Article
Environmental Sciences
Jinyao Zhu, Xin Jin, Chunhua Shi, Dan Chen
Summary: This study investigated a Rossby wave breaking (RWB) event and its impact on stratosphere-troposphere exchange (STE) over the Tibetan Plateau in mid-March 2006, using reanalysis data, satellite observations of ozone concentration, and a Lagrangian trajectory simulation. The results showed that the amplified amplitude of the Rossby wave due to increased eddy heat flux from the subtropical westerly jet contributed to the occurrence of the cyclonic RWB event. The cyclonic motion of the isentropic potential vorticity cut the tropical tropospheric air mass into the extratropical stratosphere, completing the stratosphere-troposphere mass exchange.
Article
Meteorology & Atmospheric Sciences
Rei Ueyama, Mark Schoeberl, Eric Jensen, Leonhard Pfister, Mijeong Park, Ju-Mee Ryoo
Summary: The direct impact of deep convection on the global lower stratospheric water vapor budget is still a debated issue. Two complementary modeling approaches are used to investigate this impact in different seasons. The results show that deep convection moistens the global lower stratosphere by approximately 0.3 ppmv, with a diurnal peak in winter and summer and relatively minor effect on global water vapor. The interannual variability of the convective impact is estimated to be up to 0.1 ppmv during 2006-2016.
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
(2023)
Article
Meteorology & Atmospheric Sciences
M. R. Schoeberl, R. Ueyama, L. Pfister
Summary: In this study, a forward domain filling trajectory model coupled with a new convective parcel injection system is used to investigate stratosphere-troposphere exchange (STE). The results show that the STE regions coincide with stationary forced tropical Rossby waves near the equator. Anticyclonic circulation generated by these waves isolates air over specific regions. The preferred locations of troposphere to stratosphere (T2S) and stratosphere to troposphere (S2T) exchange are mapped.
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
(2022)
Article
Meteorology & Atmospheric Sciences
Yonatan Givon, Chaim I. Garfinkel, Ian White
Summary: An intermediate complexity general circulation model is used to investigate the transient response of the NH winter stratosphere to modulated ultraviolet (UV) radiation by imposing an exaggerated UV perturbation. The enhanced UV radiation leads to immediate warming in the tropical upper stratosphere, spreading to the winter subtropics due to an accelerated Brewer-Dobson circulation. The study shows significant implications for observed stratospheric and tropospheric responses to solar variability on various time scales.
JOURNAL OF CLIMATE
(2021)
Article
Meteorology & Atmospheric Sciences
Kane A. Stone, Susan Solomon, David W. J. Thompson, Douglas E. Kinnison, John C. Fyfe
Summary: This study investigates the relationship between ENSO events and the southern hemisphere (SH) stratospheric pathway. The research finds that ENSO is associated with stratospheric anomalies in the SH, with the warm phase of the ENSO cycle generally leading to a colder spring Antarctic stratosphere. This relationship is robust and consistent across multiple models. Additionally, the study reveals that the magnitude of the stratospheric pathway is weaker compared to the tropospheric pathway, playing a secondary role.
JOURNAL OF CLIMATE
(2022)
Article
Environmental Sciences
David D. Parrish, Richard G. Derwent, Ian C. Faloona, Charles A. Mims
Summary: A nonlinear change in baseline ozone concentrations has been observed at northern midlatitudes over the past few decades. Recent studies using linear trend analyses have reported relatively small trends, which are inconsistent with earlier findings. The COVID-19-related ozone changes based on linear analysis are shown to be significantly larger than recent long-term decreases in baseline ozone. The loss of lower stratospheric ozone in the 2020 springtime Arctic stratospheric ozone depletion event also contributed to anomalously low background ozone levels. Taken together, these factors suggest that the impact of COVID-19 restrictions on background tropospheric ozone in 2020 was smaller than previously reported. A consensus understanding of baseline ozone changes and their causes is crucial for developing effective policies to improve ozone air quality.
ATMOSPHERIC CHEMISTRY AND PHYSICS
(2022)
Article
Multidisciplinary Sciences
Mang Lin, Mark H. Thiemens
Summary: Reconstruction of past solar activity or high-energy events using cosmogenic radionuclides provides valuable insights into their impacts on near space, satellite technologies, and ecosystems. The use of cosmogenic radiosulfur (35S) allows for improved tracking of solar activity and regional atmospheric circulation changes. Incorporating 35S as an independent parameter in a universal cosmogenic radionuclide model enhances the modeling of other long-lived radionuclides with different atmospheric chemistries.
PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA
(2022)
Article
Environmental Sciences
Jingwen Liu, Sihui Wang, Qiangqiang Yuan, Feng Zhang, Liye Zhu
Summary: This study derives the vertical ozone profile from the troposphere to the stratosphere by combining ozone retrievals from MLS and TES. The combined products have been validated and found to have smaller biases compared to MLS or TES alone.
Article
Environmental Sciences
Huiping Wang, Chunhua Shi, Dong Guo
Summary: This study analyzed the air particle pathways and weather systems in two types of equatorward and poleward cyclonic Rossby wave-breaking (CWB) events using ERA5 reanalysis data and trajectory analysis. The exchange of mass between the stratosphere and troposphere in both CWBs was estimated and discussed. The results showed that high potential vorticity (PV) particles were mainly transported poleward, while low PV particles displayed vertical motion and some of them moved southward. Only a small percentage of particles underwent stratosphere-troposphere exchange (STE), with the majority of high PV particles remaining in the stratosphere and low PV particles remaining in the troposphere. In equatorward CWB, STE mainly occurred 24-48 hours post breaking, with a maximum mass transport of approximately 1.54 x 10(13) kg. In poleward CWB, STE mainly occurred within 0-18 hours post breaking, with a maximum mass transport of approximately 1.48 x 10(13) kg.
Article
Meteorology & Atmospheric Sciences
Mingcheng Wang, Qiang Fu, Susan Solomon, Becky Alexander, Rachel H. White
Summary: This study investigates the changes in air mass and ozone stratosphere-troposphere exchange (STE) during the Last Glacial Maximum (LGM) compared to preindustrial climate. Using a climate model, the study finds that ozone STE is decreased in the LGM, mainly due to reduced ozone in the extratropical lower stratosphere. Air mass fluxes have a minor impact on the changes. The study also analyzes the tropospheric ozone budget and finds that ozone STE in the LGM accounts for a larger proportion of tropospheric ozone production compared to the modern climate.
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
(2022)
Article
Meteorology & Atmospheric Sciences
Ruhua Zhang, Wen Zhou, Wenshou Tian, Yue Zhang, Zhenchen Liu, Paxson K. Y. Cheung
Summary: This study re-examines the impact of El Nino-Southern Oscillation (ENSO) on the winter stratospheric polar vortex intensity (PVI) and finds that the negative correlation between ENSO and PVI has weakened in recent decades and is no longer statistically significant. This weakening is associated with changes in wave-1 fluxes entering the stratosphere.
JOURNAL OF CLIMATE
(2022)
Article
Meteorology & Atmospheric Sciences
Martin Jucker, Thomas Reichler
Summary: Based on a multimillennial climate model simulation, it is found that sudden stratospheric warmings (SSWs) in the Southern Hemisphere (SH) are mainly displacement events forced by wave-1 planetary waves. A surface signature similar to the negative phase of the Southern Annular Mode (SAM) can be detected up to two months before the onset date, but there is a tendency for a transition from wave 1 before to zonally symmetric anomalies after onset. The weakening of the Amundsen Sea low is identified as a prominent precursor for SH SSWs, and the Indian Ocean dipole is more important than El Nino-Southern Oscillation.
JOURNAL OF CLIMATE
(2023)
Article
Environmental Sciences
Andreas Schaefler, Andreas Fix, Martin Wirth
Summary: This study utilizes collocated airborne lidar observations to accurately depict the shape and composition of the ExTL, confirming established conceptual models. The trace gas distributions reveal the influence of water vapor and ozone from tropical and extratropical regions on the ExTL. Lidar data identify distinct mixing regimes and the subdivision of mixed and tropospheric air.
ATMOSPHERIC CHEMISTRY AND PHYSICS
(2021)
Article
Meteorology & Atmospheric Sciences
Emily N. Tinney, Cameron R. Homeyer
Summary: Moist convection has a significant impact on the distribution and concentration of trace gases in the upper troposphere and lower stratosphere. It typically increases humidity, reduces ozone concentration, and increases carbon monoxide levels. The effects of convection are more pronounced in tropical environments, particularly on ozone levels.
