Publications

Evidence from firn air for recent decreases in non-methane hydrocarbons and a 20th century increase in nitrogen oxides in the northern hemisphere.

Worton, D.R.; Sturges, W.T.; Reeves, C.E.; Newland, M.J.; Penkett, S.A.; Atlas, E.; Stroud, V.; Johnson, K.; Schmidbauer, N.; Solberg, S.; Schwander, J.; Barnola, J.-M.

Living with a volcano. Scientific and operational aspects.

Bagni, M.; Bignami, C.; Bosi, V.; Buongiorno, F.; Costantini, L.; Faria, B.; Fonseca, J.; Hidayati, S.; Jenkins, S.; Jousset, P.; Le Cozannet, G.; Marchetti, E.; Oppenheimer, C.; Pereira, R.L.; Prata, F.; Ripepe, M.; Silva, F.; Spinetti, C.; Sumarti, S.; Surono, Vazao, T.

Monitoring of air and precipitation quality at Tjeldbergodden October 2009 - September 2010. NILU OR

Tønnesen, D.; Haugsbakk, I.

Occurrence and seasonality of cyclic volatile methyl siloxanes in Arctic air. NILU F

Krogseth, I.S.; Breivik, K.; Schlabach, M.; Kierkegaard, A.; McLachlan, M.S.; Hansen, K.M.

Rotational Raman scattering in the O2-A and O2-B bands: simulations for Carbonsat, FLEX/FLORIS, MERIS and OLCI. NILU OR

Kylling, A.

Rotational Raman scattering (RRS) causes filling-in of absorption lines in Earth shine spectra. It is routinely accounted for in analysis of UV and visible spectra measured both by satellite and ground-based instruments. RRS is also present at longer wavelengths, however, the magnitude generally decreases with increasing wavelength due to decrease in the scattering cross section. For high-resolution spectral measurements the effect may be noticeable. Depending on the application, RRS thus needs to be quantified and possibly corrected for. Of special interest is the effect of RRS in the O2-A (759-769 nm) and O2-B (686-697 nm) bands. Here, the effect of RRS in these bands is studied for the present and future satellite instruments CarbonSat, FLEX/FLORIS, MERIS and OLCI.

An expert assessment on climate change and health - with a European focus on lungs and allergies.

Forsberg, B.; Bråbäck, L.; Keune, H.; Kobernus, M.; von Krauss, M.K.; Yang, A.; Bartonova, A.

The roles of planetary and gravity waves during a major stratospheric sudden warming as characterized in WACCM.

Limpasuvan, v.; Richter, J.H.; Orsolini, Y.J.; Stordal, F.; Kvissel, O.-K.

Modelling of secondary aerosols in urban and rural areas of southwest Spain.

Milford, C.; Castell, N.; Marrero, C.; Sánchez de la Campa, A.; Fernández-Camacho, R.; Rodriguez, S.; De la Rosa, J.; Stein, A.

Transdisciplinary conceptual modeling of socio-ecological system.

Guimaraes, M.H.; Ballé-Béganton, J.; Bailly, D.; Newton, A.; Boski, T.; Dentinho, T.

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.

Uncertainty analysis of exposure assessment of selected PFASs in the PERFOOD. NILU F

Heinemeyer, G.; Klenow, S.; Dellatte, E.; Herzke, D.

The MEMORI dosimeter for indoor environment. NILU PP

Dahlin, E.; Grøntoft, T.; Lopez-Aparicio, S.; Bellendorf, P.; Wittstadt, Schieweck, A.; Drda-Kühn, K.; Perla Colombini, M.; Bonaduce, I.; Vandenabeele, P.; Larsen, R.; Poulsen Sommer, D.V.; Potthast, A.; Marincas, O.; Thickett, D.; Andrade, G.; Tabuenca, A.; Odlyha, M.; Hackney, S.; Laurenson, P.; McDonagh, C.; Ackerman, J.J.