Articles | Volume 18, issue 7
https://doi.org/10.5194/acp-18-4519-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-18-4519-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Nucleation of nitric acid hydrates in polar stratospheric clouds by meteoric material
Alexander D. James
School of Chemistry, University of Leeds, Leeds LS2 9JT, UK
James S. A. Brooke
School of Chemistry, University of Leeds, Leeds LS2 9JT, UK
Thomas P. Mangan
School of Chemistry, University of Leeds, Leeds LS2 9JT, UK
Thomas F. Whale
School of Earth and Environment, University of Leeds, Leeds LS2 9JT,
UK
School of Chemistry, University of Leeds, Leeds LS2 9JT, UK
Benjamin J. Murray
CORRESPONDING AUTHOR
School of Earth and Environment, University of Leeds, Leeds LS2 9JT,
UK
Related authors
Robert Wagner, Alexander D. James, Victoria L. Frankland, Ottmar Möhler, Benjamin J. Murray, John M. C. Plane, Harald Saathoff, Ralf Weigel, and Martin Schnaiter
Atmos. Chem. Phys., 23, 6789–6811, https://doi.org/10.5194/acp-23-6789-2023, https://doi.org/10.5194/acp-23-6789-2023, 2023
Short summary
Short summary
Polar stratospheric clouds (PSCs) play an important role in the depletion of stratospheric ozone. They can consist of different chemical species, including crystalline nitric acid hydrates. We found that mineral dust or meteoric ablation material can efficiently catalyse the formation of a specific phase of nitric acid dihydrate crystals. We determined predominant particle shapes and infrared optical properties of these crystals, which are important inputs for remote sensing detection of PSCs.
Alexander D. James, Finn Pace, Sebastien N. F. Sikora, Graham W. Mann, John M. C. Plane, and Benjamin J. Murray
Atmos. Chem. Phys., 23, 2215–2233, https://doi.org/10.5194/acp-23-2215-2023, https://doi.org/10.5194/acp-23-2215-2023, 2023
Short summary
Short summary
Here, we examine whether several materials of meteoric origin can nucleate crystallisation in stratospheric cloud droplets which would affect ozone depletion. We find that material which could fragment on atmospheric entry without melting is unlikely to be present in high enough concentration in the stratosphere to contribute to observed crystalline clouds. Material which ablates completely then forms a new solid known as meteoric smoke can provide enough nucleation to explain observed clouds.
Joseph Robinson, Martin I. Daily, Polly B. Foster, Jack P. Macklin, James B. McQuaid, Mark D. Tarn, and Benjamin J. Murray
Aerosol Research, 4, 373–396, https://doi.org/10.5194/ar-4-373-2026, https://doi.org/10.5194/ar-4-373-2026, 2026
Short summary
Short summary
Ice formation in many clouds is initiated by airborne particles, which are often measured by collecting them on a filter and washing them into water for analysis. Using controlled laboratory experiments, we show that some of these particles adhere strongly to the filter and are not recovered. As a result, this common method can underestimate how many ice-forming particles are present in the atmosphere.
Ross J. Herbert, Larissa Lacher, Alexander Böhmländer, Mark D. Tarn, Antoine Canzi, Aidan Pantoya, Evelyn Freney, Kristina Höhler, Pia Bogert, Céline Planche, Ping Tian, Michael Adams, Sarah Barr, David Brus, Nicole Büttner, Martin Daily, Konstantinos Doulgeris, Konstantinos Eleftheriadis, Grant Forster, Romy Fösig, Dimitrios G. Georgakopoulos, Maria I. Gini, A. Gannet Hallar, Radovan Krejci, Elke Ludewig, Mauro Mazzola, Ian B. McCubbin, Athanasios Nenes, Tuukka Petäjä, Joseph Robinson, Franziska Vogel, Paul Zieger, Stephen Arnold, Kenneth S. Carslaw, Naruki Hiranuma, Ottmar Möhler, and Benjamin J. Murray
Earth Syst. Sci. Data, 18, 6465–6483, https://doi.org/10.5194/essd-18-6465-2026, https://doi.org/10.5194/essd-18-6465-2026, 2026
Short summary
Short summary
Ice formation in sub-zero clouds is influenced by airborne particles called ice-nucleating particles (INPs), whose concentrations vary substantially over short time and spatial scales. To assess the role of INPs in our climate, a comprehensive and consistent global dataset is essential. Our GloPINE model-ready dataset is a major step in this direction, comprising 36,000 measurements made using a single instrument design (PINE) over 70,000 hours of operation at 20 Northern Hemisphere sites.
Nicole Büttner, Romy Fösig, Alexander Böhmländer, Larissa Lacher, Franziska Vogel, Mark Tarn, Pia Bogert, Jens Nadolny, Benjamin Murray, and Ottmar Möhler
Atmos. Meas. Tech., 19, 5007–5026, https://doi.org/10.5194/amt-19-5007-2026, https://doi.org/10.5194/amt-19-5007-2026, 2026
Short summary
Short summary
We developed a new Python software tool that standardises and automates the analysis of data from a cloud simulation chamber. It identifies ice-forming particles in the atmosphere and ensures consistent data quality through built-in checks, making results more comparable across studies. We also analysed measurement data to provide recommendations for improving instrument reliability and long-term monitoring of atmospheric ice-forming particles. This helps to better understand how clouds behave.
Michael Biggart, Thomas W. Choularton, Martin W. Gallagher, Keith N. Bower, Gary Lloyd, Paul J. Connolly, Benjamin J. Murray, Mark D. Tarn, Erin N. Raif, and Steven J. Abel
EGUsphere, https://doi.org/10.5194/egusphere-2026-1272, https://doi.org/10.5194/egusphere-2026-1272, 2026
Short summary
Short summary
Microphysical processes controlling the phase of mixed-phase clouds in cold air outbreaks (CAOs) are poorly represented by climate models. Of these, secondary ice production (SIP) is a major contributor to uncertainties in the mixed-phase cloud response to warming. We examine observations made in CAOs to understand which SIP processes are dominating and under which conditions. Our results inform future modelling, helping reduce radiative flux biases and uncertainties in climate sensitivity.
Yuwen Li, Wuhu Feng, John M. C. Plane, Tijian Wang, and Martyn P. Chipperfield
Atmos. Chem. Phys., 26, 3621–3635, https://doi.org/10.5194/acp-26-3621-2026, https://doi.org/10.5194/acp-26-3621-2026, 2026
Short summary
Short summary
The space industry is growing rapidly, but its environmental effects remain uncertain. We used a global chemistry-climate model to study how chlorine released by rocket launches could affect the ozone layer and its recovery from past depletion. Even with large growth in launches, global ozone loss remains small but could locally slow the healing of the ozone layer. These findings highlight the need to consider rocket emissions in future environmental policies.
