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1. Transient Response of the Southern Ocean to Changing Ozone: Regional Responses and Physical Mechanisms

   https://doi.org/10.1175/JCLI-D-16-0474.1  

   Seviour, William J. ; Gnanadesikan, Anand ; Waugh, Darryn ; Pradal, Marie-Aude ( April 2017 , Journal of Climate)
2. Ozone Transport‐Radiation Feedbacks in the Tropical Tropopause Layer

   https://doi.org/10.1029/2019GL084679  

   Charlesworth, Edward J. ; Birner, Thomas ; Albers, John R. ( December 2019 , Geophysical Research Letters)
3. Stratospheric Ozone and Climate Forcing Sensitivity to Cruise Altitudes for Fleets of Potential Supersonic Transport Aircraft

   https://doi.org/10.1029/2021JD034971  

   Zhang, Jun ; Wuebbles, Donald ; Kinnison, Douglas ; Baughcum, Steven L. ( August 2021 , Journal of Geophysical Research: Atmospheres)
4. Dynamics of ENSO-driven stratosphere-to-troposphere transport of ozone over North America

   https://doi.org/10.5194/acp-22-13035-2022  

   Albers, John R. ; Butler, Amy H. ; Langford, Andrew O. ; Elsbury, Dillon ; Breeden, Melissa L. ( January 2022 , Atmospheric Chemistry and Physics)

   Abstract. The El Niño–Southern Oscillation (ENSO) is known to modulate the strength and frequency of stratosphere-to-troposphere transport (STT) of ozone over the Pacific–North American region during late winter to early summer. Dynamical processes that have been proposed to account for this variability include variations in the amount of ozone in the lowermoststratosphere that is available for STT and tropospheric circulation-relatedvariations in the frequency and geographic distribution of individual STTevents. Here we use a large ensemble of Whole Atmosphere Community Climate Model(WACCM) simulations (forced by sea-surface temperature (SST) boundaryconditions consistent with each phase of ENSO) to show that variability inlower-stratospheric ozone and shifts in the Pacific tropospheric jetconstructively contribute to the amount of STT of ozone in the NorthAmerican region during both ENSO phases. In terms of stratosphericvariability, ENSO drives ozone anomalies resembling the Pacific–NorthAmerican teleconnection pattern that span much of the lower stratospherebelow 50 hPa. These ozone anomalies, which dominate over other ENSO-drivenchanges in the Brewer–Dobson circulation (including changes due to both thestratospheric residual circulation and quasi-isentropic mixing), stronglymodulate the amount of ozone available for STT transport. As a result,during late winter (February–March), the stratospheric ozone response to theteleconnections constructively reinforces anomalous ENSO-jet-driven STT ofozone. However, as ENSO forcing weakens asmore »spring progresses into summer(April–June), the direct effects of the ENSO-jet-driven STT transportweaken. Nevertheless, the residual impacts of the teleconnections on theamount of ozone in the lower stratosphere persist, and these anomalies inturn continue to cause anomalous STT of ozone. These results should provehelpful for interpreting the utility of ENSO as a subseasonal predictor ofboth free-tropospheric ozone and the probability of stratospheric ozoneintrusion events that may cause exceedances in surface air qualitystandards.« less
5. Intrathecal antibody distribution in the rat brain: surface diffusion, perivascular transport and osmotic enhancement of delivery: Mechanisms of intrathecal antibody transport

   https://doi.org/10.1113/JP275105  

   Pizzo, Michelle E. ; Wolak, Daniel J. ; Kumar, Niyanta N. ; Brunette, Eric ; Brunnquell, Christina L. ; Hannocks, Melanie-Jane ; Abbott, N. Joan ; Meyerand, M. Elizabeth ; Sorokin, Lydia ; Stanimirovic, Danica B. ; et al ( February 2018 , The Journal of Physiology)