Chemical depletion of Arctic ozone in winter 1999/2000 (Articolo in rivista)

Type
Label
  • Chemical depletion of Arctic ozone in winter 1999/2000 (Articolo in rivista) (literal)
Anno
  • 2002-01-01T00:00:00+01:00 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
  • 10.1029/2001JD000533 (literal)
Alternative label
  • Rex M, Salawitch RJ, Harris NRP, von der Gathen P, Braathen GO, Schulz A, Deckelmann H, Chipperfield M, Sinnhuber BM, Reimer E, Alfier R, Bevilacqua R, Hoppel K, Fromm M, Lumpe J, Kullmann H, Kleinbohl A, Bremer H, von Konig M, Kunzi K, Toohey D, Vomel H, Richard, E (Richard, E); Aikin, K (Aikin, K); Jost, H (Jost, H); Greenblatt, JB (Greenblatt, JB); Loewenstein, M (Loewenstein, M); Podolske, JR (Podolske, JR); Webster, CR (Webster, CR); Flesch, GJ (Flesch, GJ); Scott, DC (Scott, DC); Herman, RL (Herman, RL); Elkins, JW (Elkins, JW); Ray, EA (Ray, EA); Moore, FL (Moore, FL); Hurst, DF (Hurst, DF); Romashkin, P (Romashkin, P); Toon, GC (Toon, GC); Sen, B (Sen, B); Margitan, JJ (Margitan, JJ); Wennberg, P (Wennberg, P); Neuber, R (Neuber, R); Allart, M (Allart, M); Bojkov, BR (Bojkov, BR); Claude, H (Claude, H); Davies, J (Davies, J); Davies, W (Davies, W); De Backer, H (De Backer, H); Dier, H (Dier, H); Dorokhov, V (Dorokhov, V); Fast, H (Fast, H); Kondo, Y (Kondo, Y); Kyro, E (Kyro, E); Litynska, Z (Litynska, Z); Mikkelsen, IS (Mikkelsen, IS); Molyneux, MJ (Molyneux, MJ); Moran, E (Moran, E); Nagai, T (Nagai, T); Nakane, H (Nakane, H); Parrondo, C (Parrondo, C); Ravegnani, F (Ravegnani, F); Skrivankova, P (Skrivankova, P); Viatte, P (Viatte, P); Yushkov, V (Yushkov, V) (2002)
    Chemical depletion of Arctic ozone in winter 1999/2000
    in Journal of Geophysical Research: Atmospheres
    (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
  • Rex M, Salawitch RJ, Harris NRP, von der Gathen P, Braathen GO, Schulz A, Deckelmann H, Chipperfield M, Sinnhuber BM, Reimer E, Alfier R, Bevilacqua R, Hoppel K, Fromm M, Lumpe J, Kullmann H, Kleinbohl A, Bremer H, von Konig M, Kunzi K, Toohey D, Vomel H, Richard, E (Richard, E); Aikin, K (Aikin, K); Jost, H (Jost, H); Greenblatt, JB (Greenblatt, JB); Loewenstein, M (Loewenstein, M); Podolske, JR (Podolske, JR); Webster, CR (Webster, CR); Flesch, GJ (Flesch, GJ); Scott, DC (Scott, DC); Herman, RL (Herman, RL); Elkins, JW (Elkins, JW); Ray, EA (Ray, EA); Moore, FL (Moore, FL); Hurst, DF (Hurst, DF); Romashkin, P (Romashkin, P); Toon, GC (Toon, GC); Sen, B (Sen, B); Margitan, JJ (Margitan, JJ); Wennberg, P (Wennberg, P); Neuber, R (Neuber, R); Allart, M (Allart, M); Bojkov, BR (Bojkov, BR); Claude, H (Claude, H); Davies, J (Davies, J); Davies, W (Davies, W); De Backer, H (De Backer, H); Dier, H (Dier, H); Dorokhov, V (Dorokhov, V); Fast, H (Fast, H); Kondo, Y (Kondo, Y); Kyro, E (Kyro, E); Litynska, Z (Litynska, Z); Mikkelsen, IS (Mikkelsen, IS); Molyneux, MJ (Molyneux, MJ); Moran, E (Moran, E); Nagai, T (Nagai, T); Nakane, H (Nakane, H); Parrondo, C (Parrondo, C); Ravegnani, F (Ravegnani, F); Skrivankova, P (Skrivankova, P); Viatte, P (Viatte, P); Yushkov, V (Yushkov, V) (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume
  • 107 (literal)
Rivista
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroFascicolo
  • D20 (literal)
Note
  • ISI Web of Science (WOS) (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