Thomas F. Whale, Sarah L. Barr, and Trystan Surawy-Stepney
EGUsphere, https://doi.org/10.5194/egusphere-2026-680, https://doi.org/10.5194/egusphere-2026-680, 2026
Short summary
Short summary
Droplet-freezing experiments are used to study ice formation in the atmosphere, but standard methods to show uncertainty or test whether two results differ are lacking. We borrow from medical ‘time-to-event’ statistics to add easily-calculated confidence intervals to fraction-frozen curves and derived quantities without binning or assumptions about underlying physics, and adapt a test to judge whether curves differ beyond random variation. This will make comparison of studies easier.
Xinyi Huang, Paul R. Field, Ross J. Herbert, Benjamin J. Murray, Floortje van den Heuvel, Daniel P. Grosvenor, Rachel W. N. Sansom, and Kenneth S. Carslaw
EGUsphere, https://doi.org/10.5194/egusphere-2026-311, https://doi.org/10.5194/egusphere-2026-311, 2026
Short summary
Short summary
Aerosol-cloud interactions and ice formation processes are key to modelling mixed-phase clouds in cold-air outbreaks. However, no studies have investigated the joint effects of these processes. Here, we used perturbed parameter ensembles and model emulators to show that these processes have strongly interacting effects on the properties of cold air outbreak clouds. Single sensitivity tests may therefore provide incomplete information about cloud-controlling factors.
Xinyi Huang, Paul R. Field, Benjamin J. Murray, Daniel P. Grosvenor, Floortje van den Heuvel, and Kenneth S. Carslaw
Atmos. Chem. Phys., 25, 11363–11406, https://doi.org/10.5194/acp-25-11363-2025, https://doi.org/10.5194/acp-25-11363-2025, 2025
Short summary
Short summary
Cold-air outbreak (CAO) clouds play a vital role in climate prediction. This study explores the responses of CAO clouds to aerosols and ice production under different environmental conditions. We found that CAO cloud responses vary with cloud temperature and are strongly controlled by the liquid–ice partitioning in these clouds, suggesting the importance of good representations of cloud microphysics properties to predict the behaviours of CAO clouds in a warming climate.
Declan L. Finney, Alan M. Blyth, Paul R. Field, Martin I. Daily, Benjamin J. Murray, Mengyu Sun, Paul J. Connolly, Zhiqiang Cui, and Steven Böing
Atmos. Chem. Phys., 25, 10907–10929, https://doi.org/10.5194/acp-25-10907-2025, https://doi.org/10.5194/acp-25-10907-2025, 2025
Short summary
Short summary
We present observation-informed modelling from the Deep Convective Microphysics Experiment (DCMEX) to study how environmental conditions and cloud processes affect anvil cloud albedo and radiation. Aerosols influencing cloud droplets or influencing ice formation yield varying radiative effects. We introduce fingerprint metrics to discern these effects. Using detailed observations and modelling, we offer insights into high-cloud radiative effects and feedbacks.
Kathleen A. Alden, Paul Bieber, Anna J. Miller, Nicole Link, Benjamin J. Murray, and Nadine Borduas-Dedekind
Atmos. Chem. Phys., 25, 6179–6195, https://doi.org/10.5194/acp-25-6179-2025, https://doi.org/10.5194/acp-25-6179-2025, 2025
Short summary
Short summary
Lignin and Snomax are surface-active macromolecules that show a relationship between increasing concentrations, decreasing surface tension, and increasing ice-nucleating ability. However, this relationship did not hold for agricultural soil extracts collected in the UK and Canada. To explain this difference, we propose that as the complexity of the sample increases, the hydrophobic interfaces in the bulk compete with the air–water interface.
Ulrike Proske, Michael P. Adams, Grace C. E. Porter, Mark A. Holden, Jaana Bäck, and Benjamin J. Murray
Atmos. Chem. Phys., 25, 979–995, https://doi.org/10.5194/acp-25-979-2025, https://doi.org/10.5194/acp-25-979-2025, 2025
Short summary
Short summary
Ice-nucleating particles (INPs) aid the freezing of water droplets in clouds and thus modify cloud properties. In a campaign in a Finnish boreal forest, biological INPs were observed, despite many of their potential biological sources being snow-covered. We sampled tree-dwelling lichens that were not covered in snow and tested their ice nucleation ability in the laboratory. We found that the lichen harbours INPs, which may be important in similar snowy environments.
Ross J. Herbert, Alberto Sanchez-Marroquin, Daniel P. Grosvenor, Kirsty J. Pringle, Stephen R. Arnold, Benjamin J. Murray, and Kenneth S. Carslaw
Atmos. Chem. Phys., 25, 291–325, https://doi.org/10.5194/acp-25-291-2025, https://doi.org/10.5194/acp-25-291-2025, 2025
Short summary
Short summary
Aerosol particles that help form ice in clouds vary in number and type around the world and with time. However, in many weather and climate models cloud ice is not linked to aerosols that are known to nucleate ice. Here we report the first steps towards representing ice-nucleating particles within the UK Earth System Model. We conclude that in addition to ice nucleation by sea spray and mineral components of soil dust, we also need to represent ice nucleation by the organic components of soils.
Erin N. Raif, Sarah L. Barr, Mark D. Tarn, James B. McQuaid, Martin I. Daily, Steven J. Abel, Paul A. Barrett, Keith N. Bower, Paul R. Field, Kenneth S. Carslaw, and Benjamin J. Murray
Atmos. Chem. Phys., 24, 14045–14072, https://doi.org/10.5194/acp-24-14045-2024, https://doi.org/10.5194/acp-24-14045-2024, 2024
Short summary
Short summary
Ice-nucleating particles (INPs) allow ice to form in clouds at temperatures warmer than −35°C. We measured INP concentrations over the Norwegian and Barents seas in weather events where cold air is ejected from the Arctic. These concentrations were among the highest measured in the Arctic. It is likely that the INPs were transported to the Arctic from distant regions. These results show it is important to consider hemispheric-scale INP processes to understand INP concentrations in the Arctic.
Jianfei Wu, Wuhu Feng, Xianghui Xue, Daniel Robert Marsh, and John Maurice Campbell Plane
Atmos. Chem. Phys., 24, 12133–12141, https://doi.org/10.5194/acp-24-12133-2024, https://doi.org/10.5194/acp-24-12133-2024, 2024
Short summary
Short summary
Metal layers occur in the mesosphere and lower thermosphere region 80–120 km from the ablation of cosmic dust. Nonmigrating diurnal tides are persistent global oscillations. We investigate nonmigrating diurnal tidal variations in metal layers using satellite observations and global climate model simulations; these have not been studied previously due to the limitations of measurements. The nonmigrating diurnal tides in temperature are strongly linked to the corresponding change in metal layers.
