Scott Polar Research InstituteSPRI library catalogue
Search the catalogue
Browse recordsView 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 It is no longer being updated, so does not reliably reflect our current library holdings.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 #88539:
- #88539
Main publication details
MARC recordHigh concentrations of chlorine monoxide at low altitudes in the Antarctic spring stratosphere: secular variation / P.M. Solomon, B. Connor, R.L. de Zafra, A. Parrish, J. Barrett, M. Jaramillo.
| Title: | High concentrations of chlorine monoxide at low altitudes in the Antarctic spring stratosphere: secular variation / P.M. Solomon, B. Connor, R.L. de Zafra, A. Parrish, J. Barrett, M. Jaramillo. |
| Author(s): | Solomon, P. M. Connor, B. Zafra, R. L. de. Parrish, A. Barrett, J. Jaramillo, M. |
| Date: | 1987. |
| In: | Nature. (1987.), Vol. 328(6127) (1987) |
| Abstract: | Shows that ClO concentration declines during latter half of September and disappears by early October. As ClO is directly involved in catalytic ozone destruction cycle, these observations suggest that ozone hole is caused by chemical depletion mechanism which operates in early spring. |
| Notes: | Nature. Vol. 328(6127) :411-413 (1987). |
| Keywords: | 551.510.534 -- Ozone layer. 551.510.41 -- Atmosphere, chemical properties. 551.510.532 -- Stratosphere. D -- Atmospheric sciences. (*7) -- Antarctic regions. |
| SPRI record no.: | 88539 |
LDR 01274naa#a2200000#a#4500 001 SPRI-88539 005 20230329083122.0 007 ta 008 230329s1987####xx#a##|##|###|0||#0|eng#d 035 ## ‡aSPRI-88539 040 ## ‡aUkCU-P‡beng‡eaacr 245 00 ‡aHigh concentrations of chlorine monoxide at low altitudes in the Antarctic spring stratosphere :‡bsecular variation /‡cP.M. Solomon, B. Connor, R.L. de Zafra, A. Parrish, J. Barrett, M. Jaramillo. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1987. 300 ## ‡ap. 411-413 :‡bdiags. 500 ## ‡aNature. Vol. 328(6127) :411-413 (1987). 520 3# ‡aShows that ClO concentration declines during latter half of September and disappears by early October. As ClO is directly involved in catalytic ozone destruction cycle, these observations suggest that ozone hole is caused by chemical depletion mechanism which operates in early spring. 650 07 ‡a551.510.534 -- Ozone layer.‡2udc 650 07 ‡a551.510.41 -- Atmosphere, chemical properties.‡2udc 650 07 ‡a551.510.532 -- Stratosphere.‡2udc 650 07 ‡aD -- Atmospheric sciences.‡2local 651 #7 ‡a(*7) -- Antarctic regions.‡2udc 700 1# ‡aSolomon, P. M. 700 1# ‡aConnor, B. 700 1# ‡aZafra, R. L. de. 700 1# ‡aParrish, A. 700 1# ‡aBarrett, J. 700 1# ‡aJaramillo, M. 773 0# ‡7nnas ‡tNature. ‡gVol. 328(6127) (1987) ‡wSPRI-1046 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20230329