Open AccessValidation of the Aura Microwave Limb Sounder middle atmosphere water vapor and nitrous oxide measurements
Author(s) -
Lambert A.,
Read W. G.,
Livesey N. J.,
Santee M. L.,
Manney G. L.,
Froidevaux L.,
Wu D. L.,
Schwartz M. J.,
Pumphrey H. C.,
Jimenez C.,
Nedoluha G. E.,
Cofield R. E.,
Cuddy D. T.,
Daffer W. H.,
Drouin B. J.,
Fuller R. A.,
Jarnot R. F.,
Knosp B. W.,
Pickett H. M.,
Perun V. S.,
Snyder W. V.,
Stek P. C.,
Thurstans R. P.,
Wagner P. A.,
Waters J. W.,
Jucks K. W.,
Toon G. C.,
Stachnik R. A.,
Bernath P. F.,
Boone C. D.,
Walker K. A.,
Urban J.,
Murtagh D.,
Elkins J. W.,
Atlas E.
Publication year - 2007
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/2007jd008724
Subject(s) - microwave limb sounder , stratopause , stratosphere , water vapor , environmental science , mesosphere , atmosphere (unit) , accuracy and precision , atmospheric sciences , nitrous oxide , remote sensing , atmospheric infrared sounder , geology , meteorology , chemistry , physics , quantum mechanics , organic chemistry
The quality of the version 2.2 (v2.2) middle atmosphere water vapor and nitrous oxide measurements from the Microwave Limb Sounder (MLS) on the Earth Observing System (EOS) Aura satellite is assessed. The impacts of the various sources of systematic error are estimated by a comprehensive set of retrieval simulations. Comparisons with correlative data sets from ground‐based, balloon and satellite platforms operating in the UV/visible, infrared and microwave regions of the spectrum are performed. Precision estimates are also validated, and recommendations are given on the data usage. The v2.2 H 2 O data have been improved over v1.5 by providing higher vertical resolution in the lower stratosphere and better precision above the stratopause. The single‐profile precision is ∼0.2–0.3 ppmv (4–9%), and the vertical resolution is ∼3–4 km in the stratosphere. The precision and vertical resolution become worse with increasing height above the stratopause. Over the pressure range 0.1–0.01 hPa the precision degrades from 0.4 to 1.1 ppmv (6–34%), and the vertical resolution degrades to ∼12–16 km. The accuracy is estimated to be 0.2–0.5 ppmv (4–11%) for the pressure range 68–0.01 hPa. The scientifically useful range of the H 2 O data is from 316 to 0.002 hPa, although only the 82–0.002 hPa pressure range is validated here. Substantial improvement has been achieved in the v2.2 N 2 O data over v1.5 by reducing a significant low bias in the stratosphere and eliminating unrealistically high biased mixing ratios in the polar regions. The single‐profile precision is ∼13–25 ppbv (7–38%), the vertical resolution is ∼4–6 km and the accuracy is estimated to be 3–70 ppbv (9–25%) for the pressure range 100–4.6 hPa. The scientifically useful range of the N 2 O data is from 100 to 1 hPa.