K-band radar in vegetation mapping.
Vegetation mapping from K-band radar imagery using image discrimination, enhancement, combination and sampling system
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Vegetation mapping from K-band radar imagery using image discrimination, enhancement, combination and sampling system
Electronically-scanned K-band passive phased array for spaceborne radiometry
Systems design of K-band electron density probe
Two dimensional electronically scanned k-band phased array antenna design and performance, discussing radiometric system
Geologic evaluation of anomalies between like-polarized and cross-polarized K-band side-looking radar imagery of Yellowstone National Park
Vegetation penetration with K-band side-looking airborne imaging radars, noting multifrequency multipolarization system application for terrain reconnaissance
The temperature effects on the attenuation of K-band microwaves, at a frequency of 26,500 plus or minus 30 megacycles per second, through natural-gas and propane flames containing added alkali halide salts, were investigated over a temperature range from 1900 to 2500 K. The preliminary data of this investigation indicated that the attenuation varies appreciably with the sodium-line-reversal temperatures of the flames and is independent of the particular hydrocarbon fuels that were used for temperature sources and of the particular halide components of the compounds used in the concentrations employed to produce easily measurable attenuation. A reproducibility of plus or minus 25 K was obtainable.
Geologic evaluation of aerial K band radar photography
Snow field mapping with K band radar imagery determining signal return difference with surrounding terrain, noting role of volume scattering and old snow structure
Side-looking airborne radar for K band mapping of snowfields
X-ray analyses on K-band spectral structure for titanium absorption in nitrides and carbides
We have discovered that SDSS J105213.51+442255.7 (T0.5 ± 1.0) is a binary in Keck laser guide star adaptive optics imaging, displaying a large J- to K-band flux reversal (ΔJ=−0.45±0.09 mag, ΔK=0.52±0.05 mag). We determine a total dynamical mass from Keck orbital monitoring (88 ± 5 M{sub Jup}) and a mass ratio by measuring the photocenter orbit from CFHT/WIRCam absolute astrometry (M{sub B}/M{sub A}=0.78±0.07). Combining these provides the first individual dynamical masses for any field L or T dwarfs, 49 ± 3 M{sub Jup} for the L6.5±1.5 primary and 39 ± 3 M{sub Jup} for the T1.5±1.0 secondary. Such a low mass ratio for a nearly equal luminosity binary implies a shallow mass–luminosity relation over the L/T transition (Δlog L{sub bol}/Δlog M=0.6{sub −0.8}{sup +0.6}). This provides the first observational support that cloud dispersal plays a significant role in the luminosity evolution of substellar objects. Fully cloudy models fail our coevality test for this binary, giving ages for the two components that disagree by 0.2 dex (2.0σ). In contrast, our observed masses and luminosities can be reproduced at a single age by “hybrid” evolutionary tracks where a smooth change from a cloudy to cloudless photosphere around 1300 K causes slowing of luminosity evolution. Remarkably, such models also match our observed JHK flux ratios and colors well. Overall, it seems that the distinguishing features SDSS J1052+4422AB, like a J-band flux reversal and high-amplitude variability, are normal for a field L/T binary caught during the process of cloud dispersal, given that the age (1.11{sub −0.20}{sup +0.17} Gyr) and surface gravity (log g = 5.0–5.2) of SDSS J1052+4422AB are typical for field ultracool dwarfs.
The objective of this project is to complement the U.S. Department of Energy Atmospheric Radiation Measurement (ARM) User Facility second ARM Mobile Facility (AMF2) deployment at kennaook-Cape Grim (CAPE-k) with a micro-rain radar (MRR-PRO) mounted on top of one of the ARM containers. This was done to locate the MRR-PRO close to the ARM cloud radars (Ka-band ARM Zenith Radar [KAZR] and Marine W-band ARM Cloud Radar [MWACR]). This will allow for a continuous calibration check of the ARM cloud radars against the MRR-PRO and Parsivel-2 disdrometers. Scientifically, it will add one radar frequency to the analysis of vertical profiles of cloud and precipitation properties (K-band).
Ten-kilogauss air-cooled magnet for use in microwave measurements at k-band frequencies in magnetoplasma research
Radio astronomy - Haystack-Millstone OH INTERFEROMETER, K-band spectrum measurements of sun, inference of atmospheric attenuation from balloon flights, and microwave emission
Evaluating rangeland resources by multispectral photography, line-scan imagery, thermal infrared and K-band radar imagery, and spacecraft color photography
Airborne K-band radar imagery of Caliente and Temblor range area
The image enhancement system is described, as well as the kinds of enhancement attained. Results were obtained from various kinds of remote sensing imagery (mainly black and white multiband, color, color infrared, thermal infrared, and side-looking K-band radar) of parts of Yellowstone National Park. Possible additional fields of application of these techniques are considered.