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Fant 10466 publikasjoner. Viser side 263 av 419:

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Global emission of mercury to the atmosphere from anthropogenic sources in 2005 and projections to 2020.

Pacyna, E.G.; Pacyna, J.M.; Sundseth, K.; Munthe, J.; Kindborn, K.; Wilson, S.; Steenhuisen, F.; Maxson, P.

2010

Global climate model development: Adding microplastics to the UK Earth System Model

McErlich, Cameron; Hardacre, Catherine; Goddard, Felix; Evangeliou, Nikolaos; Revell, Laura

2025

Global climate change impact on built heritage and cultural landscapes.

Sabbioni, C.; Cassar, M.; Brimblecombe, P.; Tidblad, J.; Kozlowski, R.; Drácky, M.; Saiz-Jimenez, C.; Grøntoft, T.; Wainwright, I.; Ariño, X.

2006

Global Carbon Project N2O Budget: Contribution from Inversions

Thompson, Rona Louise; Tian, H.; Canadell, P.; Lassaletta, Luis; Patra, Prabir; Wilson, C.; Wells, Kelley C.; Gressent, Alicia; Koffi, Ernest; Chipperfield, Martyn P.; Winiwarter, Wilfried; Peters, G

2020

Global carbon monoxide products from combined AIRS, TES and MLS measurements on A-train satellites.

Warner, J. X.; Yang, R.; Wei, Z.; Carminati, F.; Tangborn, A.; Sun, Z.; Lahoz, W.; Attié, J.-L.; El Amraoui, L.; Duncan, B.

2014

Global Carbon and Other Biogeochemical Cycles and Feedbacks

Canadell, Josep G.; Monteiro, Pedro M.S.; Costa, Marcos H.; Cox, Peter M.; Eliseev, Alexey; Henson, Stephanie; Ishii, Masao; Jaccard, Samuel; Koven, Charles; Lohila, Annalea; Patra, Prabir K.; Piao, Shilong; Rogelj, Joeri; Syampungani, Stephen; Zaehle, Sönke; Zickfeld, Kirsten; Thompson, Rona Louise; al, ... et

2021

Global black carbon emissions from 2015-2022 constrained by observations and transport modelling 

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

Black carbon (BC) is a product of incomplete combustion, is climate relevant and has negative impacts on human health. It absorbs radiation as an aerosol in the atmosphere, but also changes the albedo of snow covered surfaces and leads to earlier melting. The origins are either anthropogenic or natural, with different annual cycles. While anthropogenic sources like domestic burning peak in the winter, natural sources like wild fires and agricultural burning peak during spring and summer. Due to its short lifetime are the global atmospheric concentrations highly variable.We use ground based observational data from different global networks, and the atmospheric transport model FLEXPART driven by ERA5 meteorological analysis, emission inventories and the inversion framework FLEXINVERT. By minimizing the mismatch modelled and observed BC concentration we improve the emission inventories for natural emissions (GFAS) and anthropogenic emissions (LRTAP). For every year up to 50 stations are used and each observation is matched with a 50 day FLEXPART backward calculation.We discuss the distribution and sources of global BC aerosols over the period 2015 to 2022 and compare existing emission inventories with the improved constraints of the global BC emissions derived with the FLEXINVERT inversion framework.

2026

Global Black Carbon emissions constrained using a Bayesian inversion technique

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

2019

Global Atmospheric Microplastics Emissions Estimated Using Constrained Bayesian Inverse Modeling

Tichý, Ondřej; Uliáš, Michal; Evangelou, Ioanna; Šmídl, Václav; Evangeliou, Nikolaos

We present an analysis of global atmospheric microplastics (MPs) concentration and deposition measurements using constrained Bayesian inverse modeling to estimate global MPs emissions. The proposed Bayesian framework explicitly accounts for unknown ratios between size fractions inherent to MPs measurements and incorporates prior emission information to stabilize the inversion. The coupling between observations and unknown emissions is established using the atmospheric transport model FLEXPART version 11 operated in backward mode for each measurement. Model parameters are inferred using a variational Bayes approach, resulting in an iterative estimation scheme that updates both model parameters and the effective spatial structure of the computational domain. This methodology reduces the need for manual intervention during the inversion process and limits potential bias in the results. The resulting global MPs emission estimates are evaluated against previously published ones. Acknowledgment:This research has been supported by the Czech Science Foundation (grant no. GA24-10400S). N.E. was funded by the Norwegian Research Council (NFR) project MAGIC (No.: 334086). FLEXPART model simulations are cross-atmospheric research infrastructure services provided by ATMO-ACCESS (EU grant agreement No 101008004). The computations were performed on resources provided by Sigma2 - the National Infrastructure for High Performance Computing and Data Storage in Norway.

2026

Global anthropogenic mercury emission inventory for 2000.

Pacyna, E.G.; Pacyna, J.M.; Steenhuisen, F.; Wilson, S.

2006

Global anthropogenic emissions of mercury to the atmosphere.

Pacyna, J.M.; Pacyna, E.G.; Steenhuisen, F.; Wilson, S. (Lead authors); Zaikowski, L. (Topic editor).

2007

Global anthropogenic emissions of mercury and their future scenarios. NILU F

Pacyna, J.M.; Pacyna, E.G.; Sundseth, K.

