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Record #104479:
- #104479
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MARC recordVisible and near-ultraviolet spectroscopy at McMurdo Station, Antarctica. 7. OClO diurnal photochemistry and implications for ozone destruction / S. Solomon, R.W. Sanders, H.L. Miller, Jr.
| Title: | Visible and near-ultraviolet spectroscopy at McMurdo Station, Antarctica. 7. OClO diurnal photochemistry and implications for ozone destruction / S. Solomon, R.W. Sanders, H.L. Miller, Jr. |
| Author(s): | Solomon, S. Sanders, R. W. Miller, H. L., |
| Date: | 1990. |
| In: | Journal of Geophysical Research. (1990.), Vol. 95(D9) (1990) |
| Abstract: | Observations of the ratio between the change in slant column abundance of OClO and that of ozone as a function of solar zenith used to deduce the diurnal cycle of the daytime OClO column abundance above Antarctica during 1987. This approach effectively normalises other factors such as air mass factor changes and allows study of the photochemical variations of OClO during twilight. |
| Notes: | Journal of Geophysical Research. Vol. 95(D9) :13, 807-13, 817 (1990). |
| Keywords: | 551.510.534 -- Ozone layer. 551.510.41 -- Atmosphere, chemical properties. 551.508.95 -- Atmosphere, measurement of composition. 551.521.6 -- Radiation of special wave lengths. D -- Atmospheric sciences. (*7) -- Antarctic regions. (*764) -- Ross Island. |
| SPRI record no.: | 104479 |
LDR 01500naa#a2200000#a#4500 001 SPRI-104479 005 20230323104723.0 007 ta 008 230323s1990####xx#a##|##|###|0||#0|eng#d 035 ## ‡aSPRI-104479 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aSolomon, S. 245 10 ‡aVisible and near-ultraviolet spectroscopy at McMurdo Station, Antarctica. 7. OClO diurnal photochemistry and implications for ozone destruction /‡cS. Solomon, R.W. Sanders, H.L. Miller, Jr. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1990. 300 ## ‡ap. 13, 807-13, 817 :‡bdiags., tables. 500 ## ‡aJournal of Geophysical Research. Vol. 95(D9) :13, 807-13, 817 (1990). 520 3# ‡aObservations of the ratio between the change in slant column abundance of OClO and that of ozone as a function of solar zenith used to deduce the diurnal cycle of the daytime OClO column abundance above Antarctica during 1987. This approach effectively normalises other factors such as air mass factor changes and allows study of the photochemical variations of OClO during twilight. 650 07 ‡a551.510.534 -- Ozone layer.‡2udc 650 07 ‡a551.510.41 -- Atmosphere, chemical properties.‡2udc 650 07 ‡a551.508.95 -- Atmosphere, measurement of composition.‡2udc 650 07 ‡a551.521.6 -- Radiation of special wave lengths.‡2udc 650 07 ‡aD -- Atmospheric sciences.‡2local 651 #7 ‡a(*7) -- Antarctic regions.‡2udc 651 #7 ‡a(*764) -- Ross Island.‡2udc 700 1# ‡aSanders, R. W. 700 1# ‡aMiller, H. L.,‡cJr. 773 0# ‡7nnas ‡tJournal of Geophysical Research. ‡gVol. 95(D9) (1990) ‡wSPRI-35252 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20230323