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Fant 9831 publikasjoner. Viser side 30 av 394:

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Reproducible pipelines and readiness levels in plastic monitoring

Nikiforov, Vladimir; Aliani, Stefano; Lusher, Amy Lorraine; Galgani, Francois; Herzke, Dorte; Primpke, Sebastian; Roscher, Lisa; da Silva, Vitor Hugo; Strand, Jakob; Suaria, Giuseppe; Vanavermaete, David; De Witte, Bavo P.; van Bavel, Bert

2023

Quality assurance of precipitation measurements in Norway

Guerreiro, Cristina; Halvorsen, Helene Lunder

2023

Chemical analysis of POPs and heavy metals in precipitation at NILU

Uggerud, Hilde Thelle; Halvorsen, Helene Lunder

2023

Støv – hva er det og hvordan måler vi det?

Weydahl, Torleif; Hak, Claudia

2023

Svovelskya kom – slik gjekk det

Tørseth, Kjetil (intervjuobjekt); Baas, Jarand Aga (journalist)

2023

Aerosol and dynamical contributions to cloud droplet formation in Arctic low-level clouds

Motos, Ghislain; Freitas, Gabriel; Georgakaki, Paraskevi; Wieder, Jörg; Li, Guangyu; Aas, Wenche; Lunder, Chris Rene; Krejci, Radovan; Pasquier, Julie Thérèse; Henneberger, Jan; David, Robert Oscar; Ritter, Christoph; Mohr, Claudia; Zieger, Paul; Nenes, Athanasios

2023

Solkrem er viktigst akkurat nå

Solbakken, Christine Forsetlund

Norges forskningsråd

2023

Røyk fra Canada kommer fortsatt inn over Norge

Solbakken, Christine Forsetlund

Norges forskningsråd

2023

Mapping and Visualizing Air Quality

Hassani, Amirhossein; Schneider, Philipp

2023

Deployment and Evaluation of Networks of Open Air Quality Sensor Systems - Experiences from deployments in Stavanger and Oslo

Schneider, Philipp; Vogt, Matthias; Haugen, Rolf; Hassani, Amirhossein; Castell, Nuria; Peters, Jan; Yatkin, Sinan; Gerboles, Michel; Matheeussen, Christina; Davila, Silvije; Signorini, Marco; Dauge, Franck Rene; Skaar, Jøran Solnes; Bartonova, Alena

2023

Evaluation of TROPOMI observations for estimating surface NO2 concentrations over Europe using XGBoost Model

Shetty, Shobitha; Schneider, Philipp; Stebel, Kerstin; Kylling, Arve; Berntsen, Terje Koren; Hamer, Paul David

2023

Analysis of nitro- and oxy-PAH emissions from a pilot scale silicon process with flue gas recirculation

Arnesen, Kamilla; Andersen, Vegar; Jakovljevic, Katarina; Enge, Ellen Katrin; Gaertner, Heiko; Aarhaug, Thor Anders; Einarsrud, Kristian Etienne; Tranell, Maria Gabriella

Silicon alloys are produced by carbothermic reduction of quartz in a submerged arc furnace. This high-temperature pyrolytic process is a source of polycyclic aromatic hydrocarbons (PAHs), which are a group of aromatic organic molecules with known mutagenic and carcinogenic properties. In this study, the emission of oxy- and nitro-PAHs from a pilot-scale Si furnace, with varying process conditions such as oxygen level, flue gas recirculation (FGR), and off-gas flow, was investigated. Analysis shows the presence of both oxy- and nitro-PAH species in all experiments, believed to be formed from radical-induced substitution reactions initiated by SiO combustion and NOx formation. During Si production without FGR, the levels of oxy- and nitro-PAHs range between 1.1 and 4.4 μg Nm−3, independent of the flue gas flow rate. With increasing FGR (0–82.5%) and decreasing oxygen level (20.7–13.3%), the concentrations of both oxy- and nitro-PAHs increase to 36.6 and 65.9 μg Nm−3, respectively. When the levels of substituted PAHs increase, species such as 4-nitropyrene and 1,2-benzanthraquinone are in abundance compared to their parent PAHs. Experiments at lower flue gas flow (500 Nm3 h−1 versus 1000 Nm3 h−1) generally produce less substituted PAHs, as well as SiO2 particulate matter and NOx, where the latter two parameters have a 99% correlation in this study.

Royal Society of Chemistry (RSC)

2023

Equilibrium Climate after Spectral and Bolometric Irradiance Reduction in Grand Solar Minimum Simulations

Tartaglione, Nazario; Toniazzo, Thomas; Otterå, Odd Helge; Orsolini, Yvan Joseph Georges Emile G.

In this study, we use the Whole Atmosphere Community Climate Model, forced by present-day atmospheric composition and coupled to a Slab Ocean Model, to simulate the state of the climate under grand solar minimum forcing scenarios. Idealized experiments prescribe time-invariant solar irradiance reductions that are either uniform (percentage-wise) across the total solar radiation spectrum (TOTC) or spectrally localized in the ultraviolet (UV) band (SCUV). We compare the equilibrium condition of these experiments with the equilibrium condition of a control simulation, forced by perpetual solar maximum conditions. In SCUV, we observe large stratospheric cooling due to ozone reduction. In both the Northern Hemisphere (NH) and the Southern Hemisphere (SH), this is accompanied by a weakening of the polar night jet during the cold season. In TOTC, dynamically induced polar stratospheric cooling is observed in the transition seasons over the NH, without any ozone deficit. The global temperature cooling values, compared with the control climate, are 0.55±0.03 K in TOTC and 0.39±0.03 K in SCUV. The reductions in total meridional heat transport outside of the subtropics are similar in the two experiments, especially in the SH. Despite substantial differences in stratospheric forcing, similarities exist between the two experiments, such as cloudiness; meridional heating transport in the SH; and strong cooling in the NH during wintertime, although this cooling affects two different regions, namely, North America in TOTC and the Euro–Asian continent in SCUV.

MDPI

2023

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