The DOI matches its Crossref record; 50 of the 51 references it cites were found in a registry or an index.
Radiative forcing of climate by changes in the vertical distribution of ozone
Abstract
We describe a simple method for evaluating the radiative forcing of surface temperature caused by changes in the vertical distribution of ozone. The method employs a parameterization based on one‐dimensional radiative‐convective equilibrium calculations; these calculations predict that the surface temperature should warm in response to both decreases in ozone above 30 km and increases in ozone below 30 km. The parameterization is used to investigate the response of surface temperature to observed changes in the vertical distribution of ozone at northern mid‐latitudes. We show that the observed ozone trends, taken at face value, suggest a cooling of the surface temperature at northern mid‐latitudes during the 1970s equal in magnitude to about half the warming predicted for CO 2 for the same time period. However, the measurement uncertainty of the observed trends is large, with the best estimates for mid‐latitude cooling being −0.05±0.05°C. The surface cooling is caused by ozone decreases in the lower stratosphere, which outweigh the warming effects of ozone increases in the troposphere. The results obtained differ from predictions based on one‐dimensional photochemical model simulations of ozone trends for the 1970s, which suggest a warming of the surface temperature equal to ∼20% of the warming contributed by CO 2 . Also, the ozone decreases observed in the lower stratosphere during the 1970s produce atmospheric cooling by several tenths of a degree in the 12‐ to 20‐km altitude region over the northern mid‐latitudes. This temperature decrease is larger than the cooling due to CO 2 and thus may obscure the expected stratospheric CO 2 greenhouse signature.
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“Numerous studies have reported its potency as a greenhouse gas at these altitudes, due to its ability to absorb IR, UV and visible radiation [146][147][148][149].”
From Investigation of Biofuel as a Potential Renewable Energy Source (2021) · cites this paper as [147]
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Items 201–300 of 552
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A 3D chemistry transport model study of changes in atmospheric ozone due to aircraft NOx emissions
Wauben, W. M. F., van Velthoven, P. F. J., & Kelder, H. M. (1997) · Atmospheric Environment · doi:10.1016/s1352-2310(96)00332-9 · Cited by 46
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“O3 is more efficient as a GHG in the upper troposphere than in the lower troposphere mostly because of the thermal vertical structure of the atmosphere (90).”
BackgroundMa, J., Liu, H., & Hauglustaine, D. A. (2002) · Journal of Geophysical Research Atmospheres · doi:10.1029/2001jd001354 · Cited by 45
Global atmospheric distributions and source strengths of light hydrocarbons and tetrachloroethene
Gupta, M. L., Cicerone, R. J., Blake, D. R., Rowland, F. S., & Isaksen, I. S. A. (1998) · Journal of Geophysical Research Atmospheres · doi:10.1029/98jd02645 · Cited by 47
Allen, D. J., Pickering, K., Bucsela, E. J., et al. (2021) · Journal of Geophysical Research Atmospheres · doi:10.1029/2020jd034174 · Cited by 44
“…[NO] + nitrogen dioxide [NO2]) produced by lightning (LNOx) via the Zel’dovich mechanism (Zel’dovich et al., 1947) are important contributors to tropospheric atmospheric composition and radiative forcing (Finney et al., 2018; Lacis et al., 1990; Liaskos et al., 2015; W. Wang et al., 1993).”
Changes in tropospheric ozone over India: Variability, long-term trends and climate forcing
Rathore, A., Gopikrishnan, G. P., & Kuttippurath, J. (2023) · Atmospheric Environment · doi:10.1016/j.atmosenv.2023.119959 · Cited by 47
Measurements of surface ozone at semi-arid site Anantapur (14.62°N, 77.65°E, 331 m asl) in India
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“Ozone is a strong greenhouse gas whose radiative forcing is largest in the upper troposphere (Lacis et al., 1990; Forster and Shine, 1997).”
