
Mid‐upper tropospheric methane in the high Northern Hemisphere: Spaceborne observations by AIRS, aircraft measurements, and model simulations
Author(s) -
Xiong Xiaozhen,
Barnet Christopher D.,
Zhuang Qianlai,
Machida Toshinobu,
Sweeney Colm,
Patra Prabir K.
Publication year - 2010
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 - 10.1029/2009jd013796
Subject(s) - troposphere , northern hemisphere , atmospheric infrared sounder , environmental science , atmospheric sciences , climatology , southern hemisphere , chemical transport model , methane , seasonality , polar , geology , chemistry , statistics , mathematics , organic chemistry , astronomy , physics
Spaceborne measurements by the Atmospheric Infrared Sounder (AIRS) on the EOS/Aqua satellite provide a global view of the methane (CH 4 ) distribution in the mid‐upper troposphere (MUT‐CH 4 ). The focus of this study is to examine the spatiotemporal variation of MUT‐CH 4 in the high Northern Hemisphere (HNH) using AIRS retrievals, aircraft measurements, and simulations from a forward chemistry‐transport model (i.e., ACTM). Data from 2004 and 2005 focusing over two regions (Alaska and Siberia) are analyzed. An important feature in the seasonal variation of CH 4 we found is the summer increase of MUT‐CH 4 , which is nearly opposite to the summer minimum of CH 4 in the marine boundary layer (MBL). This study also demonstrated an apparent increase of CH 4 over Alaska associated with the 2004 Alaska forest fire and a negative bias of the ACTM simulations in the HNH. The larger bias of the model simulations in the late winter to early spring may indicate possible unidentified CH 4 emission sources (e.g., the use of energy or gas leakage) during this period, but more studies will be needed due to the retrieval uncertainties in the polar winter season. The summer increase of MUT‐CH 4 is related to surface emission, but the enhanced convection in summer is likely the most important driver.