Airborne/ground-based sensor intercomparison: SRL/LASE Paolo Di Girolamo, Domenico Sabatino, David Whiteman, Belay Demoz, Edward Browell, Richard Ferrare IHOP_2002 Water Vapor Intercomparison Workshop, 2-3 October 2003, NCAR, Boulder, CO
SRL operated for approximately 35 days during IHOP Most of the measurements were carried out in vertically pointing mode Present availability of analyzed data: 11 days 29 May 2002, 30 May 2002, 31 May 2002, 3June 2002, 4June 2002, 9June 2002, 10June 2002, 12June 2002, 14June 2002, 19June 2002, 20 June 2002 both daytime and night-time cases. Water vapor data have been processed using a single, height independent calibration constant determined from 20 nighttime datasets of SRL water vapor and SuomiNet GPS measurements of total precipitable water both taken at Greenbelt, MD in the September November, 2002 period for Aqua validation purposes. IHOP_2002 Water Vapor Intercomparison Workshop, 2-3 October 2003, NCAR, Boulder, CO NASA Scanning Raman Lidar, SRL
Time resolution: 1 minute intervals Vertical resolution: 0-1 km : 60m, 1-2 km : 100m, 2-3 km : 150m, 3-4 km : 200m, >4 km : 300m Vertical extent (for the present data release): 0-6 km. IHOP_2002 Water Vapor Intercomparison Workshop, 2-3 October 2003, NCAR, Boulder, CO
Statistical error associated with the Raman lidar signals and Measurement uncertainty Systematic error associated with the determination of the calibration constant K(z). Random error is a function time of day, altitude and amount of water vapour. During IHOP: day <10% in BL night <2% in BL, <10% to 6km Water vapor data have been processed using a single, height independent calibration constant determined from 20 nighttime datasets of SRL water vapor and SuomiNet GPS measurements of total precipitable water both taken at Greenbelt, MD in the September November, 2002 period for Aqua validation purposes.
Vertical data interval: 30 m Horizontal interval: 6 sec or 1.4 km Vertical resolution: 330 m Horizontal resolution: 1 min or 14 km LASE measurement accuracy: better than 6 % or 0.01 g/kg, across the troposphere Water vapor mixing ratio: calculated using molecular density profiles derived from the Homestead radiosondes. NASA LASE
Comparison between SRL and LASE Comparison between SRL and LASE data are possible on 30 May, 3 June, 9 June and 14 June. 24 comparisons available Date: May 30, 2002 time[UTC] distance[km] 18:28: :28: :44: :34: :49: Date: June 03, 2002 time[UTC] distance[km] 19:29: :30: :32: Date: June 09, 2002 time[UTC] distance[km] 18:06: :17: :31: Date: June 14, 2002 time[UTC] distance[km] 14:03: :03: :44: :14: :14: :56: :27: :27: :10: :10: :38: :19: :49: Comparisons are based on 10 minute data averaging for SRL and 1 minute data averaging for LASE. Based on 10 minute data averaging, 10 % random uncertainty for SRL is reached between km. In order to compute deviations, SRL data have been interpolated at LASE heights. IHOP_2002 Water Vapor Intercomparison Workshop, 2-3 October 2003, NCAR, Boulder, CO
Agreement is very good when distance between LASE footprint and SRL does not exceed 2.5 km. Average RMS deviation: 2.2 % in the height interval km Average BIAS: 0.3 % in the height interval km IHOP_2002 Water Vapor Intercomparison Workshop, 2-3 October 2003, NCAR, Boulder, CO Distance between LASE footprint and SRL = 0.9 km statistical error gets lower than 10 % around 5 km Sun zenith angle=30-40 deg Background signal is 50 % smaller than Sun at zenith When distances are larger than 2.5 km, differences in air masses properties are appreciable deviations between LASE and SRL are larger.
RMS deviations and BIAS Total RMS deviations and BIAS in the altitude region km and km, together with contributions from different height intervals: km, km, km, km, km Error exceeding 100 % have been excluded from the average
RMS deviations and BIAS between SRL and mean value IHOP_2002 Water Vapor Intercomparison Workshop, 2-3 October 2003, NCAR, Boulder, CO expected to be the best estimate of truth (g/kg)
RMS deviations and BIAS between LASE and mean value IHOP_2002 Water Vapor Intercomparison Workshop, 2-3 October 2003, NCAR, Boulder, CO expected to be the best estimate of truth (g/kg)
RMS deviations and BIAS between the sensors IHOP_2002 Water Vapor Intercomparison Workshop, 2-3 October 2003, NCAR, Boulder, CO
DateTime km km km km km km km km 30 May May May May May June June June June June June June June June June June June June June June June June June June Average
DateTime km km km km km km km km 30 May May May May May June June June June June June June June June June June June June June June June June June June Average
DateTime km km km km km km km km 30 May May May May May June June June June June June June June June June June June June June June June June June June Average
DateTime km km km km km km km km 30 May May May May May June June June June June June June June June June June June June June June June June June June Average
RMS deviations and BIAS between the sensors
DateTime km km km km km km km km 30 May May May May May June June June June June June June June June June June June June June June June June June June Average
DateTime km km km km km km km km 30 May May May May May June June June June June June June June June June June June June June June June June June June Average
Average (over 24 comparisons) RMS deviation and BIAS Between SRL and mean Average RMS deviation < 4.19 % 1.3 < z < 2.8 km, Average BIAS < 0.34 % 1.3 < z < 3.3 km Between LASE and mean Error exceeding 100 % have been excluded from the average. Average RMS deviation < 4.23 % 1.3 < z < 2.8 km, Average BIAS < 0.4 % 1.3 < z < 3.3 km Between SRL and LASE Error exceeding 100 % have been excluded from the average. Average RMS deviation < 8.4 % 1.3 < z < 2.8 km, Average BIAS < 0.68 % 1.3 < z < 3.3 km AVERAGE RMS Deviation ( in the height region km ) between SRL/LASE and the mean value does not exceed 4.2 % AVERAGE BIAS (height region km) between SRL/LASE and the mean value does not exceed 0.4 %