Springtime Arctic aerosol: Smoke versus haze, a case study for March 2008

被引:18
作者
Stock, M. [1 ]
Ritter, C. [1 ]
Herber, A. [2 ]
von Hoyningen-Huene, W. [4 ]
Baibakov, K. [2 ,3 ]
Graeser, J. [1 ]
Orgis, T. [1 ]
Treffeisen, R. [2 ]
Zinoviev, N. [5 ]
Makshtas, A. [5 ]
Dethloff, K. [1 ]
机构
[1] Helmholtz Assoc, Alfred Wegener Inst Polar & Marine Res, D-14473 Potsdam, Germany
[2] Helmholtz Assoc, Alfred Wegener Inst Polar & Marine Res, D-27568 Bremerhaven, Germany
[3] Univ Sherbrooke, Ctr Res & Applicat Remote Sensing CARTEL, Sherbrooke, PQ J1K 2R1, Canada
[4] Univ Bremen, D-28359 Bremen, Germany
[5] Arctic & Antarctic Res Inst, St Petersburg 199397, Russia
关键词
Arctic Haze; Arctic Smoke; Aerosol; Photometer; Lidar; AIR-POLLUTION; TROPOSPHERIC AEROSOL; OPTICAL DEPTH; RAMAN LIDAR; EXTINCTION; RETRIEVAL; INVERSION; PROFILES; ORIGINS;
D O I
10.1016/j.atmosenv.2011.06.051
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
During March 2008 photometer observations of Arctic aerosol were performed both at a Russian ice-floe drifting station (NP-35) at the central Arctic ocean (56.7-42.0 degrees E, 85.5-84.2 degrees N) and at Ny-Alesund, Spitsbergen (78.9 degrees N, 11.9 degrees E). Next to a persistent increase of AOD over NP-35, two pronounced aerosol events have been recorded there, one originating from early season forest fires close to the city of Khabarovsk ("Arctic Smoke"), the other one showed trajectories from central Russia and resembled more the classical Arctic Haze. The latter event has also been recorded two days later over Ny-Alesund, both in photometer and lidar. From these remote sensing instruments volume distribution functions are derived and discussed. Only subtle differences between the smoke and the haze event have been found in terms of particle microphysics. Different trajectory analysis, driven by NCEP and ECMWF have been performed and compared. For the data set presented here the meteorological field, due to sparseness of data in the central Arctic, mainly limits the precision of the air trajectories. (C) 2011 Elsevier Ltd. All rights reserved.
引用
收藏
页码:48 / 55
页数:8
相关论文
共 45 条
[1]  
Angstrom A., 1929, GEOGR ANN, V11, P156, DOI [DOI 10.2307/519399, 10.2307/519399]
[2]   INDEPENDENT MEASUREMENT OF EXTINCTION AND BACKSCATTER PROFILES IN CIRRUS CLOUDS BY USING A COMBINED RAMAN ELASTIC-BACKSCATTER LIDAR [J].
ANSMANN, A ;
WANDINGER, U ;
RIEBESELL, M ;
WEITKAMP, C ;
MICHAELIS, W .
APPLIED OPTICS, 1992, 31 (33) :7113-7131
[3]   ARCTIC AIR-POLLUTION - AN OVERVIEW OF CURRENT KNOWLEDGE [J].
BARRIE, LA .
ATMOSPHERIC ENVIRONMENT, 1986, 20 (04) :643-663
[4]   Calculation of the calibration constant of polarization lidar and its dependency on atmospheric temperature [J].
Behrendt, A ;
Nakamura, T .
OPTICS EXPRESS, 2002, 10 (16) :805-817
[5]  
Böckmann C, 2001, APPL OPTICS, V40, P1329, DOI 10.1364/AO.40.001329
[6]   SOOT IN THE ARCTIC SNOWPACK - A CAUSE FOR PERTURBATIONS IN RADIATIVE-TRANSFER [J].
CLARKE, AD ;
NOONE, KJ .
ATMOSPHERIC ENVIRONMENT, 1985, 19 (12) :2045-2053
[7]   Around the world in 17 days - hemispheric-scale transport of forest fire smoke from Russia in May 2003 [J].
Damoah, R ;
Spichtinger, N ;
Forster, C ;
James, P ;
Mattis, I ;
Wandinger, U ;
Beirle, S ;
Wagner, T ;
Stohl, A .
ATMOSPHERIC CHEMISTRY AND PHYSICS, 2004, 4 :1311-1321
[8]  
Draxler R.R., 2010, HYSPLIT HYBRID SINGL
[9]   Present-day climate forcing and response from black carbon in snow [J].
Flanner, Mark G. ;
Zender, Charles S. ;
Randerson, James T. ;
Rasch, Philip J. .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2007, 112 (D11)
[10]   Photochemical and Other Sources of Organic Compounds in the Canadian High Arctic Aerosol Pollution during Winter-Spring [J].
Fu, Pingqing ;
Kawamura, Kimitaka ;
Barrie, Leonard A. .
ENVIRONMENTAL SCIENCE & TECHNOLOGY, 2009, 43 (02) :286-292