Complex experiment on studying the microphysical, chemical,  and optical properties of aerosol particles and estimating the contribution of atmospheric aerosol-to-earth radiation budget

Matvienko, Gennadii G.; Belan, B. D.; Panchenko, Mikhail V.; Romanovskii, О. А.; Сакерин, С. М.; Kabanov, Dmitry M.; Turchinovich, S. A.; Turchinovich, Yu. S.; Eremina, T. A.; Kozlov, V. S.; Terpugova, Svetlana A.; Полькин, В. В.; Yausheva, Elena P.; Chernov, D. G.; Zhuravleva, T. B.; Bedareva, T. V.; Odintsov, S. L.; Burlakov, V. D.; Nevzorov, Aleksey V.; Arshinov, M.; Ivlev, G. A.; Savkin, D. E.; Fofonov, A. V.; Gladkikh, V. A.; Kamardin, A. P.; Balin, Yu. S.; Kokhanenko, Grigorii; Penner, Ioganes E.; Самойлова, С. В.; Antokhin, P. N.; Arshinova, V. G.; Davydov, Denis; Козлов, А. В.; Pestunov, D. A.; Rasskazchikova, T. M.; Simonenkov, D. V.; Sklyadneva, T. K.; Tolmachev, Gennadii N.; Belan, Sergey; Shmargunov, V. P.; Kozlov, A. S.; Malyshkin, S. B.

doi:10.5194/amt-8-4507-2015

Cited by 31 publications

(16 citation statements)

References 19 publications

(17 reference statements)

Supporting

Mentioning

Contrasting

Order By: Relevance

“…; Matvienko et al, 2015). It is representative of a background boreal environment and is situated on the bank of River Ob, 60 km west of the city of Tomsk.…”

Section: Rural Sitesmentioning

confidence: 99%

Global analysis of continental boundary layer new particle formation based on long-term measurements

Nieminen¹,

Kerminen²,

Petäj̈ä³

et al. 2018

Preprint

Self Cite

View full text Add to dashboard Cite

Atmospheric new particle formation (NPF) is an important phenomenon in terms of the global particle number concentrations. Here we investigated the frequency of NPF, formation rates of 10 nm particles and growth rates in the size range of 10-25 nm using at least one year of aerosol number size-distribution observations at 36 different locations around the world. The majority of these measurement sites are in the Northern Hemisphere. We found that the NPF frequency has a strong seasonal variability, taking place on about 30% of the days in March-May and on about 10% of the days in December-February. The median formation rate of 10 nm particles varies by about three orders of magnitude (0.01-10 cm −3 s −1 ) and the growth rate by about an order of magnitude (1-10 nm h −1 ). The smallest values of both formation and growth rates were observed at polar sites and the largest ones in urban environments or anthropogenically influenced rural sites. The correlation between the NPF event frequency and the particle formation and growth rate was at best moderate between the different measurement sites, as well as between the sites belonging to a certain environmental regime. For a better understanding of atmospheric NPF and its regional importance, we would need more observational data from different urban areas in practically all parts of the world, from additional remote and rural locations in Northern America, Asia and most of the Southern Hemisphere (especially Australia), from polar areas, and from at least a few locations over the oceans.

show abstract

“…; Matvienko et al, 2015). It is representative of a background boreal environment and is situated on the bank of River Ob, 60 km west of the city of Tomsk.…”

Section: Rural Sitesmentioning

confidence: 99%

Global analysis of continental boundary layer new particle formation based on long-term measurements

Nieminen¹,

Kerminen²,

Petäj̈ä³

et al. 2018

Preprint

Self Cite

View full text Add to dashboard Cite

show abstract

“…The experiments performed [2] have shown the complete correspondence of the prototype specifications to the technical assignment.…”

Section: Introductionmentioning

confidence: 99%

“…The prototype consists of the following main parts: Gas-analysis unit; aerosol unit; actinometric unit; airlines of communications; meteorological unit; and interface, control, and data processing unit. 2 , NO x , and O 3 gas analyzers (1, 2, 3, 4, and 5, respectively); ultrasonic anemometers (6); temperature and humidity sensors inside a radiation protective case (7); automated precipitation gauge at a rod (8); pyranometers at actinometric holder (9); atmospheric pressure sensor (10); aerosol diffusion spectrometer (11); optical aerosol spectrometer (12); nephelometer (13) The following components are provided in the prototype for monitoring trace gases: Greenhouse gas analyzer (CO 2 , CH 4 , and H 2 O) (1); CO analyzer (2); gas analyzers for chemically active gases (SO 2 , NO x , and O 3 ) (3, 4, and 5, respectively); high-pressure tanks filled with calibration gas mixtures (CO 2 , CH 4 , and CO) (19 and 20); high-pressure tank filled with a reference gas mixture (21); calibration SO 2 and NO 2 microstream sources (26 and 27); airflow distributors (17 and 18); and sampling devices (15, 24, 25, 28, 29, 30, 32, 33, 34, and 35). Main specifications of the prototype are given in [2].…”

Section: Introductionmentioning

confidence: 99%

Development of Remote and Contact Techniques for Monitoring the Atmospheric Composition, Structure, and Dynamics

Belan

Balin

Banakh

et al. 2017

Proceedings of the Scientific-Practical Conference "Research and Development - 2016"

Self Cite

View full text Add to dashboard Cite

Prototypes of a typical automated station for monitoring the atmospheric composition and state, as well as lidars and sodars, have been designed and manufactured within the project, which are to be the components of monitoring stations. Experimental tests of the instruments confirmed their designed-in specifications and functions. For contact measurements of air parameters, a complex air monitoring station and an aerosol multiwave diffusion spectrometer have been also designed and manufactured in accordance with technical assignment requirements. The measurement results have shown a continuous increase in the concentrations of

show abstract

“…The satellite data were received by the 2.4 XLB satellite data reception station (Orbital Systems, USA) put into operation at IAO SB RAS in 2011 [21]. The information from the station allows comparison between the satellite data and SLS lidar sounding data.…”

Section: Iasi/metopmentioning

confidence: 99%

Intercomparison of Ozone Vertical Profile Measurements by Differential Absorption Lidar and IASI/MetOp Satellite in the Upper Troposphere–Lower Stratosphere

Dolgii

Nevzorov

et al. 2017

Remote Sensing

View full text Add to dashboard Cite

This paper introduces the technique of retrieving the profiles of vertical distribution of ozone considering temperature and aerosol correction in DIAL sounding of the atmosphere. The authors determine wavelengths, which are promising for measurements of ozone profiles in the upper troposphere-lower stratosphere. An ozone differential absorption lidar is designed for the measurements. The results of applying the developed technique to the retrieval of the vertical profiles of ozone considering temperature and aerosol correction in the altitude range 6-15 km in DIAL sounding of the atmosphere confirm the prospects of ozone sounding at selected wavelengths of 341 and 299 nm with the proposed lidar. The 2015 ozone profiles retrieved were compared with satellite IASI data and the Kruger model.

show abstract

Complex experiment on studying the microphysical, chemical, and optical properties of aerosol particles and estimating the contribution of atmospheric aerosol-to-earth radiation budget

Cited by 31 publications

References 19 publications

Global analysis of continental boundary layer new particle formation based on long-term measurements

Global analysis of continental boundary layer new particle formation based on long-term measurements

Development of Remote and Contact Techniques for Monitoring the Atmospheric Composition, Structure, and Dynamics

Intercomparison of Ozone Vertical Profile Measurements by Differential Absorption Lidar and IASI/MetOp Satellite in the Upper Troposphere–Lower Stratosphere

Contact Info

Product

Resources

About