BackgroundGlobal distribution of CO 2 in the upper troposphere and stratosphere
Diallo, M., Legras, B., Ray, E., Engel, A., & Añel, J. A. (2017) · Atmospheric chemistry and physics · doi:10.5194/acp-17-3861-2017 · Cited by 45
“…also called the Brewer–Dobson circulation (BDC), was recognized as a major component of the climate system, which affects radiative forcing (Lacis et al., 1990; Forster and Shine, 1997; Forster et al., 2007) and atmospheric circulation (Andrews et al., 1987; Holton et al., 1995; Salby and…”
BackgroundEffect of changes in radiatively active species upon the lower stratospheric temperatures
Ramaswamy, V., & Bowen, M. (1994) · Journal of Geophysical Research Atmospheres · doi:10.1029/94jd01310 · Cited by 44
Zhang, Y., Liu, H., Crawford, J. H., Considine, D. B., Chan, C., Oltmans, S. J., & Thouret, V. (2012) · Journal of Geophysical Research Atmospheres · doi:10.1029/2012jd017498 · Cited by 43
“Introduction [ 2 ] Tropospheric ozone (O 3 ) is the principal source of the hydroxyl radical (OH) that controls the oxidizing capacity of the atmosphere [ Thompson , 1992], and is an important greenhouse gas in the upper troposphere (UT) [ Lacis et al. , 1990].”
BackgroundInfluentialRapid uplift of nonmethane hydrocarbons in a cold front over central Europe
Purvis, R. M., Lewis, A. C., Carney, R. A., et al. (2003) · Journal of Geophysical Research Atmospheres · doi:10.1029/2002jd002521 · Cited by 43
“Once in the relatively dry upper troposphere, ozone itself has an enhanced photochemical lifetime allowing intercontinental transport and a proportionally greater influence on climate than at the surface [Lacis et al., 1990].”
BackgroundMarelle, L., Raut, J., Law, K. S., & Duclaux, O. (2018) · Journal of Geophysical Research Atmospheres · doi:10.1029/2018jd028863 · Cited by 45
“Radiative effects are also known to be very sensitive to vertical pollutant distributions (Flanner, 2013; Lacis et al., 1990; Rap et al., 2015).”
BackgroundIndications of thin cirrus clouds in the stratosphere at mid-latitudes
Keckhut, P. L., Hauchecorne, A., Bekki, S., et al. (2005) · Atmospheric chemistry and physics · doi:10.5194/acp-5-3407-2005 · Cited by 42
“(Lacis et al., 1990; Ramaswamy et al., 1992).”
Radiative forcing due to increased tropospheric ozone concentrations
Chalita, S., Hauglustaine, D. A., Treut, H. L., & Müller, J. (1996) · Atmospheric Environment · doi:10.1016/1352-2310(95)00431-9 · Cited by 42
Rapid vertical trace gas transport by an isolated midlatitude thunderstorm
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Jurkat, T., Kaufmann, S., Voigt, C., Schäuble, D., Jeßberger, P., & Ziereis, H. (2016) · Atmospheric measurement techniques · doi:10.5194/amt-9-1907-2016 · Cited by 41
“Photochemical processing, convection and downward transport change ozone and nitric acid concentrations in the upper troposphere, thereby affecting the radiative budget of the free troposphere and upper troposphere and lower stratosphere region (UTLS) (Lacis et al., 1990).”
BackgroundHodnebrog, Ø., Berntsen, T. K., Dessens, O., Gauss, M., Grewe, V., Isaksen, I. S. A., Koffi, B., Myhre, G., Olivié, D., Prather, M. J., et al. (2011) · Atmospheric chemistry and physics · doi:10.5194/acp-11-11293-2011 · Cited by 36
“, 2008) because changes in ozone have their largest impact on climate when they occur in the UTLS (upper troposphere/lower stratosphere) region, due to the low temperatures found near the tropopause (Wang and Sze, 1980; Lacis et al., 1990; Hansen et al., 1997).”
BackgroundFlatøy, F., & Hov, Ø. (1996) · Journal of Geophysical Research Atmospheres · doi:10.1029/95jd03070 · Cited by 40
Kraabøl, A. G., Berntsen, T. K., Sundet, J. K., & Stordal, F. (2002) · Journal of Geophysical Research Atmospheres · doi:10.1029/2001jd001019 · Cited by 41
The Impact of Stratospheric Ozone Feedbacks on Climate Sensitivity Estimates
Nowack, P. J., Abraham, N. L., Braesicke, P., & Pyle, J. A. (2018) · Journal of Geophysical Research Atmospheres · doi:10.1002/2017jd027943 · Cited by 47
“We note that upper stratospheric ozone increases such as the ones suppressed in D1/D2 have mostly been associated with negative SW radiative forcing in studies with idealized ozone perturbations (e.g., Hansen et al., 1997; Lacis et al., 1990).”
