skip to primary navigation skip to content
 

 

You are not currently logged in

SPRI library catalogue

View a record

Please note: You are viewing the legacy database of the Scott Polar Research Institute Library catalogue. It is no longer being updated, so does not reliably reflect our current library holdings.

Please search for material in iDiscover for up-to-date information about the library collection.


Record #172382:

Dynamical control of NH and SH winter/spring total ozone from GOME observations in 1995-2002 / M. Weber, S. Dhomse, F. Wittrock, A. Richter, B.-M. Sinnhuber, J.P. Burrows.

Title: Dynamical control of NH and SH winter/spring total ozone from GOME observations in 1995-2002 / M. Weber, S. Dhomse, F. Wittrock, A. Richter, B.-M. Sinnhuber, J.P. Burrows.
Author(s): Weber, M.
Dhomse, S.
Wittrock, F.
Richter, A.
Sinnhuber, B. -M.
Burrows, J. P.
Date: 2003.
In: Geophysical Research Letters. (2003.), Vol. 30(11) (2003)
Abstract: Examines interannual variability in total ozone and chlorine activation as measured by Global Ozone Monitoring Experiment (GOME) combining data from northern (NH) and southern (SH) hemispheres. Abnormal high wave activity in austral spring 2002 led to first observation of major stratospheric warming in SH, resulting in net winter increase of mid- to high latitude total ozone until September 2002. In previous years chemical ozone depletion inside Antarctic vortex was sufficiently high to reduce mean total ozone south of 50° in September to values slightly below that of March as observed by GOME during period 1995-2001. Absolute winter eddy heat flux between 43° and 70° latitudes at 100 hPa correlates extremely well with spring-to-autumn ratio of total ozone polewards of 50° and anti-correlates with winter integrated maximum OClO column amounts using this combined data set. Unusual ozone ratio for austral winter/spring 2002 lies almost midway between typical values for Antarctica and those for recent cold Arctic winter/spring seasons.
Notes:

Geophysical Research Letters. Vol. 30(11) :1583/1-4 (2003).

Keywords: 551.5 -- Meteorology.
551.51 -- Atmosphere. Structure, mechanics and thermodynamics.
551.510.5 -- Atmosphere, structure.
551.510.534 -- Ozone layer.
551.510.41 -- Atmosphere, chemical properties.
551.513 -- Atmosphere, general circulation.
551.510.52 -- Troposphere.
551.510.532 -- Stratosphere.
546.13 -- Chlorine.
546.214 -- Ozone.
001.89 -- Research programmes: Global Ozone Monitoring Experiment (GOME).
D -- Atmospheric sciences.
(*2) -- Polar regions.
(*3) -- Arctic regions.
(*7) -- Antarctic regions.
SPRI record no.: 172382

MARCXML

LDR 02666naa#a2200000#a#4500
001 SPRI-172382
005 20240328185558.0
007 ta
008 240328s2003####xx####|##|###|0||#0|eng#d
035 ## ‡aSPRI-172382
040 ## ‡aUkCU-P‡beng‡eaacr
245 00 ‡aDynamical control of NH and SH winter/spring total ozone from GOME observations in 1995-2002 /‡cM. Weber, S. Dhomse, F. Wittrock, A. Richter, B.-M. Sinnhuber, J.P. Burrows.
260 ## ‡a[S.l.] :‡b[s.n.],‡c2003.
300 ## ‡ap. 1583/1-4.
500 ## ‡aGeophysical Research Letters. Vol. 30(11) :1583/1-4 (2003).
520 3# ‡aExamines interannual variability in total ozone and chlorine activation as measured by Global Ozone Monitoring Experiment (GOME) combining data from northern (NH) and southern (SH) hemispheres. Abnormal high wave activity in austral spring 2002 led to first observation of major stratospheric warming in SH, resulting in net winter increase of mid- to high latitude total ozone until September 2002. In previous years chemical ozone depletion inside Antarctic vortex was sufficiently high to reduce mean total ozone south of 50° in September to values slightly below that of March as observed by GOME during period 1995-2001. Absolute winter eddy heat flux between 43° and 70° latitudes at 100 hPa correlates extremely well with spring-to-autumn ratio of total ozone polewards of 50° and anti-correlates with winter integrated maximum OClO column amounts using this combined data set. Unusual ozone ratio for austral winter/spring 2002 lies almost midway between typical values for Antarctica and those for recent cold Arctic winter/spring seasons.
530 ## ‡aAlso issued online ‡uurn:doi:10.1029/2002GL016799‡uhttps://dx.doi.org/10.1029/2002GL016799
650 07 ‡a551.5 -- Meteorology.‡2udc
650 07 ‡a551.51 -- Atmosphere. Structure, mechanics and thermodynamics.‡2udc
650 07 ‡a551.510.5 -- Atmosphere, structure.‡2udc
650 07 ‡a551.510.534 -- Ozone layer.‡2udc
650 07 ‡a551.510.41 -- Atmosphere, chemical properties.‡2udc
650 07 ‡a551.513 -- Atmosphere, general circulation.‡2udc
650 07 ‡a551.510.52 -- Troposphere.‡2udc
650 07 ‡a551.510.532 -- Stratosphere.‡2udc
650 07 ‡a546.13 -- Chlorine.‡2udc
650 07 ‡a546.214 -- Ozone.‡2udc
650 07 ‡a001.89 -- Research programmes: Global Ozone Monitoring Experiment (GOME).‡2udc
650 07 ‡aD -- Atmospheric sciences.‡2local
651 #7 ‡a(*2) -- Polar regions.‡2udc
651 #7 ‡a(*3) -- Arctic regions.‡2udc
651 #7 ‡a(*7) -- Antarctic regions.‡2udc
700 1# ‡aWeber, M.
700 1# ‡aDhomse, S.
700 1# ‡aWittrock, F.
700 1# ‡aRichter, A.
700 1# ‡aSinnhuber, B. -M.
700 1# ‡aBurrows, J. P.
773 0# ‡7nnas ‡tGeophysical Research Letters. ‡gVol. 30(11) (2003) ‡wSPRI-1033
916 ## ‡a2005/10/18 -- HS
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20240328 ‡bHS