Yu. I. BARANOV, W. J. LAFFERTY, and G. T. Fraser Optical Technology Division Optical Technology Division National Institute of Standards and Technology,

Slides:



Advertisements
Similar presentations
Yu. I. BARANOV, W. J. LAFFERTY, and G. T. Fraser Optical Technology Division Optical Technology Division National Institute of Standards and Technology,
Advertisements

TAFTS: Comparing Uncertainties in Atmospheric Profiles with the Water Vapour Continuum Ralph Beeby, Paul Green, Juliet Pickering, John Harries.
1 Water vapour self-continuum: Recent update from Reading/RAL Semi-annual CAVIAR meeting UCL, London Igor Ptashnik, Keith Shine, Andrey Vigasin.
1 Water vapour self-continuum: Recent interpretation Igor Ptashnik, Keith Shine, Andrey Vigasin University of Reading (UK) Zuev Institute of Atmospheric.
1 Annual CAVIAR meeting, , Imperial College London Water vapour continuum absorption in near- and middle-IR: Recent investigations Department.
1 Analysis of BBCRDS Spectra: Inferred Upper Limits for Water Dimer Absorption A.J.L. Shillings 1, S.M. Ball 2 and R.L. Jones 1 1 University of Cambridge,
Molecular pairs in the atmosphere, the carriers of continuum-like absorption Andrei A. Vigasin General Physics & Atmospheric Physics Institutes, Russian.
CAVIAR – Continuum Absorption by Visible and Infrared Radiation and its Atmospheric Relevance PI: Keith Shine Department of Meteorology, University of.
CAVIAR – Continuum Absorption by Visible and Infrared Radiation and its Atmospheric Relevance PI: Keith Shine Department of Meteorology, University of.
Thinh Bui1, Daniel Hogan1, Priyanka M. Rupasinghe1, Mitchio Okumura1
Philosophical Transactions A
Laboratory Measurement of CO 2 ( 2 ) + O Temperature-Dependent Vibrational Energy Transfer Karen J. Castle, 1 Michael Simione, 1 Eunsook S. Hwang, 2 and.
High sensitivity CRDS of the a 1 ∆ g ←X 3 Σ − g band of oxygen near 1.27 μm: magnetic dipole and electric quadrupole transitions in different bands of.
Yu. I. BARANOV and W. J. LAFFERTY Optical Technology Division Optical Technology Division National Institute of Standards and Technology, Gaithersburg,
Pacific Northwest National Laboratory The Ohio State University 20 June 2006 T. Masiello, T.J. Johnson and S.W. Sharpe Pacific Northwest National Laboratory.
TEMPERATURE DEPENDENCES OF MECHANISMS RESPONCIBLE FOR THE WATER-VAPOR CONTINUUM Q. Ma NASA/Goddard Institute for Space Studies & Department of Applied.
MULTIPLEXED CHIRPED PULSE QUANTUM CASCADE LASER MEASUREMENTS OF AMMONIA AND OTHER SMALL MOLECULES Craig Picken, David Wilson, Nigel Langford and Geoffrey.
CAVIAR water vapour laboratory FTS measurements Dr Robert McPheat CAVIAR Meeting Cosners’ House, 15/12/2009.
EXPERIMENTAL AND THEORETICAL STUDY OF WATER-VAPOR CONTINUUM ABSORPTION IN THE THZ REGION FROM 0.3 TO 2.7 THZ V.B. PODOBEDOV, D.F. PLUSQUELLIC, K.M. SIEGRIST.
Update on the Leicester lab studies (WP2.2 cavity ringdown spectroscopy) Stephen Ball & Simon Neil (Leicester University) CAVIAR science meeting, NPL,
David Paynter, Igor Ptashnik, Keith Shine Department of Meteorology University of Reading Kevin Smith (RAL) June 2006 Pure water vapor continuum measurements.
