the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Strong particle production and condensational growth in the upper troposphere sustained by biogenic VOCs from the canopy of the Amazon Basin
- 1Minerva Research Group, Max Planck Institute for Chemistry, 55128 Mainz, Germany
- 2Multiphase Chemistry Department, Max Planck Institute for Chemistry, 55128 Mainz, Germany
- 3Max Planck Institute for Chemistry, 55128 Mainz, Germany
- 4Scripps Institution of Oceanography, University of California, San Diego, La Jolla, CA, USA
- 5Institute of Inorganic and Analytical Chemistry, Johannes Gutenberg University Mainz, Mainz, Germany
- 6Experimental Aerosol and Cloud Microphysics Department, Leibniz Institute for Tropospheric Research, Leipzig, Germany
- 7Faculty of Physics and Earth Sciences, Leipzig Institute for Meteorology, Leipzig University, Leipzig, Germany
- 8Institute of Physics, University of São Paulo, São Paulo, Brazil
- 1Minerva Research Group, Max Planck Institute for Chemistry, 55128 Mainz, Germany
- 2Multiphase Chemistry Department, Max Planck Institute for Chemistry, 55128 Mainz, Germany
- 3Max Planck Institute for Chemistry, 55128 Mainz, Germany
- 4Scripps Institution of Oceanography, University of California, San Diego, La Jolla, CA, USA
- 5Institute of Inorganic and Analytical Chemistry, Johannes Gutenberg University Mainz, Mainz, Germany
- 6Experimental Aerosol and Cloud Microphysics Department, Leibniz Institute for Tropospheric Research, Leipzig, Germany
- 7Faculty of Physics and Earth Sciences, Leipzig Institute for Meteorology, Leipzig University, Leipzig, Germany
- 8Institute of Physics, University of São Paulo, São Paulo, Brazil
Abstract. Nucleation and condensation associated with biogenic volatile organic compounds (BVOCs) are important aerosol formation pathways, yet their contribution to the upper tropospheric aerosols remains inconclusive, hindering the understanding of aerosol climate effects. Here, we develop new schemes describing these organic aerosol formation processes in the WRF-Chem model and investigate their impact on the abundance of cloud condensation nuclei (CCN) in the upper troposphere (UT) over the Amazon Basin. We find that the new schemes significantly increase the simulated CCN number concentrations in the UT (e.g., up to ~400 cm-3 at 0.52 % supersaturation) and greatly improve the agreement with the aircraft observations. Organic condensation enhances the simulated CCN concentration by 90 % through promoting particle growth, while organic nucleation, by replenishing new particles, contributes an additional 14 %. Deep convection determines the rate of these organic aerosol formation processes in the UT through controlling the upward transport of biogenic precursors (i.e., BVOCs). This finding emphasizes the importance of the biosphere-atmosphere coupling in regulating upper tropospheric aerosol concentrations over the tropical forest and calls for attention to its potential role in anthropogenic climate change.
Yunfan Liu et al.
Status: final response (author comments only)
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RC1: 'Comment on acp-2022-530', Anonymous Referee #1, 23 Aug 2022
This manuscript compares simulations from the WRF-Chem model along with field-campaign data to study nucleation and growth in the upper troposphere above the Amazon. The authors conclude that BVOCs from the Amazon, transported through deep convection to the UT, are key to nucleation and growth in this UT region. I have several issues that I feel need to be addressed prior to final publication.
Comments
Why did this manuscript need to be as short as it is? I would appreciate at least the key methods being moved to the main text. It was strange to need to go to the SI to find out what the “binary nucleation” scheme was given that this is a nucleation & growth manuscript (and the findings greatly depend on the initial nucleation scheme).
