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Found 10083 publications. Showing page 143 of 404:

Publication  
Year  
Category

Nitrous oxide emissions 1999 to 2009 from a global atmospheric inversion.

Thompson, R.L.; Chevallier, F.; Crotwell, A.M.; Dutton, G.; Langenfelds, R.L.; Prinn, R.G.; Weiss, R.F.; Tohjima, Y.; Nakazawa, T.; Krummel, P.B.; Steele, L.P.; Fraser, P.; Ishijima, K.; Aoki, S.

2014

Nitrous oxide emission from North America based on bottom-up and top-down approaches: trends, drivers, and comparison

Xu, Rongting; Tian, Hanqin; Thompson, Rona Louise; Canadell, Josep G.; Team, * GCP/INI Synthesis

2019

Nitrogen: den ukjente klimatrusselen

Tørseth, Kjetil; Austnes, Kari (interview subjects); Høseggen, Simen (journalist)

2019

Nitrogen oxides.

Lövblad, G.; Tarrasón, L.; Tørseth, K.

2004

Nitrogen fertilisers are incredibly efficient, but they make climate change a lot worse

Canadell, P.; Tian, Hanqin; Patra, Prabir; Thompson, Rona Louise

2020

Nitrogen as a threat to European air quality.

Moldanova, J.; Grennfelt, P.; Jonsson, Å.; Simpson, D.; Spranger, T.; Aas, W.; Munthe, J.; Rabl, A.

2011

Nitrogen and biodiversity.

Fowler, D.; Wright, D.; de Wit, H.; Tørseth, K.; Mareckova, K.; LeGall, A.-C.; Rabago, I.; Hettelingh, J.-P.; Almodovar, P.; Scavo, K.; Haeuber, R.; Lynch, J.; Funk, C.; Kerr, K.; Berton, E.; Pritula, D.; Reiss, I.

2016

Nitric oxide response to the April 2010 electron precipitation event: Using WACCM and WACCM-D with and without medium-energy electrons

Smith-Johnsen, Christine; Marsh, Daniel R.; Orsolini, Yvan; Tyssøy, Hilde Nesse; Hendrickx, Koen; Sandanger, Marit Irene J.; Ødegaard, Linn-Kristine Glesnes; Stordal, Frode

Energetic electrons from the magnetosphere deposit their energy in the atmosphere and lead to production of nitric oxide (NO) in the mesosphere and lower thermosphere. We study the atmospheric NO response to a geomagnetic storm in April 2010 with WACCM (Whole Atmosphere Community Climate Model). Modeled NO is compared to observations by Solar Occultation For Ice Experiment/Aeronomy of Ice in the Mesosphere at 72–82°S latitudes. We investigate the modeled NOs sensitivity to changes in energy and chemistry. The electron energy model input is either a parameterization of auroral electrons or a full range energy spectrum (1–750 keV) from National Oceanic and Atmospheric Administration/Polar Orbiting Environmental Satellites and European Organisation for the Exploitation of Meteorological Satellites/Meteorological Operational satellites. To study the importance of ion chemistry for the production of NO, WACCM‐D, which has more complex ion chemistry, is used. Both standard WACCM and WACCM‐D underestimate the storm time NO increase in the main production region (90–110 km), using both electron energy inputs. At and below 80 km, including medium‐energy electrons (>30 keV) is important both for NO directly produced at this altitude region and for NO transported from other regions (indirect effect). By using WACCM‐D the direct NO production is improved, while the indirect effects on NO suffer from the downward propagating deficiency above. In conclusion, both a full range energy spectrum and ion chemistry is needed throughout the mesosphere and lower thermosphere region to increase the direct and indirect contribution from electrons on NO.

2018

Nitric oxide response to the April 2010 electron precipitation event - using WACCM and WACCM-D with and without medium energy electrons

Smith-Johnsen, Christine; Marsh, Daniel R.; Orsolini, Yvan; Tyssøy, Hilde Nesse; Hendrickx, Koen; Sandanger, Marit Irene J.; Ødegaard, Linn-Kristine Glesnes; Stordal, Frode

2018

Nitric oxide response to the April 2010 electron precipitation event

Smith-Johnsen, Christine; Marsh, Daniel R.; Orsolini, Yvan; Tyssøy, Hilde Nesse; Sandanger, Marit Irene J.; Ødegaard, Linn-Kristine Glesnes; Stordal, Frode

2018

Nitric oxide produced by energetic electron precipitation during a geomagnetic storm in April 2010.

Smith-Johnsen, C.; Tyssøy, H.N.; Ødegaard, L.-C. G.; Stordal, F.; Orsolini, Y.; Hendricks, K.; Megner, L.

2015

Nitric acid phase partitioning and cycling in the New England coastal atmosphere.

Fischer, E.; Pszenny, A.; Keene, W.; Maben, J.; Smith, A.; Stohl, A.; Talbot, R.

2006

Nitrate dry deposition in Svalbard.

Björkman, M.P.; Kühnel, R.; Partridge, D.G.; Roberts, T.J.; Aas, W.; Mazzola, M.; Viola, A.; Hodson, A.; Ström, J.; Isaksson, E.

2013

NILUs SIS-er for 2016-2019.

Solbakken, C.F.

2016

NILUs aktiviteter knyttet til stråling, partikler og isskyer i Arktiske områder. NILU F

Svendby, T.; Schaug, J.; Stebel, K.; Myhre, C.L.

2005

NILU’s Environmental Management Report 2018

Braathen, Ole-Anders; Marsteen, Leif; Langholen, Trine; Andresen, Eva Beate; Fjeldstad, Heidi

One of NILU’s main goals is to study the impact of pollution and supply decision-makers with a sound scientific platform for choosing measures to reduce the negative impacts. Furthermore, it is very important for the institute to have control of the impact the institute’s own activities may have on the environment and to reduce negative impacts as far as possible.

NILU has for many years been working to improve the status of the environment and to reduce negative impacts. In order to
take this one step further, it was decided that the institute should restructure the work according to a relevant environmental standard and to seek certification according to the same standard.

The chosen standard is ISO 14001 (Environmental management systems—Requirements with guidance for use) and NILU
achieved certification according to this standard in October 2010. This report summarizes the results of the system in 2018.

NILU

2019

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