Author
A. R. Ravishankara
Other affiliations: Cooperative Institute for Research in Environmental Sciences, University of Colorado Boulder
Bio: A. R. Ravishankara is an academic researcher from National Oceanic and Atmospheric Administration. The author has contributed to research in topics: Reaction rate constant & Kinetics. The author has an hindex of 41, co-authored 88 publications receiving 5129 citations. Previous affiliations of A. R. Ravishankara include Cooperative Institute for Research in Environmental Sciences & University of Colorado Boulder.
Papers published on a yearly basis
Papers
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TL;DR: In this article, the first reversible addition of CH{sub 3}S + O{sub 2} {r_equilibrium} CH {sub 3]SOO, in the gas phase (T = 216-258 K), was observed by detecting CH{ sub 3} S radicals.
Abstract: This report observes for the first time the reversible addition of: CH{sub 3}S + O{sub 2} {r_equilibrium} CH{sub 3}SOO, in the gas phase (T = 216-258 K) by detecting CH{sub 3}S radicals. Also briefly described is the thermochemical and kinetic information of this system and its importance to the atmospheric oxidation of reduced sulfur compounds.
68 citations
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67 citations
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TL;DR: In this paper, the quantum yields for OH, O(3P), O(1D), and H(2S) from the photolysis of HNO3 have been determined at 248, 222, and 193 nm at 298 K.
Abstract: The quantum yields for OH, O(3P), O(1D), and H(2S) from the photolysis of HNO3 have been determined at 248, 222, and 193 nm at 298 K. The quantum yield for OH was observed to be near unity at 248 [Φ(OH)=0.95±0.09] and 222 nm [Φ(OH)=0.90±0.11]. However, at 193 nm the quantum yield for OH was found to be 0.33±0.06. The quantum yield for O atoms [O(3P)+O(1D)], Φ(O), was observed to be 0.031±0.010, 0.20±0.03, 0.81±0.13, at 248, 222, and 193 nm, respectively. Both O(3P) and O(1D) were observed at 222 and 193 nm, but only O(3P) was detected at 248 nm. It was observed that 40% of the O atoms formed at both 193 and 222 nm were O(1D) atoms. The upper limits for H(2S) quantum yields: Φ(H)≤0.002 at 248 nm, ≤0.01 at 222 nm, and ≤0.012 at 193 nm were also determined. This present work quantifies the photolysis channel producing HONO+O and show that it accounts for a large fraction at HNO3 photolysis at 193 nm.
65 citations
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TL;DR: In this paper, the rate coefficients for the reaction of OD radical with between 220 and 410 K were measured and the results showed that OD reactions were slightly (ca.10-15%) higher than those for OH reactions.
Abstract: The rate coefficients for the reaction of OH radical with
CH
3
ONO
2
(k
1
),
CD
3
ONO
2
(k
6
),
C
2
H
5
ONO
2
(k
2
) and
2-C
3
H
7
ONO
2
(k
3
) between 220 and 410 K were measured
to be:
k
1
=(8.2±1.6)×10
-13
exp{-(1020±60)/T},
k
6
=(1.6±0.2)×10
-12
exp{-(1730±40)/T},
k
2
=3.68×10
-12
exp(-1077/T)+5.32×10
-14
exp(126/T) and
k
3
=4.3×10
-12
exp(-1250/T)+2.5×10
-13
exp(-32/T) cm
3
molecule
-1
s
-1
. The quoted errors in the Arrhenius
expressions are at the 95% confidence limit and include
estimated systematic errors. The measured rate coefficients
for the reactions of 18
OH were roughly the same
as those for 16
OH reactions while the rate
constants for OD reactions were slightly (ca.
10–15%) higher than those for OH reactions. The
hydroxyl radicals were generated by pulsed laser photolysis
and detected by pulsed laser induced fluorescence. The
observed large primary kinetic isotope effect
(k
1
/k
6
=4.5 at 298
K), the independence of the measured rate coefficients on
the gas composition, and the trend in the reactivity with
the alkyl group suggests that the above reactions proceed
via abstraction of an H atom from the alkyl group.