I believe that organics being the key missing ingredient in growing particles to CCN sizes in the UT above the Amazon is likely a robust finding (achieved through closure for both OA mass and CCN number). However, I do not believe that the findings about the role of organics-only nucleation are robust, and I believe these findings are overstated. The base WRF-Chem simulations had only a single, very old binary nucleation “scheme” (Wexler 1994 only gives the critical H2SO4 concentration required for nucleation to initiate, one still needs to assume a nucleation rate!). No recent binary or ternary schemes (e.g., Dunne) were investigated, nor organic-sulfuric nucleation (e.g., Riccobono with the Yu temperature correction). How can we say with confidence that organics-only nucleation dominates in the UT above the Amazon? We can’t. The fractional increases in the CN and CCN concentrations due to the organics-only scheme is entirely dependent on Wexler 1994 being the starting point. Please soften these findings to have the effect of “we find the organics-only nucleation can reproduce CN and CCN concentrations, but in the absence of testing other schemes, we cannot say definitively if organics-only nucleation dominates in the UT above the Amazon.”
Throughout the manuscript, values of concentrations, rates-per-volume, and the condensation sink are given without stating if the values are for local temperature and pressure or at STP. This information is critical since a lot of the values are for 8 km, far from STP (and sometimes are put next to mixing ratios that do not depend on T&P).
L190: 1e^-3 cm^-3 s^-1. Is this supposed to be 1x10^-3 cm^-3 s^-1 (or equivalently 1E-3 cm^-3 s^-1)? Very weird to use base e for scientific notation.
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RC2: 'Comment on acp-2022-530', Eimear Dunne, 09 Sep 2022
This manuscript describes a set of simulations using the WRF-Chem model to investigate the impact of organic nucleation above the Amazon, and compares their findings with aircraft observations. The authors conclude that organic nucleation is the dominant pathway in the UT in this region.
I see that the other referee has already recommended my nucleation parameterisation, so I might as well put my name on this comment! (In response to my fellow referee: I think the reason the manuscript itself is so short is that it has been submitted to ACP Letters.) Sorry for missing the deadline, but I generally get things done at the last minute anyway, and my niece was born on Wednesday which was both a delight and a distraction!
Many of my concerns have been addressed by Referee #1, so I will start with minor cosmetic issues:
- the value 1 e^{-3} on line 190 is definitely wrong somehow, and probably meant to read 1E-3 or equivalent
-Figure A4 (a) would benefit from having a log scale on the x-axis, maybe as an extra panel
- It is claimed that Figure A5 shows a fair agreement with observations, but A5 only shows simulated values - please support your claim by also plotting the relevant observations
With those issues out of the way, it's time to address my main concern: the Wexler et al. (1994) nucleation parameterisation. I understand why the paper did not update the default nucleation scheme in WRF-Chem; after all, the authors were already implementing a new nucleation scheme, and it makes sense to compare it to the existing set-up. This is especially true for a model like WRF, where there are so many different configurations available. So I don't think it would be even slightly reasonable to suggest rejecting the paper on these grounds, but I do think that there needs to be more acknowledgement of how a nucleation parameterisation affects CCN in the simulated upper troposphere. The Wexler et al. (1994) publication explicitly states:
"The number of particles produced by this nucleation operator is somewhat arbitrary [...] Any error produced by this treatment is mitigated in the SoCAB because the vast majority of the aerosol loading is due to primary emission and condensation of secondary organic compounds. In locations where nucleation is more significant, this treatment may not be sufficiently accurate."
In the upper troposphere, nucleation is the only local source of aerosols. If the real conditions being simulated are actually saturated with respect to freshly nucleated particles, and the default nucleation parameterisation under-predicts the true nucleation rate significantly, then changing to any parameterisation which predicts a value close to the saturation limit will improve predictions; but it cannot then be concluded that the nucleation pathway is the dominant one in that region, even if that is the case in reality.
I would agree with Referee #1 that the conclusions ought to be softened. If any nucleation scheme that was known to be more robust in the UT had been used, I would have been happy to accept the conclusions as they stand. However, I would also be happy to discuss implementing the Dunne et al. (2016) scheme in WRF-Chem with the authors, if they would be interested in a future collaboration where their stronger conclusions might yet be validated!
Finally, to give some purely positive feedback: I was very pleased with the set of simulations used in this experiment, as they would have constituted an excellent comparison had the default WRF nucleation mechanism been more suitable. I was also happy to see the extension of the size bins available in MOSAIC, as the default configuration is not at all suited to nucleation simulations.
Yunfan Liu et al.
Yunfan Liu et al.
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