Franziska Vogel, Michael P. Adams, Larissa Lacher, Polly B. Foster, Grace C. E. Porter, Barbara Bertozzi, Kristina Höhler, Julia Schneider, Tobias Schorr, Nsikanabasi S. Umo, Jens Nadolny, Zoé Brasseur, Paavo Heikkilä, Erik S. Thomson, Nicole Büttner, Martin I. Daily, Romy Fösig, Alexander D. Harrison, Jorma Keskinen, Ulrike Proske, Jonathan Duplissy, Markku Kulmala, Tuukka Petäjä, Ottmar Möhler, and Benjamin J. Murray
Atmos. Chem. Phys., 24, 11737–11757, https://doi.org/10.5194/acp-24-11737-2024, https://doi.org/10.5194/acp-24-11737-2024, 2024
Short summary
Short summary
Primary ice formation in clouds strongly influences their properties; hence, it is important to understand the sources of ice-nucleating particles (INPs) and their variability. We present 2 months of INP measurements in a Finnish boreal forest using a new semi-autonomous INP counting device based on gas expansion. These results show strong variability in INP concentrations, and we present a case that the INPs we observe are, at least some of the time, of biological origin.
Nina L. H. Kinney, Charles A. Hepburn, Matthew I. Gibson, Daniel Ballesteros, and Thomas F. Whale
Biogeosciences, 21, 3201–3214, https://doi.org/10.5194/bg-21-3201-2024, https://doi.org/10.5194/bg-21-3201-2024, 2024
Short summary
Short summary
Molecules released from plant pollen induce the formation of ice from supercooled water at temperatures warm enough to suggest an underlying function for this activity. In this study we show that ice nucleators are ubiquitous in pollen. We suggest the molecules responsible fulfil some unrelated biological function and nucleate ice incidentally. The ubiquity of ice-nucleating molecules in pollen and particularly active examples reveal a greater potential for pollen to impact weather and climate.
Mark D. Tarn, Bethany V. Wyld, Naama Reicher, Matan Alayof, Daniella Gat, Alberto Sanchez-Marroquin, Sebastien N. F. Sikora, Alexander D. Harrison, Yinon Rudich, and Benjamin J. Murray
Aerosol Research, 2, 161–182, https://doi.org/10.5194/ar-2-161-2024, https://doi.org/10.5194/ar-2-161-2024, 2024
Short summary
Short summary
Ambient ice-nucleating particle (INP) concentrations were measured in Israel, which experiences air masses from a variety of sources. We found that the INP activity is typically dominated by K-feldspar mineral dust but that air masses passing over regions of fertile soils correlated with high INP concentrations and indicators of biological activity. This suggests that these fertile regions could be sporadic sources of warm-temperature biogenic INPs and warrants further study of these areas.
Declan L. Finney, Alan M. Blyth, Martin Gallagher, Huihui Wu, Graeme J. Nott, Michael I. Biggerstaff, Richard G. Sonnenfeld, Martin Daily, Dan Walker, David Dufton, Keith Bower, Steven Böing, Thomas Choularton, Jonathan Crosier, James Groves, Paul R. Field, Hugh Coe, Benjamin J. Murray, Gary Lloyd, Nicholas A. Marsden, Michael Flynn, Kezhen Hu, Navaneeth M. Thamban, Paul I. Williams, Paul J. Connolly, James B. McQuaid, Joseph Robinson, Zhiqiang Cui, Ralph R. Burton, Gordon Carrie, Robert Moore, Steven J. Abel, Dave Tiddeman, and Graydon Aulich
Earth Syst. Sci. Data, 16, 2141–2163, https://doi.org/10.5194/essd-16-2141-2024, https://doi.org/10.5194/essd-16-2141-2024, 2024
Short summary
Short summary
The DCMEX (Deep Convective Microphysics Experiment) project undertook an aircraft- and ground-based measurement campaign of New Mexico deep convective clouds during July–August 2022. The campaign coordinated a broad range of instrumentation measuring aerosol, cloud physics, radar signals, thermodynamics, dynamics, electric fields, and weather. The project's objectives included the utilisation of these data with satellite observations to study the anvil cloud radiative effect.
Larissa Lacher, Michael P. Adams, Kevin Barry, Barbara Bertozzi, Heinz Bingemer, Cristian Boffo, Yannick Bras, Nicole Büttner, Dimitri Castarede, Daniel J. Cziczo, Paul J. DeMott, Romy Fösig, Megan Goodell, Kristina Höhler, Thomas C. J. Hill, Conrad Jentzsch, Luis A. Ladino, Ezra J. T. Levin, Stephan Mertes, Ottmar Möhler, Kathryn A. Moore, Benjamin J. Murray, Jens Nadolny, Tatjana Pfeuffer, David Picard, Carolina Ramírez-Romero, Mickael Ribeiro, Sarah Richter, Jann Schrod, Karine Sellegri, Frank Stratmann, Benjamin E. Swanson, Erik S. Thomson, Heike Wex, Martin J. Wolf, and Evelyn Freney
Atmos. Chem. Phys., 24, 2651–2678, https://doi.org/10.5194/acp-24-2651-2024, https://doi.org/10.5194/acp-24-2651-2024, 2024
Short summary
Short summary
Aerosol particles that trigger ice formation in clouds are important for the climate system but are very rare in the atmosphere, challenging measurement techniques. Here we compare three cloud chambers and seven methods for collecting aerosol particles on filters for offline analysis at a mountaintop station. A general good agreement of the methods was found when sampling aerosol particles behind a whole air inlet, supporting their use for obtaining data that can be implemented in models.
Joel Ponsonby, Leon King, Benjamin J. Murray, and Marc E. J. Stettler
Atmos. Chem. Phys., 24, 2045–2058, https://doi.org/10.5194/acp-24-2045-2024, https://doi.org/10.5194/acp-24-2045-2024, 2024
Short summary
Short summary
Aerosol emissions from aircraft engines contribute to the formation of contrails, which have a climate impact as important as that of aviation’s CO2 emissions. For the first time, we experimentally investigate the freezing behaviour of water droplets formed on jet lubrication oil aerosol. We show that they can activate to form water droplets and discuss their potential impact on contrail formation. Our study has implications for contrails produced by future aircraft engine and fuel technologies.
Stefan Noll, John M. C. Plane, Wuhu Feng, Konstantinos S. Kalogerakis, Wolfgang Kausch, Carsten Schmidt, Michael Bittner, and Stefan Kimeswenger
Atmos. Chem. Phys., 24, 1143–1176, https://doi.org/10.5194/acp-24-1143-2024, https://doi.org/10.5194/acp-24-1143-2024, 2024
Short summary
Short summary
The Earth's nighttime radiation in the range from the near-UV to the near-IR mainly originates between 75 and 105 km and consists of lines of different species, which are important indicators of the chemistry and dynamics at these altitudes. Based on astronomical spectra, we have characterised the structure and variability of a pseudo-continuum of a high number of faint lines and discovered a new emission process in the near-IR. By means of simulations, we identified HO2 as the likely emitter.
