The NOx-Limiting Regime of Photochemical Ozone Generation in a Weakly Polluted Convective Boundary Layer: Observations at the ZOTTO Tall Tower Observatory in Central Siberia, 2007–2015     

Moiseenko  K. B.  Berezina  E. V.  Vasileva  A. V.  Shtabkin  Yu. A.  Skorokhod  A. I.  Elanskii  N. F.  Belikov  I. B. 《Doklady Earth Sciences》2019,487(2):981-985

Doklady Earth Sciences - Estimates of the photochemical ozone generation rate, PQ, and the ozone production efficiency (OPE) per molecule of NOx (=NO + NO2), ∆P, are obtained for the region...  相似文献   

Concentration and Isotopic Composition of Methane,Associated Gases,and Black Carbon over Russian Arctic Seas (Shipborne Measurements)     

Pankratova  N. V.  Belikov  I. B.  Belousov  V. A.  Kopeikin  V. M.  Skorokhod  A. I.  Shtabkin  Yu. A.  Malafeev  G. V.  Flint  M. V. 《Oceanology》2020,60(5):593-602

Oceanology - In Russian Arctic seas, observations of surface methane concentrations (CH4), ozone, nitrogen and carbon oxides, as well as the content of $${{\delta...  相似文献   

Regional Photochemical Surface-Ozone Sources in Europe and Western Siberia     

K. B. Moiseenko  Yu. A. Shtabkin  E. V. Berezina  A. I. Skorokhod 《Izvestiya Atmospheric and Oceanic Physics》2018,54(6):545-557

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Sources of and variations in tropospheric CO in Central Siberia: Numerical experiments and observations at the Zotino Tall Tower Observatory     

Yu. A. Shtabkin  K. B. Moiseenko  A. I. Skorokhod  A. V. Vasileva  M. Heimann 《Izvestiya Atmospheric and Oceanic Physics》2016,52(1):45-56

Contributions of climatically significant natural and anthropogenic emission sources in northern Eurasia to seasonal carbon monoxide (CO) variations observed at the Zotino Tall Tower Observatory (ZOTTO) in Central Siberia in 2007–2011 have quantitatively been estimated using the GEOS-Chem chemical transport model. It is shown that the formation of a stable continental pollution plume from sources in Western Europe, European Russia and southern Siberia during winter plays an important role in the regional balance of surface CO and allows one to explain 55–80% of the amplitude of the CO annual cycle observed at the ZOTTO station (~70–90 ppbv). During the warm period, the effect of the anthropogenic factor is weakly pronounced, and the background concentration of CO is regulated, first and foremost, by the oxidation of biogenic volatile organic compounds and fire activity in the region.  相似文献