81 citations as recorded by crossref.

1. Old carbon reservoirs were not important in the deglacial methane budget M. Dyonisius et al. 10.1126/science.aax0504
2. Isotopic constraint on the twentieth-century increase in tropospheric ozone L. Yeung et al. 10.1038/s41586-019-1277-1
3. Lightning NO<sub>x</sub>, a key chemistry–climate interaction: impacts of future climate change and consequences for tropospheric oxidising capacity A. Banerjee et al. 10.5194/acp-14-9871-2014
4. Nitrogen oxides in the global upper troposphere: interpreting cloud-sliced NO<sub>2</sub> observations from the OMI satellite instrument E. Marais et al. 10.5194/acp-18-17017-2018
5. Small Impact of Stratospheric Dynamics and Chemistry on the Surface Temperature of the Last Glacial Maximum in CESM2(WACCM6ma) J. Zhu et al. 10.1029/2022GL099875
6. Uncertainties in isoprene photochemistry and emissions: implications for the oxidative capacity of past and present atmospheres and for climate forcing agents P. Achakulwisut et al. 10.5194/acp-15-7977-2015
7. Bayesian Analysis of the Glacial‐Interglacial Methane Increase Constrained by Stable Isotopes and Earth System Modeling P. Hopcroft et al. 10.1002/2018GL077382
8. Effects of Chemical Feedbacks on Decadal Methane Emissions Estimates N. Nguyen et al. 10.1029/2019GL085706
9. WAIS Divide ice core suggests sustained changes in the atmospheric formation pathways of sulfate and nitrate since the 19th century in the extratropical Southern Hemisphere E. Sofen et al. 10.5194/acp-14-5749-2014
10. Quasi-Biennial Oscillation and Sudden Stratospheric Warmings during the Last Glacial Maximum Q. Fu et al. 10.3390/atmos11090943
11. The self-cleansing ability of prehistoric air M. Hegglin 10.1038/546041a
12. Origins and characterization of CO and O<sub>3</sub> in the African upper troposphere V. Lannuque et al. 10.5194/acp-21-14535-2021
13. GCAP 2.0: a global 3-D chemical-transport model framework for past, present, and future climate scenarios L. Murray et al. 10.5194/gmd-14-5789-2021
14. Tropospheric Ozone During the Last Interglacial Y. Yan et al. 10.1029/2022GL101113
15. Southern Hemisphere atmospheric history of carbon monoxide over the late Holocene reconstructed from multiple Antarctic ice archives X. Faïn et al. 10.5194/cp-19-2287-2023
16. Trends in global tropospheric hydroxyl radical and methane lifetime since 1850 from AerChemMIP D. Stevenson et al. 10.5194/acp-20-12905-2020
17. Antarctic and global climate history viewed from ice cores E. Brook & C. Buizert 10.1038/s41586-018-0172-5
18. Atmospheric methane variability: Centennial‐scale signals in the Last Glacial Period R. Rhodes et al. 10.1002/2016GB005570
19. Strong impacts on aerosol indirect effects from historical oxidant changes I. Karset et al. 10.5194/acp-18-7669-2018
20. Implications of carbon monoxide bias for methane lifetime and atmospheric composition in chemistry climate models S. Strode et al. 10.5194/acp-15-11789-2015
21. An observation-based, reduced-form model for oxidation in the remote marine troposphere C. Baublitz et al. 10.1073/pnas.2209735120
22. Modulation of hydroxyl variability by ENSO in the absence of external forcing A. Turner et al. 10.1073/pnas.1807532115
23. ESD Reviews: Climate feedbacks in the Earth system and prospects for their evaluation C. Heinze et al. 10.5194/esd-10-379-2019
24. Methyl Chloroform Continues to Constrain the Hydroxyl (OH) Variability in the Troposphere P. Patra et al. 10.1029/2020JD033862
25. A machine learning methodology for the generation of a parameterization of the hydroxyl radical D. Anderson et al. 10.5194/gmd-15-6341-2022
26. The Brewer‐Dobson Circulation During the Last Glacial Maximum Q. Fu et al. 10.1029/2019GL086271
27. Description and evaluation of tropospheric chemistry and aerosols in the Community Earth System Model (CESM1.2) S. Tilmes et al. 10.5194/gmd-8-1395-2015
28. Large Scale Anthropogenic Reduction of Forest Cover in Last Glacial Maximum Europe J. Kaplan et al. 10.1371/journal.pone.0166726