2010

Global and regional trends of atmospheric sulfur

Aas, Wenche; Mortier, Augustin; Bowersox, Van C.; Cherian, Ribu; Faluvegi, Greg; Fagerli, Hilde; Hand, Jenny; Klimont, Zbigniew; Galy-Lacaux, Corinne; Lehmann, Christopher M.B.; Myhre, Cathrine Lund; Myhre, Gunnar; Oliviè, Dirk Jan Leo; Sato, Keiichi; Quaas, Johannes; Rao, Pasumarthi Surya Prakasa; Schulz, Michael; Shindell, Drew; Skeie, Ragnhild Bieltvedt; Stein, Ariel; Takemura, Toshihiko; Tsyro, Svetlana; Vet, Robert; Xu, Xiaobin

The profound changes in global SO2 emissions over the last decades have affected atmospheric composition on a regional and global scale with large impact on air quality, atmospheric deposition and the radiative forcing of sulfate aerosols. Reproduction of historical atmospheric pollution levels based on global aerosol models and emission changes is crucial to prove that such models are able to predict future scenarios. Here, we analyze consistency of trends in observations of sulfur components in air and precipitation from major regional networks and estimates from six different global aerosol models from 1990 until 2015. There are large interregional differences in the sulfur trends consistently captured by the models and observations, especially for North America and Europe. Europe had the largest reductions in sulfur emissions in the first part of the period while the highest reduction came later in North America and East Asia. The uncertainties in both the emissions and the representativity of the observations are larger in Asia. However, emissions from East Asia clearly increased from 2000 to 2005 followed by a decrease, while in India a steady increase over the whole period has been observed and modelled. The agreement between a bottom-up approach, which uses emissions and process-based chemical transport models, with independent observations gives an improved confidence in the understanding of the atmospheric sulfur budget.

2019

Global and regional emissions of HFC-125 (CHF2CF3) from in situ and air archive atmospheric observations at AGAGE and SOGE observatories.

O'Doherty, S.; Cunnold, D.M.; Miller, B.R.; Muhle, J.; McCulloch, A.; Simmonds, P.G.; Manning, A.J.; Reimann, S.; Vollmer, M.K.; Greally, B.R.; Prinn, R.G.; Fraser, P.J.; Steele, L.P.; Krummel, P.B.; Dunse, B.L.; Porter, L.W.; Lunder, C.R.; Schmidbauer, N.; Hermansen, O.; Salameh, P.K.; Harth, C.M.; Wang, R.H.J.; Weiss, R.F.

2009

Global and regional emissions estimates of 1,1-difluoroethane (HFC-152a, CH3CHF2) from in situ and air archive observations.

Simmonds, P. G.; Rigby, M.; Manning, A. J.; Lunt, M. F.; O'Doherty, S.; Young, D.; McCulloch, A.; Fraser, P. J.; Henne, S.; Vollmer, M. K.; Reimann, S.; Wenger, A.; Mühle, J.; Harth, C. M.; Salameh, P. K.; Arnold, T.; Weiss, R. F.; Krummel, P. B.; Steele, L. P.; Dunse, B. L.; Miller, B. R.; Lunder, C. R.; Hermansen, O.; Schmidbauer, N.; Saito, T.; Yokouchi, Y.; Park, S.; Li, S.; Yao, B.; Zhou, L. X.; Arduini, J.; Maione, M.; Wang, R. H. J.; Prinn, R. G.

2016

Global and regional emission estimates for HCFC-22.

Saikawa, E.; Rigby, M.; Prinn, R.G.; Montzka, S.; Miller, B.; Kuijpers, L.; Fraser, P.; Vollmer, M.; Yao, B.; Zhou, L.; Saito, T.; Yokouchi, Y.; Kim, J.; Park, S.; Young, D.; ODoherty, S.; Simmonds, P.; Harth, C.; Muhle, J.; Weiss, R.; Krummel, P.; Maione, M.; Lunder, C.; Sweeney, C.; Andrews, A.; Tans, P.

2012

Global and regional emission estimates for HCFC-22.

Saikawa, E.; Rigby, M.; Prinn, R. G.; Montzka, S. A.; Miller, B. R.; Kuijpers, L. J. M.; Fraser, P. J. B.; Vollmer, M. K.; Saito, T.; Yokouchi, Y.; Harth, C. M.; Mühle, J.; Weiss, R. F.; Salameh, P. K.; Kim, J.; Li, S.; Park, S.; Kim, K.-R.; Young, D.; O'Doherty, S.; Simmonds, P. G.; McCulloch, A.; Krummel, P. B.; Steele, L. P.; Lunder, C.; Hermansen, O.; Maione, M.; Arduini, J.; Yao, B.; Zhou, L. X.; Wang, H. J.; Elkins, J. W.; Hall, B.

2012

2017

Global and gene specific DNA methylation in breast cancer cells was not affected during epithelial-to-mesenchymal transition in vitro.

Smolkova, B.; Miklikova, S.; Kajabova, V. H.; Babelova, A.; El Yamani, N.; Zduriencikova, M.; Fridrichova, I.; Zmetakova, I.; Krivulcik, T.; Kalinkova, L.; Matuskova, M.; Kucerova, M.; Dusinska, M.

2016

Global and Arctic methane

Platt, Stephen Matthew; Myhre, Cathrine Lund; Ferré, Benedicte; Silyakova, Anna; Hermansen, Ove; Pisso, Ignacio; Schmidbauer, Norbert; Jansson, Pär; Stohl, Andreas; Eckhardt, Sabine; Vadakkepuliyambatta, Sunil; Fisher, Rebecca; Nisbet, Euan; Lowry, D.; Myhre, Gunnar; Mienert, Jürgen; Roekmann, Thomas

2019

Global ammonia inversions with CrIS satellite retrievals and ensemble Kalman smoother approximation for emission estimates optimization

Boufidou, Filothei; Gialesakis, N.; Gkouvousis, A.; Nuss, R.; Daskalakis, N.; Evangeliou, Nikolaos

2024

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