Seasonal variation of methane, water vapor, and nitrogen oxides near the tropopause: Satellite observations and model simulations

By Mijeong Park, William J. Randel, Douglas E. Kinnison, R. Garcia, W. Choi. 2004

174 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/28409a142deb7b997457d9255b58475dcede89fa

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Citations in the corpus

Deep convective influence on the Asian summer monsoon anticyclone and associated tracer variability observed with Atmospheric Infrared Sounder (AIRS) (2006, background): “, 2001], and methane, nitrogen oxides [Park et al., 2004], and carbon monoxide [Li et al.”
Validation of Tropospheric Emission Spectrometer (TES) nadir ozone profiles (2008, methodology): “The ozone a priori profile (also used as the initial guess) and covariance matrix are derived from a climatology developed using the Model of Ozone and Related Tracers (MOZART) model [Brasseur et al., 1998; Park et al., 2004].”
THE EXTRATROPICAL UPPER TROPOSPHERE AND LOWER STRATOSPHERE (2011, methodology): “The Asian and North American monsoons significantly impact tracer distributions in the Ex ‐ UTLS, as evidenced by satellite data [ Park et al. , 2004; Randel et al. , 2006; Fu et al. , 2006; Park et al. , 2008] and aircraft measurements [ Schuck et al. , 2010].”
Modelling the effect of size on the aerial dispersal of microorganisms (2012, unknown): “We have conducted global annual ‘dust’ simulations for 2001 using the GEOS-Chem, a global chemical transport model (CTM) driven by assimilated meteorological data from the NASA Global Modeling and Assimilation Office (GMAO) (Bey et al., 2001; Park et al., 2004).”
Tropical tropopause layer (2009, background): “The generally higher values observed by the HALOE instrument (NOx in the range of 500–800 pptv [Park et al., 2004]) compared with the in situ observations from the Airborne Southern Hemi-”
Dynamical Mechanism for the Increase in Tropical Upwelling in the Lowermost Tropical Stratosphere during Warm ENSO Events (2010, background): “Nevertheless, there is some indication that, in WACCM, it is related to the injection of water vapor into the lowermost stratosphere by the circulation associated with the northern summer monsoon (cf. Park et al. 2004).”
Impact of monsoon circulations on the upper troposphere and lower stratosphere (2004, methodology): “model have been recently used by Park et al. [2004] to analyze methane, water vapor and nitrogen oxides near the tropical tropopause, by Horowitz et al.”