Alberto Sanchez-Marroquin, Sarah L. Barr, Ian T. Burke, James B. McQuaid, and Benjamin J. Murray
Atmos. Chem. Phys., 23, 13819–13834, https://doi.org/10.5194/acp-23-13819-2023, https://doi.org/10.5194/acp-23-13819-2023, 2023
Short summary
Short summary
The sources and concentrations of ice-nucleating particles (INPs) in the Arctic are still poorly understood. Here we report aircraft-based INP concentrations and aerosol composition in the western North American Arctic. The concentrations of INPs and all aerosol particles were low. The aerosol samples contained mostly sea salt and dust particles. Dust particles were more relevant for the INP concentrations than sea salt. However, dust alone cannot account for all of the measured INPs.
John M. C. Plane, Jörg Gumbel, Konstantinos S. Kalogerakis, Daniel R. Marsh, and Christian von Savigny
Atmos. Chem. Phys., 23, 13255–13282, https://doi.org/10.5194/acp-23-13255-2023, https://doi.org/10.5194/acp-23-13255-2023, 2023
Short summary
Short summary
The mesosphere or lower thermosphere region of the atmosphere borders the edge of space. It is subject to extreme ultraviolet photons and charged particles from the Sun and atmospheric gravity waves from below, which tend to break in this region. The pressure is very low, which facilitates chemistry involving species in excited states, and this is also the region where cosmic dust ablates and injects various metals. The result is a unique and exotic chemistry.
Jonas Elm, Aladár Czitrovszky, Andreas Held, Annele Virtanen, Astrid Kiendler-Scharr, Benjamin J. Murray, Daniel McCluskey, Daniele Contini, David Broday, Eirini Goudeli, Hilkka Timonen, Joan Rosell-Llompart, Jose L. Castillo, Evangelia Diapouli, Mar Viana, Maria E. Messing, Markku Kulmala, Naděžda Zíková, and Sebastian H. Schmitt
Aerosol Research, 1, 13–16, https://doi.org/10.5194/ar-1-13-2023, https://doi.org/10.5194/ar-1-13-2023, 2023
Robert Wagner, Alexander D. James, Victoria L. Frankland, Ottmar Möhler, Benjamin J. Murray, John M. C. Plane, Harald Saathoff, Ralf Weigel, and Martin Schnaiter
Atmos. Chem. Phys., 23, 6789–6811, https://doi.org/10.5194/acp-23-6789-2023, https://doi.org/10.5194/acp-23-6789-2023, 2023
Short summary
Short summary
Polar stratospheric clouds (PSCs) play an important role in the depletion of stratospheric ozone. They can consist of different chemical species, including crystalline nitric acid hydrates. We found that mineral dust or meteoric ablation material can efficiently catalyse the formation of a specific phase of nitric acid dihydrate crystals. We determined predominant particle shapes and infrared optical properties of these crystals, which are important inputs for remote sensing detection of PSCs.
Alexander D. James, Finn Pace, Sebastien N. F. Sikora, Graham W. Mann, John M. C. Plane, and Benjamin J. Murray
Atmos. Chem. Phys., 23, 2215–2233, https://doi.org/10.5194/acp-23-2215-2023, https://doi.org/10.5194/acp-23-2215-2023, 2023
Short summary
Short summary
Here, we examine whether several materials of meteoric origin can nucleate crystallisation in stratospheric cloud droplets which would affect ozone depletion. We find that material which could fragment on atmospheric entry without melting is unlikely to be present in high enough concentration in the stratosphere to contribute to observed crystalline clouds. Material which ablates completely then forms a new solid known as meteoric smoke can provide enough nucleation to explain observed clouds.
Outi Meinander, Pavla Dagsson-Waldhauserova, Pavel Amosov, Elena Aseyeva, Cliff Atkins, Alexander Baklanov, Clarissa Baldo, Sarah L. Barr, Barbara Barzycka, Liane G. Benning, Bojan Cvetkovic, Polina Enchilik, Denis Frolov, Santiago Gassó, Konrad Kandler, Nikolay Kasimov, Jan Kavan, James King, Tatyana Koroleva, Viktoria Krupskaya, Markku Kulmala, Monika Kusiak, Hanna K. Lappalainen, Michał Laska, Jerome Lasne, Marek Lewandowski, Bartłomiej Luks, James B. McQuaid, Beatrice Moroni, Benjamin Murray, Ottmar Möhler, Adam Nawrot, Slobodan Nickovic, Norman T. O’Neill, Goran Pejanovic, Olga Popovicheva, Keyvan Ranjbar, Manolis Romanias, Olga Samonova, Alberto Sanchez-Marroquin, Kerstin Schepanski, Ivan Semenkov, Anna Sharapova, Elena Shevnina, Zongbo Shi, Mikhail Sofiev, Frédéric Thevenet, Throstur Thorsteinsson, Mikhail Timofeev, Nsikanabasi Silas Umo, Andreas Uppstu, Darya Urupina, György Varga, Tomasz Werner, Olafur Arnalds, and Ana Vukovic Vimic
Atmos. Chem. Phys., 22, 11889–11930, https://doi.org/10.5194/acp-22-11889-2022, https://doi.org/10.5194/acp-22-11889-2022, 2022
Short summary
Short summary
High-latitude dust (HLD) is a short-lived climate forcer, air pollutant, and nutrient source. Our results suggest a northern HLD belt at 50–58° N in Eurasia and 50–55° N in Canada and at >60° N in Eurasia and >58° N in Canada. Our addition to the previously identified global dust belt (GDB) provides crucially needed information on the extent of active HLD sources with both direct and indirect impacts on climate and environment in remote regions, which are often poorly understood and predicted.
Bingkun Yu, Xianghui Xue, Christopher J. Scott, Mingjiao Jia, Wuhu Feng, John M. C. Plane, Daniel R. Marsh, Jonas Hedin, Jörg Gumbel, and Xiankang Dou
Atmos. Chem. Phys., 22, 11485–11504, https://doi.org/10.5194/acp-22-11485-2022, https://doi.org/10.5194/acp-22-11485-2022, 2022
Short summary
Short summary
We present a study on the climatology of the metal sodium layer in the upper atmosphere from the ground-based measurements obtained from a lidar network, the Odin satellite measurements, and a global model of meteoric sodium in the atmosphere. Comprehensively, comparisons show good agreement and some discrepancies between ground-based observations, satellite measurements, and global model simulations.
Alexander D. Harrison, Daniel O'Sullivan, Michael P. Adams, Grace C. E. Porter, Edmund Blades, Cherise Brathwaite, Rebecca Chewitt-Lucas, Cassandra Gaston, Rachel Hawker, Ovid O. Krüger, Leslie Neve, Mira L. Pöhlker, Christopher Pöhlker, Ulrich Pöschl, Alberto Sanchez-Marroquin, Andrea Sealy, Peter Sealy, Mark D. Tarn, Shanice Whitehall, James B. McQuaid, Kenneth S. Carslaw, Joseph M. Prospero, and Benjamin J. Murray
Atmos. Chem. Phys., 22, 9663–9680, https://doi.org/10.5194/acp-22-9663-2022, https://doi.org/10.5194/acp-22-9663-2022, 2022
Short summary
Short summary
The formation of ice in clouds fundamentally alters cloud properties; hence it is important we understand the special aerosol particles that can nucleate ice when immersed in supercooled cloud droplets. In this paper we show that African desert dust that has travelled across the Atlantic to the Caribbean nucleates ice much less well than we might have expected.