BackgroundInfluentialRadiative forcing due to changes in ozone: a comparison of different codes
Shine, K. P., Briegleb, B. P., Grossman, A. S., Hauglustaine, D. A., Mao, H., Ramaswamy, V., Schwarzkopf, M. D., van Dorland, R., & Wang, W.-C. (1995) · Springer eBooks · doi:10.1007/978-3-642-79869-6_23 · Cited by 39
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“991 ozone production in the upper troposphere, a region where ozone is most effective as a radiatively active gas (Lacis et al. 1990).”
BackgroundOn the solar ultraviolet spectral irradiance during the Maunder Minimum
Lean, J. L., White, O. R., & Skumanich, A. (1995) · Global Biogeochemical Cycles · doi:10.1029/95gb00159 · Cited by 38
An evaluation of upper troposphere NOx with two models
Penner, J. E., Bergmann, D. J., Walton, J. J., et al. (1998) · Journal of Geophysical Research Atmospheres · doi:10.1029/98jd01565 · Cited by 38
Secondary ozone peaks in the troposphere over the Himalayas
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“13 C, based on the vertical profile of ozone forcing (Lacis et al., 1990).”
InfluentialZhao, K., Hu, C., Yuan, Z., Xu, D., Zhang, S., Luo, H., Wang, J., & Jiang, R. (2020) · Atmospheric Research · doi:10.1016/j.atmosres.2020.105158 · Cited by 37
Kunhikrishnan, T., Lawrence, M. G., von Kuhlmann, R., Wenig, M. O., Asman, W. A. H., Richter, A., & Burrows, J. P. (2006) · Journal of Geophysical Research Atmospheres · doi:10.1029/2005jd006036 · Cited by 37
Jeker, D., Pfister, L., Thompson, A. M., et al. (2000) · Journal of Geophysical Research Atmospheres · doi:10.1029/1999jd901053 · Cited by 37
Further estimates of radiative forcing due to tropospheric ozone changes
Forster, P. M. D. F., Johnson, C. E., Law, K. S., Pyle, J. A., & Shine, K. P. (1996) · Geophysical Research Letters · doi:10.1029/96gl03277 · Cited by 36
Trace gas evolution in the lowermost stratosphere from Aura Microwave Limb Sounder measurements
Santee, M. L., Manney, G. L., Livesey, N. J., Froidevaux, L., Schwartz, M., & Read, W. G. (2011) · Journal of Geophysical Research Atmospheres · doi:10.1029/2011jd015590 · Cited by 36
Evaluation of simulated photochemical partitioning of oxidized nitrogen in the upper troposphere
Henderson, B. H., Pinder, R. W., Crooks, J., et al. (2011) · Atmospheric chemistry and physics · doi:10.5194/acp-11-275-2011 · Cited by 35
“As a greenhouse gas, ozone is 10 times more efficient in the upper troposphere than in the lower troposphere (Lacis et al., 1990).”
BackgroundHuang, J., Liu, H., Crawford, J. H., Chan, C., Considine, D. B., Zhang, Y., Zheng, X., Zhao, C., Thouret, V., Oltmans, S. J., et al. (2015) · Atmospheric chemistry and physics · doi:10.5194/acp-15-5161-2015 · Cited by 35
“Tropospheric ozone (O3) is an effective greenhouse gas, especially in the upper troposphere (UT) (Lacis et al., 1990).”
BackgroundAkimoto, H., Kurokawa, J., Sudo, K., Nagashima, T., Takemura, T., Klimont, Z., Amann, M. C., & Suzuki, K. (2015) · Atmospheric Environment · doi:10.1016/j.atmosenv.2015.10.003 · Cited by 35
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Han, H., Liu, J. J., Yuan, H., Zhuang, B., Zhu, Y., Wu, Y., Yan, Y., & Ding, A. (2018) · Atmospheric chemistry and physics · doi:10.5194/acp-18-4251-2018 · Cited by 37
“Owing to the high radiative forcing efficiency, the change in ozone concentrations in the upper troposphere can impact climate more significantly than that in the lower troposphere (Lacis et al., 1990).”
