Publikasjoner

NILU instruments at ALOMAR: Status and scientific results 2003. NILU F

Hansen, G.; Edvardsen, K.; Stebel, K.; Tørnkvist, K.K.

NILU i Arktis og Antarktis. NILU F

Lunder, C.R.; Aas, W.; Myhre, C.L.; Bohlin-Nizzetto, P.; Tørseth, K.; Stohl, A.; Fiebig, M.; Yttri, K.E.; Eckhardt, S.; Pfaffhuber, K.A.; Edvardsen, K.; Hansen, G.; Kallenborn, R.; Stebel, K.; Hermansen, O.; Bäcklund, A.; Wasseng, J.H.; Schmidbauer, N.

NILU contribution to ESA CCI Soil Moisture: Use of data assimilation to add value to soil moisture datasets. NILU F

Lahoz, W.

NILU as National Reference Laboratory for ambient air quality. NILU F

Tørnkvist, K.

NILU / GMES projekt. Powerpointpresentasjon. NILU F

Holmén, K.

NILU – Making a difference for the environment

Solbakken, Christine Forsetlund

NILU - viktig for miljøet.

Braathen, O.A.

NILU - en introduksjon.

Solbakken, C.F.

Nikolaos Evangeliou : « L’idéal serait d’interdire l’utilisation des voitures »

Evangeliou, Nikolaos (intervjuobjekt); Brun, Raphael (journalist)

Nighttime secondary ozone layer during major stratospheric sudden warmings in specified-dynamics WACCM. NILU F

Orsolini, Y.; Tweedy, O.; Limpasuvan, V.; Randall, C.; Smith, A.; Garcia, R.; Chandran, A.; Harvey, L.

Nighttime mesospheric ozone enhancements during the 2002 southern hemispheric major stratospheric warming

Smith-Johnsen, Christine; Orsolini, Yvan; Stordal, Frode; Limpasuvan, Varavut; Pérot, Kristell

Sudden Stratospheric Warmings (SSW) affect the chemistry and dynamics of the middle atmosphere. Major warmings occur roughly every second winter in the Northern Hemisphere (NH), but has only been observed once in the Southern Hemisphere (SH), during the Antarctic winter of 2002. Observations by the Global Ozone Monitoring by Occultation of Stars (GOMOS, an instrument on board Envisat) during this rare event, show a 40% increase of ozone in the nighttime secondary ozone layer at subpolar latitudes compared to non-SSW years. This study investigates the cause of the mesospheric nighttime ozone increase, using the National Center for Atmospheric Research (NCAR) Whole Atmosphere Community Climate Model with specified dynamics (SD-WACCM). The 2002 SH winter was characterized by several reductions of the strength of the polar night jet in the upper stratosphere before the jet reversed completely, marking the onset of the major SSW. At the time of these wind reductions, corresponding episodic increases can be seen in the modelled nighttime secondary ozone layer. This ozone increase is attributed largely to enhanced upwelling and the associated cooling of the altitude region in conjunction with the wind reversal. This is in correspondence to similar studies of SSW induced ozone enhancements in NH. But unlike its NH counterpart, the SH secondary ozone layer appeared to be impacted less by episodic variations in atomic hydrogen. Seasonally decreasing atomic hydrogen plays however a larger role in SH compared to NH.

Elsevier

New technologies using trace metals of concern. Strüngmann Forum Reports, 16

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