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Found 9895 publications. Showing page 366 of 396:

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Year  
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Top-down estimates of black carbon emissions at high latitudes using an atmospheric transport model and a Bayesian inversion framework

Evangeliou, Nikolaos; Thompson, Rona Louise; Eckhardt, Sabine; Stohl, Andreas

This paper presents the results of BC inversions at high northern latitudes (>50°N) for the 2013–2015 period. A sensitivity analysis was performed to select the best representative species for BC and the best a priori emission dataset. The same model ensemble was used to assess the uncertainty of the a posteriori emissions of BC due to scavenging and removal and due to the use of different a priori emission inventory. A posteriori concentrations of BC simulated over Arctic regions were compared with independent observations from flight and ship campaigns showing, in all cases, smaller bias, which in turn witnesses the success of the inversion. The annual a posteriori emissions of BC at latitudes above 50°N were estimated as 560±171ktyr−1, significantly smaller than in ECLIPSEv5 (745ktyr−1), which was used and the a priori information in the inversions of BC. The average relative uncertainty of the inversions was estimated to be 30%.

A posteriori emissions of BC in North America are driven by anthropogenic sources, while biomass burning appeared to be less significant as it is also confirmed by satellite products. In northern Europe, a posteriori emissions were estimated to be half compared to the a priori ones, with the highest releases to be in megacities and due to biomass burning in eastern Europe. The largest emissions of BC in Siberia were calculated along the transect between Yekaterinsburg and Chelyabinsk. The optimised emissions of BC were high close to the gas flaring regions in Russia and in western Canada (Alberta), where numerous power and oil and gas production industries operate. Flaring emissions in Nenets–Komi oblast (Russia) were estimated to be much lower than in the a priori emissions, while in Khanty-Mansiysk (Russia) they remained the same after the inversions of BC. Increased emissions at the borders between Russia and Mongolia are probably due to biomass burning in villages along the Trans-Siberian Railway. The maximum BC emissions in high northern latitudes (>50°N) were calculated for summer months due to biomass burning and they are controlled by seasonal variations in Europe and Asia, while North America showed a much smaller variability.

2018

Top-down estimates of European CH4 and N2O emissions based on four different inverse models.

Bergamaschi, P.; Corazza, M.; Karstens, U.; Athanassiadou, M.; Thompson, R.L.; Pison, I.; Manning, A.J.; Bousquet, P.; Segers, A.; Vermeulen, A.T.; Janssens-Maenhout, G.; Schmidt, M.; Ramonet, M.; Meinhardt, F.; Aalto, T.; Haszpra, L.; Moncrieff, J.; Popa, M.E.; Lowry, D.; Steinbacher, M.; Jordan, A.; O'Doherty, S.; Piacentino, S.; Dlugokencky, E.

2014

Top-down estimates of European CH4 and N2O emissions based on four different inverse models.

Bergamaschi, P.; Corazza, M.; Karstens, U.; Athanassiadou, M.; Thompson, R. L.; Pison, I.; Manning, A. J.; Bousquet, P.; Segers, A.; Vermeulen, A. T.; Janssens-Maenhout, G.; Schmidt, M.; Ramonet, M.; Meinhardt, F.; Aalto, T.; Haszpra, L.; Moncrieff, J.; Popa, M. E.; Lowry, D.; Steinbacher, M.; Jordan, A.; O'Doherty, S.; Piacentino, S.; Dlugokencky, E.

2015

Top-down estimates of N2O emissions over the past two decades

Thompson, Rona Louise; Wells, Kelley C.; Wilson, Chris J.; Gressent, Alicia; Koffi, Ernest; Bergamaschi, Peter; Millet, Dylan B.; Patra, Prabir Kumar; Prather, Michael J.; Tian, Hanqin; Suntharalingam, Parvadha; Canadell, Josep Gili

2018

Top-down estimates of N2O emissions over the past two decades

Thompson, Rona Louise; Lassaletta, Luis; Patra, Prabir; Wilson, C.; Wells, Kelley C.; Gressent, Alicia; Koffi, Ernest; Chipperfield, M. P; Winiwarter, Wilfried; Davidson, E. A.; Tian, H.; Canadell, P.

2019

Top-down validation of global and East Asian emissions of tetrafluoromethane and hexaflurorethane. NILU F

Kim, J.; Muhle, J.; Fraser, P.J.; Li, S.; Arnold, T.; Harth, C.M.; Salameh, P.; Steele, P.; Krummel, P.B.; Leist, M.; Stohl, A.; Park, M.; Weiss, R.F.; Kim, K.

2010

TOR: An Overview of Tropospheric Ozone Research Transport and Chemical Transformation of Pollutants in the Troposphere, 3373, vol. 1

Hov, Ø.; Kley, D.; Volz-Thomas, A.; Beck, J.; Grennfelt, P.; Penkett, S.A.

2000

Total deposition of major inorganic ions at non-urban sites in China, 2000-2004 (part II).

Jin, L.; Shao, M.; Aas, W.; Duan, L.; Vogt, R.D.; Zhao, D.; Xiang, R.; Zhang, J.; Xiao, J.

2005

Total deposition of major inorganic ions at non-urban sites in China, 2001-2003 (part II). NILU PP

Jin, L.; Shao, M.; Aas, W.; Duan, L.; Vogt, R.D.; Zhao, D.; Xiang, R.; Zhang, J.; Xiao, J.

2005

Total deposition of major inorganic ions at non-urban sites in China, 2001-2003.

Jin, L.; Shaoi, M.; Aas, W.; Duan, L.; Vogt, R.D.; Zhao, D.; Xiang, J. Zhang, J.; Xiao, J.