BackgroundChoi, Y., Kim, J., Eldering, A., et al. (2009) · Geophysical Research Letters · doi:10.1029/2009gl039381 · Cited by 34
“…O3 has a larger radiative forcing efficiency than its lower tropospheric counterpart; for example, an increase in O3 of 10 Dobson units in the upper troposphere (8–12 km) affects the surface temperature six times more than the same increase in the boundary layer (0–2 km) [Lacis et al., 1990].”
BackgroundResultInfluentialHendricks, J., Lippert, E., Petry, H., & Ebel, A. (1999) · Journal of Geophysical Research Atmospheres · doi:10.1029/1998jd100098 · Cited by 34
Christiansen, B., Guldberg, A., Hansen, A. W., et al. (1997) · Journal of Geophysical Research Atmospheres · doi:10.1029/97jd00529 · Cited by 33
The role of the stratosphere in climate change
Rind, D. H., & Lacis, A. A. (1993) · Surveys in Geophysics · doi:10.1007/bf02179221 · Cited by 33
Staufer, J., Staehelin, J., Stübi, R., Peter, T., Tummon, F., & Thouret, V. (2013) · Atmospheric measurement techniques · doi:10.5194/amt-6-3393-2013 · Cited by 32
“Perturbations in the O3 distributions in this region have strongest impact on surface temperatures when they are introduced around the tropopause (Lacis et al., 1990; Forster and Shine, 1997).”
BackgroundTinney, E. N., & Homeyer, C. R. (2020) · Journal of Geophysical Research Atmospheres · doi:10.1029/2020jd033657 · Cited by 32
“O3 has its greatest radiative forcing in the UT, with concentration increases in the UTLS leading to surface warming (Lacis et al., 1990).”
BackgroundSurface ozone variability in the urban and nearby rural locations of tropical India
Londhe, A. L., Jadhav, D. B., Buchunde, P., et al. (2008) · Open Access Digital Repository of Ministry of Earth Sciences, Government of India (Government of India) · Cited by 32
Ridley, B. A., Atlas, E., Selkirk, H. B., Pfister, L., Montzka, D. D., Walega, J. G., Donnelly, S. G., Stroud, V., Richard, E. C., Kelly, K. K., et al. (2004) · Atmospheric Environment · doi:10.1016/j.atmosenv.2003.11.038 · Cited by 32
Wild, O., Prather, M. J., Akimoto, H., Sundet, J. K., Isaksen, I. S. A., Crawford, J. H., Davis, D. D., Avery, M. A., Kondo, Y., Sachse, G. W., et al. (2004) · Journal of Geophysical Research Atmospheres · doi:10.1029/2003jd004041 · Cited by 35
“…of ozone in the troposphere from precursor species such as nitrogen oxides (NO x ), carbon monoxide (CO) and hydrocarbons leads to a degradation of local air quality [ Haagen-Smit , 1952] and to a global increase in O 3 that leads to a global warming [ Lacis et al. , 1990; Hansen et al. , 1997].”
Phoenix, D. B., & Homeyer, C. R. (2021) · Journal of Geophysical Research Atmospheres · doi:10.1029/2021jd034568 · Cited by 31
O’Connor, F. M., Johnson, B. T. T., Jamil, O., Andrews, T., Mulcahy, J. P., & Manners, J. C. (2022) · Journal of Advances in Modeling Earth Systems · doi:10.1029/2022ms002991 · Cited by 31
“This is as a result of O3 forcing being dominated by changes in the upper troposphere and lower stratosphere (UTLS) (Lacis et al., 1990; Skeie et al., 2020) and the lack of atmospheric mass Figure 2.”
BackgroundInfluentialCauses of interannual variability over the southern hemispheric tropospheric ozone maximum
Liu, J., Rodríguez, J. M., Steenrod, S. D., et al. (2017) · Atmospheric chemistry and physics · doi:10.5194/acp-17-3279-2017 · Cited by 31
“Over the SHTOM region, IAV in the stratospheric contribution is found to be the most important factor driving the IAV of ozone, especially over the upper troposphere, where O3 changes have strong radiative effects (Lacis et al., 1990).”
