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Record #34512:
Antarctic stratospheric circulation and ozone observations / W.B. Moreland.
Title: | Antarctic stratospheric circulation and ozone observations / W.B. Moreland. |
Author(s): | Moreland, W. B. |
Date: | 1960. |
Publisher: | New York: Pergamon Press, Symposium Publications Division, on behalf of the Director of Meteorology, Melbourne, Australia |
In: | Antarctic meteorology : proceedings of the symposium held in Melbourne, February 1959. (1960.), |
Abstract: | Evidence based upon short-term records indicate that the wintertime thermal structure of the stratosphere is controlled primarily by Infrared radiative processes and secondarily by dynamic processes of advection and vertical motion. Springtime maximum ozone values are related to rapid transformation of stratospheric circulation. |
Notes: | In: Antarctic meteorology : proceedings of the symposium held in Melbourne, February 1959 / Commonwealth of Australia. Bureau of Meteorology. |
Keywords: | 551.5 -- Meteorology. 551.510.532 -- Stratosphere. 551.510.534 -- Ozone layer. D -- Atmospheric sciences. (*7) -- Antarctic regions. |
SPRI record no.: | 34512 |
LDR 01528naa#a2200000#a#4500 001 SPRI-34512 005 20240328084922.0 007 ta 008 240328s1960####nyub###|#####|0||#0#eng#d 035 ## ‡aSPRI-34512 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aMoreland, W. B. 245 10 ‡aAntarctic stratospheric circulation and ozone observations /‡cW.B. Moreland. 260 ## ‡aNew York :‡bPergamon Press, Symposium Publications Division, on behalf of the Director of Meteorology, Melbourne, Australia,‡c1960. 300 ## ‡ap. 394- 409 :‡btable, graphs, maps. 500 ## ‡aIn: Antarctic meteorology : proceedings of the symposium held in Melbourne, February 1959 / Commonwealth of Australia. Bureau of Meteorology. 520 3# ‡aEvidence based upon short-term records indicate that the wintertime thermal structure of the stratosphere is controlled primarily by Infrared radiative processes and secondarily by dynamic processes of advection and vertical motion. Springtime maximum ozone values are related to rapid transformation of stratospheric circulation. 650 07 ‡a551.5 -- Meteorology.‡2udc 650 07 ‡a551.510.532 -- Stratosphere.‡2udc 650 07 ‡a551.510.534 -- Ozone layer.‡2udc 650 07 ‡aD -- Atmospheric sciences.‡2local 651 #7 ‡a(*7) -- Antarctic regions.‡2udc 773 0# ‡7c2am ‡aCommonwealth of Australia. Bureau of Meteorology. ‡tAntarctic meteorology : proceedings of the symposium held in Melbourne, February 1959. ‡dNew York : Pergamon Press, Symposium Publications Division, on behalf of the Director of Meteorology, Melbourne, Australia, 1960. ‡wSPRI-34227 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20240328