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Earth Science: Atmospheric Chemical and Dynamical Studies Using Tunable Infrared Diode-Laser Spectroscopy

RO#

17505

Location

Ames Research Center
Moffett Field, CA 94035-1000

Advisor Information

NamePhoneEmail
Loewenstein, M. (650)604-5504 mloewenstein@mail.arc.nasa.gov
Podolske, James Robert (650)604-4853 jpodolske@mail.arc.nasa.gov

Research Area

Earth and Atmospheric Sciences

Keywords

Atmospheric chemistry; Atmospheric trace constituents; Stratosphere; Atmospheric ozone; Laser spectra; Infrared spectra; Diode lasers;

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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