Laser spectroscopic study of ozone in the 100←000 band for the SWIFT instrument M. Guinet, C. Janssen, D. Mondelain, C. Camy-Peyret LPMAA, CNRS- UPMC (France)
The electromagnetic spectrum covers a continuous range of wavelengths and frequencies, from radio waves at the low-frequency end to gamma (  ) rays at.
(8) Absorption – Visible and IR Physics of the Atmosphere II Atmo II 193a.
THE ACE SATELLITE SOLAR SPECTRUM
Pat Arnott, ATMS 749, UNR, 2008 Chapter 9: Absorption by Atmospheric Gases Visible and UV Absorption: due to electronic transitions. Monatomic - polyatomic.
LINE PARAMETERS OF WATER VAPOR IN THE NEAR- AND MID-INFRARED REGIONS DETERMINED USING TUNEABLE LASER SPECTROSCOPY Nofal IBRAHIM, Pascale CHELIN, Johannes.
First high resolution analysis of the 5 3 band of nitrogen dioxide (NO 2 ) near 1.3 µm Didier Mondelain 1, Agnès Perrin 2, Samir Kassi 1 & Alain Campargue.
HIGH-RESOLUTION ABSORPTION CROSS SECTIONS OF C 2 H 6 AND C 3 H 8 AT LOW TEMPERATURES ROBERT J. HARGREAVES DANIEL J. FROHMAN
IR/THz Double Resonance Spectroscopy in the Pressure Broadened Regime: A Path Towards Atmospheric Gas Sensing Sree H. Srikantaiah Dane J. Phillips Frank.
Self- and Air-Broadening, Shifts, and Line Mixing in the ν 2 Band of CH 4 M. A. H. Smith 1, D. Chris Benner 2, V. Malathy Devi 2, and A. Predoi-Cross 3.
Self- and air-broadened line shape parameters in the band of 12 CH 4 : cm -1 V. Malathy Devi Department of Physics The College of William.
New H 2 16 O measurements of line intensities around 1300 cm -1 and 8800 cm - 1 Oudot Charlotte Groupe de Spectrométrie Moléculaire et Atmosphérique Reims,
1 Forward Modeling for Far-Infrared Remote Sensing: Spectroscopic Issues and Line-by-Line Modeling Tony Clough Clough Radiation Associates, LLC CRA and.
Emission Spectra of H 2 17 O and H 2 18 O from 320 to 2500 cm -1 Semen MIKHAILENKO 1, Georg MELLAU 2, and Vladimir TYUTEREV 3 1 Laboratory of Theoretical.
Pressure Broadening and Spectral Overlap in the Millimeter Wave Spectrum of Ozone International Symposium on Molecular Spectroscopy 65 th Meeting — June.
Physics of the Atmosphere II
PUMP-PROBE MEASUREMENTS OF ROTATIONAL ENERGY TRANSFER RATES IN HBr + HBr COLLISIONS M. H. Kabir, I. O. Antonov, and M. C. Heaven Emory University Department.
Beers Law for a Single Component Sample I0I0 A = Absorbance = - log 10 I I / I 0 b = Optical path length c = Solution Concentration (M/L) ε = Molar Absorptivity.
1 N. NISHIMIYA and T. YUKIYA Tokyo Polytechnic University, Kanagawa, JAPAN. HIGH – RESOLUTION LASER SPECTROSCOPY OF THE A 3 Π 1 ← X 1 Σ + SYSTEM OF ICl.
Electronic Spectroscopy of Palladium Dimer (Pd 2 ) 68th OSU International Symposium on Molecular Spectroscopy Yue Qian, Y. W. Ng and A. S-C. Cheung Department.
Comparison of Experimental and Theoretical Cross-sections of PFBAm By: Paul J. Godin, Stephanie Conway, Angela Hong, Karine Le Bris, Scott Mabury, and.
Misure ottiche su atmosfere planetarie in laboratorio
Precision Measurement of CO 2 Hotband Transition at 4.3  m Using a Hot Cell PEI-LING LUO, JYUN-YU TIAN, HSHAN-CHEN CHEN, Institute of Photonics Technologies,
Tony Clough, Mark Shephard and Jennifer Delamere Atmospheric & Environmental Research, Inc. Colleagues University of Wisconsin International Radiation.