Martin I. Daily, Mark D. Tarn, Thomas F. Whale, and Benjamin J. Murray
Atmos. Meas. Tech., 15, 2635–2665, https://doi.org/10.5194/amt-15-2635-2022, https://doi.org/10.5194/amt-15-2635-2022, 2022
Short summary
Short summary
Mineral dust and particles of biological origin are important types of ice-nucleating particles (INPs) that can trigger ice formation of supercooled cloud droplets. Heat treatments are used to detect the presence of biological INPs in samples collected from the environment as the activity of mineral INPs is assumed unchanged, although not fully assessed. We show that the ice-nucleating ability of some minerals can change after heating and discuss how INP heat tests should be interpreted.
Zoé Brasseur, Dimitri Castarède, Erik S. Thomson, Michael P. Adams, Saskia Drossaart van Dusseldorp, Paavo Heikkilä, Kimmo Korhonen, Janne Lampilahti, Mikhail Paramonov, Julia Schneider, Franziska Vogel, Yusheng Wu, Jonathan P. D. Abbatt, Nina S. Atanasova, Dennis H. Bamford, Barbara Bertozzi, Matthew Boyer, David Brus, Martin I. Daily, Romy Fösig, Ellen Gute, Alexander D. Harrison, Paula Hietala, Kristina Höhler, Zamin A. Kanji, Jorma Keskinen, Larissa Lacher, Markus Lampimäki, Janne Levula, Antti Manninen, Jens Nadolny, Maija Peltola, Grace C. E. Porter, Pyry Poutanen, Ulrike Proske, Tobias Schorr, Nsikanabasi Silas Umo, János Stenszky, Annele Virtanen, Dmitri Moisseev, Markku Kulmala, Benjamin J. Murray, Tuukka Petäjä, Ottmar Möhler, and Jonathan Duplissy
Atmos. Chem. Phys., 22, 5117–5145, https://doi.org/10.5194/acp-22-5117-2022, https://doi.org/10.5194/acp-22-5117-2022, 2022
Short summary
Short summary
The present measurement report introduces the ice nucleation campaign organized in Hyytiälä, Finland, in 2018 (HyICE-2018). We provide an overview of the campaign settings, and we describe the measurement infrastructure and operating procedures used. In addition, we use results from ice nucleation instrument inter-comparison to show that the suite of these instruments deployed during the campaign reports consistent results.
Rachel E. Hawker, Annette K. Miltenberger, Jill S. Johnson, Jonathan M. Wilkinson, Adrian A. Hill, Ben J. Shipway, Paul R. Field, Benjamin J. Murray, and Ken S. Carslaw
Atmos. Chem. Phys., 21, 17315–17343, https://doi.org/10.5194/acp-21-17315-2021, https://doi.org/10.5194/acp-21-17315-2021, 2021
Short summary
Short summary
We find that ice-nucleating particles (INPs), aerosols that can initiate the freezing of cloud droplets, cause substantial changes to the properties of radiatively important convectively generated anvil cirrus. The number concentration of INPs had a large effect on ice crystal number concentration while the INP temperature dependence controlled ice crystal size and cloud fraction. The results indicate information on INP number and source is necessary for the representation of cloud glaciation.
Jianfei Wu, Wuhu Feng, Han-Li Liu, Xianghui Xue, Daniel Robert Marsh, and John Maurice Campbell Plane
Atmos. Chem. Phys., 21, 15619–15630, https://doi.org/10.5194/acp-21-15619-2021, https://doi.org/10.5194/acp-21-15619-2021, 2021
Short summary
Short summary
Metal layers occur in the MLT region (80–120 km) from the ablation of cosmic dust. The latest lidar observations show these metals can reach a height approaching 200 km, which is challenging to explain. We have developed the first global simulation incorporating the full life cycle of metal atoms and ions. The model results compare well with lidar and satellite observations of the seasonal and diurnal variation of the metals and demonstrate the importance of ion mass and ion-neutral coupling.
Heather Guy, Ian M. Brooks, Ken S. Carslaw, Benjamin J. Murray, Von P. Walden, Matthew D. Shupe, Claire Pettersen, David D. Turner, Christopher J. Cox, William D. Neff, Ralf Bennartz, and Ryan R. Neely III
Atmos. Chem. Phys., 21, 15351–15374, https://doi.org/10.5194/acp-21-15351-2021, https://doi.org/10.5194/acp-21-15351-2021, 2021
Short summary
Short summary
We present the first full year of surface aerosol number concentration measurements from the central Greenland Ice Sheet. Aerosol concentrations here have a distinct seasonal cycle from those at lower-altitude Arctic sites, which is driven by large-scale atmospheric circulation. Our results can be used to help understand the role aerosols might play in Greenland surface melt through the modification of cloud properties. This is crucial in a rapidly changing region where observations are sparse.
Cited articles
Bardeen, C. G., Toon, O. B., Jensen, E. J., Marsh, D. R., and Harvey, V. L.:
Numerical simulations of the three-dimensional distribution of meteoric dust
in the mesosphere and upper stratosphere, J. Geophys. Res.-Atmos., 113,
D17202, https://doi.org/10.1029/2007JD009515, 2008.
Beyer, K. D. and Hansen, A. R.: Phase diagram of the nitric acid/water
system:? implications for polar stratospheric clouds, J. Phys. Chem. A, 106,
10275–10284, https://doi.org/10.1021/jp025535o, 2002.
Biermann, U. M., Presper, T., Koop, T., Mößinger, J., Crutzen, P. J.,
and Peter, T.: The unsuitability of meteoritic and other nuclei for polar
stratospheric cloud freezing, Geophys. Res. Lett., 23, 1693–1696, https://doi.org/10.1029/96gl01577, 1996.
Bogdan, A., Molina, M. J., Kulmala, M., MacKenzie, A. R., and Laaksonen, A.:
Study of finely divided aqueous systems as an aid to understanding the
formation mechanism of polar stratospheric clouds: Case of HNO3/H2O
and H2SO4/H2O systems, J. Geophys. Res.-Atmos., 108, 4302, https://doi.org/10.1029/2002JD002605, 2003.
Brakebusch, M., Randall, C. E., Kinnison, D. E., Tilmes, S., Santee, M. L.,
and Manney, G. L.: Evaluation of Whole Atmosphere Community Climate Model
simulations of ozone during Arctic winter 2004–2005, J. Geophy. Res.-Atmos., 118, 2673–2688,
https://doi.org/10.1002/jgrd.50226, 2013.
