30-year lidar observations of the stratospheric aerosol layer state over Tomsk (Western Siberia, Russia)

被引:30
|
作者
Zuev, Vladimir V. [1 ,2 ,3 ]
Burlakov, Vladimir D. [4 ]
Nevzorov, Aleksei V. [4 ]
Pravdin, Vladimir L. [1 ]
Savelieva, Ekaterina S. [1 ]
Gerasimov, Vladislav V. [1 ,2 ]
机构
[1] Inst Monitoring Climat & Ecol Syst SB RAS, Tomsk 634055, Russia
[2] Tomsk State Univ, Tomsk 634050, Russia
[3] Tomsk Polytech Univ, Tomsk 634050, Russia
[4] VE Zuev Inst Atmospher Opt SB RAS, Tomsk 634055, Russia
基金
俄罗斯科学基金会;
关键词
VOLCANIC AEROSOL; LONG-TERM; ERUPTION; OZONE; IMPACT; CLOUD; CLIMATOLOGY; CHEMISTRY; DYNAMICS; PLUME;
D O I
10.5194/acp-17-3067-2017
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
There are only four lidar stations in the world which have almost continuously performed observations of the stratospheric aerosol layer (SAL) state over the last 30 years. The longest time series of the SAL lidar measurements have been accumulated at the Mauna Loa Observatory (Hawaii) since 1973, the NASA Langley Research Center (Hampton, Virginia) since 1974, and Garmisch-Partenkirchen (Germany) since 1976. The fourth lidar station we present started to perform routine observations of the SAL parameters in Tomsk (56.48 degrees N, 85.05 degrees E, Western Siberia, Russia) in 1986. In this paper, we mainly focus on and discuss the stratospheric background period from 2000 to 2005 and the causes of the SAL perturbations over Tomsk in the 2006-2015 period. During the last decade, volcanic aerosol plumes from tropical Mt. Manam, Soufriere Hills, Rabaul, Merapi, Nabro, and Kelut and extratropical (northern) Mt. Okmok, Kasatochi, Redoubt, Sarychev Peak, Eyjafjallajokull, and Grimsvotn were detected in the stratosphere over Tomsk. When it was possible, we used the NOAA HYSPLIT trajectory model to assign aerosol layers observed over Tomsk to the corresponding volcanic eruptions. The trajectory analysis highlighted some surprising results. For example, in the cases of the Okmok, Kasatochi, and Eyjafjallajokull eruptions, the HYSPLIT air mass backward trajectories, started from altitudes of aerosol layers detected over Tomsk with a lidar, passed over these volcanoes on their eruption days at altitudes higher than the maximum plume altitudes given by the Smithsonian Institution Global Volcanism Program. An explanation of these facts is suggested. The role of both tropical and northern volcanic eruptions in volcanogenic aerosol loading of the midlatitude stratosphere is also discussed. In addition to volcanoes, we considered other possible causes of the SAL perturbations over Tomsk, i.e., the polar stratospheric cloud (PSC) events and smoke plumes from strong forest fires. At least two PSC events were detected in 1995 and 2007. We also make an assumption that the Kelut volcanic eruption (Indonesia, February 2014) could be the cause of the SAL perturbations over Tomsk during the first quarter of 2015.
引用
收藏
页码:3067 / 3081
页数:15
相关论文
共 50 条
  • [41] Ten years (1986-1995) of lidar observations of temporal and vertical structure of stratospheric aerosols over Siberia
    Zuev, VV
    Burlakov, VD
    El'nikov, AV
    JOURNAL OF AEROSOL SCIENCE, 1998, 29 (10) : 1179 - 1187
  • [42] LIDAR OBSERVATIONS OF STRATOSPHERIC AEROSOL OVER MENLO-PARK, CALIFORNIA - OCTOBER 1972, MARCH 1974
    VIEZEE, W
    RUSSELL, PB
    HAKE, RD
    TRANSACTIONS-AMERICAN GEOPHYSICAL UNION, 1974, 55 (12): : 1126 - 1127
  • [43] Multiwavelength lidar observations of the decay phase of the stratospheric aerosol layer produced by the eruption of Mount Pinatubo in June 1991
    Kent, GS
    Hansen, GM
    APPLIED OPTICS, 1998, 37 (18): : 3861 - 3872
  • [44] Multiwavelength lidar observations of the decay phase of the stratospheric aerosol layer produced by the eruption of Mount Pinatubo in June 1991
    Science and Technology Corporation, 101 Research Drive, Hampton, VA 23666-1340, United States
    Appl. Opt., 18 (3861-3872):
  • [45] Aerosol disturbances of the stratosphere over Tomsk according to data of lidar observations in volcanic activity period 2006-2011
    Makeev, Andrey P.
    Burlakov, Vladimir D.
    Dolgii, Sergey I.
    Nevzorov, Aleksey V.
    Trifonov, Dmitry A.
    EIGHTEENTH INTERNATIONAL SYMPOSIUM ON ATMOSPHERIC AND OCEAN OPTICS/ATMOSPHERIC PHYSICS, 2012, 8696
  • [46] Evaluation of Outdoor Thermal Comfort Conditions in Northern Russia over 30-year Period (Arkhangelsk Region)
    Konstantinov, Pavel
    Shartova, Natalia
    Varentsov, Mikhail
    Revich, Boris
    GEOGRAPHICA PANNONICA, 2020, 24 (04): : 252 - 260
  • [47] ARRIVAL OF PINATUBO DISTURBANCES IN THE STRATOSPHERIC AEROSOL LAYER OVER FORT-COLLINS, CO, OBSERVED BY A LIDAR AT 589 NM
    CHEN, H
    YU, JR
    SHE, CY
    APPLIED PHYSICS B-PHOTOPHYSICS AND LASER CHEMISTRY, 1992, 55 (02): : 159 - 163
  • [48] Decreased ozone content over Western Siberia and Tomsk in winter 2017-2018 according to lidar measurements and Aura OMI and MLS data
    Bazhenov, O. E.
    24TH INTERNATIONAL SYMPOSIUM ON ATMOSPHERIC AND OCEAN OPTICS: ATMOSPHERIC PHYSICS, 2018, 10833
  • [49] Dynamics of development and relaxation of stratospheric aerosol layer after the Mt. Pinatubo eruption based on the observations at Siberian lidar station
    Zuev, VV
    Burlakov, VD
    Elnikov, AV
    Marichev, VN
    NUCLEATION AND ATMOSPHERIC AEROSOLS 1996, 1996, : 304 - 307
  • [50] One year of Raman lidar observations of free-tropospheric aerosol layers over South Africa
    Giannakaki, E.
    Pfuller, A.
    Korhonen, K.
    Mielonen, T.
    Laakso, L.
    Vakkari, V.
    Baars, H.
    Engelmann, R.
    Beukes, J. P.
    Van Zyl, P. G.
    Josipovic, M.
    Tiitta, P.
    Chiloane, K.
    Piketh, S.
    Lihavainen, H.
    Lehtinen, K. E. J.
    Komppula, M.
    ATMOSPHERIC CHEMISTRY AND PHYSICS, 2015, 15 (10) : 5429 - 5442