DQRID : D140416.3
Start DateStart TimeEnd DateEnd Time
03/25/2014150003/26/20141215
more
Subject:
SGP/RLPROF/C1 - Reduced SNR due to partial laser blockage
DataStreams:sgp60rlproftemp1newsC1.c0, sgprlprofmerge1turnC1.c0, sgp10rlprofdep1turnC1.c1,
sgp10rlprofasr1ferrC1.c1, sgp10rlprofbe1newsC1.c1, sgp10rlproftemp1newsC1.c0,
sgp10rlprofext1ferrC1.c1, sgp10rlprofmr1turnC1.c1
Description:
The laser output was partially blocked. This resulted in reduced SNR in all detection 
channels.
Suggestions: 
The data are useable but one may notice a slight increase in the noise.
Measurements:sgp10rlprofext1ferrC1.c1:
  • Maximum altitude used in the calculation of the aerosol optical depth from the
    extinction_1 profile(aod_1_max_ht)
  • Uncertainty of the aerosol extinction coefficient profile calculated from the
    aerosol backscatter coefficient(extinction_from_backscatter_error)
  • Aerosol optical depth from the surface computed from the
    extinction_from_backscatter profiles(aod_bscat_profile)
  • Aerosol extinction coefficient profile from the high N2 channel data(extinction_high)
  • Aerosol extinction coefficient profile created by marrying the merged extinction
    from N2 data with the extinction from backscatter data(extinction_married1)
  • Error in the aerosol optical depth calculated from the extinction_1 profile(aod_1_error)
  • Uncertainty of the aerosol extinction coefficient profile from the low N2
    channel(extinction_low_error)
  • Error in the aerosol optical depth calculated from the
    extinction_from_backscatter profile(aod_bscat_error)
  • Vertical resolution of the low aerosol extinction coefficient profile data(extinction_low_resolution)
  • Aerosol backscatter coefficient at 355 nm - smoothed to N2 extinction resolution(smoothed_backscatter)
  • Maximum altitude used in the calculation of the aerosol optical depth from the
    extinction_from_backscatter profile(aod_bscat_max_ht)
  • Aerosol optical depth from the surface computed from the married1 extinction
    profiles(aod_married1_profile)
  • Aerosol extinction coefficient profile from the low N2 channel data(extinction_low)
  • Uncertainty of the married aerosol extinction coefficient profile(extinction_married1_error)
  • Aerosol optical depth calculated from the extinction_from_backscatter profile(aod_bscat)
  • Uncertainty in the aerosol backscatter coefficient at 355 nm(backscatter_error)
  • Uncertainty in the aerosol backscatter coefficient at 355 nm - smoothed to N2
    extinction resolution(smoothed_backscatter_error)
  • Vertical resolution of the high aerosol extinction coefficient profile data(extinction_high_resolution)
  • Aerosol optical depth calculated from the extinction_married1 profile(aod_married1)
  • Error in the aerosol optical depth calculated from the extinction_married1
    profile(aod_married1_error)
  • Uncertainty of the aerosol extinction coefficient profile from the high N2
    channel(extinction_high_error)
  • Aerosol extinction coefficient profile calculated from backscatter and the
    extinction-to-backscatter ratio(extinction_from_backscatter)
  • Maximum altitude used in the calculation of the aerosol optical depth from the
    extinction_married1 profile(aod_married1_max_ht)
  • Aerosol optical depth from the surface computed from the extinction_1 profiles(aod_1_profile)
  • Aerosol volume backscattering coefficient at 355 nm(backscatter)
  • Aerosol extinction coefficient profile created by merging the two N2 channels
    extinction profiles(extinction_1)
  • Mask indicating from where the extinction value came from in the aerosol
    extinction coefficient profile created by marrying the merged extinction from N2
    data w(extinction_married1_mask)
  • Aerosol optical depth calculated from the extinction_1 profile(aod_1)
  • Uncertainty of the aerosol extinction coefficient profile from the overlap
    corrected high N2 channel(extinction_high_olap_corrected_error)
