The German-Israeli intercomparison experiment on the investigation of vertical profiles of horizontal wind speed and optical turbulence in the lower atmospheric boundary layer from 4th to 7th May 2015 was characterized by frontal activity in the atmosphere. The newly developed remote LIDAR-device of the Soreq institute for the investigation of the vertical wind and turbulence field was compared to the routinely performed measurements at the VerTurM (Vertical Turbulence Measurements) field site in Meppen, Germany. The long-term experiment VerTurM is focused on measurements of the optical turbulence and comprises scintillometer measurements close to the ground (1.15 m height), sonic anemometer measurements on a tall tower at 4 m, 8 m, 32 m, and 64 m and a SODAR-RASS-system. The temporal development of the vertical profiles of horizontal wind speed and optical turbulence Cn 2 during the frontal passage is investigated. Additional radiosonde measurements were performed to characterize the boundary layer height during the day.
The water vapor profile derived from Raman lidar measurements is obtained by taking the ratio of water vapor and nitrogen Raman-shifted signals. The proportionality factor that converts the signal ratio to water vapor/air mixing ratio is referred to as lidar calibration constant. The calibration constant depends on the water vapor and nitrogen Raman cross sections and on the efficiencies of the respective Raman channels including the photomultiplier tube (PMT) efficiency. Unequal, gradual changes in the PMTs efficiencies due to fatigue effects may lead to gradual alteration of the calibration constant. Such an effect has been observed during the seven- year continuous operation of the RAman Lidar for Moisture Observations (RALMO)1 . A more detailed research2 , has shown that the calibration constant change is more pronounced during summer time probably due to the higher light exposure. Periodical recalibration of the lidar with radiosonde measurements is used to correct the calibration constant. This approach, however, induces additional systematic errors due to the nature of the calibration procedure and the dispersion of the radiosonde parameters. We present a new, instrumental method for automated correction of the calibration constant. By this method, a correction factor is deduced from the ratio of the signals of the two photomultipliers which are illuminated simultaneously by a single, stabilized UV-LED light source. The LED light is delivered to the photomultipliers by a set of additional mirrors and a beam splitter installed inside the grating polychromator used to separate the Raman signals. The correction measurements are taken before midnight. To minimize the data loss, the lidar’s laser is operated during the measurements and a shatter at the polychromator entrance is used to block any atmospheric signals. The use of stabilized light source also allows evaluating the individual photomultipliers aging rates, essential for the instrument maintenance.
The Enhanced Photodissociation Fluorescence method is a novel approach to overcome several limitations associated
with remote optical detection of vapors emanating from NO containing explosives. By using an additional laser source to
enhance their evaporation, a sufficient concentration-level is achieved to extend the scope of optically detected materials.
The enhanced system has successfully demonstrated detection of low vapor pressure explosives (RDX, PETN, C4,
Composition B and SEMTEX) from a distance of 30m in outdoor, day-light conditions.
We report on developing of a prototype LIDAR for remote measurements of cross-wind profile, using backscattering
from aerosol in a single-ended scheme. The system contains a pulsed Nd:YAG laser with 500 Hz repetition rate and ~20
nsec pulse width, as a transmitter, and a matrix of 7 detectors, placed at the focus of Cassegrain-type telescope, as a
receiver. To realize detection of signals with high-sampling resolution, a high-sampling-rate digitizer with 8
simultaneously sampled channels and 60 Msamples/sec-per-channel sampling rate was incorporated into the system. To
check the ability to detect a local cross-wind flow, we performed an experiment using the cooling tower of Soreq reactor
as a vertical wind simulator. We recorded the detector signals from aerosol scattering at different distances, and analyzed
the temporal-spatial cross-correlation function. The analysis of the asymmetry and shift of the cross-correlation function
shows good ability for qualitative mapping of local cross-wind. Next development steps will include improvement of the
electronic circuits, in order to increase the sampling resolution along the line of sight, performing of additional controlled
experiments and developing of wind-profile algorithm.