BackgroundAccurate Measurements of Hydrocarbons in the Atmosphere (AMOHA): Three European intercomparisons
Slemr, J., Slemr, F., Partridge, R. H., D'Souza, H., & Schmidbauer, N. (2002) · Journal of Geophysical Research Atmospheres · doi:10.1029/2001jd001357 · Cited by 31
In situ measurements of the NOx distribution and variability over the eastern North Atlantic
Ziereis, H., Schlager, H., Schulte, P., Köhler, I., Marquardt, R., & Feigl, C. (1999) · Journal of Geophysical Research Atmospheres · doi:10.1029/1999jd900175 · Cited by 31
Is methane‐driven deglaciation consistent with the ice core record?
Thorpe, R. B., Law, K. S., Bekki, S., Pyle, J. A., & Nisbet, E. G. (1996) · Journal of Geophysical Research Atmospheres · doi:10.1029/96jd02547 · Cited by 31
Phoenix, D. B., Homeyer, C. R., Barth, M. C., et al. (2020) · Journal of Geophysical Research Atmospheres · doi:10.1029/2019jd032016 · Cited by 30
“Upper tropospheric O3 plays an important role in the climate system due to its radiative forcing (Forster & Shine, 1997; Lacis et al., 1990).”
BackgroundImpact of biomass burning and stratospheric intrusions in the remote South Pacific Ocean troposphere
Daskalakis, N., Gallardo, L., Kanakidou, M., Nüß, J. R., Menares, C., Rondanelli, R., Thompson, A. M., & Vrekoussis, M. (2022) · Atmospheric chemistry and physics · doi:10.5194/acp-22-4075-2022 · Cited by 31
What controls ozone sensitivity in the upper tropical troposphere?
Nussbaumer, C. M., Fischer, H., Lelieveld, J., & Pozzer, A. (2023) · Atmospheric chemistry and physics · doi:10.5194/acp-23-12651-2023 · Cited by 32
“changes in ozone exert (and will continue to exert) a particularly large impact on the earth’s radiative forcing – especially in the tropopause region and the tropical UT (Lacis et al., 1990; Mohnen et al., 1993; Wuebbles, 1995; Lelieveld and van Dorland, 1995; van Dorland et al., 1997; Staehelin et al., 2001; Iglesia…”
BackgroundThe role of refrigerants in climate change
Wuebbles, D. J. (1994) · International Journal of Refrigeration · doi:10.1016/0140-7007(94)90082-5 · Cited by 30
An annotated bibliography on the greenhouse effect and climate change
Handel, M. D., & Risbey, J. S. (1992) · Climatic Change · doi:10.1007/bf00140914 · Cited by 29
Robinson, T. D., & Crisp, D. (2018) · Journal of Quantitative Spectroscopy and Radiative Transfer · doi:10.1016/j.jqsrt.2018.03.002 · Cited by 29
Particulate Nitrate Photolysis as a Possible Driver of Rising Tropospheric Ozone
Shah, V. P., Keller, C. A., Knowland, K. E., Christiansen, A., Hu, L., Wang, H., Lu, X. H., Alexander, B., & Jacob, D. J. (2024) · Geophysical Research Letters · doi:10.1029/2023gl107980 · Cited by 34
“Ozone increases in the free troposphere have a larger effect on climate than increases near the surface (Lacis et al., 1990).”
BackgroundGuo, H. F., Ling, Z., Simpson, I. J., et al. (2012) · Journal of Geophysical Research Atmospheres · doi:10.1029/2012jd017750 · Cited by 29
“These emissions have a major influence on the chemistry of the lower atmosphere, the oxidizing capacity of the atmosphere, visibility degradation, and consequently on the global climate [Lacis et al., 1990; Crutzen, 1995; Saunders et al., 2003].”