Line list of HD 18 O rotation-vibration transitions for atmospheric applications Semen MIKHAILENKO, Olga NAUMENKO, and Sergei TASHKUN Laboratory of Theoretical.
DIODE-LASER AND FOURIER-TRANSFORM SPECTROSCOPY OF 14 NH 3 AND 15 NH 3 IN THE NEAR-INFRARED (1.5 µm) Nofal IBRAHIM, Pascale CHELIN, Johannes ORPHAL Laboratoire.
Beamline AILES : Mid IR to THz Spectroscopy The AILES Infrared and THz High Resolution Spectroscopy beamline at SOLEIL (Saclay, 30 km south of Paris) –
CO 2 Lineshapes Near 2060nm Thinh Q. Bui California Institute of Technology ISMS 2014.
CH 3 D Near Infrared Cavity Ring-down Spectrum Reanalysis and IR-IR Double Resonance S. Luna Yang George Y. Schwartz Kevin K. Lehmann University of Virginia.
SELF- AND CO 2 -BROADENED LINE SHAPE PARAMETERS FOR THE 2 AND 3 BANDS OF HDO V. MALATHY DEVI, D. CHRIS BENNER, Department of Physics, College of William.
Physical basis of the Greenhouse Effect -The “wavelength shift”- 1.Black body radiation, 2.Absorption spectra 3.Conservation of energy Energy & Environment.
Line Mixing in Atmospheric Ozone Corey Casto and Frank C. De Lucia The Ohio State University International Symposium on Molecular Spectroscopy 66 th Meeting.
Collision-Dependent Line Areas in the a 1 Δ g ←X 3 Σ − g Band of O 2 Vincent Sironneau, Adam J. Fleisher,* and Joseph T. Hodges Material Measurement Laboratory.
Yu. I. BARANOV, and W. J. LAFFERTY Optical Technology Division Optical Technology Division National Institute of Standards and Technology, Gaithersburg,
D. Mondelain, A. Campargue, S. Kassi Laboratoire Interdisciplinaire de Physique Université Grenoble 1/CNRS The water vapor self-continuum in the 1.6 µm.
ROTATION-VIBRATIONAL ANALYSIS OF THE BANDS OF FORMALDEHYDE FALLING IN THE 3900 TO 5300 CM -1 REGION W.J. LAFFERTY Optical Technology Division NIST Gaithersburg,
OBSERVATION AND ANALYSIS OF THE A 1 -A 2 SPLITTING OF CH 3 D M. ABE*, H. Sera and H. SASADA Department of Physics, Faculty of Science and Technology, Keio.
The Cyclic CO 2 Trimer: Observation of two parallel bands and determination of intermolecular out-of-plane torsional frequencies Steacie Institute for.
EXPERIMENTAL TRANSMISSION SPECTRA OF HOT AMMONIA IN THE INFRARED Monday, June 22 nd 2015 ISMS 70 th Meeting Champaign, Illinois EXPERIMENTAL TRANSMISSION.
Line mixing and collision induced absorption in the A-band of molecular oxygen: catching oxygen in collisions! Wim J. van der Zande, Maria Kiseleva +,
1 Atmospheric Radiation – Lecture 13 PHY Lecture 13 Remote sensing using emitted IR radiation.
Frequency-comb referenced spectroscopy of v 4 =1 and v 5 =1 hot bands in the 1. 5 µm spectrum of C 2 H 2 Trevor Sears Greg Hall Talk WF08, ISMS 2015 Matt.
Date of download: 6/1/2016 Copyright © 2016 SPIE. All rights reserved. Schematic view of the pulsed PA spectrometer. Figure Legend: From: Investigation.
Erin M. Adkins, Melanie Ghysels, David A. Long, and Joseph T. Hodges
The Near-IR Spectrum of CH3D
Z. Reed,* O. Polyansky,† J. Hodges*
Nofal IBRAHIM, Pascale CHELIN, Johannes ORPHAL
An accurate and complete empirical line list for water vapor
A. M. Daly, B. J. Drouin, J. C. Pearson, K. Sung, L. R. Brown
Presentation transcript:

