Articles | Volume 15, issue 5
https://doi.org/10.5194/acp-15-2313-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/acp-15-2313-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| Highlight paper
| 
03 Mar 2015
Research article | Highlight paper |
| 03 Mar 2015
Persistent after-effects of heavy rain on concentrations of ice nuclei and rainfall suggest a biological cause
E. K. Bigg
11 Wesley St., Elanora Heights, NSW 2101, Australia
S. Soubeyrand
INRA, UR546 Biostatistics and Spatial Processes, 84914 Avignon, France
C. E. Morris
CORRESPONDING AUTHOR
INRA, UR0407 Pathologie Végétale, 84143 Montfavet, France
Dept. Plant Sciences and Plant Pathology, Montana State University, Bozeman, MT 59717-3150, USA
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45 citations as recorded by crossref.
- Characterization of free amino acids, bacteria and fungi in size-segregated atmospheric aerosols in boreal forest: seasonal patterns, abundances and size distributions A. Helin et al. 10.5194/acp-17-13089-2017
- Airborne soil organic particles generated by precipitation B. Wang et al. 10.1038/ngeo2705
- Contrasting local and long-range-transported warm ice-nucleating particles during an atmospheric river in coastal California, USA A. Martin et al. 10.5194/acp-19-4193-2019
- Active microorganisms thrive among extremely diverse communities in cloud water P. Amato et al. 10.1371/journal.pone.0182869
- Full Issue PDF 10.1094/PBIOMES-2-2
- Survival and ice nucleation activity of Pseudomonas syringae strains exposed to simulated high-altitude atmospheric conditions G. de Araujo et al. 10.1038/s41598-019-44283-3
- Bioaerosols and atmospheric ice nuclei in a Mediterranean dryland: community changes related to rainfall K. Tang et al. 10.5194/bg-19-71-2022
- One-year study of airborne sugar compounds: Cross-interpretation with other chemical species and meteorological conditions F. Oduber et al. 10.1016/j.atmosres.2020.105417
- Influence of rain on the abundance of bioaerosols in fine and coarse particles C. Rathnayake et al. 10.5194/acp-17-2459-2017
- Airborne bacteria in the atmosphere: Presence, purpose, and potential W. Smets et al. 10.1016/j.atmosenv.2016.05.038
- Bioaerosols in the Earth system: Climate, health, and ecosystem interactions J. Fröhlich-Nowoisky et al. 10.1016/j.atmosres.2016.07.018
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- Applying the multi-level perspective to climate geoengineering: Sociotechnical bottlenecks for negative emissions and cloud seeding technologies K. Herman & B. Sovacool 10.1016/j.erss.2024.103637
- Atmospheric Processing and Variability of Biological Ice Nucleating Particles in Precipitation at Opme, France G. Pouzet et al. 10.3390/atmos8110229
- Overview of biological ice nucleating particles in the atmosphere S. Huang et al. 10.1016/j.envint.2020.106197
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- Antibiotic resistance genes in bioaerosols: Emerging, non-ignorable and pernicious pollutants P. Chen et al. 10.1016/j.jclepro.2022.131094
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- Ice nucleation active bacteria in precipitation are genetically diverse and nucleate ice by employing different mechanisms K. Failor et al. 10.1038/ismej.2017.124
- Cultivable halotolerant ice-nucleating bacteria and fungi in coastal precipitation C. Beall et al. 10.5194/acp-21-9031-2021
- Rainfall drives atmospheric ice-nucleating particles in the coastal climate of southern Norway F. Conen et al. 10.5194/acp-17-11065-2017
- Ultrafine particles over Eastern Australia: an airborne survey W. Junkermann & J. Hacker 10.3402/tellusb.v67.25308
- Bioaerosol field measurements: Challenges and perspectives in outdoor studies T. Šantl-Temkiv et al. 10.1080/02786826.2019.1676395
- Sources of organic ice nucleating particles in soils T. Hill et al. 10.5194/acp-16-7195-2016
- Influence of the ambient humidity on the concentration of natural deposition-mode ice-nucleating particles M. López & E. Ávila 10.5194/acp-16-927-2016
- Comprehensive insights into advances in ambient bioaerosols sampling, analysis and factors influencing bioaerosols composition B. Sajjad et al. 10.1016/j.envpol.2023.122473
- Ground level ice nuclei particle measurements including Saharan dust events at a Po Valley rural site (San Pietro Capofiume, Italy) F. Belosi et al. 10.1016/j.atmosres.2016.11.012
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- Atmospheric ice nuclei concentration measurements over a high altitude-station in the Western Ghats, India V. Kumar et al. 10.1016/j.atmosres.2019.104795
- Characterization of bacterial diversity and ice-nucleating ability during different monsoon seasons over a southern tropical Indian region M. Akila et al. 10.1016/j.atmosenv.2018.08.026
- Phytobiomes Contribute to Climate Processes that Regulate Temperature, Wind, Cloud Cover, and Precipitation C. Morris 10.1094/PBIOMES-12-17-0050-P
- Bacteria in atmospheric waters: Detection, characteristics and implications W. Hu et al. 10.1016/j.atmosenv.2018.02.026
- High-Flow-Rate Impinger for the Study of Concentration, Viability, Metabolic Activity, and Ice-Nucleation Activity of Airborne Bacteria T. Šantl-Temkiv et al. 10.1021/acs.est.7b01480
- Mapping Rainfall Feedback to Reveal the Potential Sensitivity of Precipitation to Biological Aerosols C. Morris et al. 10.1175/BAMS-D-15-00293.1
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- Variations of ice nuclei concentration induced by rain and snowfall within a local forested site in Japan K. Hara et al. 10.1016/j.atmosenv.2015.12.009
- An Unknown Maximum Lag‐Correlation Between Rainfall and Aerosols at 140–160 Minutes P. Alpert et al. 10.1029/2020GL089334
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- Microbial ice nucleators scavenged from the atmosphere during simulated rain events R. Hanlon et al. 10.1016/j.atmosenv.2017.05.030
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Discussed (final revised paper)
Latest update: 21 Nov 2024
Short summary
We show that atmospheric load of ice nuclei is enhanced for up to 20 days after key rainfall events. The rate of enhancement decreases exponentially with time. Rainfall quantity and frequency are increased for a similar duration and with similar exponential decreases thereby supporting the notion of rainfall feedback.
We reveal series of significant feedback in rainfall patterns across Australia over the past century and marked changes in feedback patterns, and we indicate their locations.
We show that atmospheric load of ice nuclei is enhanced for up to 20 days after key rainfall...
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