Long range, combined UV-IR LIDAR system was built and tested. The system was developed to
operate as a multi-wavelength DIAL in the IR (8-11 μm), dual exciting wavelengths LIF LIDAR in the
UV, and aerosol map and track at 1.5 μm. The IR transmitter is a continuous tunable solid-state
Tandem Optical Parametric Oscillator (OPO) [1]. The first OPO stage generates the 1.5 μm beam and
the second OPO stage pumped by the first, generates the IR band. In the UV the transmitter generates
and transmits either the 266 nm or the 355 nm wavelengths sequentially. All the outgoing laser beams
are prealigned to ensure geometric overlap over the measured paths. Energy references are measured
for each beam on every pulse. The receiver is based on a single reflective telescope with coatings
optimized for both the UV and the IR. The optical signal is routed between the different detection
packages by means of a computerized optical scanner mirror. The receiver-transmitter layout is
based on periscope geometry and is equipped with a large θ-φ scanner. Computer control enables fast
switching between the different measurements and wavelengths, data acquisition and spatial scan as
well.
The system was built inside a mobile trailer and was field tested to descriminate aerosol types in a
complex enviroment [2].
We present a theoretical and experimental investigation of the efficiency, beam quality and signal bandwidth of a confocal, unstable OPO resonator. Reduction by more than 20 times of the divergence as well as bandwidth narrowing by factor of ~5 of the signal beam, in comparison to the plane-parallel resonator, are obtained. Resonator configurations have been found where the beam quality of the signal exceeds the beam quality of the pump.
A compact IR transmitter for the 8-12 micrometers atmospheric window is presented. The transmitter consists of two optical parametric oscillators (OPOs) in series, pumped by a 1.064 micrometers Nd:YAG laser. The first conversion stage is a double-pass non-critically phase-matched KTP OPO. A singly resonant configuration is used - the signal at 1.574 micrometers is resonated and coupled out with a 73 percent reflectivity output mirror. The first OPO's signal serves as a pump for a double-pass type I phase-matched AgGaSe2 OPO. This second OPO resonates the signal and couples out the idler at 8-11 micrometers . We eliminate high oscillating intensities inside the cavity by means of a low feedback. The low feedback causes a high threshold level, but have a minor influence on the total efficiency. Pumped by 6.5mJ at 1.574 micrometers , the AgGaSe2 OPO produced up to 0.5mJ at 8.5 micrometers , with beam quality of M2 equals 4-5 and spectral width of 4-5cm-1. Small physical dimensions, simplicity, and fairly good stability, makes this tandem OPO system usable for remote sensing applications. The described system is currently used for laboratory aerosol backscatter measurements.
A demonstration of narrow linewidth, low threshold OPO is presented. Two basic line-narrowing methods are applied. One method employs an intra-cavity grazing incident grating, and compensates the high losses caused by the grating by adding a laser gain element to the cavity. In the second method, a single element birefringent filter with low insertion loss is introduced in the cavity. Both configurations allow an efficient, compact design of tunable source with low pump threshold and narrow linewidth.
Spatial distribution of aerosol density in the boundary layer can be measured with a scanning lidar system. These measurements can be used to visualize, through color coded R-H maps, the inversion layer height and the dispersion of aerosols from natural and manmade sources. Lidar inversion height measurements were verified by taking simultaneously temperature profiles measurements with a meteorological balloon. The results obtained were in good agreement, suggesting lidar as a powerful tool to investigate aerosol dispersion in boundary layer.
Spatial distribution of aerosol density in the boundary layer can be measured with a scanning LIDAR system. These measurements can be used to visualize, through color coded R-H maps, the inversion layer height and the dispersion of aerosols from natural and manmade sources. LIDAR inversion height measurements were verified by simultaneously taking temperature profiles measurements with a meteorological balloon. The results obtained were in good agreement, suggesting LIDAR as a powerful tool to investigate aerosol dispersion in the boundary layer.
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