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Fant 9759 publikasjoner. Viser side 98 av 391:

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Direct and indirect electron precipitation effect on nitric oxide during the April 2010 electron precipitation events, Part 1: Observations, Part 2: WACCM.

Tyssøy, H. N.; Smith-Johnsen, C.; Orsolini, Y.; Marsh, D. R.; Hendrickx, K.; Sandanger, M. I. J.; Ødegaard, L.-K. G.; Kishore Kumar, G.; Stordal, F.; Megner, L.

2017

Direct and indirect electron precipitation effect on nitric oxide in the polar middle atmosphere, using a full-range energy spectrum.

Smith-Johnsen, C.; Nesse Tyssøy, H.; Hendrickx, K.; Orsolini, Y.; Kishore Kumar, G.; Ødegaard, L.-K. G.; Sandanger, M. I.; Stordal, F.; Megner, L.

2017

Direct and indirect electron precipitation effect on nitric oxide, using a full range energy spectrum.

Smith-Johnsen, C.; Tyssøy, H. N.; Hendrickx, K.; Orsolini, Y.; Kishore Kumar, G.; Ødegaaard, L.-K. G.; Stordal, F.; Megner, L.

2017

Direct transport of midlatitude stratospheric ozone into the lower troposphere and marine boundary layer of the tropical Pacific Ocean.

Cooper, O.; Stohl, A.; Hübler, G.; Hsie, E.Y.; Parrish, D.D.; Tuck, A.F.; Kiladis, G.N.; Oltmans, S.J.; Johnson, B.J.; Shapiro, M.; Moody, J.L.; Lefohn, A.

2005

Direct validation of satellite-derived trends in tropospheric NO2 with ground-based MAX-DOAS instruments. NILU F

Schneider, P.; Stebel, K.; Pinardi, G.; van Roozendael, M.; Hendrick, F.; Kanaya, Y.

2014

Discounting the effect of meteorology on trends in surface ozone: Development of statistical tools

Solberg, Sverre; Walker, Sam-Erik; Schneider, Philipp; Guerreiro, Cristina; Colette, Augustin

This report presents the results using a statistical method to single out the influence of interannual meteorological variability on surface ozone. The reason for using such a tool is two-fold: Firstly, to explain the ozone levels in one specific year in terms of weather anomalies and secondly, to estimate the part of long-term ozone trends that is due to the meteorology alone. The method is a so-called GAM (generalized additive model), which could be regarded an advanced multiple regression method relating daily ozone levels to certain meteorological variables. The performance of the method was evaluated by comparing observed ozone data with those predicted by the GAM. This revealed a good to very good agreement in central Europe and Germany in particular. For southern Europe the performance was poorer. The method indicated that meteorology contributed to the downward trend in ozone seen at most sites for both 1990-2000 and 2000-2010.

ETC/ACM

2018

Discounting the impact of meteorology to the ozone concentration trends . ETC/ACM Technical Paper, 2015/9

Solberg, S.; Colette, A.; Bessagnet, B.; Réal, E.; Couvidat, F.; Guerreiro, C.

2015

Discrepancy between simulated and observed ethane and propane levels explained by underestimated fossil emissions

Dalsøren, Stig Bjørløw; Myhre, Gunnar; Hodnebrog, Øivind; Myhre, Cathrine Lund; Stohl, Andreas; Pisso, Ignacio; Schwietzke, Stefan; Höglund-Isaksson, Lena; Helmig, Detlev; Reimann, Stefan; Sauvage, Stéphane; Schmidbauer, Norbert; Read, Katie A.; Carpenter, Lucy J.; Lewis, Alastair C.; Punjabi, Shalini; Wallasch, Markus

2018

Discussion on the representativeness of current methodologies to assess indoor air quality

Vogt, Matthias; Hak, Claudia; Lopez-Aparicio, Susana; Dauge, Franck Rene; Holøs, Sverre Bjørn; Mysen, Mads

2018

Discussion on the representativeness of current methodologies to assess indoor air quality

Vogt, Matthias; Hak, Claudia; Lopez-Aparicio, Susana; Dauge, Franck Rene; Holøs, Sverre Bjørn; Yang, Aileen; Mysen, Mads

2018

Disentangling Aerosol and Cloud effects on Dimming and Brightening in Observations and CMIP6

Julsrud, Ingeborg Rian; Storelvmo, Trude; Schulz, Michael; Moseid, Kine Onsum; Wild, Martin

Periods of dimming and brightening have been recorded in observational datasets of surface solar radiation (SSR) between the mid-20th century and present day. Atmospheric components affect SSR, including aerosols and clouds, though studies disagree somewhat about the relative effect of each component in different regions. Current Earth system models (ESMs) are unable to simulate observed trends in SSR. This study includes an investigation into observed SSR variations between 1961 and 2014 and an evaluation of the effects of cloud cover variations and impacts of aerosol extinction, using timeseries of SSR and cloud cover from in-situ measurements. Historical simulations by 42 ESMs participating in the Coupled Model Intercomparison Project Phase 6 (CMIP6) have also been studied and compared to observations. The observational study indicates that cloud cover has had a dampening effect on the variations of SSR and that emissions of aerosol and aerosol precursors are the main cause of the general trends in observed SSR in four regions—China, Japan, Europe and the United States—during 1961-2014. The study of simulated SSR in CMIP6 yields the conclusion that current ESMs remain unable to simulate the magnitude of observed dimming and brightening in China, Japan and the United States, but that the European SSR trends between 1961 and 2014 are fairly well reproduced in the ESMs. A rough quantification of the regional surface radiation extinction efficiency of aerosol and precursor emissions in the simulations is found to agree with observed values in Europe, but not in the other three regions.

American Geophysical Union (AGU)

2022

Dispersion models. NILU F

Sivertsen, B.

2002

Disposition of PCB during the winter emaciation of the anadromous Arctic char.

Foshaug, H.; Jørgensen, E.H.; Plotitsyna, N.; Burkow, I.

2000

Disse miljøgiftene fant forskerne igjen i de ville dyrene

Solbakken, Christine Forsetlund

Norges forskningsråd

2024

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