Yu. I. BARANOV, W. J. LAFFERTY, and G. T. Fraser Optical Technology Division Optical Technology Division National Institute of Standards and Technology, Gaithersburg, MD , USA The water-vapor continuum and selective absorption in the 8 to 12 μm and 3 to 5 μm windows at temperatures from 311 to 363K.

Introduction  The water vapor continuum absorption in the atmospheric 8 to 12 and 3 to 5 μm windows strongly affects the Earth’s outgoing and the Sun’s incoming radiation and therefore is of great importance for radiative balance calculations.

Introduction  Increasing use of lasers, spectrometers, and other IR techniques in atmospheric research, remote sensing, and environment protection also requires more precise data on water vapor continuum absorption coefficients

Introduction  Over the past twenty years many scientific groups in the world have used long-base (up to 100 m) long-path (up to several thousands m) cells to measure the H 2 O continuum.

Introduction  The other high-sensitive techniques, like photo-acoustic or cavity ring-down spectroscopy (CRDS) have also been employed for these measurements.  Revised and selected data were put on the basis of the CKD (a) continuum model, widely used for atmospheric spectroscopy applications. a S. A. Clough, F. X. Kneizys, and R. W. Davies, Atmos. Res. 23, (1989).

Experimental set-up view

Experimental conditions Spectral resolution is 0.1 cm -1 Spectral range 800 to 3500 cm -1 Temperature K (±0.3K) Pressure range kPa (torr) Path length m Number of spectra to 6.07 (21.2 to 45.5) to 7.42 (25.5 to 55.7) to 11.5 (33.7 to 86.3) to 12.3 (39.1 to 92.0) to 15.1 (43.2 to 113) to 13.7 (41.1 to 103)

An example of IR water vapor spectrum

The quick data treatment method

The basic data treatment method Two spectra at: Θ=318K L=116m P=51.2 torr Θ=352K L=116m P=111.9 torr

The basic data treatment method

Two spectra at: Θ=318K L=116m P=51.2 torr Θ=352K L=116m P=111.9 torr

The basic data treatment method Two spectra at: Θ=318K L=116m P=51.2 torr Θ=352K L=116m P=111.9 torr

The basic data treatment method Every data array for a given temperature Θ was fitted by function: using standard least square method.

Water vapor continuum binary absorption coefficients C s in cm -1 (mol/cm 3 ) -1 atm -1 compared with CKD model values Wavenumber, cm -1 The CKD values are shown as solid lines 310.8K 325.8K 351.9K

The temperature dependence of the continuum binary absorption coefficient at 942 cm -1 Nordstrom et al.,1978, (CO2-laser, White cell) Peterson et al., 1979, (CO2-laser, White cell) Eng and Mantz, 1980, (diode laser, White cell) Burch et al., 1982, (spectrometer, White cell) Loper et al., 1983, (CO2-laser, spectrophone) Hinderling, 1987, (CO2-laser, spectrophone) Cormier et al., 2005, (CO2-laser, CRDS) NIST 2006, (spectrometer, White cell) Clough, CKD model

The temperature dependence of the continuum binary absorption coefficient at 1203 cm -1 Montgomery, 1978 Burch et al., 1982 NIST, 2006 Clough CKD model

The temperature dependence of the continuum binary absorption coefficient Temperature, 1000/Θ, K -1

On a possible continuum origin

Pure nitrogen roto-translational band and CIA spectrum

On a possible continuum origin

Is the continuum a cumulative contribution of line far wings? Yes: Theoretical justification. No: It is hard to understand continuum’s not uniform temperature dependence. It is hard to explain why the continuum is shaped like typical CIA spectrum?

On a possible continuum origin Is the continuum absorption by water dimers? Yes: Water dimers exist. No: The main reason for the continuum “dimer” conception is its exponential temperature dependence with the exponent value close to the energy of dimer dissociation. But really it is not exponential and not uniform. There is no reasonable explanation for the nitrogen broadened continuum? It is hard to explain why the continuum is shaped like typical CIA spectrum?

On a possible continuum origin Is the continuum a water vapor Collision Induced Spectrum? Yes: It is shaped like collision induced spectrum. There is a very easy and clear explanation of the nitrogen broadened continuum. Water vapor CIA spectrum exists and it is expected to be very strong because of the first order magnitude dipole-dipole induction. No: A. Brown, R. H. Tipping, “Collision-induced absorption in dipolar molecule-homonuclear diatomic pairs”, C. Camy-Peyret and A. A. Vigasin (eds.), Weakly Interacting Molecular Pairs: Unconventional Absorbers of Radiation in the Atmosphere, (2003) Kluwer Academic Publisher

Summary  Pure water vapor spectra have been recorded over a wide range of temperatures and pressures.  Continuum binary absorption coefficients have been determined in the regions 800 to 1300 and 1930 to 2300 cm -1.  In the 800 to 1300 cm -1 region our data for lower temperature reasonably agree with data provided with CKD model. But the disagreement increases up to 50% at high temperatures.  In the high frequency segment our data satisfactory agree with CKD values around 2000 cm -1. But at higher wavenumbers the measured values greatly exceed the model.  The data presented show that over both regions the absorption coefficient temperature dependence is not purely exponential and not uniform.