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Earth Science: Atmospheric Chemical and Dynamical Studies Using Tunable Infrared Diode-Laser Spectroscopy
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RO#
17505 |
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Location
Ames Research Center
Moffett Field, CA 94035-1000 |
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Advisor Information
| Name | Phone | Email |
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Loewenstein, M.
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(650)604-5504
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mloewenstein@mail.arc.nasa.gov
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Podolske, James Robert
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(650)604-4853
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jpodolske@mail.arc.nasa.gov
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Research Area
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Earth and Atmospheric Sciences
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Keywords
Atmospheric chemistry; Atmospheric trace constituents; Stratosphere; Atmospheric ozone; Laser spectra; Infrared spectra; Diode lasers; |
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Description
Atmospheric motions play an important role in the transport of
stratospheric ozone and chemicals that affect the stratospheric
ozone layer. These motions are an important aspect of
chemical/dynamical models that are used to model stratospheric ozone
and to predict possible human-induced impacts on the ozone layer. To
define the dynamical part of the atmospheric system, a number of
tracers (e.g., methane, nitrous oxide, and carbon monoxide) of
atmospheric motion are readily measured using tunable diode-lasers.
All of these are present at small but measurable concentrations, and
all have characteristic and well-known horizontal and vertical
distributions in the stratosphere.
Several different molecular families are responsible for
establishing the steady-state concentration levels of ozone in the
atmosphere. One family of current interest is the odd nitrogen
family. Within this family, the molecules of HNO3 and
NO2 are particularly important. NO2 provides a
source of nitrogen radicals that remove ozone, while HNO3
provides a reservoir that sequesters odd nitrogen in an inert form,
with respect of ozone.
We are developing and deploying-for field atmospheric
measurements-tunable infrared diode-laser-based instruments using
wavelength modulation techniques. The Airborne Tunable Laser
Absorption Spectrometer, dedicated to measuring the tracer
N2O, has been flying on the ER-2 high-altitude aircraft
since 1986. Argus, a two-channel diode-laser instrument, measures
CH4 and N2O on balloon platforms and unmanned
aero vehicles, and has been operational since 1996. Finally, an
entirely new instrument (OPTIMA) has recently been deployed on the
DC-8 aircraft to measure NO2 and HNO3.
In conjunction with the efforts described above, we maintain a
well-equipped laboratory for infrared spectroscopy to support the
variety of experimental, laser testing, and spectral simulation
needs required in developing and calibrating our airborne
instruments.
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