  • Aerosol extinction coefficient profile from the high N2 channel data, where the
    low N2 channel was used to correct for the overlap of the high channel(extinction_high_olap_corrected)
  • Uncertainty of the aerosol extinction coefficient profile created by merging the
    two N2 channels extinction profiles(extinction_1_error)
  • Vertical resolution of the merged aerosol extinction coefficient profile data(extinction_1_resolution)
more
sgprlprofmerge1turnC1.c0:
  • Number of photons counted in the low elastic (aerosol) channel(elastic_counts_low)
  • Number of photons counted in the high elastic (aerosol) channel(elastic_counts_high)
  • Number of photons counted in the liquid water channel(liquid_counts_high)
  • Count rate in the high water vapor channel(water_counts_high)
  • Number of photons counted in the high nitrogen channel(nitrogen_counts_high)
  • Number of photons counted in the temperature 1 channel(t1_counts_high)
  • Number of photons counted in the temperature 2 channel(t2_counts_high)
  • Number of photons counted in the low water vapor channel(water_counts_low)
  • Number of photons counted in the low nitrogen channel(nitrogen_counts_low)
  • Count rate in the high depolarization channel(depolarization_counts_high)
more
sgp10rlprofasr1ferrC1.c1:
  • Aerosol volume backscattering coefficient at 355 nm(backscatter)
  • Uncertainty of the aerosol scattering ratio profile created by merging the two
    channels(asr_1_error)
  • Uncertainty of the aerosol scattering ratio profile created by merging the two
    Calibrated channels(cal_asr_1_error)
  • Aerosol scattering ratio profile created by merging the two Calibrated channels(cal_asr_1)
  • Uncertainty of the Calibrated aerosol scattering ratio profile from the low
    channel(cal_asr_error_low)
  • Aerosol scattering ratio profile created by merging the two channels(asr_1)
  • Calibrated Aerosol scattering ratio profile from the high channel(cal_asr_high)
  • Uncertainty of the aerosol scattering ratio profile from the high channel(asr_error_high)
  • Uncertainty of the Calibrated aerosol scattering ratio profile from the high
    channel(cal_asr_error_high)
  • Uncertainty of the aerosol scattering ratio profile from the low channel(asr_error_low)
  • Calibrated Aerosol scattering ratio profile from the low channel(cal_asr_low)
  • Aerosol scattering ratio profile from the high channel(asr_high)
  • Aerosol scattering ratio profile from the low channel(asr_low)
more
sgp10rlproftemp1newsC1.c0:
  • Background subtracted rotational Raman signal at 353nm(tp1)
  • Background subtracted rotational Raman signal at 354nm(tp2)
  • Error in the background of the rotational Raman signal at 354nm(tp2_bkg_error)
  • Error in calibration coefficient a(a_coef_error)
  • Calibrated rotational Raman temperature(rot_raman_temperature)
  • Solar background correction factor applied to the calibration coefficient b(b_coef_scale)
  • Error in calibration coefficient b(b_coef_error)
  • Error in the background subtracted rotational Raman signal at 354nm(tp2_error)
  • Calibration coefficient a(a_coef)
  • Error in calibrated rotational Raman temperature(rot_raman_temperature_error)
  • Error in the background subtracted rotational Raman signal at 353nm(tp1_error)
  • Background of the rotational Raman signal at 353nm(tp1_bkg)
  • Raw rotational ratio error(rot_raman_ratio_error)
  • Solar background correction factor applied to the calibration coefficient a(a_coef_scale)
  • Raw rotational Raman ratio(rot_raman_ratio)
  • Error in the background of the rotational Raman signal at 353nm(tp1_bkg_error)
  • Background of the rotational Raman signal at 354nm(tp2_bkg)
  • Calibration coefficient b(b_coef)
more
sgp10rlprofmr1turnC1.c1:
  • Uncertainty of the water vapor mixing ratio profile from the high channel(mixing_ratio_error_high)
  • Water vapor mixing ratio profile from the low channel(mixing_ratio_low)