Broadley, S. L., Murray, B. J., Herbert, R. J., Atkinson, J. D., Dobbie, S.,
Malkin, T. L., Condliffe, E., and Neve, L.: Immersion mode heterogeneous ice
nucleation by an illite rich powder representative of atmospheric mineral
dust, Atmos. Chem. Phys., 12, 287–307,
https://doi.org/10.5194/acp-12-287-2012, 2012.
Brooke, J. S. A., Feng, W., Carrillo-Sánchez, J. D., Mann, G. W., James,
A. D., Bardeen, C. G., and Plane, J. M. C.: Meteoric smoke deposition in the
polar regions: A comparison of measurements with global atmospheric models,
J. Geophys. Res.-Atmos., 122, 11112–111130, https://doi.org/10.1002/2017JD027143, 2017.
Carrillo-Sánchez, J. D., Nesvorný, D., Pokorný, P., Janches, D.,
and Plane, J. M. C.: Sources of cosmic dust in the Earth's atmosphere,
Geophys. Res. Lett., 43, 11979–11986, https://doi.org/10.1002/2016GL071697, 2016.
Clarke, R., Jarosevich, E., Mason, B., Nelen, J., Gomez, M., and Hyde, J. R.:
The Allende, Mexico, Meteoroite Shower, Smithsonian Institution Press,
Washington, 1971.
Clegg, S. L., Brimblecombe, P., and Wexler, A. S.: Thermodynamic model of the
system H+-NH -SO -NO -H2O at
tropospheric temperatures, J. Phys. Chem. A, 102, 2137–2154,
https://doi.org/10.1021/jp973042r, 1998.
Cziczo, D. J., Thomson, D. S., and Murphy, D. M.: Ablation, flux, and
atmospheric implications of meteors inferred from stratospheric aerosol,
Science, 291, 1772–1775, https://doi.org/10.1126/science.1057737, 2001.
Dhomse, S. S., Saunders, R. W., Tian, W., Chipperfield, M. P., and Plane, J.
M. C.: Plutonium-238 observations as a test of modeled transport and surface
deposition of meteoric smoke particles, Geophys. Res. Lett., 40, 4454–4458,
2013.
Frankland, V. L., James, A. D., Feng, W., and Plane, J. M. C.: The uptake of
HNO3 on meteoric smoke analogues, J. Atmos. Sol.-Terr. Phy., 127,
150–160, https://doi.org/10.1016/j.jastp.2015.01.010, 2015.
Gómez-Martín, J. C., Bones, D. L., Carrillo-Sánchez, J. D.,
James, A. D., Trigo-Rodríguez, J. M., B. Fegley, J., and Plane, J. M.
C.: Novel experimental simulations of the atmospheric injection of meteoric
metals, Astrophys. J., 836, 212–238, 2017.
Grothe, H., Tizek, H., and Ortega, I. K.: Metastable nitric acid
hydrates-possible constituents of polar stratospheric clouds?, Faraday
Discss., 137, 223–234, 2008.
Harrison, A. D., Whale, T. F., Carpenter, M. A., Holden, M. A., Neve, L.,
O'Sullivan, D., Vergara Temprado, J., and Murray, B. J.: Not all feldspars
are equal: a survey of ice nucleating properties across the feldspar group of
minerals, Atmos. Chem. Phys., 16, 10927–10940,
https://doi.org/10.5194/acp-16-10927-2016, 2016.
Herbert, R. J., Murray, B. J., Whale, T. F., Dobbie, S. J., and Atkinson, J.
D.: Representing time-dependent freezing behaviour in immersion mode ice
nucleation, Atmos. Chem. Phys., 14, 8501–8520,
https://doi.org/10.5194/acp-14-8501-2014, 2014.
Hiranuma, N., Hoffmann, N., Kiselev, A., Dreyer, A., Zhang, K., Kulkarni, G.,
Koop, T., and Möhler, O.: Influence of surface morphology on the immersion
mode ice nucleation efficiency of hematite particles, Atmos. Chem. Phys., 14,
2315–2324, https://doi.org/10.5194/acp-14-2315-2014, 2014.
Hiranuma, N., Augustin-Bauditz, S., Bingemer, H., Budke, C., Curtius, J.,
Danielczok, A., Diehl, K., Dreischmeier, K., Ebert, M., Frank, F., Hoffmann,
N., Kandler, K., Kiselev, A., Koop, T., Leisner, T., Möhler, O., Nillius,
B., Peckhaus, A., Rose, D., Weinbruch, S., Wex, H., Boose, Y., DeMott, P. J.,
Hader, J. D., Hill, T. C. J., Kanji, Z. A., Kulkarni, G., Levin, E. J. T.,
McCluskey, C. S., Murakami, M., Murray, B. J., Niedermeier, D., Petters, M.
D., O'Sullivan, D., Saito, A., Schill, G. P., Tajiri, T., Tolbert, M. A.,
Welti, A., Whale, T. F., Wright, T. P., and Yamashita, K.: A comprehensive
laboratory study on the immersion freezing behavior of illite NX particles: a
comparison of 17 ice nucleation measurement techniques, Atmos. Chem. Phys.,
15, 2489–2518, https://doi.org/10.5194/acp-15-2489-2015, 2015.
Höpfner, M., Luo, B. P., Massoli, P., Cairo, F., Spang, R., Snels, M., Di
Donfrancesco, G., Stiller, G., von Clarmann, T., Fischer, H., and Biermann,
U.: Spectroscopic evidence for NAT, STS, and ice in MIPAS infrared limb
emission measurements of polar stratospheric clouds, Atmos. Chem. Phys., 6,
1201–1219, https://doi.org/10.5194/acp-6-1201-2006, 2006.
Hoyle, C. R., Engel, I., Luo, B. P., Pitts, M. C., Poole, L. R., Grooß,
J.-U., and Peter, T.: Heterogeneous formation of polar stratospheric clouds
– Part 1: Nucleation of nitric acid trihydrate (NAT), Atmos. Chem. Phys.,
13, 9577–9595, https://doi.org/10.5194/acp-13-9577-2013, 2013.
Iannarelli, R. and Rossi, M. J.: The mid-IR absorption cross sections of
α- and β-NAT (HNO3 ⋅ 3H2O) in the range 170 to
185 K and of metastable NAD (HNO3 ⋅ 2H2O) in the range 172 to
182 K, J. Geophys. Res.-Atmos., 120, 11707–11727, https://doi.org/10.1002/2015JD023903,
2015.
James, A. D., Frankland, V. L. F., Trigo-Rodríguez, J. M.,
Alonso-Azcárate, J., Gómez Martín, J.-C., and Plane, J. M. C.:
Synthesis and characterisation of analogues for interplanetary dust and
meteoric smoke particles, J. Atmos. Sol.-Terr. Phy., 162, 178–191,
https://doi.org/10.1016/j.jastp.2016.08.011, 2017.
