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Validation of the Aura Microwave Limb Sounder temperature and geopotential height measurements

TLDR
In this article, the authors describe the retrievals algorithm used to determine temperature and height from radiance measurements by the Microwave Limb Sounder on EOS Aura, which is a "limbscanning" instrument, meaning that it views the atmosphere along paths that do not intersect the surface.
Abstract
This paper describes the retrievals algorithm used to determine temperature and height from radiance measurements by the Microwave Limb Sounder on EOS Aura. MLS is a "limbscanning" instrument, meaning that it views the atmosphere along paths that do not intersect the surface - it actually looks forwards from the Aura satellite. This means that the temperature retrievals are for a "profile" of the atmosphere somewhat ahead of the satellite. Because of the need to view a finite sample of the atmosphere, the sample spans a box about 1.5km deep and several tens of kilometers in width; the optical characteristics of the atmosphere mean that the sample is representative of a tube about 200-300km long in the direction of view. The retrievals use temperature analyses from NASA's Goddard Earth Observing System, Version 5 (GEOS-5) data assimilation system as a priori states. The temperature retrievals are somewhat deperrde~zt on these a priori states, especially in the lower stratosphere. An important part of the validation of any new dataset involves comparison with other, independent datasets. A large part of this study is concerned with such comparisons, using a number of independent space-based measurements obtained using different techniques, and with meteorological analyses. The MLS temperature data are shown to have biases that vary with height, but also depend on the validation dataset. MLS data are apparently biased slightly cold relative to correlative data in the upper troposphere and slightly warm in the middle stratosphere. A warm MLS bias in the upper stratosphere may be due to a cold bias in GEOS-5 temperatures.

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The Atmospheric Chemistry Experiment (ACE): Mission Overview

TL;DR: ACE as discussed by the authors is a Canadian satellite mission that will provide measurements leading to an improved understanding of the chemical and dynamical processes that control the distribution of ozone in the stratosphere, including a Fourier transform infrared spectrometer, a UV/visible/near IR spectrograph and a two-channel solar imager.
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Aura Microwave Limb Sounder Observations of Dynamics and Transport During the Record-Breaking 2009 Arctic Stratospheric Major Warming

TL;DR: A major stratospheric sudden warming (SSW) in January 2009 was the strongest and most prolonged on record as discussed by the authors, and the 2009 SSW had a more profound impact on the lower stratosphere than any previously observed SSW, with no significant recovery of the vortex in that region.
References
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Book

Inverse Methods for Atmospheric Sounding: Theory and Practice

TL;DR: This book treats the inverse problem of remote sounding comprehensively, and discusses a wide range of retrieval methods for extracting atmospheric parameters of interest from the quantities such as thermal emission that can be measured remotely.
Journal ArticleDOI

Gravity wave dynamics and effects in the middle atmosphere

TL;DR: In this article, a review of gravity wave sources and characteristics, the evolution of the gravity wave spectrum with altitude and with variations of wind and stability, the character and implications of observed climatologies, and the wave interaction and instability processes that constrain wave amplitudes and spectral shape are discussed.
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Observing Earth's atmosphere with radio occultation measurements using the Global Positioning System

TL;DR: In this article, the authors present the first systematic, extensive error analysis of the spacecraft radio occultation technique using a combination of analytical and simulation methods to establish a baseline accuracy for retrieved profiles of refractivity, geopotential, and temperature.
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A “Vertically Lagrangian” Finite-Volume Dynamical Core for Global Models

TL;DR: In this paper, a finite-volume dynamical core with a terrain-following Lagrangian control-volume discretization is described, which reduces the dimensionality of the physical problem from three to two with the resulting dynamical system closely resembling that of the shallow water system.
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