Open AccessFive year (2004–2009) observations of upper tropospheric water vapor and cloud ice from MLS and comparisons with GEOS‐5 analyses
Author(s) -
Jiang Jonathan H.,
Su Hui,
Pawson Steven,
Liu HuiChun,
Read William G.,
Waters Joe W.,
Santee Michelle L.,
Wu Dong L.,
Schwartz Michael J.,
Livesey Nathaniel J.,
Lambert Alyn,
Fuller Ryan A.,
Lee Jae N.
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 - 10.1029/2009jd013256
Subject(s) - microwave limb sounder , troposphere , water vapor , atmospheric sciences , convection , climatology , chemical transport model , environmental science , intertropical convergence zone , deep convection , tropics , equator , geology , meteorology , physics , latitude , precipitation , fishery , biology , geodesy
This paper gives an overview of August 2004 through February 2010 upper tropospheric (UT) water vapor (H 2 O) and ice water content (IWC) from the Aura Microwave Limb Sounder (MLS) and comparisons with outputs from the NASA Goddard Earth Observing System Version 5 (GEOS‐5) data assimilation system. Both MLS and GEOS‐5 show that high values of H 2 O and IWC at 215 to 147 hPa are associated with areas of deep convection. They exhibit good (within ∼15%) agreement in IWC at these altitudes, but GEOS‐5 H 2 O is ∼50% (215 hPa) to ∼30% (147 hPa) larger than MLS values, possibly due to higher temperatures in the data assimilation system at these altitudes. A seasonally migrating band of tropical deep convection is clearly evident in both the MLS and GEOS‐5 UT H 2 O and IWC, but GEOS‐5 produces a weaker intertropical convergence zone than MLS. MLS and GEOS‐5 both show spatial anticorrelation between IWC and H 2 O at 100 hPa, where low H 2 O is associated with low temperatures in regions of tropical convection. At 100 hPa, GEOS‐5 produces 50% less IWC and 15% less H 2 O in the tropics, and ∼20% more H 2 O in the extratropics, than does MLS. Behavior of the 100 hPa H 2 O is consistent with it being controlled by temperature. The seasonal cycle in the vertical transport of tropical mean H 2 O from ∼147 hPa to ∼10 hPa appears much stronger in MLS than in GEOS‐5. The UT IWC and H 2 O interannual variations, from both MLS and GEOS‐5, show clear imprints of the El Niño–Southern Oscillation.