James, A. D., Brooke, J. S. A.,
Mangan, T. P., Whale, T. F., Plane, J. M. C., and
Murray, B. J.: Numerical data pertaining to “Nucleation of nitric acid hydrates
in polar stratospheric clouds by meteoric material”, University of Leeds research data management,
available at: https://doi.org/10.5518/312, last access:
3 April 2018.
Jessberger, E. K., Stephan, T., Rost, D., Arndt, P., Maetz, M., Stadermann,
F. J., Brownlee, D. E., Bradley, J. P., and Kurat, G.: Properties of
interplanetary dust: information from collected samples, in: Interplanetary
Dust, edited by: Grün, E., Gustafson, B. Å. S., Dermott, S., and
Fechtig, H., Springer Berlin Heidelberg, Berlin, Heidelberg, 253–294, 2001.
Knopf, D. A.: Do NAD and NAT form in liquid stratospheric aerosols by
pseudoheterogeneous nucleation?, J. Phys. Chem. A, 110, 5745–5750,
https://doi.org/10.1021/jp055376j, 2006.
Knopf, D. A., Koop, T., Luo, B. P., Weers, U. G., and Peter, T.: Homogeneous
nucleation of NAD and NAT in liquid stratospheric aerosols: insufficient to
explain denitrification, Atmos. Chem. Phys., 2, 207–214,
https://doi.org/10.5194/acp-2-207-2002, 2002.
Lambert, A., Santee, M. L., and Livesey, N. J.: Interannual variations of
early winter Antarctic polar stratospheric cloud formation and nitric acid
observed by CALIOP and MLS, Atmos. Chem. Phys., 16, 15219–15246,
https://doi.org/10.5194/acp-16-15219-2016, 2016.
Mann, G. W., Carslaw, K. S., Chipperfield, M. P., Davies, S., and Eckermann,
S. D.: Large nitric acid trihydrate particles and denitrification caused by
mountain waves in the Arctic stratosphere, J. Geophys. Res.-Atmos., 110,
D08202, https://doi.org/10.1029/2004JD005271, 2005.
Marsh, D. R., Mills, M. J., Kinnison, D. E., Lamarque, J. F., Calvo, N., and
Polvani, L. M.: Climate Change from 1850 to 2005 Simulated in CESM1 (WACCM),
J. Climate, 26, 7372–7391, https://doi.org/10.1175/jcli-d-12-00558.1, 2013.
Martin, S. T.: Phase transitions of aqueous atmospheric particles, Chem.
Rev., 100, 3403–3454, https://doi.org/10.1021/cr990034t, 2000.
Meilinger, S. K., Koop, T., Luo, B. P., Huthwelker, T., Carslaw, K. S.,
Krieger, U., Crutzen, P. J., and Peter, T.: Size-dependent stratospheric
droplet composition in Lee wave temperature fluctuations and their potential
role in PSC freezing, Geophys. Res. Lett., 22, 3031–3034,
https://doi.org/10.1029/95GL03056, 1995.
Möhler, O., Bunz, H., and Stetzer, O.: Homogeneous nucleation rates of
nitric acid dihydrate (NAD) at simulated stratospheric conditions – Part II:
Modelling, Atmos. Chem. Phys., 6, 3035–3047,
https://doi.org/10.5194/acp-6-3035-2006, 2006.
Murphy, D. M., Froyd, K. D., Schwarz, J. P., and Wilson, J. C.: Observations
of the chemical composition of stratospheric aerosol particles, Q. J. Roy. Meteor. Soc., 140, 1269–1278, 2014.
Murray, B. J. and Bertram, A. K.: Inhibition of solute crystallisation in
aqueous H+-NH4+-SO -H2O droplets, Phys. Chem. Chem.
Phys., 10, 3287–3301, https://doi.org/10.1039/B802216J, 2008.
Murray, B. J., O'Sullivan, D., Atkinson, J. D., and Webb, M. E.: Ice
nucleation by particles immersed in supercooled cloud droplets, Chem. Soc.
Rev., 41, 6519–6554, https://doi.org/10.1039/C2CS35200A, 2012.
Neely, R. R., English, J. M., Toon, O. B., Solomon, S., Mills, M., and
Thayer, J. P.: Implications of extinction due to meteoritic smoke in the
upper stratosphere, Geophys. Res. Lett., 38, L24808, https://doi.org/10.1029/2011gl049865,
2011.
Niedermeier, D., Hartmann, S., Clauss, T., Wex, H., Kiselev, A., Sullivan, R.
C., DeMott, P. J., Petters, M. D., Reitz, P., Schneider, J., Mikhailov, E.,
Sierau, B., Stetzer, O., Reimann, B., Bundke, U., Shaw, R. A., Buchholz, A.,
Mentel, T. F., and Stratmann, F.: Experimental study of the role of
physicochemical surface processing on the IN ability of mineral dust
particles, Atmos. Chem. Phys., 11, 11131–11144,
https://doi.org/10.5194/acp-11-11131-2011, 2011.
Peter, T. and Grooß, J. U.: Polar stratospheric clouds and sulfate
aerosol particles: Microphysics, denitrification and heterogeneous chemistry,
Chapter 4, in: Stratospheric Ozone Depletion and Climate Change, edited by:
Muller, R., The Royal Society of Chemistry,
Cambridge, UK, 108–144, 2012.
Plane, J. M. C., Feng, W., and Dawkins, E. C. M.: The mesosphere and metals:
Chemistry and changes, Chem. Rev., 115, 4497–4541, https://doi.org/10.1021/cr500501m,
2015.
Pruppacher, H. R. and Klett, J. D.: Microphysics of clouds and precipitation,
D. Reidel Publishing Company, Dordrecht,
Holland, 1978.
Rienecker, M. M., Suarez, M. J., Gelaro, R., Todling, R., Bacmeister, J.,
Liu, E., Bosilovich, M. G., Schubert, S. D., Takacs, L., Kim, G. K., Bloom,
S., Chen, J. Y., Collins, D., Conaty, A., Da Silva, A., Gu, W., Joiner, J.,
Koster, R. D., Lucchesi, R., Molod, A., Owens, T., Pawson, S., Pegion, P.,
Redder, C. R., Reichle, R., Robertson, F. R., Ruddick, A. G., Sienkiewicz,
M., and Woollen, J.: MERRA: NASA's Modern-Era Retrospective Analysis for
Research and Applications, J. Climate, 24, 3624–3648,
https://doi.org/10.1175/jcli-d-11-00015.1, 2011.
Russell, S. S., Zolensky, M., Righter, K., Folco, L., Jones, R., Connolly, H.
C., Grady, M. M., and Grossman, J. N.: The meteoritical bulletin, No. 89,
2005 September, Meteorit. Plan. Sci., 40, A201–A263,
https://doi.org/10.1111/j.1945-5100.2005.tb00425.x, 2005.
Saunders, R. W. and Plane, J. M. C.: A laboratory study of meteor smoke
analogues: Composition, optical properties and growth kinetics, J. Atmos.
