1) wavelength number
波长数
2) wavelength exponent
波长指数
1.
Raman--Mie lidar measurements of aerosol wavelength exponent in the troposphere;
Raman-Mie激光雷达探测对流层气溶胶波长指数
2.
Uncertainty analysis of aerosol wavelength exponent measured by Raman-Mie lidars;
RML探测大气气溶胶波长指数的不确定分析
3.
The regressive equation between atmospheric transmittance on clearsky(T_a) and ngstrm turbidity coefficient(β) and the regressive equation between the β and aerosol wavelength exponent(α) were obtained using least square method.
利用回归方程,从该地区晴空大气透射比中提取出了ngstr m浑浊度系数,利用ngstr m浑浊度系数与波长指数的关系,计算了五道梁地区波长指数的变化。
4) wavelength rank
波长阶数
1.
The results show that forward and backward waves amplitudes develope sinusoidally along the grating,the number of their amplitude maximums is equate to the corresponding rank of wavelength,their maximums are dependent of the wavelength rank and independent of their position in the grating,and their maximums distribute periodically along the grating;the minimum of backward wave amplitude is zero.
结果表明:前、后向波的振幅呈正弦震荡且震荡步调一致,极大值个数与波长阶数相同,极大值大小亦与波长阶数有关,而与在光栅中的位置无关,极大值周期分布于整个光栅长度;后向波振幅极小值为零。
5) wave constant
波长常数
6) Angstrom wavelength exponent
Angstrom波长指数
1.
Atmospheric aerosol optical depth(AOD_λ=500nm),Angstrom turbidity coefficient(β) and Angstrom wavelength exponent(α) are obtained using the CERN sun hazemeter network from Aug to Dec,2004.
利用2004年秋冬季全国联网资料,给出中国19个典型区域大气气溶胶的光学厚度(AODλ=500nm)、Angstrom混浊系数(β)和Angstrom波长指数(α)。
补充资料：数不胜数
1.数也数不清。形容很多。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
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