  • Uncertainty of the water vapor mixing ratio profile created by merging the two
    calibrated channels(mixing_ratio_3_error)
  • Uncertainty of the water vapor mixing ratio profile created by merging the two
    channels(mixing_ratio_1_error)
  • Relative humidity over ice calculated from the merged water vapor mixing ratio
    data(relative_humidity_over_ice)
  • Relative humidity calculated from the merged water vapor mixing ratio data(relative_humidity)
  • Water vapor mixing ratio(mixing_ratio_other)
  • Random error in the precipitable water vapor observed by the Raman lidar(pwv_rl_err)
  • Water vapor mixing ratio profile created by merging the two calibrated channels
    together with the surface in-situ measurements(mixing_ratio_3)
  • Water vapor mixing ratio profile created by merging the two calibrated channels(mixing_ratio_2)
  • Uncertainty of the water vapor mixing ratio profile created by merging the two
    calibrated channels(mixing_ratio_2_error)
  • Water vapor mixing ratio profile created by merging the two channels(mixing_ratio_1)
  • Fraction of the total precipitable water vapor in the column sensed by the Raman
    lidar(pwv_rl_fraction)
  • Uncertainty of the water vapor mixing ratio profile from the low channel(mixing_ratio_error_low)
  • Precipitable water vapor observed by the Raman lidar(pwv_rl)
  • Water vapor mixing ratio profile from the high channel(mixing_ratio_high)
more
sgp10rlprofdep1turnC1.c1:
  • Linear depolarization ratio profile(depolarization_ratio)
  • Cloud optical thickness computed from aerosol (elastic) data(cloud_optical_thickness_aer)
  • Cloud optical thickness computed from nitrogen data(cloud_optical_thickness_n2)
  • Uncertainty of the linear depolarization ratio profile(depolarization_ratio_error)
more
sgp10rlprofbe1newsC1.c1:
  • Aerosol extinction coefficient(ext)
  • Aerosol optical depth profiles at 355 nm(aod_profile)
  • Precipitable water vapor(pwv)
  • Aerosol scattering ratio(asr)
  • Fraction of the total column amount of water vapor the Raman lidar senses(pwv_fraction)
  • Aerosol optical depth uncertainty(aod_err)
  • Estimated 1-sigma uncertainty in pwv(pwv_err)
  • Linear depolarization ratio uncertainty(dep_err)
  • Cloud optical depth from elastic data(cot)
  • Uncertainty in water vapor mixing ratio observed by the Raman lidar(mr_err)
  • Aerosol scattering ratio uncertainty(asr_err)
  • Uncertainty in cloud optical depth from elastic data(cot_err)
  • Aerosol optical depth at 355 nm(aod)
  • Random error in the aerosol extinction coefficient profile(ext_err)
  • Water vapor mixing ratio observed by the Raman lidar(mr)
  • Linear depolarization ratio profile(dep)
more
sgp60rlproftemp1newsC1.c0:
  • Background of the rotational Raman signal at 353nm(tp1_bkg)
  • Error in the background subtracted rotational Raman signal at 353nm(tp1_error)
  • Raw rotational ratio error(rot_raman_ratio_error)
  • Error in the background of the rotational Raman signal at 353nm(tp1_bkg_error)
  • Solar background correction factor applied to the calibration coefficient a(a_coef_scale)
  • Calibrated rotational Raman temperature(rot_raman_temperature)
  • Solar background correction factor applied to the calibration coefficient b(b_coef_scale)
  • Error in calibration coefficient b(b_coef_error)
  • Raw rotational Raman ratio(rot_raman_ratio)
  • Background subtracted rotational Raman signal at 353nm(tp1)
  • Calibration coefficient a(a_coef)
  • Background of the rotational Raman signal at 354nm(tp2_bkg)
  • Calibration coefficient b(b_coef)
  • Error in calibration coefficient a(a_coef_error)
  • Background subtracted rotational Raman signal at 354nm(tp2)
  • Error in the background subtracted rotational Raman signal at 354nm(tp2_error)
  • Error in calibrated rotational Raman temperature(rot_raman_temperature_error)
  • Error in the background of the rotational Raman signal at 354nm(tp2_bkg_error)
more

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