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
(2021)
Article
Meteorology & Atmospheric Sciences
Chengyang Zhang, Wenshou Tian, Jiankai Zhang, Tuantuan Zhang, Wei Yu, Song Yang, Tao Wang
Summary: The premonsoon circulation over South Asia in May shows interannual variations and can be influenced by the stratosphere-troposphere modes over the North Atlantic in April. These modes exhibit NAO-like circulation patterns, but have different circulation patterns and planetary wave activity. The first mode is a stratosphere-troposphere-coupled mode, which leads to a reduction in sea ice over the northern Barents Sea, generating anomalous circulation and strengthening the premonsoon circulation. The second mode, influenced by ENSO, also has a significant effect on the South Asian premonsoon circulations in May and is related to the NAO-like circulation.
JOURNAL OF CLIMATE
(2023)
Article
Multidisciplinary Sciences
Stephen Po-Chedley, Benjamin D. Santer, Stephan Fueglistaler, Mark D. Zelinka, Philip J. Cameron-Smith, Jeffrey F. Painter, Qiang Fu
Summary: There is a discrepancy between GCMs and satellite observations regarding the warming trend of the midtroposphere temperature in the tropics. Some model simulations show trends that align with observations while others exhibit subdued warming, particularly in the tropical Pacific. The latest generation of GCMs also demonstrate muted tropical tropospheric warming trends over the central and eastern Pacific.
PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA
(2021)
Article
Meteorology & Atmospheric Sciences
Laurence Y. Yeung, Lee T. Murray, Asmita Banerjee, Xin Tie, Yuzhen Yan, Elliot L. Atlas, Sue M. Schauffler, Kristie A. Boering
Summary: This study developed an online scheme to simulate tropospheric (OO)-O-18-O-18 abundances within the GEOS-Chem chemical transport model in order to investigate uncertainties in previous offline box-model frameworks. By incorporating pressure dependence and efficient titration effects into the calculation scheme, the model results showed quantitative agreement with all available observations, indicating that tropospheric ozone burden increased less than 40% over the twentieth century.
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
(2021)
Article
Meteorology & Atmospheric Sciences
Gara Villalba, Mary Whelan, Stephen A. Montzka, Philip J. Cameron-Smith, Marc Fischer, Andrew Zumkehr, Tim Hilton, James Stinecipher, Ian Baker, Ray P. Bambha, Hope A. Michelsen, Brian W. LaFranchi, Carme Estruch, Elliott Campbell
Summary: Cities are implementing additional urban greenery to capture CO2 and become more carbon neutral, but there is still uncertainty in measuring the effectiveness of these measures. Using OCS as a tracer of photosynthesis can help track the urban biosphere signal, but improvements in modeling transport, boundary layer variability, and estimating gross primary productivity are needed. The urban biosphere signal is an important contributor to simulated CO2 mole fractions.
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
(2021)
Article
Meteorology & Atmospheric Sciences
Sofia M. Chelpon, Laura L. Pan, Zhengzhao J. Luo, Elliot L. Atlas, Shawn B. Honomichl, Warren P. Smith, Siyuan Wang, Kirk Ullmann, Samuel R. Hall, Eric C. Apel, Rebecca S. Hornbrook
Summary: This study investigates the feasibility of using airborne in situ measurements to derive transit time distributions over the highly convective tropical western Pacific. The study demonstrates the method's effectiveness through measurements from the CONTRAST experiment. By quantifying uncertainties associated with chemical lifetimes and characterizing the source region contributing to transport, the study supports the hypothesis that there is enough information in measurements to resolve dynamical variability in the region.
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
(2021)
Article
Geosciences, Multidisciplinary
James R. Stinecipher, Philip Cameron-Smith, Le Kuai, Norbert Glatthor, Michael Hoepfner, Ian Baker, Christian Beer, Kevin Bowman, Meemong Lee, Scot M. Miller, Nicholas Parazoo, J. Elliott Campbell
Summary: Understanding the magnitude of tropical gross primary production (GPP) is crucial for carbon cycle modeling and climate projections, but it is not well constrained at regional scales. This study uses the biospheric uptake of carbonyl sulfide (OCS) to estimate regional GPP in the Amazon basin. Comparison with satellite retrievals reveals a regional GPP estimate of 2375 +/- 914 g(C) m(-2) yr(-1), consistent with previous estimates.
