Comparative Analysis of Hygroscopic Properties of Atmospheric Aerosols at ZOTTO Siberian Background Station during Summer and Winter Campaigns of 2011

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Comparative Analysis of Hygroscopic Properties of Atmospheric Aerosols at ZOTTO Siberian Background Station during Summer and Winter Campaigns of 2011. / Ryshkevich, T. I.; Mironov, G. N.; Mironova, S. Yu.; Vlasenko, S. S.; Chi, X.; Andreae, M. O.; Mikhailov, E. F.

In: IZVESTIYA. ATMOSPHERIC AND OCEANIC PHYSICS, Vol. 51, No. 5, 2015, p. 512-519.

Research output: Contribution to journal › Article › peer-review

BibTeX

@article{736d0bee296a4de88dd09b3c1f063d05,

title = "Comparative Analysis of Hygroscopic Properties of Atmospheric Aerosols at ZOTTO Siberian Background Station during Summer and Winter Campaigns of 2011",

abstract = "The results of measurements of hygroscopic properties and chemical analysis of atmospheric aerosol samples collected from June 10 to 20 and December 15 to 25, 2011, at the ZOTTO background sta tions (60.8° N, 89.35° E) in Central Siberia are presented. The sorption properties of aerosols are studied with the help of a differential analyzer of absorbed water mass in the relative humidity range of 5 to 99%. It has been found that the hygroscopic growth factor of aerosol particles collected during the winter campaign is on average 45% higher than that of the aerosol collected in the summer campaign, which leads to a 40% decrease in the critical supersaturation threshold of cloud activation of particles. The measurement data are analyzed and parameterized using a new approach that takes into account the concentration effects in the particle–water vapor system at low humidities. Based on the chemical analysis, the content of watersoluble substancesin the winter sample is 2.5 times higher than in the summer sample.",

keywords = "гигроскопические свойства, облачные ядра конденсации, состав атмосферного аэрозоля, бореальные леса",

author = "Ryshkevich, {T. I.} and Mironov, {G. N.} and Mironova, {S. Yu.} and Vlasenko, {S. S.} and X. Chi and Andreae, {M. O.} and Mikhailov, {E. F.}",

year = "2015",

doi = "DOI: 10.7868/S0002351515050119",

language = "English",

volume = "51",

pages = "512--519",

journal = "Izvestiya, Atmospheric and Oceanic Physics",

issn = "0001-4338",

publisher = "МАИК {"}Наука/Интерпериодика{"}",

number = "5",

}

RIS

TY - JOUR

T1 - Comparative Analysis of Hygroscopic Properties of Atmospheric Aerosols at ZOTTO Siberian Background Station during Summer and Winter Campaigns of 2011

AU - Ryshkevich, T. I.

AU - Mironov, G. N.

AU - Mironova, S. Yu.

AU - Vlasenko, S. S.

AU - Chi, X.

AU - Andreae, M. O.

AU - Mikhailov, E. F.

PY - 2015

Y1 - 2015

N2 - The results of measurements of hygroscopic properties and chemical analysis of atmospheric aerosol samples collected from June 10 to 20 and December 15 to 25, 2011, at the ZOTTO background sta tions (60.8° N, 89.35° E) in Central Siberia are presented. The sorption properties of aerosols are studied with the help of a differential analyzer of absorbed water mass in the relative humidity range of 5 to 99%. It has been found that the hygroscopic growth factor of aerosol particles collected during the winter campaign is on average 45% higher than that of the aerosol collected in the summer campaign, which leads to a 40% decrease in the critical supersaturation threshold of cloud activation of particles. The measurement data are analyzed and parameterized using a new approach that takes into account the concentration effects in the particle–water vapor system at low humidities. Based on the chemical analysis, the content of watersoluble substancesin the winter sample is 2.5 times higher than in the summer sample.

AB - The results of measurements of hygroscopic properties and chemical analysis of atmospheric aerosol samples collected from June 10 to 20 and December 15 to 25, 2011, at the ZOTTO background sta tions (60.8° N, 89.35° E) in Central Siberia are presented. The sorption properties of aerosols are studied with the help of a differential analyzer of absorbed water mass in the relative humidity range of 5 to 99%. It has been found that the hygroscopic growth factor of aerosol particles collected during the winter campaign is on average 45% higher than that of the aerosol collected in the summer campaign, which leads to a 40% decrease in the critical supersaturation threshold of cloud activation of particles. The measurement data are analyzed and parameterized using a new approach that takes into account the concentration effects in the particle–water vapor system at low humidities. Based on the chemical analysis, the content of watersoluble substancesin the winter sample is 2.5 times higher than in the summer sample.

KW - гигроскопические свойства

KW - облачные ядра конденсации

KW - состав атмосферного аэрозоля

KW - бореальные леса

U2 - DOI: 10.7868/S0002351515050119

DO - DOI: 10.7868/S0002351515050119

M3 - Article

VL - 51

SP - 512

EP - 519

JO - Izvestiya, Atmospheric and Oceanic Physics

JF - Izvestiya, Atmospheric and Oceanic Physics

SN - 0001-4338

IS - 5

ER -

ID: 3948669