BackgroundIn‐flight measurement of aircraft CO and nonmethane hydrocarbon emission indices
Slemr, F., Giehl, H., Habram, M., Slemr, J., Schlager, H., Schulte, P., Haschberger, P., Lindermeir, E., Döpelheuer, A., & Plohr, M. (2001) · Journal of Geophysical Research Atmospheres · doi:10.1029/2000jd900580 · Cited by 29
Ozone loss episodes in the free Antarctic troposphere, suggesting a possible climate feedback
Roscoe, H. K., Kreher, K., & Frieß, U. (2001) · Geophysical Research Letters · doi:10.1029/2000gl012583 · Cited by 29
Solar Influences on Global Change
National Research Council (1994) · National Academies Press eBooks · doi:10.17226/4778 · Cited by 29
“Changes in ozone, temperature, and other trace gases have been widely implicated in a variety of the mechanisms by which changes in the middle atmosphere might influence the biosphere by physically coupling to the troposphere and modifying the climate (NAS, 1982; Lacis et al., 1990; Schwarzkopf and Ramaswamy, 1993; Ha…”
BackgroundMeier, A. C., & Hendricks, J. (2002) · Journal of Geophysical Research Atmospheres · doi:10.1029/2001jd000735 · Cited by 29
A modeling study of effective radiative forcing and climate response due to tropospheric ozone
Xie, B., Zhang, H., Wang, Z., Zhao, S., & Fu, Q. (2016) · Advances in Atmospheric Sciences · doi:10.1007/s00376-016-5193-0 · Cited by 29
Regional and seasonal radiative forcing by perturbations to aerosol and ozone precursor emissions
Bellouin, N., Baker, L., Hodnebrog, Ø., Olivié, D., Cherian, R., MacIntosh, C. R., Samset, B. H., Esteve, A. R., Aamaas, B., Quaas, J., et al. (2016) · Atmospheric chemistry and physics · doi:10.5194/acp-16-13885-2016 · Cited by 30
“…aerosols too high in the atmosphere leads to overestimating RFari (Samset et al., 2013) and underestimating rapid adjustments tropo-sphere with a maximum near the tropopause (Lacis et al., 1990) so ozone being located too low in models introduces a low bias in the SRF exerted by ozone precursors.”
BackgroundHe, J., Zhang, Y., Wang, K., et al. (2017) · Atmospheric Environment · doi:10.1016/j.atmosenv.2017.06.015 · Cited by 28
“For example, changes in the amount and spatial distribution of tropospheric ozone (O3) can affect the radiative forcing of climate change (Lacis et al., 1990; Forster et al., 2007; Stevenson et al., 2013).”
BackgroundEffect of tropopause height changes on the calculation of ozone trends and their radiative forcing
Forster, P. M. D. F., & Tourpali, K. (2001) · Journal of Geophysical Research Atmospheres · doi:10.1029/2000jd900813 · Cited by 28
Tropospheric temperature response to stratospheric ozone recovery in the 21st century
Hu, Y., Xia, Y., & Fu, Q. (2011) · Atmospheric chemistry and physics · doi:10.5194/acp-11-7687-2011 · Cited by 28
“…yr of the 20th century, and its impact on troposphere-surface temperatures had been investigated using radiation transfer models (Wang et al., 1980; Lacis et al., 1990; Wang, et al., 1993; Forster and Shine, 1997), the general circulation model (GCM) (Ramaswamy et al., 1992) and satellite…”
MethodWong, S., Wang, W., Isaksen, I. S. A., Berntsen, T. K., & Sundet, J. K. (2004) · Journal of Geophysical Research Atmospheres · doi:10.1029/2003jd003998 · Cited by 32
Vay, S. A., Anderson, B. E., Jensen, E. J., et al. (2000) · Journal of Geophysical Research Atmospheres · doi:10.1029/1999jd901019 · Cited by 28
Zachariasse, M., Smit, H. G. J., van Velthoven, P. F. J., et al. (2001) · Journal of Geophysical Research Atmospheres · doi:10.1029/2001jd900061 · Cited by 28
Harper, K., & Unger, N. (2018) · Atmospheric chemistry and physics · doi:10.5194/acp-18-16931-2018 · Cited by 30
“…in RF. P18 L5-7: “increase in regional surface ozone concentrations is unlikely to have a significant impact on the induced ozone forcing since, as Lacis et al. (1990) find, changes in surface ozone have a much smaller effect on climate forcing relative to equivalent ozone changes in the upper…”
BackgroundBowman, K. W., Jones, D. B. A., Logan, J. A., Worden, H. M., Boersma, K. F., Chang, R., Kulawik, S. S., Osterman, G. B., Hamer, P., & Worden, J. R. (2009) · Atmospheric chemistry and physics · doi:10.5194/acp-9-3563-2009 · Cited by 27
“…atmosphere, radiative forcing of the climate system , and air quality (Worden et al., 2008; Fishman et al., 1979, 1991; Fishman and Larsen, 1987; Lacis et al., 1990; Kiehl et al., 1999; Portmann et al., 1997; Naik et al., 2005; Jacob, 1999; Li et al., 2002) Earth-observing satellites provide a…”
BackgroundStrong modification of stratospheric ozone forcing by cloud and sea-ice adjustments
Xia, Y., Hu, Y., & Huang, Y. (2016) · Atmospheric chemistry and physics · doi:10.5194/acp-16-7559-2016 · Cited by 27
“It is known that ozone is a greenhouse gas, and that stratospheric ozone has a warming effect on tropospheric-surface climate, which has been demonstrated by early simulation works with radiative-convective models (Ramanathan and Dickinson, 1979; Lacis et al., 1990).”
