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Aerosol Research Branch (ARB) 48 inch Lidar (ARB_48_IN_LIDAR) Langley DAAC Data Set Document |
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The ARB_48_IN_LIDAR data set contains data collected from a 48-inch lidar system located at NASA Langley Research Center. Each granule consists of one year of data. Data are available from 1982 through the present. Data are continuously being collected. The days of data are different in each granule. Each measurement consists of four parameters: integrated backscatter over altitude, altitude levels, scattering ratio at each altitude level, and aerosol backscattering coefficient at each altitude level. An image has been produced to represent the data collected for each granule.
| ARB_48_IN_LIDAR | Aerosol Research Branch (ARB) 48 inch Lidar |
This document summarizes measurements obtained using the ground-based 48-inch lidar system operated at 694 nm at the NASA Langley Research Center in Hampton, Virginia from 1982 to the present.
Routine ground-based lidar measurements have been taken at the Langley Research Center, Hampton, Virginia (37.1 degrees North, 76.3 degrees West), since May 1974. (Measurements prior to 1982 are not currently available in digital forms.) These lidar measurements provide high-resolution vertical profiles of the stratospheric and upper tropospheric aerosols. The lidar system, often referred to as the 48-inch lidar system because of its 48-inch telescope, has evolved over the years and provides a valuable long-term history of the mid-latitude stratospheric aerosol.
The lidar parameters provided for each measurement profile of approximately 100-200 laser shots are: altitude (km), scattering ratio, aerosol backscattering coefficient (1/km-sr); and integrated backscatter (1/sr), all at a wavelength of 694 mm.
The lidar backscatter ratio (or scattering ratio) is defined as
(Equation 1)
R(z) = (BA(z) + BM(z)) /
BM(z) = 1 + BA(z) /
BM(z)
where BA is the aerosol backscattering function, or scattering
function, and BM is the molecular backscattering function, both in
units of (km-sr)-1 and both at altitude z. The function
BM(z) is calculated from a temperature-pressure profile
obtained from the radiosonde launch at Wallops Island, Virginia (120 km
northeast of the lidar system), just prior to or just after the lidar data are
collected. The scattering ratio R(z) is calculated by evaluating
(Equation 2)
R(z) = kS(z)z2 /
BM(z)q2(z)
where S(z) is the lidar signal received from altitude z,
q2(z) is the two-way atmospheric transmittance, and k
is a system constant determined by normalizing the right-hand side of equation
(2) to an expected minimum value of R (Rmin) over a specified
altitude range. The transmittance q2(z) is calculated from a
combination of radiosonde-derived molecular extinction, model or lidar-derived
aerosol extinction, and model ozone absorption. During periods of background or
moderate aerosol loading, aerosol extinction can be adequately modeled.
However, since the eruptions of El Chichon in late March-early April 1982,
aerosol extinction has been calculated directly from the aerosol
backscattering function. The lidar equation (2) is solved three times using an
updated value for aerosol extinction for the second and third iterations. The
integrated aerosol backscatter is defined as (Equation 3)

where BA is the aerosol backscattering function (km-sr)-1
at altitude z, and hT is the height of the tropopause.
A smaller version (a 14-inch telescope) of this ground-based system has been used for airborned observations of the stratospheric aerosol and polar stratospheric clouds.
Dr. Chris Hostetler, PI, ARB, NASA Langley Research Center
Aerosol Research Branch (ARB) 48-inch Lidar
Lidar measurements are analyzed according to the method outlined by P. B. Russell, T. J. Swissler, and M. P. McCormick in "Methodology for error analysis and simulation of lidar aerosol measurements," Applied Optics, Vol 18, no 22, November 15, 1979.
The 48-inch lidar system consists of a 48-inch (1.22-m) Cassegrainian telescope and a ruby laser that nominally emitted 1 joule per pulse at a wavelength λ of 694 nm at a repetition rate of 0.15 Hz. The divergence of the transmitted beam is approximately 1.0 mrad, and the maximum receiver field of view is 4.0 mrad. The electronic bandwidth of the receiver is 1 MHz, which provides a 150-m vertical resolution. Three photomultiplier tubes, electronically switched on (gated) at different deleay times after laser firing, are used to provide a large dynamic range. The photomultiplier tube output signals are processed by 12-bit Computer Automated Measurement and Control (CAMAC) based digitizers and acquired by a personal computer. The data are archived on optical discs.
