scholarly journals Micro-Spec: an ultracompact, high-sensitivity spectrometer for far-infrared and submillimeter astronomy

2014 ◽  
Vol 53 (6) ◽  
pp. 1094 ◽  
Author(s):  
Giuseppe Cataldo ◽  
Wen-Ting Hsieh ◽  
Wei-Chung Huang ◽  
S. Harvey Moseley ◽  
Thomas R. Stevenson ◽  
...  
2004 ◽  
Author(s):  
Robert F. Silverberg ◽  
Christine A. Allen ◽  
Sachidananda R. Babu ◽  
Dominic J. Benford ◽  
David T. Chuss ◽  
...  

2002 ◽  
Vol 80 (1) ◽  
pp. 136-138 ◽  
Author(s):  
Y. Kawaguchi ◽  
K. Hirakawa ◽  
M. Saeki ◽  
K. Yamanaka ◽  
S. Komiyama

2017 ◽  
Vol 88 (8) ◽  
pp. 083508 ◽  
Author(s):  
Y. G. Li ◽  
Y. Zhou ◽  
Y. Li ◽  
Z. C. Deng ◽  
H. X. Wang ◽  
...  

2016 ◽  
Vol 87 (11) ◽  
pp. 11E125 ◽  
Author(s):  
B. H. Deng ◽  
M. Beall ◽  
J. Schroeder ◽  
G. Settles ◽  
P. Feng ◽  
...  

2019 ◽  
Vol 485 (2) ◽  
pp. 2844-2860 ◽  
Author(s):  
C Dickinson ◽  
A Barr ◽  
H C Chiang ◽  
C Copley ◽  
R D P Grumitt ◽  
...  

ABSTRACT The C-Band All-Sky Survey (C-BASS) is a high sensitivity all-sky radio survey at an angular resolution of 45 arcmin and a frequency of 4.7 GHz. We present a total intensity map of the North Celestial Pole (NCP) region of sky, above declination >+80°, which is limited by source confusion at a level of ≈0.6 mK rms. We apply the template-fitting (cross-correlation) technique to WMAP and Planck data, using the C-BASS map as the synchrotron template, to investigate the contribution of diffuse foreground emission at frequencies ∼20–40 GHz. We quantify the anomalous microwave emission (AME) that is correlated with far-infrared dust emission. The AME amplitude does not change significantly (${\lt }10\, {{\ \rm per\ cent}}$) when using the higher frequency C-BASS 4.7 GHz template instead of the traditional Haslam 408 MHz map as a tracer of synchrotron radiation. We measure template coefficients of 9.93 ± 0.35 and $9.52\pm 0.34\,$ K per unit τ353 when using the Haslam and C-BASS synchrotron templates, respectively. The AME contributes $55\pm 2\, \mu$K rms at 22.8 GHz and accounts for ${\approx } 60{{\ \rm per\ cent}}$ of the total foreground emission. Our results show that a harder (flatter spectrum) component of synchrotron emission is not dominant at frequencies ≳5 GHz; the best-fitting synchrotron temperature spectral index is β = −2.91 ± 0.04 from 4.7 to 22.8 GHz and β = −2.85 ± 0.14 from 22.8 to 44.1 GHz. Free–free emission is weak, contributing ${\approx } 7\, \mu$K rms (${\approx } 7{{\ \rm per\ cent}}$) at 22.8 GHz. The best explanation for the AME is still electric dipole emission from small spinning dust grains.


2014 ◽  
Vol 31 (7) ◽  
pp. 1502-1515 ◽  
Author(s):  
Maziar Bani Shahabadi ◽  
Yi Huang

Abstract This study examines the ability of an infrared spectral sensor flying at the tropopause level for retrieving stratospheric H2O. Synthetic downwelling radiance spectra simulated by the line-by-line radiative transfer model are used for this examination. The potential of high-sensitivity water vapor retrieval is demonstrated by an ideal sensor with low detector noise, high spectral resolution, and full infrared coverage. A suite of hypothetical sensors with varying specifications is then examined to determine the technological requirements for a satisfactory retrieval. This study finds that including far infrared in the sensor’s spectral coverage is essential for achieving accurate H2O retrieval with an accuracy of 0.4 ppmv (1-sigma). The uncertainties in other gas species such as CH4, N2O, O3, and CO2 do not significantly affect the H2O retrieval. Such a hyperspectral instrument may afford an advantageous tool, especially for detecting small-scale lower-stratospheric moistening events.


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