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Research Opportunities
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NASA Earth Expeditions Blog
Documents
Related Links
Videos
Platforms
All Platforms
Aircraft Comparison
Mission Map
Asset Tracker
Flight Request
Aircraft Activities by Flight Request
ASP Sensor Network
Schedule
Aircraft Current Status
Aircraft Overview Schedule
Aircraft Detailed Schedule
5 - Year Plan
Instruments
Instrument Database
Facility Instruments
Instrument TRL levels
Engineering Support
ASP Sensor Network
Payload Information Form
Instrument FAQs
General Use Equipment
Mission Tools
Aircraft Tracker
MTS
NEX
JPL Hurricane Tool
LaRC Sub-Orbital Order Tool (SOOT)
ASP Data Repository
3D Models
Flight Request
PI Support
Current Call Letter
Transport of passengers on NASA Aircraft
Pre-Proposal Support
Costing Support
SATCOM Requirements
Engineering Support
Flight Request Procedures
Situational Awareness FAQs
SOFRS FAQs
Inactive Aircraft
ASP Sensor Network
Mishap Preparedness and Contingency Plan
Home
>
Atmospheric Composition
> Upper Atmosphere Research Program
Acronym:
UARP
Manager:
Ken Jucks
Subtropical and midlatitude ozone trends in the stratosphere: Implications for recovery
Nair, P. J.,
et al.
(2015),
Subtropical and midlatitude ozone trends in the stratosphere: Implications for recovery
,
J. Geophys. Res., 120
, 7247-7257, doi:10.1002/2014JD022371.
Read more
about Subtropical and midlatitude ozone trends in the stratosphere: Implications for recovery
An update on ozone profile trends for the period 2000 to 2016
Steinbrecht, W.,
et al.
(2017),
An update on ozone profile trends for the period 2000 to 2016
,
Atmos. Chem. Phys., 17
, 10675-10690, doi:10.5194/acp-17-10675-2017.
Read more
about An update on ozone profile trends for the period 2000 to 2016
Recent Northern Hemisphere stratospheric HCl increase due to atmospheric circulation changes
Mahieu, E.,
et al.
(2017),
Recent Northern Hemisphere stratospheric HCl increase due to atmospheric circulation changes
,
Nature
, doi:10.1038/nature13857.
Read more
about Recent Northern Hemisphere stratospheric HCl increase due to atmospheric circulation changes
16 Measurements and modeling of O12C17O spectroscopic parameters at 2 mm
Jacquemart, D.
,
et al.
(2017),
16 Measurements and modeling of O12C17O spectroscopic parameters at 2 mm
,
J. Quant. Spectrosc. Radiat. Transfer
, doi:10.1016/j.jqsrt.2017.03.002.
Read more
about 16 Measurements and modeling of O12C17O spectroscopic parameters at 2 mm
Using high-resolution laboratory and ground-based solar spectra to assess CH4 absorption coefficient calculations
Mendonca, J.
,
et al.
(2017),
Using high-resolution laboratory and ground-based solar spectra to assess CH4 absorption coefficient calculations
,
J. Quant. Spectrosc. Radiat. Transfer, 190
, 48-59, doi:10.1016/j.jqsrt.2016.12.013.
Read more
about Using high-resolution laboratory and ground-based solar spectra to assess CH4 absorption coefficient calculations
A Match-based approach to the estimation of polar stratospheric ozone loss using Aura Microwave Limb Sounder observations
Livesey, N.
,
M. Santee
, and
G. L. Manney
(2015),
A Match-based approach to the estimation of polar stratospheric ozone loss using Aura Microwave Limb Sounder observations
,
Atmos. Chem. Phys., 15
, 9945-9963, doi:10.5194/acp-15-9945-2015.
Read more
about A Match-based approach to the estimation of polar stratospheric ozone loss using Aura Microwave Limb Sounder observations
OH Radical Reaction Rate Coefficients, Infrared Spectrum, and Global Warming Potential of (CF3)2CFCHHCHF (HFO-1438ezy(E))
Papadimitriou, V. C., and
J. Burkholder
(2016),
OH Radical Reaction Rate Coefficients, Infrared Spectrum, and Global Warming Potential of (CF3)2CFCHHCHF (HFO-1438ezy(E))
,
J. Phys. Chem. A, 120
, 6618-6628, doi:10.1021/acs.jpca.6b06096.
Read more
about OH Radical Reaction Rate Coefficients, Infrared Spectrum, and Global Warming Potential of (CF3)2CFCHHCHF (HFO-1438ezy(E))
Rate Coefficient for the Gas-Phase OH + CHF=CF2 Reaction between 212 and 375 K
(2016),
Rate Coefficient for the Gas-Phase OH + CHF=CF2 Reaction between 212 and 375 K
.
Read more
about Rate Coefficient for the Gas-Phase OH + CHF=CF2 Reaction between 212 and 375 K
UV and infrared absorption spectra, atmospheric lifetimes, and ozone depletion and global warming potentials for CCl2FCCl2F (CFC-112), CCl3CClF2 (CFC-112a), CCl3CF3 (CFC-113a), and CCl2FCF3 (CFC-114a)
Davis, M. E.,
et al.
(2016),
UV and infrared absorption spectra, atmospheric lifetimes, and ozone depletion and global warming potentials for CCl2FCCl2F (CFC-112), CCl3CClF2 (CFC-112a), CCl3CF3 (CFC-113a), and CCl2FCF3 (CFC-114a)
,
Atmos. Chem. Phys., 16
, 8043-8052, doi:10.5194/acp-16-8043-2016.
Read more
about UV and infrared absorption spectra, atmospheric lifetimes, and ozone depletion and global warming potentials for CCl2FCCl2F (CFC-112), CCl3CClF2 (CFC-112a), CCl3CF3 (CFC-113a), and CCl2FCF3 (CFC-114a)
CBrF3 (Halon-1301): UV absorption spectrum between 210 and 320 K, atmospheric lifetime, and ozone depletion potential
Bernard, F.,
et al.
(2015),
CBrF3 (Halon-1301): UV absorption spectrum between 210 and 320 K, atmospheric lifetime, and ozone depletion potential
,
Journal of Photochemistry and Photobiology A: Chemistry, 306
, 13-20, doi:10.1016/j.jphotochem.2015.03.012.
Read more
about CBrF3 (Halon-1301): UV absorption spectrum between 210 and 320 K, atmospheric lifetime, and ozone depletion potential
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