Nighttime; no dense clouds.
The 48-inch lidar system is contained in a building and operated through a hole in the roof.
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Measurements are obtained weekly, weather permitting.
Vertical profiles.
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Approximately 100-200 laser shots are averaged into one measurement data set.
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| Data Set Name |
Min Lat |
Max Lat |
Min Lon |
Max Lon |
|---|---|---|---|---|
| ARB_48_IN_LIDAR | 37.10 | 37.10 | -76.30 | -76.30 |
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| Data Set Name |
Begin Date |
End Date |
|---|---|---|
| ARB_48_IN_LIDAR | 01/05/1982 | 11/23/1994 (on going) |
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| Parameter Name |
Min Value |
Max Value |
Units |
|---|---|---|---|
| Integrated Backscatter | 0.0 | 1.E-1 (or 0.1) | 1/sr |
| Altitude | 0.0 | 33.0 | Kilometers |
| Scattering Ratio | -1000.0 | 1000.0 | Unitless |
| Aerosol Scattering Coefficient | -1.E-1 (or -0.1) | 1.E-1 (0.1) | 1/(km-sr) |
See above.
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DATE (GMT) # ALTITUDES INT BCKSC (1/sr)
61482 221 7.74E-4
ALT(km) SCATT RATIO AER COEFF(1/km-sr)
0.00 9999.000 9.9990E+03
0.15 9999.000 9.9990E+03
0.30 9999.000 9.9990E+03
...
4.05 1.060 2.0945E-05
4.20 1.051 1.7657E-05
4.35 1.033 1.1072E-05
4.50 1.021 7.1247E-06
4.65 1.037 1.2286E-05
4.80 1.066 2.1401E-05
4.95 1.105 3.3442E-05
...
Each granule consists of one year of data.
A general
description of data granularity as it applies to the Information Management
System (IMS) appears in the
EOSDIS Glossary.
All data granules are in ASCII format.
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There are no plans for reprocessing.
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There is a browse product available for each granule in this data set.
Derivation of scattering ratios is subject to a number of uncertainties arising from the measurements themselves and from the assumptions used in the data analysis. The random error in the scattering ratio contains contributions from signal measurement error, error in the correction for two-way transmittance, density errors, and error in the assumed value of Rmin. The magnitude of these errors is related to the amount of aerosol loading, the proximity in time and space to a measured molecular density profile, the number of laser shots averaged together in a sequence, the background lighting conditions, and the models used for atmospheric attenuation.
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The Langley DAAC performs an inspection process on this data received by the data producer via ftp. The DAAC checks to see if the transfer of the data completed and were delivered in their entirety. An inspection software was developed by the DAAC to see if the code was able to read every granule. The code also checks to see if every parameter of data falls within the ranges which are included in the granule. This same code extracts the metadata required for ingesting the data into the IMS. If any discrepancies are found, the data producer is contacted. The discrepancies are corrected before the data are archived at the DAAC.
There are no known limitations or unreliable aspects in the algorithms implemented to generate the 48-inch lidar science data.
There are no known problems or inconsistencies in the ERBE data.
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Additional granules will be added to the archive list as data become available.
Sample read software is available for this data set. This code is written in C. A makefile and a readme file are also available to work with the code and data.
The software can be obtained through the Langley DAAC. Please refer to the contact information below. The software can also be obtained at the same time the user is ordering this data set.
Data, programs for reading the data, and user's guides can be obtained through the EOSDIS Langley DAAC on-line system which will allow users to search through the data inventory and place orders on-line.
Langley DAAC User and Data Services OfficeThe Langley DAAC User and Data Services staff provides technical and operational support for users ordering data.
The Langley DAAC will continue to archive this data.
There is a browse image for each granule of data archived at the Langley DAAC.