Temperature dependence of the water vapor self-continuum by cavity ring-down spectroscopy in the 1.6 µm transparency window

2014 ◽  
Vol 119 (9) ◽  
pp. 5625-5639 ◽  
Author(s):  
D. Mondelain ◽  
S. Manigand ◽  
S. Kassi ◽  
A. Campargue
Keyword(s):  
Water Vapor ◽  
Temperature Dependence ◽  
Transparency Window ◽  
Cavity Ring Down Spectroscopy ◽  
Cavity Ring Down

Water-vapor measurement via cavity ring down spectroscopy in the visible

1998 ◽  
Author(s):  
Fuge Sun ◽  
Dongxu Dai ◽  
Lu Kang ◽  
Guohea Sha ◽  
JinChun Xie ◽  
...  
Keyword(s):  
Water Vapor ◽  
Cavity Ring Down Spectroscopy ◽  
Cavity Ring Down

scholarly journals Field Testing of Cavity Ring-Down Spectroscopy Analyzers Measuring Carbon Dioxide and Water Vapor

2012 ◽  
Vol 29 (3) ◽  
pp. 397-406 ◽  
Author(s):  
Scott J. Richardson ◽  
Natasha L. Miles ◽  
Kenneth J. Davis ◽  
Eric R. Crosson ◽  
Chris W. Rella ◽  
...  
Keyword(s):  
Water Vapor ◽  
Field Measurements ◽  
Field Testing ◽  
The United States ◽  
Upper Midwest ◽  
Cavity Ring Down Spectroscopy ◽  
The North ◽  
Improved Stability ◽  
Field Deployment ◽  
Cavity Ring Down

Abstract Prevalent methods for making high-accuracy tower-based measurements of the CO2 mixing ratio, notably nondispersive infrared spectroscopy (NDIR), require frequent system calibration and sample drying. Wavelength-scanned cavity ring-down spectroscopy (WS-CRDS) is an emerging laser-based technique with the advantages of improved stability and concurrent water vapor measurements. Results are presented from 30 months of field measurements from WS-CRDS systems at five sites in the upper Midwest of the United States. These systems were deployed in support of the North American Carbon Program’s Mid-Continent Intensive (MCI) from May 2007 to November 2009. Excluding one site, 2σ of quasi-daily magnitudes of the drifts, before applying field calibrations, are less than 0.38 ppm over the entire 30-month field deployment. After applying field calibrations using known tanks sampled every 20 h, residuals from known values are, depending on site, from 0.02 ±0.14 to 0.17 ±0.07 ppm. Eight months of WS-CRDS measurements collocated with a National Oceanographic and Atmospheric Administrations (NOAA)/Earth System Research Laboratory (ESRL) NDIR system at West Branch, Iowa, show median daytime-only differences of −0.13 ±0.63 ppm on a daily time scale.

scholarly journals High-accuracy continuous airborne measurements of greenhouse gases (CO<sub>2</sub> and CH<sub>4</sub>) using the cavity ring-down spectroscopy (CRDS) technique

2010 ◽  
Vol 3 (2) ◽  
pp. 375-386 ◽  
Author(s):  
H. Chen ◽  
J. Winderlich ◽  
C. Gerbig ◽  
A. Hoefer ◽  
C. W. Rella ◽  
...  
Keyword(s):  
Water Vapor ◽  
Greenhouse Gases ◽  
Ambient Air ◽  
High Accuracy ◽  
Mean Difference ◽  
Pressure Broadening ◽  
Cavity Ring Down Spectroscopy ◽  
Airborne Measurements ◽  
The Mean ◽  
Cavity Ring Down

Abstract. High-accuracy continuous measurements of greenhouse gases (CO2 and CH4) during the BARCA (Balanço Atmosférico Regional de Carbono na Amazônia) phase B campaign in Brazil in May 2009 were accomplished using a newly available analyzer based on the cavity ring-down spectroscopy (CRDS) technique. This analyzer was flown without a drying system or any in-flight calibration gases. Water vapor corrections associated with dilution and pressure-broadening effects for CO2 and CH4 were derived from laboratory experiments employing measurements of water vapor by the CRDS analyzer. Before the campaign, the stability of the analyzer was assessed by laboratory tests under simulated flight conditions. During the campaign, a comparison of CO2 measurements between the CRDS analyzer and a nondispersive infrared (NDIR) analyzer on board the same aircraft showed a mean difference of 0.22±0.09 ppm for all flights over the Amazon rain forest. At the end of the campaign, CO2 concentrations of the synthetic calibration gases used by the NDIR analyzer were determined by the CRDS analyzer. After correcting for the isotope and the pressure-broadening effects that resulted from changes of the composition of synthetic vs. ambient air, and applying those concentrations as calibrated values of the calibration gases to reprocess the CO2 measurements made by the NDIR, the mean difference between the CRDS and the NDIR during BARCA was reduced to 0.05±0.09 ppm, with the mean standard deviation of 0.23±0.05 ppm. The results clearly show that the CRDS is sufficiently stable to be used in flight without drying the air or calibrating in flight and the water corrections are fully adequate for high-accuracy continuous airborne measurements of CO2 and CH4.

Cavity ring-down spectroscopy of 17O-enriched water vapor between 12,055 and 12,260 cm−1

2019 ◽  
Vol 239 ◽  
pp. 106651 ◽  
Author(s):  
A.-W. Liu ◽  
G.-L. Liu ◽  
X.-Q. Zhao ◽  
J. Wang ◽  
Y. Tan ◽  
...  
Keyword(s):  
Water Vapor ◽  
Cavity Ring Down Spectroscopy ◽  
Cavity Ring Down
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