Stratospheric effects of 27-day solar ultraviolet variations: The column ozone response and comparisons of solar cycles 21 and 22

Two unresolved observational issues concerning the response of stratospheric ozone to 27-day solar ultraviolet variations are as follows: (1) the amplitude of the column ozone response and whether it is consistent with the predictions of current two-dimensional stratospheric models and (2) whether t...

Full description

Bibliographic Details
Main Authors: Hood, L. L., Zhou, S.
Other Authors: Univ Arizona, Lunar & Planetary Lab
Language:en
Published: AMER GEOPHYSICAL UNION 1999
Online Access:http://hdl.handle.net/10150/624008
http://arizona.openrepository.com/arizona/handle/10150/624008
id ndltd-arizona.edu-oai-arizona.openrepository.com-10150-624008
record_format oai_dc
spelling ndltd-arizona.edu-oai-arizona.openrepository.com-10150-6240082017-06-09T03:00:32Z Stratospheric effects of 27-day solar ultraviolet variations: The column ozone response and comparisons of solar cycles 21 and 22 Hood, L. L. Zhou, S. Univ Arizona, Lunar & Planetary Lab Two unresolved observational issues concerning the response of stratospheric ozone to 27-day solar ultraviolet variations are as follows: (1) the amplitude of the column ozone response and whether it is consistent with the predictions of current two-dimensional stratospheric models and (2) whether the ozone profile response in the upper stratosphere differed appreciably during the solar cycle 22 maximum period (around 1990) as compared with the solar cycle 21 maximum period (around 1980). To investigate these issues, two separate 4-year intervals (1979–1982 and 1989–1992) of daily zonal mean Nimbus 7 Total Ozone Mapping Spectrometer, Nimbus 7 solar backscattered ultraviolet (SBUV), and/or NOAA 11 SBUV/2 data for tropical latitudes (30°S to 30°N) are analyzed using cross correlation and cross-spectral and regression methods. The Mg II core-to-wing ratio is employed as a measure of solar UV variations near 200 nm. Results show that the mean tropical column ozone sensitivity (percent change of ozone for a 1% change in solar flux) is 0.09±0.01 at a lag of 4–6 days during both intervals and is approximately consistent with model predictions. Ozone profile sensitivities and phase lags are also in agreement between the two 4-year intervals when statistical uncertainties and differences in data processing algorithms are considered. 1999-11-20 Article Stratospheric effects of 27-day solar ultraviolet variations: The column ozone response and comparisons of solar cycles 21 and 22 1999, 104 (D21):26473 Journal of Geophysical Research: Atmospheres 01480227 10.1029/1999JD900466 http://hdl.handle.net/10150/624008 http://arizona.openrepository.com/arizona/handle/10150/624008 Journal of Geophysical Research: Atmospheres en http://doi.wiley.com/10.1029/1999JD900466 Copyright 1999 by the American Geophysical Union. AMER GEOPHYSICAL UNION
collection NDLTD
language en
sources NDLTD
description Two unresolved observational issues concerning the response of stratospheric ozone to 27-day solar ultraviolet variations are as follows: (1) the amplitude of the column ozone response and whether it is consistent with the predictions of current two-dimensional stratospheric models and (2) whether the ozone profile response in the upper stratosphere differed appreciably during the solar cycle 22 maximum period (around 1990) as compared with the solar cycle 21 maximum period (around 1980). To investigate these issues, two separate 4-year intervals (1979–1982 and 1989–1992) of daily zonal mean Nimbus 7 Total Ozone Mapping Spectrometer, Nimbus 7 solar backscattered ultraviolet (SBUV), and/or NOAA 11 SBUV/2 data for tropical latitudes (30°S to 30°N) are analyzed using cross correlation and cross-spectral and regression methods. The Mg II core-to-wing ratio is employed as a measure of solar UV variations near 200 nm. Results show that the mean tropical column ozone sensitivity (percent change of ozone for a 1% change in solar flux) is 0.09±0.01 at a lag of 4–6 days during both intervals and is approximately consistent with model predictions. Ozone profile sensitivities and phase lags are also in agreement between the two 4-year intervals when statistical uncertainties and differences in data processing algorithms are considered.
author2 Univ Arizona, Lunar & Planetary Lab
author_facet Univ Arizona, Lunar & Planetary Lab
Hood, L. L.
Zhou, S.
author Hood, L. L.
Zhou, S.
spellingShingle Hood, L. L.
Zhou, S.
Stratospheric effects of 27-day solar ultraviolet variations: The column ozone response and comparisons of solar cycles 21 and 22
author_sort Hood, L. L.
title Stratospheric effects of 27-day solar ultraviolet variations: The column ozone response and comparisons of solar cycles 21 and 22
title_short Stratospheric effects of 27-day solar ultraviolet variations: The column ozone response and comparisons of solar cycles 21 and 22
title_full Stratospheric effects of 27-day solar ultraviolet variations: The column ozone response and comparisons of solar cycles 21 and 22
title_fullStr Stratospheric effects of 27-day solar ultraviolet variations: The column ozone response and comparisons of solar cycles 21 and 22
title_full_unstemmed Stratospheric effects of 27-day solar ultraviolet variations: The column ozone response and comparisons of solar cycles 21 and 22
title_sort stratospheric effects of 27-day solar ultraviolet variations: the column ozone response and comparisons of solar cycles 21 and 22
publisher AMER GEOPHYSICAL UNION
publishDate 1999
url http://hdl.handle.net/10150/624008
http://arizona.openrepository.com/arizona/handle/10150/624008
work_keys_str_mv AT hoodll stratosphericeffectsof27daysolarultravioletvariationsthecolumnozoneresponseandcomparisonsofsolarcycles21and22
AT zhous stratosphericeffectsof27daysolarultravioletvariationsthecolumnozoneresponseandcomparisonsofsolarcycles21and22
_version_ 1718456686618869760