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 It is no longer being updated, so does not reliably reflect our current library holdings.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 #122433:

Stratospheric ClO and ozone from the Microwave Limb Sounder on the Upper Atmosphere Research Satellite / J.W. Waters, and 7 others.

Title: Stratospheric ClO and ozone from the Microwave Limb Sounder on the Upper Atmosphere Research Satellite / J.W. Waters, and 7 others.
Author(s): Waters, J. W.
Date: 1993.
In: Nature. (1993.), Vol. 362(6421) (1993)
Abstract: Reports concentrations of atmospheric ozone and ClO for both Arctic and Antarctic winters of past 18 months. Chlorine in lower stratosphere almost completely converted to chemically reactive forms in both northern and southern polar winter vortices. Over Antarctica, this occurred long before development of ozone hole suggesting that ozone loss can be masked by influx of ozone-rich air.
Notes:

Nature. Vol. 362(6421) :597-602 (1993).

Keywords: 551.510.534 -- Ozone layer.
551.510.532 -- Stratosphere.
546.214 -- Ozone.
629.783 -- Satellites: Upper Atmosphere Research Satellite (UARS).
D -- Atmospheric sciences.
(*2) -- Polar regions.
(*3) -- Arctic regions.
(*7) -- Antarctic regions.
SPRI record no.: 122433

MARCXML

LDR 01336naa#a2200000#a#4500
001 SPRI-122433
005 20231206121235.0
007 ta
008 231206s1993####xx#a##|##|###|0||#0|eng#d
035 ## ‡aSPRI-122433
040 ## ‡aUkCU-P‡beng‡eaacr
100 1# ‡aWaters, J. W.
245 10 ‡aStratospheric ClO and ozone from the Microwave Limb Sounder on the Upper Atmosphere Research Satellite /‡cJ.W. Waters, and 7 others.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1993.
300 ## ‡ap. 597-602 :‡bill., diags.
500 ## ‡aNature. Vol. 362(6421) :597-602 (1993).
520 3# ‡aReports concentrations of atmospheric ozone and ClO for both Arctic and Antarctic winters of past 18 months. Chlorine in lower stratosphere almost completely converted to chemically reactive forms in both northern and southern polar winter vortices. Over Antarctica, this occurred long before development of ozone hole suggesting that ozone loss can be masked by influx of ozone-rich air.
650 07 ‡a551.510.534 -- Ozone layer.‡2udc
650 07 ‡a551.510.532 -- Stratosphere.‡2udc
650 07 ‡a546.214 -- Ozone.‡2udc
650 07 ‡a629.783 -- Satellites: Upper Atmosphere Research Satellite (UARS).‡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
773 0# ‡7nnas ‡tNature. ‡gVol. 362(6421) (1993) ‡wSPRI-1046
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20231206