29. Isotopic evidence of multiple controls on atmospheric oxidants over climate transitions L. Geng et al. 10.1038/nature22340
30. Technical note: Constraining the hydroxyl (OH) radical in the tropics with satellite observations of its drivers – first steps toward assessing the feasibility of a global observation strategy D. Anderson et al. 10.5194/acp-23-6319-2023
31. On the Causes and Consequences of Recent Trends in Atmospheric Methane H. Schaefer 10.1007/s40641-019-00140-z
32. Enhancement of aerosol responses to changes in emissions over East Asia by gas‐oxidant‐aerosol coupling and detailed aerosol processes H. Matsui & M. Koike 10.1002/2015JD024671
33. Current understanding of the global cycling of carbon dioxide, methane, and nitrous oxide T. NAKAZAWA 10.2183/pjab.96.030
34. Millennial‐Scale Changes in Terrestrial and Marine Nitrous Oxide Emissions at the Onset and Termination of Marine Isotope Stage 4 J. Menking et al. 10.1029/2020GL089110
35. Exploring the drivers of tropospheric hydroxyl radical trends in the Geophysical Fluid Dynamics Laboratory AM4.1 atmospheric chemistry–climate model G. Chua et al. 10.5194/acp-23-4955-2023
36. Atmospheric methane variability through the Last Glacial Maximum and deglaciation mainly controlled by tropical sources B. Riddell-Young et al. 10.1038/s41561-023-01332-x
37. Radiative Forcing of Climate: The Historical Evolution of the Radiative Forcing Concept, the Forcing Agents and their Quantification, and Applications V. Ramaswamy et al. 10.1175/AMSMONOGRAPHS-D-19-0001.1
38. Atmospheric methane underestimated in future climate projections T. Kleinen et al. 10.1088/1748-9326/ac1814
39. Stratospheric Ozone in the Last Glacial Maximum M. Wang et al. 10.1029/2020JD032929
40. Glacial/interglacial wetland, biomass burning, and geologic methane emissions constrained by dual stable isotopic CH 4 ice core records M. Bock et al. 10.1073/pnas.1613883114
41. The relative importance of methane sources and sinks over the Last Interglacial period and into the last glaciation A. Quiquet et al. 10.1016/j.quascirev.2015.01.004
42. Representation of the Community Earth System Model (CESM1) CAM4-chem within the Chemistry-Climate Model Initiative (CCMI) S. Tilmes et al. 10.5194/gmd-9-1853-2016
43. Terrestrial methane emissions from the Last Glacial Maximum to the preindustrial period T. Kleinen et al. 10.5194/cp-16-575-2020
44. Spatial and temporal variability in the hydroxyl (OH) radical: understanding the role of large-scale climate features and their influence on OH through its dynamical and photochemical drivers D. Anderson et al. 10.5194/acp-21-6481-2021
45. Effects of land use and anthropogenic aerosol emissions in the Roman Empire A. Gilgen et al. 10.5194/cp-15-1885-2019
46. Observing U.S. Regional Variability in Lightning NO2 Production Rates J. Lapierre et al. 10.1029/2019JD031362
47. Tropospheric ozone radiative forcing uncertainty due to pre-industrial fire and biogenic emissions M. Rowlinson et al. 10.5194/acp-20-10937-2020
48. GISS Model E2.2: A Climate Model Optimized for the Middle Atmosphere—2. Validation of Large‐Scale Transport and Evaluation of Climate Response C. Orbe et al. 10.1029/2020JD033151
49. Inter-model comparison of global hydroxyl radical (OH) distributions and their impact on atmospheric methane over the 2000–2016 period Y. Zhao et al. 10.5194/acp-19-13701-2019
50. Paleo-Perspectives on Potential Future Changes in the Oxidative Capacity of the Atmosphere Due to Climate Change and Anthropogenic Emissions B. Alexander & L. Mickley 10.1007/s40726-015-0006-0
51. Apportionment of the Pre‐Industrial to Present‐Day Climate Forcing by Methane Using UKESM1: The Role of the Cloud Radiative Effect F. O’Connor et al. 10.1029/2022MS002991
52. Constraining remote oxidation capacity with ATom observations K. Travis et al. 10.5194/acp-20-7753-2020
53. Oxygen isotope mass balance of atmospheric nitrate at Dome C, East Antarctica, during the OPALE campaign J. Savarino et al. 10.5194/acp-16-2659-2016