Our results are compared with those from previous studies.
64 citations
Cited by
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Harvard University1, University of Reims Champagne-Ardenne2, College of William & Mary3, Old Dominion University4, University of Lisbon5, University of Burgundy6, California Institute of Technology7, Centre national de la recherche scientifique8, Université catholique de Louvain9, University of York10, University College London11, National Institute of Standards and Technology12, University of Waterloo13, National Center for Atmospheric Research14, University of Cologne15, Karlsruhe Institute of Technology16, Langley Research Center17
TL;DR: The new HITRAN is greatly extended in terms of accuracy, spectral coverage, additional absorption phenomena, added line-shape formalisms, and validity, and molecules, isotopologues, and perturbing gases have been added that address the issues of atmospheres beyond the Earth.
Abstract: This paper describes the contents of the 2016 edition of the HITRAN molecular spectroscopic compilation. The new edition replaces the previous HITRAN edition of 2012 and its updates during the intervening years. The HITRAN molecular absorption compilation is composed of five major components: the traditional line-by-line spectroscopic parameters required for high-resolution radiative-transfer codes, infrared absorption cross-sections for molecules not yet amenable to representation in a line-by-line form, collision-induced absorption data, aerosol indices of refraction, and general tables such as partition sums that apply globally to the data. The new HITRAN is greatly extended in terms of accuracy, spectral coverage, additional absorption phenomena, added line-shape formalisms, and validity. Moreover, molecules, isotopologues, and perturbing gases have been added that address the issues of atmospheres beyond the Earth. Of considerable note, experimental IR cross-sections for almost 300 additional molecules important in different areas of atmospheric science have been added to the database. The compilation can be accessed through www.hitran.org. Most of the HITRAN data have now been cast into an underlying relational database structure that offers many advantages over the long-standing sequential text-based structure. The new structure empowers the user in many ways. It enables the incorporation of an extended set of fundamental parameters per transition, sophisticated line-shape formalisms, easy user-defined output formats, and very convenient searching, filtering, and plotting of data. A powerful application programming interface making use of structured query language (SQL) features for higher-level applications of HITRAN is also provided.
7,638 citations
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TL;DR: In this article, the authors present a document, redatto, voted and pubblicato by the Ipcc -Comitato intergovernativo sui cambiamenti climatici - illustra la sintesi delle ricerche svolte su questo tema rilevante.
Abstract: Cause, conseguenze e strategie di mitigazione Proponiamo il primo di una serie di articoli in cui affronteremo l’attuale problema dei mutamenti climatici. Presentiamo il documento redatto, votato e pubblicato dall’Ipcc - Comitato intergovernativo sui cambiamenti climatici - che illustra la sintesi delle ricerche svolte su questo tema rilevante.
4,187 citations
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01 Jan 2014
TL;DR: Myhre et al. as discussed by the authors presented the contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change (IPCC) 2013: Anthropogenic and Natural Radiative forcing.
Abstract: This chapter should be cited as: Myhre, G., D. Shindell, F.-M. Bréon, W. Collins, J. Fuglestvedt, J. Huang, D. Koch, J.-F. Lamarque, D. Lee, B. Mendoza, T. Nakajima, A. Robock, G. Stephens, T. Takemura and H. Zhang, 2013: Anthropogenic and Natural Radiative Forcing. In: Climate Change 2013: The Physical Science Basis. Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change [Stocker, T.F., D. Qin, G.-K. Plattner, M. Tignor, S.K. Allen, J. Boschung, A. Nauels, Y. Xia, V. Bex and P.M. Midgley (eds.)]. Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA. Coordinating Lead Authors: Gunnar Myhre (Norway), Drew Shindell (USA)
3,684 citations
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TL;DR: The present status of knowledge of the gas phase reactions of inorganic Ox, Hox and NOx species and of selected classes of volatile organic compounds (VOCs) and their degradation products in the troposphere is discussed in this paper.
2,722 citations
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2,290 citations