Sol.-Terr. Phy., 68, 2182–2202,
https://doi.org/10.1016/j.jastp.2006.09.006, 2006.
Saunders, R. W., Dhomse, S., Tian, W. S., Chipperfield, M. P., and Plane, J.
M. C.: Interactions of meteoric smoke particles with sulphuric acid in the
Earth's stratosphere, Atmos. Chem. Phys., 12, 4387–4398,
https://doi.org/10.5194/acp-12-4387-2012, 2012.
Solomon, S.: Stratospheric ozone depletion: A review of concepts and history,
Rev. Geophys., 37, 275–316, https://doi.org/10.1029/1999RG900008, 1999.
Solomon, S., Kinnison, D., Bandoro, J., and Garcia, R.: Simulation of polar
ozone depletion: An update, J. Geophys. Res.-Atmos., 120, 7958–7974,
https://doi.org/10.1002/2015JD023365, 2015.
Stetzer, O., Möhler, O., Wagner, R., Benz, S., Saathoff, H., Bunz, H., and
Indris, O.: Homogeneous nucleation rates of nitric acid dihydrate (NAD) at
simulated stratospheric conditions – Part I: Experimental results, Atmos.
Chem. Phys., 6, 3023–3033, https://doi.org/10.5194/acp-6-3023-2006, 2006.
Subasinghe, D., Campbell-Brown, M. D., and Stokan, E.: Physical
characteristics of faint meteors by light curve and high-resolution
observations, and the implications for parent bodies, Mon. Not. Royal Astro.
Soc., 457, 1289–1298, 2016.
Taylor, S., Matrajt, G., and Guan, Y.: Fine-grained precursors dominate the
micrometeorite flux, Meteorit. Planet. Sci., 47, 550–564,
https://doi.org/10.1111/j.1945-5100.2011.01292.x, 2012.
Toon, O. B., Turco, R. P., Hamill, P., Kiang, C. S., and Whitten, R. C.:
One-dimensional model describing aerosol formation and evolution in the
stratosphere. 2. Sensitivity studies and comparison with observations, J.
Atmos. Sci., 36, 718–736,
https://doi.org/10.1175/1520-0469(1979)036<0718:aodmda>2.0.co;2, 1979.
Toon, O. B., Turco, R. P., Westphal, D., Malone, R., and Liu, M.: A
Multidimensional Model for Aerosols: Description of Computational Analogs, J.
Atmos. Sci., 45, 2123–2144,
https://doi.org/10.1175/1520-0469(1988)045<2123:ammfad>2.0.co;2, 1988.
Turco, R. P., Hamill, P., Toon, O. B., Whitten, R. C., and Kiang, C. S.:
One-dimensional model describing aerosol formation and evolution in the
stratosphere. 1. Physical processes and mathematical analogs, J. Atmos. Sci.,
36, 699–717,
https://doi.org/10.1175/1520-0469(1979)036<0699:aodmda>2.0.co;2, 1979.
Voigt, C., Schlager, H., Luo, B. P., Dörnbrack, A., Roiger, A., Stock, P.,
Curtius, J., Vössing, H., Borrmann, S., Davies, S., Konopka, P., Schiller,
C., Shur, G., and Peter, T.: Nitric Acid Trihydrate (NAT) formation at low
NAT supersaturation in Polar Stratospheric Clouds (PSCs), Atmos. Chem. Phys.,
5, 1371–1380, https://doi.org/10.5194/acp-5-1371-2005, 2005.
Wegner, T., Grooß, J.-U., von Hobe, M., Stroh, F., Suminska-Ebersoldt,
O., Volk, C. M., Hösen, E., Mitev, V., Shur, G., and Müller, R.:
Heterogeneous chlorine activation on stratospheric aerosols and clouds in the
Arctic polar vortex, Atmos. Chem. Phys., 12, 11095–11106,
https://doi.org/10.5194/acp-12-11095-2012, 2012.
Weigel, R., Volk, C. M., Kandler, K., Hösen, E., Günther, G., Vogel, B.,
Grooß, J.-U., Khaykin, S., Belyaev, G. V., and Borrmann, S.: Enhancements
of the refractory submicron aerosol fraction in the Arctic polar vortex:
feature or exception?, Atmos. Chem. Phys., 14, 12319–12342,
https://doi.org/10.5194/acp-14-12319-2014, 2014.
Weisberg, M. K., Smith, C., Benedix, G., Folco, L., Righter, K., Zipfel, J.,
Yamaguchi, A., and Aoudjehane, H. C.: The Meteoritical Bulletin, No. 94,
September 2008, Meteorit. Planet. Sci., 43, 1551–1584,
https://doi.org/10.1111/j.1945-5100.2008.tb01027.x, 2008.
Weiss, F., Kubel, F., Gálvez, Ó., Hoelzel, M., Parker, S. F., Baloh,
P., Iannarelli, R., Rossi, M. J., and Grothe, H.: Metastable nitric acid
trihydrate in ice clouds, Angew. Chem. Int. Ed., 55, 3276–3280,
https://doi.org/10.1002/anie.201510841, 2016.
Whale, T. F., Murray, B. J., O'Sullivan, D., Wilson, T. W., Umo, N. S.,
Baustian, K. J., Atkinson, J. D., Workneh, D. A., and Morris, G. J.: A
technique for quantifying heterogeneous ice nucleation in microlitre
supercooled water droplets, Atmos. Meas. Tech., 8, 2437–2447,
https://doi.org/10.5194/amt-8-2437-2015, 2015.
Whale, T. F., Holden, M. A., Kulak, A. N., Kim, Y. Y., Meldrum, F. C.,
Christenson, H. K., and Murray, B. J.: The role of phase separation and
related topography in the exceptional ice-nucleating ability of alkali
feldspars, Phys. Chem. Chem. Phys., 19, 31186–31193,
https://doi.org/10.1039/C7CP04898J, 2017.
Wise, M. E., Brooks, S. D., Garland, R. M., Cziczo, D. J., Martin, S. T., and
Tolbert, M. A.: Solubility and freezing effects of Fe2+ and Mg2+ in
H2SO4 solutions representative of upper tropospheric and lower
stratospheric sulfate particles, J. Geophys. Res.-Atmos., 108, 4434, https://doi.org/10.1029/2003JD003420, 2003.
Short summary
Crystal nucleation in polar stratospheric clouds (PSCs) has a direct impact on stratospheric chemistry and ozone. However, the mechanism of nucleation has been unclear for decades, limiting prediction of the response of ozone to atmospheric changes. We experimentally demonstrate that meteoric material can trigger nucleation heterogeneously and this can produce observed crystal concentrations in PSCs. This discovery paves the way to robust modelling of past and future trends in PSCs and ozone.
Crystal nucleation in polar stratospheric clouds (PSCs) has a direct impact on stratospheric...
Altmetrics
Final-revised paper
Preprint