What percentage of the oceanic mixed layer is accessible to marine lidar? Global and the Gulf of Mexico prospective

被引:6
作者
Bogucki, D. J. [1 ]
Spiers, G. [2 ]
机构
[1] Texas A&M Univ, Dept Phys & Environm Sci, Corpus Christi, TX 78412 USA
[2] Jet Prop Lab, Pasadena, CA 91109 USA
关键词
SEA-WATER; SCATTERING COEFFICIENT; BACKWARD DIRECTION; BEAM ATTENUATION; DEPTHS; MODEL;
D O I
10.1364/OE.21.023997
中图分类号
O43 [光学];
学科分类号
070207 ; 0803 ;
摘要
The oceanic mixed layer is a nearly homogenous region of the upper ocean which, in principle, has a little or no variation in turbulence strength, temperature or density with depth. This layer mediates oceanic fluxes of gas, momentum and heat. Here, based on the chosen [1] marine Lidar system, we have carried out estimates of the depth penetration of the Lidar when compared to the local mixed layer depth. On average, we have found that at least 50% of the global oceanic mixed layer depth is accessible to the Lidar observations. When operating in a single scattering mode, which is more attenuating but more amenable to analysis, the modeled Lidar was found to access 0.4 of global mixed layer depth in half of the cases. The single scattering Lidar was found to access a large fraction of the equatorial mixed layer - a region very important when addressing global climatic issues. In a coastal environment such as the Gulf of Mexico the single scattering Lidar was found to penetrate upper half of the mixed layer, underscoring the potential for Lidar to address environmental issues there. (C) 2013 Optical Society of America
引用
收藏
页码:23997 / 24014
页数:18
相关论文
共 36 条
[1]  
Abramowitz M., 1974, Handbook of Mathematical Functions, with Formulas, Graphs, and Mathematical Tables, DOI DOI 10.5555/1953048.2021068
[2]  
Acker J.G., 2007, EOS T AM GEOPHYS UN, V88, P14, DOI DOI 10.1029/2007EO020003
[3]   Probing the subsurface ocean processes using ocean LIDARS [J].
Arnone, Robert ;
Derada, Sergio ;
Ladner, Sherwin ;
Trees, Charles .
OCEAN SENSING AND MONITORING IV, 2012, 8372
[4]   SPECTRAL DEPENDENCE OF THE DIFFUSE ATTENUATION COEFFICIENT OF LIGHT IN OCEAN WATERS [J].
AUSTIN, RW ;
PETZOLD, TJ .
OPTICAL ENGINEERING, 1986, 25 (03) :471-479
[5]   REMOTE-SENSING OF SCATTERING COEFFICIENT FOR AIRBORNE LASER HYDROGRAPHY [J].
BILLARD, B .
APPLIED OPTICS, 1986, 25 (13) :2099-2108
[6]   Monte Carlo simulation of propagation of a short light beam through turbulent oceanic flow [J].
Bogucki, D. J. ;
Piskozub, J. ;
Carr, M. -E. ;
Spiers, G. D. .
OPTICS EXPRESS, 2007, 15 (21) :13988-13996
[7]   Preliminary and novel estimates of CO2 gas transfer using a satellite scatterometer during the 2001GasEx experiment [J].
Bogucki, Darek ;
Carr, Mary-Elena ;
Drennan, William M. ;
Woiceshyn, Peter ;
Hara, Tetsu ;
Schmeltz, Marjorie .
INTERNATIONAL JOURNAL OF REMOTE SENSING, 2010, 31 (01) :75-92
[8]   Relationship of light scattering at an angle in the backward direction to the backscattering coefficient [J].
Boss, E ;
Pegau, WS .
APPLIED OPTICS, 2001, 40 (30) :5503-5507
[9]   Airborne lidar detection and characterization of internal waves in a shallow fjord [J].
Churnside, James H. ;
Marchbanks, Richard D. ;
Lee, Jennifer H. ;
Shaw, Joseph A. ;
Weidemann, Alan ;
Donaghay, Percy L. .
JOURNAL OF APPLIED REMOTE SENSING, 2012, 6
[10]   Thin scattering layers observed by airborne lidar [J].
Churnside, James H. ;
Donaghay, Percy L. .
ICES JOURNAL OF MARINE SCIENCE, 2009, 66 (04) :778-789