martin Steinbacher, T. Aalto, M. Maione, Jgor Arduini, S. O'doherty, A. Grant, W. T. Sturges, G. L. Forster, C. R. Lunder, V. Privalov, N. Paramonova, A. Werner, Philippe Bousquet. A new estimation of the recent tropospheric molecular hydrogen budget using atmospheric observations and variational inversion. Atmospheric Chemistry and Physics. 2011; 11 (7):3375-3392.

Chicago/Turabian Style

C. E. Yver; I. C. Pison; A. Fortems-Cheiney; M. Schmidt; Frédéric Chevallier; M. Ramonet; A. Jordan; O. A. Søvde; Andreas Engel; Rebecca Fisher; D. Lowry; E. G. Nisbet; I. Levin; S. Hammer; J. Necki; Jakub Bartyzel; Stefan Reimann; M. K. Vollmer; Martin Steinbacher; T. Aalto; M. Maione; Jgor Arduini; S. O'doherty; A. Grant; W. T. Sturges; G. L. Forster; C. R. Lunder; V. Privalov; N. Paramonova; A. Werner; Philippe Bousquet. 2011. "A new estimation of the recent tropospheric molecular hydrogen budget using atmospheric observations and variational inversion." Atmospheric Chemistry and Physics 11, no. 7: 3375-3392.