Ground-based measurements of ClO from Mauna Kea and intercomparisons with Aura and UARS MLS

被引:10
作者
Nedoluha, Gerald E. [1 ]
Connor, Brian J. [2 ]
Barrett, James [3 ]
Mooney, Thomas [3 ]
Parrish, Alan [4 ]
Boyd, Ian [6 ]
Wrotny, Jonathan E. [7 ]
Gomez, R. Michael [1 ]
Koda, Jin [3 ]
Santee, Michelle L. [5 ]
Froidevaux, Lucien [5 ]
机构
[1] USN, Res Lab, Washington, DC 20375 USA
[2] BC Consulting, Alexandra, New Zealand
[3] SUNY Stony Brook, Stony Brook, NY 11794 USA
[4] Univ Massachusetts, Amherst, MA 01003 USA
[5] CALTECH, Jet Prop Lab, Pasadena, CA 91109 USA
[6] Natl Inst Water & Atmospher Res, Auckland 1149, New Zealand
[7] Atmospher & Environm Res Inc, Lexington, MA 02421 USA
基金
美国国家航空航天局;
关键词
CHLORINE MONOXIDE; STRATOSPHERE; VALIDATION; CHEMISTRY; OZONE; ANTARCTICA; MESOSPHERE; SATELLITE; HALOE; MODEL;
D O I
10.1029/2010JD014732
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
The ground-based measurements of upper stratospheric ClO, made with a ground-based millimeter wave instrument at Mauna Kea, Hawaii (19.8 degrees N, 204.5 degrees E) starting in 1992, are compared with UARS (Upper Atmosphere Research Satellite) MLS ClO measurements (1991-1998) and the Aura MLS ClO measurements (2004-2009). The ground-based measurements are made as part of the Network for the Detection of Atmospheric Composition Change (NDACC). Intercomparisons between the ground-based measurements and the Aura MLS measurements show that both instruments retrieve similar seasonal variations over Mauna Kea. The seasonal variation in ClO is also compared with measurements of variations in stratospheric CH4, which affects the partitioning of total inorganic chlorine. Using the ground-based instruments as a transfer standard, we find that the agreement between UARS and Aura MLS ClO measurements near the peak of the mixing ratio profile is within similar to 1%. Combining the uncertainties in the biases calculated from the coincident ground-based and satellite measurements, we find that using the ground-based data as a transfer standard allows us to provide a 2 sigma limit to the bias between the UARS and Aura measurements of 3%-4% near the peak of the ClO profile. Given agreement between UARS and Aura MLS of similar to 1%+/- 4%, there is no reason to apply any bias correction in order to use the UARS and Aura MLS ClO measurements as a single data set.
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页数:9
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