  • Alfred Wegener Inst Polar & Marine Res, D-14401 Potsdam, Germany CALTECH, Jet Prop Lab, Pasadena, CA 91109 USA Univ Cambridge, European Ozone Res Coordinating Unit, Cambridge CB2 1HE, England Norsk Inst Luftforskning, N-2007 Kjeller, Norway Univ Leeds, Leeds LS2 9JT, W Yorkshire, England Free Univ Berlin, Inst Meteorol, D-12165 Berlin, Germany USN, Res Lab, Washington, DC 20375 USA Computat Phys Inc, Springfield, VA 22151 USA Univ Bremen, Inst Environm Phys, D-28334 Bremen, Germany Univ Colorado, Program Atmospher & Ocean Sci, Boulder, CO 80309 USA Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO 80309 USA NOAA, Boulder, CO 80303 USA NASA, Ames Res Ctr, Moffett Field, CA 94035 USA CALTECH, Div Geol & Planetary Sci, Pasadena, CA 91125 USA KNMI, NL-3730 AE De Bilt, Netherlands Deutscher Wetterdienst, Observ Hohenpeissenberg, D-82383 Hohenpeissenberg, Germany Atmospher Environm Serv, Toronto, ON M3H 5T4, Canada Univ Wales, Dept Phys, Aberystwyth SY23 3BZ, Dyfed, Wales Royal Meteorol Inst Belgium, B-1180 Brussels, Belgium Meteorol Observ Lindenberg, D-15864 Lindenberg, Germany CAO, Dolgoprudnyi 141700, Russia Nagoya Univ, Solar Terr Environm Lab, Toyokawa, Aichi, Japan Sodankyla Meteorol Observ, Sodankyla, Finland Ctr Aerol, Legionowo, Poland Danish Meteorol Inst, DK-2100 Copenhagen, Denmark UK Met Off, Bracknell RG11 2SZ, Berks, England IMS, Valentia Observ, Kerry, Ireland Meteorol Res Inst, Tsukuba, Ibaraki 3050052, Japan Natl Inst Environm Studies, Tsukuba, Ibaraki 3050053, Japan INTA, Madrid, Spain CNR, Ist Fisbat, I-40126 Bologna, Italy Czech Hydromet Inst, Prague 14306, Czech Republic SMI, CH-1530 Payerne, Switzerland (literal)
Titolo
  • Chemical depletion of Arctic ozone in winter 1999/2000 (literal)
Abstract
  • During Arctic winters with a cold, stable stratospheric circulation, reactions on the surface of polar stratospheric clouds (PSCs) lead to elevated abundances of chlorine monoxide (ClO) that, in the presence of sunlight, destroy ozone. Here we show that PSCs were more widespread during the 1999/2000 Arctic winter than for any other Arctic winter in the past two decades. We have used three fundamentally different approaches to derive the degree of chemical ozone loss from ozonesonde, balloon, aircraft, and satellite instruments. We show that the ozone losses derived from these different instruments and approaches agree very well, resulting in a high level of confidence in the results. Chemical processes led to a 70% reduction of ozone for a region similar to1 km thick of the lower stratosphere, the largest degree of local loss ever reported for the Arctic. The Match analysis of ozonesonde data shows that the accumulated chemical loss of ozone inside the Arctic vortex totaled 117 +/- 14 Dobson units (DU) by the end of winter. This loss, combined with dynamical redistribution of air parcels, resulted in a 88 +/- 13 DU reduction in total column ozone compared to the amount that would have been present in the absence of any chemical loss. The chemical loss of ozone throughout the winter was nearly balanced by dynamical resupply of ozone to the vortex, resulting in a relatively constant value of total ozone of 340 +/- 50 DU between early January and late March. This observation of nearly constant total ozone in the Arctic vortex is in contrast to the increase of total column ozone between January and March that is observed during most years. (literal)
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