GEOPHYSICAL RESEARCH LETTERS
(2022)
Article
Environmental Sciences
Victoria Treadaway, Elliot Atlas, Sue Schauffler, Maria Navarro, Rei Ueyama, Leonhard Pfister, Troy Thornberry, Andrew Rollins, James Elkins, Fred Moore, Karen Rosenlof
Summary: Rapid transport by deep convection is an important mechanism for delivering surface emissions of reactive halocarbons and other trace species to the tropical tropopause layer. This study found short-lived halocarbons and other trace gases in the TTL over the western Pacific Ocean that originated from Asia. The measurements indicate an increase in chlorinated organic species and non-methane hydrocarbons, as well as a chemical composition impacted by biofuel/biomass burning and industrial emissions.
JOURNAL OF ATMOSPHERIC CHEMISTRY
(2022)
Article
Engineering, Environmental
Ariana L. Tribby, Justin S. Bois, Stephen A. Montzka, Elliot L. Atlas, Isaac Vimont, Xin Lan, Pieter P. Tans, James W. Elkins, Donald R. Blake, Paul O. Wennberg
Summary: We analyzed global airborne observations to estimate emissions from oil and gas operations. By updating the emissions configuration in a chemical transport model, we were able to simulate the global distribution of propane and ethane and compare it with observed data. We found that emissions in oil-producing basins are dominated by pre-processing activities.
ENVIRONMENTAL SCIENCE & TECHNOLOGY
(2022)
Article
Environmental Sciences
Gisele Krysztofiak, Valery Catoire, Thierry Dudok de Wit, Douglas E. Kinnison, A. R. Ravishankara, Vanessa Brocchi, Elliot Atlas, Heiko Bozem, Roisin Commane, Francesco D'Amato, Bruce Daube, Glenn S. Diskin, Andreas Engel, Felix Friedl-Vallon, Eric Hintsa, Dale F. Hurst, Peter Hoor, Fabrice Jegou, Kenneth W. Jucks, Armin Kleinboehl, Harry Kuellmann, Eric A. Kort, Kathryn McKain, Fred L. Moore, Florian Obersteiner, Yenny Gonzalez Ramos, Tanja Schuck, Geoffrey C. Toon, Silvia Viciani, Gerald Wetzel, Jonathan Williams, Steven C. Wofsy
Summary: This study examines the trends in N2O concentration from the middle troposphere to the middle stratosphere using in situ and remote sensing observations. It finds a long-term increase in global N2O concentration in the MTMS from 1987 to 2018.
Article
Meteorology & Atmospheric Sciences
Sam J. Silva, Susannah M. Burrows, Katherine Calvin, Philip J. Cameron-Smith, Xiaoying Shi, Tian Zhou
Summary: The dry deposition of ozone from the atmosphere to ecosystems plays an important role in connecting atmospheric chemistry and terrestrial biogeochemical processes. A study evaluates the influence of carbon cycle-climate responses on the parameterization of dry deposition using the results of a simulation campaign. Results show that while global annual ozone dry deposition is relatively insensitive to these effects, regional influences can reach up to 10%. The study highlights the significance of accurately representing ozone deposition to snow in Earth System Models and provides recommendations for future simulation campaigns.
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
(2023)
Article
Meteorology & Atmospheric Sciences
Dana L. McGuffin, Philip J. Cameron-Smith, Matthew A. Horsley, Brian J. Bauman, Wim De Vries, Denis Healy, Alex Pertica, Chris Shaffer, Lance M. Simms
Summary: Stellar occultation observations from space provide a fine vertical scale profiling of the stratosphere and mesosphere. These observations have the potential to observe the atmosphere above 30 km and uncover fine-scale phenomena such as atmospheric turbulence. We utilize stellar occultation techniques to retrieve atmospheric properties, including refractivity, density, and temperature, from bending angle measurements obtained by nanosatellites operated by Terran Orbital.