54. An updated review of atmospheric mercury S. Lyman et al. 10.1016/j.scitotenv.2019.135575
55. Regional Characteristics of Atmospheric Sulfate Formation in East Antarctica Imprinted on 17O‐Excess Signature S. Ishino et al. 10.1029/2020JD033583
56. Historical Trends of Biogenic SOA Tracers in an Ice Core from Kamchatka Peninsula P. Fu et al. 10.1021/acs.estlett.6b00275
57. Understanding the glacial methane cycle P. Hopcroft et al. 10.1038/ncomms14383
58. Enhanced atmospheric oxidation capacity and associated ozone increases during COVID-19 lockdown in the Yangtze River Delta Y. Wang et al. 10.1016/j.scitotenv.2020.144796
59. Effects of Ozone Isotopologue Formation on the Clumped‐Isotope Composition of Atmospheric O2 L. Yeung et al. 10.1029/2021JD034770
60. Large uncertainties in global hydroxyl projections tied to fate of reactive nitrogen and carbon L. Murray et al. 10.1073/pnas.2115204118
61. Reassessment of pre-industrial fire emissions strongly affects anthropogenic aerosol forcing D. Hamilton et al. 10.1038/s41467-018-05592-9
62. Isotopic ordering in atmospheric O2 as a tracer of ozone photochemistry and the tropical atmosphere L. Yeung et al. 10.1002/2016JD025455
63. Atmospheric methane since the last glacial maximum was driven by wetland sources T. Kleinen et al. 10.5194/cp-19-1081-2023
64. Aerosol-Climate Interactions During the Last Glacial Maximum S. Albani et al. 10.1007/s40641-018-0100-7
65. Changes in Global Tropospheric OH Expected as a Result of Climate Change Over the Last Several Decades J. Nicely et al. 10.1029/2018JD028388
66. Lightning NO x and Impacts on Air Quality L. Murray 10.1007/s40726-016-0031-7
67. Stratosphere‐Troposphere Exchanges of Air Mass and Ozone Concentration in the Last Glacial Maximum M. Wang et al. 10.1029/2021JD036327
68. Clumped‐Isotope Constraint on Upper‐Tropospheric Cooling During the Last Glacial Maximum A. Banerjee et al. 10.1029/2022AV000688
69. Halogen chemistry reduces tropospheric O<sub>3</sub> radiative forcing T. Sherwen et al. 10.5194/acp-17-1557-2017
70. Effects of postdepositional processing on nitrogen isotopes of nitrate in the Greenland Ice Sheet Project 2 ice core L. Geng et al. 10.1002/2015GL064218
71. Interpreting contemporary trends in atmospheric methane A. Turner et al. 10.1073/pnas.1814297116
72. Influences of hydroxyl radicals (OH) on top-down estimates of the global and regional methane budgets Y. Zhao et al. 10.5194/acp-20-9525-2020
73. The role of wetland expansion and successional processes in methane emissions from northern wetlands during the Holocene C. Treat et al. 10.1016/j.quascirev.2021.106864
74. Source-receptor relationships for atmospheric mercury deposition in the context of global change H. Zhang et al. 10.1016/j.atmosenv.2021.118349
75. Impact of El Niño–Southern Oscillation on the interannual variability of methane and tropospheric ozone M. Rowlinson et al. 10.5194/acp-19-8669-2019
76. On the role of trend and variability in the hydroxyl radical (OH) in the global methane budget Y. Zhao et al. 10.5194/acp-20-13011-2020
77. Multi-model study of chemical and physical controls on transport of anthropogenic and biomass burning pollution to the Arctic S. Monks et al. 10.5194/acp-15-3575-2015
78. Assessment of NO<sub>2</sub> observations during DISCOVER-AQ and KORUS-AQ field campaigns S. Choi et al. 10.5194/amt-13-2523-2020
79. Hydroxyl Radical (OH) Response to Meteorological Forcing and Implication for the Methane Budget J. He et al. 10.1029/2021GL094140
80. WAIS Divide ice core suggests sustained changes in the atmospheric formation pathways of sulfate and nitrate since the 19th century in the extratropical Southern Hemisphere E. Sofen et al. 10.5194/acpd-13-23089-2013
81. Lightning NO<sub>x</sub>, a key chemistry–climate interaction: impacts of future climate change and consequences for tropospheric oxidising capacity A. Banerjee et al. 10.5194/acpd-14-8753-2014