Peer Review10.5194/egusphere-2023-1835-ac1
Reply on RC1
Xiaopu Lyu
- 13 Mar 2024
About: The article was published on 13 Mar 2024.
read more
Chat with Paper
AI Agents for this Paper
Find similar papers on Google Scholar, PubMed and Arxiv
Write a critical review of this paper
Analyze citations of this paper to find unaddressed research gaps
Figures

Figure 3: Time series of representative OA markers, PM1 compositions, trace gases, and meteorological conditions. Blue, orange, 565 and red bars at the top represent marine, coastal, and continental air, respectively. Shaded areas represent the periods with troughs. Missing data are due to instrument maintenance. 
Figure 4: Average diurnal patterns of nine representative OA markers. Tip of the top (bottom) whisker is the 95th (5th) percentile. Top and bottom of the box denote the 75th and 25th percentiles, respectively. Line inside the box represents the median value, and 570 the mean value is indicated by red square and triangle (excluding data on June 14th – 15th for 2-MGA only). 
Figure 5: Diurnal patterns of 2-MT1 in different scenarios (a) and the comparisons of temperature (b), UV (c), 2-MT1/2-MTs ratio (d), and LWC (e) between the marine air with and without troughs. Shaded areas represent 95% confidence intervals. 
Figure 1: Location of the sampling site and the surrounding environment. Background maps are adapted from ArcGIS and 560 © Google Earth. 
Figure 7: Contributions of individual OA sources to PM1-OM: time series of bihourly data (a); averages for the scenarios of different air masses (b); and diurnal variations (c). 580 
Figure 2: Correlations between OA molecular markers with R2 not lower than 0.6. Bold are the representative species that we focus on in this study. Full names of the abbreviations are given in Table S2.
References
Evolution of Organic Aerosols in the Atmosphere
Jose L. Jimenez,Manjula R. Canagaratna,Neil M. Donahue,André S. H. Prévôt,Qi Zhang,Jesse H. Kroll,Peter F. DeCarlo,James Allan,Hugh Coe,Nga L. Ng,Allison C. Aiken,Kenneth S. Docherty,Ingrid M. Ulbrich,Andrew P. Grieshop,Allen L. Robinson,Jonathan Duplissy,Jared D. Smith,Kevin R. Wilson,V. A. Lanz,Christoph Hueglin,Yele Sun,Yele Sun,Jian Tian,Ari Laaksonen,Tomi Raatikainen,Tomi Raatikainen,J. Rautiainen,Petri Vaattovaara,Mikael Ehn,Markku Kulmala,Markku Kulmala,Jason Tomlinson,Don R. Collins,Michael J. Cubison,Edward J. Dunlea,J. A. Huffman,Timothy B. Onasch,M. R. Alfarra,Paul I. Williams,Keith Bower,Yutaka Kondo,Johannes Schneider,Frank Drewnick,Stephan Borrmann,S. Weimer,Kenneth L. Demerjian,D. Salcedo,L. Cottrell,Robert J. Griffin,Akinori Takami,Takao Miyoshi,Shiro Hatakeyama,Akio Shimono,J. Y. Sun,Y. M. Zhang,Katja Dzepina,Joel R. Kimmel,Donna Sueper,J. T. Jayne,Scott C. Herndon,A. Trimborn,Leah R. Williams,Ezra C. Wood,Ann M. Middlebrook,Charles E. Kolb,Urs Baltensperger,Douglas R. Worsnop +66 more
TL;DR: A unifying model framework describing the atmospheric evolution of OA that is constrained by high–time-resolution measurements of its composition, volatility, and oxidation state is presented, which can serve as a basis for improving parameterizations in regional and global models.
Aerosols, climate, and the hydrological cycle
TL;DR: Human activities are releasing tiny particles (aerosols) into the atmosphere that enhance scattering and absorption of solar radiation, which can lead to a weaker hydrological cycle, which connects directly to availability and quality of fresh water, a major environmental issue of the 21st century.
Atmospheric aerosols: composition, transformation, climate and health effects.
TL;DR: The current state of knowledge, major open questions, and research perspectives on the properties and interactions of atmospheric aerosols and their effects on climate and human health are outlined.
2.4K
Formation of Secondary Organic Aerosols Through Photooxidation of Isoprene
Magda Claeys,Bim Graham,Gyorgy Vas,Wu Wang,Reinhilde Vermeylen,V. A. Pashynska,Jan Cafmeyer,Pascal Guyon,Meinrat O. Andreae,Paulo Artaxo,Willy Maenhaut +10 more
TL;DR: Detailed organic analysis of natural aerosols from the Amazonian rain forest showed considerable quantities of previously unobserved polar organic compounds, which were identified as a mixture of two diastereoisomeric 2-methyltetrols: 2-methylthreitol and 2- methylerythritol, which can be explained by OH radical–initiated photooxidation of isoprene.
1.5K
Reactive intermediates revealed in secondary organic aerosol formation from isoprene
Jason D. Surratt,Arthur W. H. Chan,Nathan C. Eddingsaas,Man Nin Chan,C. L. Loza,A. J. Kwan,S. P. Hersey,Richard C. Flagan,Paul O. Wennberg,John H. Seinfeld +9 more
TL;DR: In this article, the role of epoxydiols of isoprene and methacryloylperoxynitrate (MPAN) in the formation of secondary organic aerosol (SOA) was identified.
1K