2007

Total oxidizable precursors assay for PFAS in human serum

Cioni, Lara; Nikiforov, Vladimir; Miranda Fernandes Coelho, Ana Carolina; Sandanger, Torkjel M; Herzke, Dorte

Per- and polyfluoroalkyl substances (PFAS) are a class of chemicals including over 4700 substances. As a limited number of PFAS is routinely analyzed in human serum, complementary analytical methods are required to characterize the overlooked fraction. A promising tool is the total oxidizable precursors (TOP) assay to look for precursors by oxidation to perfluoroalkyl acids (PFAA). The TOP assay was originally developed for large volumes of water and had to be adapted for 250 μL of human serum. Optimization of the method was performed on serum samples spiked with model precursors. Oxidative conditions similar to previous TOP assay methods were not sufficient for complete oxidation of model precursors. Prolonged heating time (24 h) and higher oxidant amount (95 mg of Na2S2O8 per 225 μL of serum) were needed for complete conversion of the model precursors and accomplishing PFAA yields of 35–100 %. As some precursors are not fully converted to PFAA, the TOP assay can only provide semi-quantitative estimates of oxidizable precursors in human serum. However, the TOP assay can be used to give indications about the identity of unknown precursors by evaluating the oxidation products, including perfluoroalkyl sulfonic acids (PFSA) and perfluoroalkyl ether carboxylic acids (PFECA). The optimized TOP assay for human serum opens the possibility for high-throughput screening of human serum for undetected PFAA precursors.

Elsevier

2022

Total ozone and UV measurements at the Norwegian Troll Station, Antarctica.

Hansen, G.; Svendby, T.; Dahlback, A.; Edvardsen, K.

2016

Total ozone loss during the 2005/2006 Arctic winter and comparison to previous years. Poster presentation. NILU PP

Goutail, F.; Lefèvre, F.; Pommereau, J.P.; van Roozendael, M.; Chipperfield, M.; Feng, W.; Kyro, E.; Andersen, S.B.; Stebel, K.; Dorokhov, V.

2006

Total ozone loss during the 2006/07 Arctic winter and comparison to previous year.

Goutail, F.; Lefèvre, F.; Pommereau, J.P.; Chipperfield, M.; Feng, W.; van Roozendael, M.; Andersen, S.B.; Stebel, K.; Dorokhov, V.; Kyro, E.; Fraser, A.; Strong, K.

2007

Total Ozone Loss during the 2007/2008 Arctic Winter and Comparison to Previous Years. NILU PP

Goutail, F.; Lefèvre, F.; Pommereau, J.P.; Pazmiño, A.; Chipperfield, M.; Feng, W.; Van Roozendael, M.; Eriksen, P.; Stebel, K.; Dorokhov, V.; Kyro, E.; Adams, C.; Fraser, A.M.; Strong, K.

2008

Total Ozone Loss during the 2007/2008 Arctic Winter and Comparison to Previous Years. NILU PP

Goutail, F.; Lefèvre, F.; Pommereau, J.P.; Pazmiño, A.; Chipperfield, M.; Feng, W.; Van Roozendael, M.; Eriksen, P.; Stebel, K.; Dorokhov, V.; Kyro, E.; Adams, C.; Fraser, A.M.; Strong, K.

2008

Total ozone loss during the 2008/2009 Arctic winter and comparison to previous years. NILU PP

Goutail, F.; Lefèvre, F.; Pommereau, J.P.; Pazmiño, A.; Chipperfield, M.; Feng, W.; Van Roozendael, M.; Eriksen, P.; Stebel, K.; Dorokhov, V.; Kyro, E.; Adams, C.; Fraser, A.M.; Strong, K.

2009

Total ozone loss during the 2009/10 Arctic winter and comparison to previous years. NILU PP

Goutail, F.; Lefèvre, F.; Kuttippurath, J.; Pazmiño, A.; Pommereau, J.P.; Chipperfield, M.; Feng, W.; Van Roozendael, M.; Eriksen, P.; Stebel, K.; Dorokhov, V.; Kyrö, E.; Adams, C.; Strong, K.

2010

Total ozone loss during the 2011/12 Arctic winter and comparison to previous years.

Goutail, F.; Lefevre, F.; Pommereau, J.P.; Pazmino, A.; Chipperfield, M.; Feng, W.; Van Roozendael, M.; Eriksen, P.; Stebel, K.; Dorokhov, V.; Kyro, E.; Zhao, X.; Strong, K.

2012

Total ozone loss during the 2012/13 Arctic winter and comparison to previous years.

Goutail, F.; Lefevre, F.; Pommereau, J.-P.; Pazmino, A.; Chipperfield, M.; Feng, W.; Van Roozendael, M.; Eriksen, P.; Stebel, K.; Dorokhov, V.; Kivi, R.; Zhao, X.; Strong, K.

2013

Total ozone loss during the 2013/14 Arctic winter and comparison to previous years.

Goutail, F.; Lefèvre, F.; Pommereau, J.-P.; Pazmino, A.; Chipperfield, M.; Feng, W.; Van Roozendael, M.; Eriksen, P.; Stebel, K.; Dorokhov, V.; Kivi, R.; Zhao, X.; Strong, K.

2014

Total ozone loss during the 2014/15 Arctic winter and comparison to previous years.

Goutail, F.; Lefèvre, F.; Pommereau, J.-P.; Pazmino, A.; Chipperfield, M.; Feng, W.; Van Roozendael, M.; Eriksen, P.; Stebel, K.; Kivi, R.; Zhao, X.; Strong, K.

2015

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