Effect of wind speed on aerosol optical depth over remote oceans, based on data from the Maritime Aerosol Network

被引:25
作者
Smirnov, A. [1 ,2 ]
Sayer, A. M. [2 ,3 ]
Holben, B. N. [2 ]
Hsu, N. C. [2 ]
Sakerin, S. M. [4 ]
Macke, A. [5 ]
Nelson, N. B. [6 ]
Courcoux, Y. [7 ]
Smyth, T. J. [8 ]
Croot, P. [9 ]
Quinn, P. K. [10 ]
Sciare, J. [11 ]
Gulev, S. K. [12 ]
Piketh, S. [13 ]
Losno, R. [14 ,15 ]
Kinne, S. [16 ]
Radionov, V. F. [17 ]
机构
[1] Sigma Space Corp, Lanham, MD USA
[2] NASA, Goddard Space Flight Ctr, Greenbelt, MD 20771 USA
[3] GESTAR, Columbia, MD USA
[4] Russian Acad Sci, Inst Atmospher Opt, Tomsk, Russia
[5] Leibniz Inst Tropospher Res, Leipzig, Germany
[6] Univ Calif Santa Barbara, Santa Barbara, CA 93106 USA
[7] Univ Reunion, St Denis, Reunion, France
[8] Plymouth Marine Lab, Plymouth, Devon, England
[9] Leibniz Inst Marine Sci, D-24105 Kiel, Germany
[10] NOAA PMEL, Seattle, WA USA
[11] Lab Sci Climat & Environm, Gif Sur Yvette, France
[12] PP Shirshov Oceanol Inst, Moscow, Russia
[13] Univ Witwatersrand, Johannesburg, South Africa
[14] Univ Paris 07, Creteil, France
[15] Univ Paris 12, Creteil, France
[16] Univ Hamburg, Inst Meteorol, D-2000 Hamburg, Germany
[17] Arctic & Antarctic Res Inst, St Petersburg 199226, Russia
关键词
SEA-SALT AEROSOL; SATELLITE RETRIEVALS; MARINE AEROSOL; NORTH-ATLANTIC; IN-SITU; SURFACE; MODEL; AERONET; VARIABILITY; THICKNESS;
D O I
10.5194/amt-5-377-2012
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
The Maritime Aerosol Network (MAN) has been collecting data over the oceans since November 2006. The MAN archive provides a valuable resource for aerosol studies in maritime environments. In the current paper we investigate correlations between ship-borne aerosol optical depth (AOD) and near-surface wind speed, either measured (on-board or from satellite) or modeled (NCEP). According to our analysis, wind speed influences columnar aerosol optical depth, although the slope of the linear regression between AOD and wind speed is not steep (similar to 0.004-0.005), even for strong winds over 10m s(-1). The relationships show significant scatter (correlation coefficients typically in the range 0.3-0.5); the majority of this scatter can be explained by the uncertainty on the input data. The various wind speed sources considered yield similar patterns. Results are in good agreement with the majority of previously published relationships between surface wind speed and ship-based or satellite-based AOD measurements. The basic relationships are similar for all the wind speed sources considered; however, the gradient of the relationship varies by around a factor of two depending on the wind data used.
引用
收藏
页码:377 / 388
页数:12
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