Description of the REDDY NEAR-EARTH AND MARS-CROSSING ASTEROIDS bundle V1.0 ===================================================== Bundle Generation Date: 2017-07-10 Peer Review: 2017b Asteroid Review, Wed May 31 00:00:00 MST 2017 Discipline node: Small Bodies Node Content description for the REDDY NEAR-EARTH AND MARS-CROSSING ASTEROIDS bundle ============================================================== All spectral observations were obtained using the SpeX instrument on the NASA IRTF in low-resolution prism mode. Observations were made remotely and in classical mode on site. SpeX in low resolution mode has resolving powers of R~100 across the wavelength region from ~ 0.7 to 2.5 microns. An infrared guider is available to guide on calibration stars (sidereal rates) and asteroids (non-sidereal rates). The main spectrograph uses a 1024x1024 Aladdin 3 InSb array and the guider uses a 512x512 Aladdin 2 InSb array [RAYNERETAL2004]. Low-resolution spectrographs like SpeX are ideal for resolving broad absorption features produced by abundant mafic minerals like olivine and pyroxene that make up many asteroid surface assemblages. The low resolution prism mode also helps in obtaining spectra with higher signal-to-noise-ratios (SNR) and asteroids as faint as Vmag~17.5 are routinely observed. Spectral observations for this data set were made by taking nodded spectral image pairs of the asteroid, local standard star (for telluric correction), solar-analog stars, and calibration flat-field and argon arc-lamp images. The placement of these stellar observations, temporally and spatially on the sky, in relation to the asteroid is important for producing good quality spectra. If the atmosphere over Mauna Kea is stable throughout the observing run (photometric), then the log of the flux (apparent magnitude) of the object will decrease linearly with increasing airmass. Hence, all objects are typically observed at airmasses less than 1.5, which corresponds to a zenith angle of less than 50 degrees. However, if the atmosphere is unstable over Mauna Kea, whether due to an orographic cap cloud or rapid variability of water vapor content, it often produces a non-linear magnitude-airmass relationship. Local (or extinction) standard stars close to the asteroid are observed to correct for the terrestrial atmospheric water vapor features. Generally, the greater the distance between the local standard star and the asteroid, the poorer the monitoring of the sky conditions for the asteroid. During a typical observing run, a local standard star with spectral properties similar to our Sun (i.e., G-type, main sequence stars) is paired with an asteroid and is observed over a wide airmass range that bracket the airmass range of the asteroid observations. Solar analog stars are observed to remove the solar continuum from the asteroid spectrum. At least two solar analog stars should be observed each night to eliminate the possibility of systematic errors that may be present in a single solar analog star spectrum. SpeX prism data was reduced using the IDL-based Spextool provided by the NASA IRTF [CUSHINGETAL2004]. The steps followed in the reduction process include: (1) sky background removal by subtracting the image pairs, (2) flat-fielding, (3) cosmic ray and spurious hit removals, (4) wavelength calibration, (5) division of asteroid spectra by the spectrum of the solar analog star, and (6) co-adding of individual spectra. The final files have different numbers of rows due to the quality of the data. NOTE: Definitions for keywords which may appear in the labels: EXPOSURES is the number of individual observations which have been combined to produce the final spectrum. V_APPARENT_MAGNITUDE is the apparent V magnitude of the target. FILTER_NAME (always V) is the filter of the V_APPARENT_MAGNITUDE. SOLAR_ANALOG_STAR is the name of the solar analog star used to reduce the observation. SOLAR_PHASE_ANGLE, HELIO_DISTANCE, and AIRMASS all refer to the target. Plots with all the NIR spectra are provided in a pdf file located in the document directory. Numbers in the plots refer to the asteroid number. Error bars are not included in the plots. Known issues or problems with the data ====================================== Uncertainties in spectral parameters for near-IR data are crucial for detecting and quantifying surface composition. The average wavelength resolution of the Spextool data is ~ 0.0035 microns. This is just due to spectral resolution based on the wavelength calibration. When spectra were combined the statistic used was the robust weighted mean. For this, Spextool makes use of a sigma clipping algorithm to identify outliers. The value at each pixel is then the weighted average of the good pixels and the uncertainty is given by the propagated variance. Uncertainties in the data arise primarily due to low SNR of the final average spectrum, incomplete correction of telluric absorption features, and variable sky/weather conditions.