Hexadecimal to decimal conversion tables for hexadecimal values 0-3F,FFFF - Decimal values 0-262,143
Hexadecimal to decimal system conversion tables for advanced orbital programming systems
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Hexadecimal to decimal system conversion tables for advanced orbital programming systems
Geomagnetic field geometry tables for trapped radiation and particles using scalar magnetic field intensity, invariant polar coordinants, and dipole moment
Cosmic ray deflections in geomagnetic field, variational coefficients, and diurnal intensity variations - tables
Design and analysis of automatic balancing system for three-axis air bearing table
Tables for converting seconds, hours, and days to milliseconds
Mach numbers from 0 to 100 for compressible gases with specific heat ratios 1.66 to 1.10 - table
Tables for evaluation of Faxen approximation to solution of Lamm equation
Stopping power and range tables for protons, mesons, and electrons in lithium fluoride, silicon, germanium, liquid hydrogen, propane, and freon
Thermionic and electric properties of solid and liquid elements and compounds - tables
Tables for calculating plane galactic orbits of stars
Thermochemical constants of elements and compounds - Tables
Tables of two-sided tolerance factors for normal distributions
Tables of annual variations of star constants a and a prime
Tables of joint probabilities useful in evaluating mixed acceptance sampling plans
The conference Working on the Fringe ended with a round-table discussion of the bigger picture of what it takes to ensure science gets done, in this case optical and IR interferometry.
The tidal signature in the middle atmospheric thermal structure is investigated using more than 140 hours of nighttime lidar measurements at Table Mountain (34.4 degrees north) during January 1997 and February 1998.
The Moderate Resolution Imaging Spectroradiometer (MODIS) makes observations using 36 spectral bands with wavelengths from 0.41 to 14.4 m and nadir spatial resolutions of 0.25km, 0.5km, and 1km. It is currently operating onboard the NASA Earth Observing System (EOS) Terra and Aqua satellites, launched in December 1999 and May 2002, respectively. The MODIS Level 1B (L1B) program converts the sensor's on-orbit responses in digital numbers to radiometrically calibrated and geo-located data products for the duration of each mission. Its primary data products are top of the atmosphere (TOA) reflectance factors for the sensor's reflective solar bands (RSB) and TOA spectral radiances for the thermal emissive bands (TEB). The L1B algorithms perform the TEB calibration on a scan-by-scan basis using the sensor's response to the on-board blackbody (BB) and other parameters which are stored in Lookup Tables (LUTs). The RSB calibration coefficients are processed offline and regularly updated through LUTs. In this paper we provide a brief description of the MODIS L1B calibration algorithms and associated LUTs with emphasis on their recent improvements and updates developed for the MODIS collection 5 processing. We will also discuss sensor on-orbit calibration and performance issues that are critical to maintaining L1B data product quality, such as changes in the sensor's response versus scan-angle.
First results of an intercomparison measurement campaign between three aerosol lidar instruments and in-situ backscatter sondes performed at Table Mountain Facility (34.4 degree N, 117.7 degree E, 2280 m asl) in February-March 1997 are presented.