BackgroundThe Role of Methane in the Global Environment
Wuebbles, D. J., & Tamaresis, J. S. (1993) · Springer eBooks · doi:10.1007/978-3-642-84605-2_20 · Cited by 27
Kheshgi, H. S., Jain, A. K., Kotamarthi, V. R., & Wuebbles, D. J. (1999) · Journal of Geophysical Research Atmospheres · doi:10.1029/1999jd900367 · Cited by 27
“Calculations indicate that an increase in tropospheric ozone over the past decades (suggested by some measurements) should add to global warming [Hauglustaine et al., 1994; Lacis et al., 1990; World Meteorological Organization (WMO), 1999].”
BackgroundTropical tropospheric ozone column retrieval for GOME-2
Valks, P., Hao, N., Garcìa, S. G., Loyola, D., Dameris, M., Jöckel, P., & Delcloo, A. (2014) · Atmospheric measurement techniques · doi:10.5194/amt-7-2513-2014 · Cited by 26
“Upper tropospheric ozone acts as a greenhouse gas by absorbing long-wave terrestrial radiation (Lacis et al., 1990; Foster and Shine, 1997).”
BackgroundPeiro, H., Emili, E., Cariolle, D., Barret, B., & Flochmoën, É. L. (2018) · Atmospheric chemistry and physics · doi:10.5194/acp-18-6939-2018 · Cited by 26
“It influences the atmospheric radiative forcing as one of the main absorbers of infrared and ultraviolet radiation (Wang et al., 1980; Lacis et al., 1990).”
BackgroundYearly cycle of lower tropospheric ozone at the Arctic Circle
Rummukainen, M., Laurila, T., & Kivi, R. (1996) · Atmospheric Environment · doi:10.1016/1352-2310(95)00384-3 · Cited by 26
Radiative forcing and climate sensitivity: The ozone experience
Christiansen, B. (1999) · Quarterly Journal of the Royal Meteorological Society · doi:10.1002/qj.49712556011 · Cited by 26
Liu, J., Rodriguez, J. M., Oman, L. D., Douglass, A. R., Olsen, M. A., & Hu, L. (2020) · Atmospheric Chemistry and Physics · doi:10.5194/acp-20-6417-2020 · Cited by 24
Weber, J., Keeble, J., Abraham, N. L., Beerling, D. J., & Martin, M. V. (2024) · npj Climate and Atmospheric Science · doi:10.1038/s41612-024-00678-2 · Cited by 28
Earth Systems Change over Eastern Europe
(2012) · PH "Akademperiodyka" eBooks · doi:10.15407/akademperiodyka.195.488 · Cited by 25
A 22‐Year Evaluation of Convection Reaching the Stratosphere Over the United States
Homeyer, C. R., & Bowman, K. P. (2021) · Journal of Geophysical Research Atmospheres · doi:10.1029/2021jd034808 · Cited by 24
Impacts of a near-future supersonic aircraft fleet on atmospheric composition and climate
Eastham, S., Fritz, T., Sanz-Morère, I., Prashanth, P., Allroggen, F., Prinn, R. G., Speth, R., & Barrett, S. (2022) · Environmental Science Atmospheres · doi:10.1039/d1ea00081k · Cited by 22
Impact of stratospheric variability on tropospheric climate change
Dall’Amico, M., Stott, P. A., Scaife, A. A., Gray, L. J., Rosenlof, K. H., & Karpechko, A. Y. (2009) · Climate Dynamics · doi:10.1007/s00382-009-0580-1 · Cited by 24
“The studies by Hansen et al. (1997) and Lacis et al. (1990) suggest that positive ozone perturbations in the lower stratosphere produce a small radiative forcing and that there is a level between 25 and 30 km where the radiative forcing is zero before it turns into a negative one at upper levels.”