ATMOSPHERIC MEASUREMENT TECHNIQUES
(2023)
Article
Environmental Sciences
Markus Jesswein, Rafael P. Fernandez, Lucas Berna, Alfonso Saiz-Lopez, Jens-Uwe Grooss, Ryan Hossaini, Eric C. Apel, Rebecca S. Hornbrook, Elliot L. Atlas, Donald R. Blake, Stephen Montzka, Timo Keber, Tanja Schuck, Thomas Wagenhaeuser, Andreas Engel
Summary: This study investigates the global seasonal distribution of CH2Br2 and CHBr3 and finds that CH2Br2 shows pronounced seasonality in both hemispheres, while CHBr3 exhibits larger variability and less clear seasonality. The observations and model simulations show good agreement in the lowermost stratosphere, but there is a discrepancy in the southern hemispheric autumn. More extensive observations in the southern hemisphere are needed to fully understand the impact of these substances on lowermost-stratospheric ozone loss.
ATMOSPHERIC CHEMISTRY AND PHYSICS
(2022)
Article
Geosciences, Multidisciplinary
Xue Zheng, Qing Li, Tian Zhou, Qi Tang, Luke P. Van Roekel, Jean-Christophe Golaz, Hailong Wang, Philip Cameron-Smith
Summary: This paper presents the experimental setup and general characteristics of the US Department of Energy's Energy Exascale Earth System Model (E3SMv1.0) in coupled historical and future climate simulations. The study focuses on the regional responses of atmosphere, ocean, sea ice, and land in the highest emission scenario (SSP5-8.5) designed in the Scenario Model Intercomparison Project (ScenarioMlP). The results show that E3SMv1.0 exhibits high surface warming and significant changes in precipitation, runoff, and sea ice in the future projection period.
GEOSCIENTIFIC MODEL DEVELOPMENT
(2022)
Article
Ecology
Yanan Zhao, Dennis Booge, Christa A. Marandino, Cathleen Schlundt, Astrid Bracher, Elliot L. Atlas, Jonathan Williams, Hermann W. Bange
Summary: Our understanding of the biogeochemical cycling of dimethyl sulfide (DMS) in the Peruvian upwelling system is still limited. We conducted oceanic and atmospheric measurements of DMS in this region during two shipborne cruises in December 2012 and October 2015. DMS concentrations in surface waters were influenced by nutrient availability, and no elevated concentrations were found in the oxygen minimum zone off Peru. DMS, DMSP, and DMSO may act as radical scavengers, supported by their negative correlations with NVP ratios. Atmospheric DMS concentrations varied significantly but were primarily driven by seawater DMS. The Peruvian upwelling region was identified as a source of atmospheric DMS, but emissions were moderate compared to adjacent regions.
Article
Environmental Sciences
James Keeble, Birgit Hassler, Antara Banerjee, Ramiro Checa-Garcia, Gabriel Chiodo, Sean Davis, Veronika Eyring, Paul T. Griffiths, Olaf Morgenstern, Peer Nowack, Guang Zeng, Jiankai Zhang, Greg Bodeker, Susannah Burrows, Philip Cameron-Smith, David Cugnet, Christopher Danek, Makoto Deushi, Larry W. Horowitz, Anne Kubin, Lijuan Li, Gerrit Lohmann, Martine Michou, Michael J. Mills, Pierre Nabat, Dirk Olivie, Sungsu Park, Oyvind Seland, Jens Stoll, Karl-Hermann Wieners, Tongwen Wu
Summary: This study evaluates the long-term changes in stratospheric ozone and water vapor in CMIP6 models under different emissions scenarios, highlighting both global and regional patterns. While global mean TCO is projected to recover to 1960s levels in the middle of the 21st century, tropics may not reach the same levels due to various factors including reductions in ozone-depleting substances and changes in tropospheric ozone.
ATMOSPHERIC CHEMISTRY AND PHYSICS
(2021)
Article
Geosciences, Multidisciplinary
Qi Tang, Michael J. Prather, Juno Hsu, Daniel J. Ruiz, Philip J. Cameron-Smith, Shaocheng Xie, Jean-Christophe Golaz
Summary: The new ozone chemistry module O3v2 implemented in E3SMv1 improves simulation performance in terms of stratospheric column ozone, although not as good as the UCI CTM. It enables a more accurate representation of ozone in the lowermost stratosphere and provides key diagnostics for stratosphere-troposphere exchange flux.
GEOSCIENTIFIC MODEL DEVELOPMENT
(2021)