BackgroundChlorine activation near the midlatitude tropopause
Thornton, B. F., Toohey, D. W., Tuck, A. F., Elkins, J. W., Kelly, K. K., Hovde, S. J., Richard, E. C., Rosenlof, K. H., Thompson, T. L., Mahoney, M. J., et al. (2007) · Journal of Geophysical Research Atmospheres · doi:10.1029/2006jd007640 · Cited by 23
Radiative forcing due to changes in tropospheric ozone in the period 1980 to 1996
Myhre, G., Karlsdóttir, S., Isaksen, I. S. A., & Stordal, F. (2000) · Journal of Geophysical Research Atmospheres · doi:10.1029/2000jd900187 · Cited by 24
Effects on stratospheric ozone and temperature during the Maunder Minimum
Wuebbles, D. J., Wei, C., & Patten, K. O. (1998) · Geophysical Research Letters · doi:10.1029/98gl00057 · Cited by 23
Rosanka, S., Frömming, C., & Grewe, V. (2020) · Atmospheric chemistry and physics · doi:10.5194/acp-20-12347-2020 · Cited by 22
Dynamical drivers of free-tropospheric ozone increases over equatorial Southeast Asia
Stauffer, R. M., Thompson, A. M., Kollonige, D. E., Komala, N., Al-Ghazali, H. K., Risdianto, D. Y., Dindang, A., Jamaluddin, A. F., Sammathuria, M. K., Zakaria, N. B., et al. (2024) · Atmospheric chemistry and physics · doi:10.5194/acp-24-5221-2024 · Cited by 22
Impact of Lightning on Air Chemistry and Climate
Grewe, V. (2008) · Springer eBooks · doi:10.1007/978-1-4020-9079-0_25 · Cited by 22
Climate forcing of subsonic aviation: Indirect role of sulfate particles via heterogeneous chemistry
Pitari, G., Mancini, E., & Bregman, A. (2002) · Geophysical Research Letters · doi:10.1029/2002gl015705 · Cited by 22
“[14] In terms of climate RF, mid-upper tropospheric ozone changes are much more important than those in the lower stratosphere [Lacis et al., 1990].”
BackgroundZhang, Y., Tao, M., Zhang, J., Liu, Y., Chen, H., Cai, Z., & Konopka, P. (2020) · Atmospheric chemistry and physics · doi:10.5194/acp-20-13343-2020 · Cited by 21
Tropospheric ozone, lightning, and climate change
Sinha, A., & Toumi, R. (1997) · Journal of Geophysical Research Atmospheres · doi:10.1029/96jd03710 · Cited by 22
Tropospheric ozone budget: regional and global calculationsPreprint
O’Connor, F. M., Law, K. S., Pyle, J. A., Barjat, H., Brough, N., Dewey, K., Green, T., Kent, J., & Phillips, G. J. (2004) · doi:10.5194/acpd-4-991-2004 · Cited by 22
Metadata
- Authors
- Lacis, A. A., Wuebbles, D. J., & Logan, J. A.
- Affiliations
- Goddard Institute for Space Studies (US)
- National Center for Supercomputing Applications (BG)
- Harvard University (US)
- Venue
- Journal of Geophysical Research Atmospheres
- Publisher
- American Geophysical Union (AGU)
- Published
- 1990-06-20
- Volume
- 95
- Issue
- D7
- Pages
- 9971-9981
- ISSN
- 0148-0227 (ISSN-L)
- OpenAlex
- W2057192297
- Cited by
- 556
- References
- 51
- Citations by year
- 2026: 9 · 2025: 15 · 2024: 39 · 2023: 10 · 2022: 33 · 2021: 11 · 2020: 13 · 2019: 9 · 2018: 17 · 2017: 16 · 2016: 19 · 2015: 14 · 2014: 13 · 2013: 17 · 2012: 16
- FWCI
- 10.31
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Journal of Geophysical Research Atmospheres (publishedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Atmospheric Ozone and Climate
- Physical Sciences › Environmental Science › Global and Planetary Change › Climate variability and models
- Physical Sciences › Environmental Science › Global and Planetary Change › Atmospheric aerosols and clouds
- Keywords
- radiative forcing, vertical ozone distribution, surface temperature, stratospheric ozone depletion, radiative-convective equilibrium, surface cooling, northern mid-latitudes, ozone trends
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